🌊 Environmental Engineering 🔥 Day 1
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Environmental Engineering

Ready to test your Environmental Engineering knowledge? Practice chapter-wise mock tests with worked step-by-step solutions for GATE, ESE and SSC JE.
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🎯
Environmental Engineering — Complete Study Notes
11 chapters · GATE, ESE (IES), SSC JE, State PSC, RRB JE
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Environmental Engineering covers the planning, design and operation of systems that protect public health and the environment — from water demand estimation and treatment, through sewer design and wastewater treatment, to solid waste management and air & noise pollution control. Every design formula, IS code limit, treatment-process diagram, solved example and exam-pattern table is included.

Learning Objectives

After studying this chapter you will be able to:

  • Estimate water demand using per capita norms, peak factors and population forecasting methods
  • Select pipe materials and analyse distribution networks using Hardy-Cross iteration
  • Apply Darcy's law and the Thiem/Theis well equations to design and analyse tube wells
  • Apply IS 10500 water quality limits and interpret hardness, chlorine demand and breakpoint chlorination
  • Design a conventional water treatment train: aeration, coagulation-flocculation, sedimentation, filtration, disinfection
  • Design sewers using Manning's equation, self-cleansing velocity, and hydraulic elements of circular pipes
  • Characterise sewage quality (BOD, COD, DO) and apply the Streeter-Phelps oxygen sag equation
  • Compare sewage disposal and treatment options — septic tanks, activated sludge, trickling filters, waste stabilisation ponds
  • Classify solid waste, apply the 3R waste hierarchy, and design sanitary landfills
  • Apply the Gaussian plume model, Pasquill-Gifford stability classes, and CPCB noise standards

Exam Relevance

ESE★★★★★
GATE★★★★★
SSC JE★★★★☆
State PSC★★★★☆
💡 Environmental Engineering is one of the highest-weightage subjects in GATE and ESE Civil — per capita water demand values, well-hydraulics equations, IS 10500 limits, sewer self-cleansing velocity, ASP design parameters, and the Gaussian plume model appear nearly every year.

Concept Map

Water Demand → Conduits & Distribution → Ground Water & Wells
↓
Water Quality Control → Water Treatment
↓
Sewer Design ↔ Sewage Quality ↔ Sewage Disposal ↔ Sewage Treatment
↓
Air & Noise Pollution → Solid Waste Management

Where This Fits

Prerequisite: Irrigation Engineering (canal hydraulics and well-discharge principles developed there carry over directly into water-supply conduit and groundwater design here). Leads to: Surveying, which provides the field measurement and levelling techniques needed to lay out water supply and sewerage networks.

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1. Water Demand
Sources · Per Capita Demand · Peak Factors · Population Forecasting
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1.1 Sources of Water

Source TypeExamplesQualitySuitability
Surface waterRivers, lakes, tanks, reservoirsVariable; turbid, may have bacteriaLarge cities after treatment; cheapest to develop
Ground waterWells, springs, infiltration galleries, tube wellsGenerally better; may have hardness, ironRural and small towns; often requires only disinfection
Rainwater / Rooftop harvestingRoof collection, check damsGenerally clean initiallySupplementary; arid zones
Sea water (desalination)SWRO, MSF plantsHigh TDS (35,000 mg/L)Coastal cities; expensive

1.2 Types and Per Capita Demand

Type of UseIS 1172 Per Capita (lpcd)Remarks
Domestic135 lpcd (cities >1 lakh)Drinking, cooking, bathing, flushing; 70% is indoor
Industrial50 lpcd (allowance)Highly variable; 45–450 kL/tonne of product
Commercial / Institutional20 lpcdHotels, hospitals, offices, schools
Fire demandAs per Kuichling's formulaNot added to average; governs pipe sizing at hydrants
Losses / Thefts15% of totalLeakage, metering error, illegal use
Total design170–200 lpcd (urban India)Sum of above with safety factor

1.3 Factors Affecting Water Demand

  • Population size: Larger cities → higher per capita demand (more commercial, industrial use)
  • Climate: Hot and dry → more demand; cold regions → less bathing
  • Living standards: Higher income → more water-using appliances
  • Metering: Metered supply reduces consumption by 20–25% (accounts for waste)
  • Pressure: Higher pressure in mains → more losses through leakages
  • Quality: Poor quality → less willingness to use domestically
  • System efficiency: Old pipes → more leakage losses

1.4 Variation in Demand — Peak Factors

Water demand is never constant — it varies by season, day, and hour. Design must accommodate the maximum hourly demand, not just the average, or pressure will fail during peak consumption periods.

💡 Per capita demand = 135 lpcd (domestic), Total design ≈ 200 lpcd. Peak factors: MDD = 1.8× ADD; MHD = 2.7× ADD. These specific numbers appear in almost every GATE environmental question on water demand.

1.5 Design Period and Population Forecasting

The design period is the future period for which a component is designed to be adequate — 30 years for dams and large headworks, 15–20 years for treatment plants, and 10 years for distribution networks (since distribution is cheaper to expand incrementally). Population at the end of the design period must be forecast using arithmetic, geometric, incremental-increase, or logistic (S-curve) methods, chosen based on the city's growth pattern and available census history.

1.6 Fire Demand

Fire demand is a short-duration but very high instantaneous flow requirement, governed by empirical formulae (Kuichling's, Freeman's, or the IS formula) based on population. It is not added directly to the average demand but instead governs the minimum pipe sizing needed to deliver adequate pressure and flow to hydrants during a fire event, typically for a duration of 4–8 hours per IS 3764.

Peak Demand Factors

Average Daily Demand: \( ADD = \dfrac{\text{Annual consumption}}{365} \)

Maximum Daily Demand: \( MDD = 1.8\times ADD \)

Maximum Hourly Demand: \( MHD = 1.5\times MDD = 2.7\times ADD \)

Minimum Hourly Demand \( = 0.5\times ADD \); Peak factor \( = \dfrac{MHD}{ADD} = 2.7 \)

Population Forecasting

Arithmetic growth: \( P_n = P_0 + n\times r \)

Geometric growth: \( P_n = P_0\times(1+\dfrac{r}{100})^n \)

Logistic (S-curve): \( P = \dfrac{P_s}{1+m\,e^{-kn}} \)

Fire Demand Formulae

Kuichling's: \( Q = 3182\sqrt{P} \) (L/min; P in thousands)

Freeman's: \( Q = \dfrac{1136\,(P/5+10)}{10} \)

IS formula: \( Q = 100\sqrt{P} \) (m³/hr; P in thousands)

Example 1 — Maximum Hourly Demand

Given: A city has an average daily demand of \(15{,}000\ \dfrac{\text{m}^3}{\text{day}}\). Find the maximum hourly demand.

Solution:

\( MHD = 2.7\times ADD = 2.7\times15{,}000 = 40{,}500\ \dfrac{\text{m}^3}{\text{day}} \)

Answer: \(MHD = 40{,}500\ \dfrac{\text{m}^3}{\text{day}}\).

Example 2 — Kuichling's Fire Demand

Given: A town has a population of \(64{,}000\). Estimate the fire demand using Kuichling's formula.

Solution:

\( Q = 3182\sqrt{P} = 3182\sqrt{64} = 3182\times8 = 25{,}456\ \text{L/min} \)

Answer: \(Q\approx25{,}456\ \text{L/min} \approx 1527\ \dfrac{\text{m}^3}{\text{hr}}\).

Example 3 — Geometric Population Forecast

Given: A city's current population is \(80{,}000\) with an average decadal growth rate of \(15\%\). Forecast the population after 20 years (2 decades) using geometric growth.

Solution:

\( P_n = P_0(1+\dfrac{r}{100})^n = 80{,}000\times(1.15)^2 = 80{,}000\times1.3225 = 105{,}800 \)

Answer: Forecast population \(\approx105{,}800\).

Daily demand variation curve showing average, maximum daily and maximum hourly demand Hour of day → Demand ADD (average) MDD = 1.8× ADD MHD peak = 2.7× ADD (~noon)

Fig. 1.1 — Daily demand variation: hourly consumption rises above the average during peak hours, reaching a maximum hourly demand of about 2.7 times the average daily demand.

Q1. As per IS 1172, the maximum daily demand (MDD) is taken as:
MDD = 1.8 × ADD; the maximum hourly demand (MHD) is 2.7 × ADD (i.e., 1.5 × MDD).
Q2. The design period for a distribution network is typically:
Distribution networks use a shorter 10-year design period since they can be expanded incrementally at relatively low cost, unlike dams (30 years) or treatment plants (15–20 years).
Q3. Metering of water supply typically reduces consumption by:
Metering makes consumers cost-conscious and reveals waste/leakage, typically cutting consumption by 20–25% compared to unmetered flat-rate supply.
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2. Conduits for Transporting Water
Pipe Flow Equations · Materials · Distribution Layouts · Hardy-Cross · Storage
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2.1 Pipe Flow Equations

Water conduits are analysed using different equations depending on flow type. Manning's equation applies to gravity (open-channel or partly-full) flow. The Hazen-Williams equation is the standard for pressurised water distribution mains, using an empirical roughness coefficient \(C\) that is easy to look up for common pipe materials. The Darcy-Weisbach equation, using a friction factor from the Moody chart, is the most rigorous (dimensionally consistent) head-loss formula and is preferred for precise engineering analysis.

2.2 Pipe Materials for Water Supply

MaterialAdvantagesDisadvantagesUse
Cast Iron (CI)Strong, long life, joints easyHeavy, brittle, corrodes over timeDistribution mains; 75–600 mm dia
Ductile Iron (DI)Strong + ductile; better than CIExpensiveModern distribution; replacing CI
Steel (MS)Light, strong, any sizeCorrodes; needs lining or coatingTransmission mains; large dia
PVC / CPVCLight, corrosion-proof, cheapLimited temperature/pressure rangeSmall dia distribution; house connections
HDPEFlexible, good chemical resistanceUV degradation if exposedRural supply; sliplined rehabilitation
Asbestos Cement (AC)Smooth, light, cheapBrittle; health concerns (asbestos)Now largely phased out
Pre-stressed ConcreteLarge dia; suitable for gravity mainsHeavy; joints criticalLarge transmission mains >600 mm

2.3 Distribution System Layout

The tree/dead-end system branches out from a main pipe with no interconnections; it is simple and cheap but the dead ends cause stagnation and sediment buildup, and any single pipe failure cuts off supply downstream. The ring/grid system interconnects pipes into loops, so water can reach any point from multiple directions — eliminating stagnation and maintaining supply even if one section is shut for repair, at the cost of higher construction cost and the need for iterative network analysis (Hardy-Cross). The radial/circular system divides a city into zones, each fed by a circular main from a central point, giving uniform pressure and easy fault detection in planned cities.

2.4 Hardy-Cross Method for Pipe Network Analysis

Looped (ring/grid) networks cannot be solved directly since flow splits are unknown at each junction. The Hardy-Cross iterative method starts by assuming a set of pipe flows that satisfy continuity at every junction, then computes a flow correction for each loop based on the imbalance of head losses around that loop, and repeats until the corrections become negligibly small (typically 3–5 iterations).

2.5 Service Reservoir (Storage)

A service (distribution) reservoir provides three components of storage: balancing storage to absorb the mismatch between the (constant) supply rate from the treatment plant and the (fluctuating) hourly demand; fire reserve, held specifically for fire-fighting duration; and emergency/breakdown reserve, held against unplanned outages in supply. The elevated tank's height above the service area must be enough to deliver a minimum residual pressure head to the highest and farthest consumer after accounting for pipe friction losses.

💡 Hazen-Williams C: CI (new)=130, old CI=100, PVC=140–150. Hardy-Cross ΔQ = −Σh_L / (n·Σ|h_L/Q|). Balancing storage = 1/3 of daily demand. These are the three most tested facts in this chapter.

Manning's Equation (Gravity Flow)

\( V = \dfrac{1}{n}R^{2/3}S^{1/2} \), \( Q = \dfrac{A}{n}R^{2/3}S^{1/2} \)

n: CI pipe 0.012–0.014; PVC 0.009–0.011; concrete 0.013–0.015

Hazen-Williams Equation

\( V = 0.8492\,C\,R^{0.63}S^{0.54} \)

\( Q = 0.2785\,C\,D^{2.63}S^{0.54} \)

C: CI new=130, old CI=100, steel=120, PVC=140–150

Darcy-Weisbach (Head Loss)

\( h_f = \dfrac{fLV^2}{2gD} \)

f = friction factor (Moody chart); typical 0.01–0.05

Hardy-Cross Correction

\( \Delta Q = -\dfrac{\Sigma h_L}{n\,\Sigma|h_L/Q|} \)

\(h_f = rQ^n\) (n=1.85 for HW, 2 for DW); convergence when \(\Delta Q < 0.001\ \dfrac{\text{m}^3}{\text{s}}\)

Service Reservoir Storage

Storage = balancing + fire reserve + emergency reserve

Balancing storage \(\approx \dfrac{1}{3}\) daily demand; Emergency reserve \(\approx 25\%\) daily demand

Example 1 — Hazen-Williams Discharge

Given: A new CI pipe (\(C=130\)) of diameter \(D=0.3\ \text{m}\) has a hydraulic slope \(S=0.004\). Find the discharge.

Solution:

\( Q = 0.2785\times130\times0.3^{2.63}\times0.004^{0.54} \)

\( 0.3^{2.63}\approx0.0605 \); \( 0.004^{0.54}\approx0.0487 \)

\( Q = 0.2785\times130\times0.0605\times0.0487\approx0.1067\ \dfrac{\text{m}^3}{\text{s}} \)

Answer: \(Q\approx0.107\ \dfrac{\text{m}^3}{\text{s}}\).

Example 2 — Darcy-Weisbach Head Loss

Given: Water flows at \(V=1.5\ \text{m/s}\) through a \(D=0.2\ \text{m}\) pipe, length \(L=500\ \text{m}\), \(f=0.02\). Find the head loss.

Solution:

\( h_f = \dfrac{fLV^2}{2gD} = \dfrac{0.02\times500\times1.5^2}{2\times9.81\times0.2} = \dfrac{22.5}{3.924}\approx5.73\ \text{m} \)

Answer: \(h_f\approx5.73\ \text{m}\).

Example 3 — Service Reservoir Balancing Storage

Given: A town's average daily demand is \(6000\ \text{m}^3\). Estimate the balancing storage.

Solution:

Balancing storage \(\approx \dfrac{1}{3}\times6000 = 2000\ \text{m}^3\)

Answer: Balancing storage \(\approx2000\ \text{m}^3\) (fire and emergency reserves must be added separately for total capacity).

Tree/dead-end distribution system versus ring/grid distribution system Tree / Dead-End System Dead ends → stagnation ✓ Simple; cheap Ring / Grid System ✓ Multi-directional flow; no stagnation ✗ Costly; needs Hardy-Cross analysis Radial / Circular System: City divided into zones fed from a central point; uniform pressure; easy fault detection; used in planned cities.

Fig. 2.1 — Distribution layouts: Tree system (dead-ends; simple but unreliable) versus Ring/Grid system (interconnected loops; reliable; requires Hardy-Cross analysis).

Q1. The Hazen-Williams coefficient C for a new cast iron pipe is approximately:
C=130 for new CI; it drops to about 100 as the pipe ages and corrodes/tuberculates. PVC has the highest C (140–150).
Q2. The main disadvantage of a tree (dead-end) distribution system is:
Dead ends trap stagnant water (sediment, taste issues) and any pipe failure cuts off all downstream consumers, since there's no alternate flow path — unlike a ring system.
Q3. The Hardy-Cross method is used to analyse:
Hardy-Cross is an iterative method specifically for solving looped networks, where continuity alone doesn't uniquely determine the flow split at each junction.
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3. Ground Water Development & Well Hydraulics
Aquifer Types · Darcy's Law · Well Discharge Equations · Theis Method
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3.1 Types of Aquifers

Aquifer TypeDescriptionWater TableExample
Unconfined (phreatic)Water table exposed to atmosphere; water table is upper boundaryVaries freely with seasonsAlluvial plains; dug wells
Confined (artesian)Sandwiched between impervious layers; water under pressurePiezometric surface > top of aquiferDeep tube wells; artesian wells
Semi-confined (leaky)Confining layer is semi-permeable; leakage from adjacent aquiferPiezometric varies with leakageAlluvial basins with clay lenses
Perched aquiferLocal impervious lens above main water tableLocalised; above regional WTHillside springs; seasonal

3.2 Darcy's Law

Darcy's law states that the flow rate of water through a porous medium is proportional to the hydraulic gradient and the cross-sectional area, governed by a proportionality constant called the hydraulic conductivity. It is valid only for laminar flow through the pores (low Reynolds number), and does not hold for coarse gravel or fractured rock, where velocities are high enough to produce turbulent flow.

3.3 Well Hydraulics — Steady State

When a well is pumped, water flows radially inward toward it, and the water table (unconfined) or piezometric surface (confined) is drawn down into a funnel shape called the cone of depression. The radius of influence \(R\) is the distance beyond which the pumping has no measurable effect on the water level. For a confined aquifer, the drawdown analysis uses the aquifer thickness \(b\) directly since the aquifer itself stays fully saturated even as the piezometric surface drops.

3.4 Well Discharge Equations

The Dupuit-Thiem equation for a fully-penetrating well in an unconfined aquifer under steady-state pumping relates discharge to the square of the difference between the undisturbed head and the pumped water level in the well. The analogous Thiem equation for a confined aquifer uses the linear head difference (not squared) because the saturated thickness of a confined aquifer doesn't change with pumping — only the pressure (piezometric head) does.

3.5 Transient Well Flow — Theis Method

Steady-state (Thiem) equations assume the cone of depression has stopped growing, which is only true after very long pumping durations. The Theis equation instead models the time-dependent (transient) drawdown at any point using the well function \(W(u)\), which depends on the aquifer's storage coefficient in addition to transmissivity. For small values of the dimensionless parameter \(u\), the Cooper-Jacob approximation simplifies the well function to a straight-line semi-log relationship, making field data analysis much easier.

3.6 Types of Wells

Well TypeDepthDiaMethodYield
Open / Dug well10–20 m1–6 mManual/mechanical excavationLow; 50–500 L/hr
Tube well (deep)60–300 m100–450 mmRotary/cable tool drillingHigh; 100–3000 m³/day
Infiltration gallery5–10 m—Horizontal perforated pipe near riverbankMedium; induced recharge
Spring collectionAt surface—Gravity collection of natural springVariable; gravity-fed
Collector (Ranney) well15–30 mLarge caissonRadial horizontal lateralsVery high; 1000–50,000 m³/day
💡 Unconfined: \(Q=\pi \dfrac{K(H^2-h^2)}{\ln(R/r_w)}\). Confined: \(Q=2\pi \dfrac{Kb(H-h)}{\ln(R/r_w)}\). Transmissivity \(T=Kb\) (m²/day). Radius of influence \(R=3000(H-h)\sqrt{K}\) (Sichardt). These equations appear every year.

Darcy's Law

\( Q = K\,i\,A \)

K=hydraulic conductivity; i=hydraulic gradient=dh/dL

Unconfined Well (Dupuit-Thiem)

\( Q = \dfrac{\pi K(H^2-h^2)}{\ln(R/r_w)} \)

Sichardt: \( R = 3000(H-h)\sqrt{K} \)

Confined Well (Thiem)

\( Q = \dfrac{2\pi Kb(H-h)}{\ln(R/r_w)} = \dfrac{2\pi T(H-h)}{\ln(R/r_w)} \)

\(T = Kb\) (transmissivity, m²/day)

Theis Equation (Transient)

\( s = \dfrac{Q}{4\pi T}W(u) \), \( u = \dfrac{r^2 S}{4Tt} \)

Cooper-Jacob (small u): \( s = \dfrac{2.303\,Q}{4\pi T}\log\!\left(\dfrac{2.25\,Tt}{r^2 S}\right) \)

Example 1 — Darcy's Law

Given: A soil sample has hydraulic conductivity \(K=0.02\ \text{cm/s}\), cross-sectional area \(A=100\ \text{cm}^2\), and hydraulic gradient \(i=0.05\). Find the discharge.

Solution:

\( Q = K\,i\,A = 0.02\times0.05\times100 = 0.1\ \dfrac{\text{cm}^3}{\text{s}} \)

Answer: \(Q=0.1\ \dfrac{\text{cm}^3}{\text{s}}\).

Example 2 — Unconfined Well Discharge

Given: An unconfined aquifer has \(K=40\ \text{m/day}\), \(H=25\ \text{m}\), \(h=15\ \text{m}\), \(R=200\ \text{m}\), well radius \(r_w=0.15\ \text{m}\). Find the discharge.

Solution:

\( Q = \dfrac{\pi\times40\times(25^2-15^2)}{\ln(200/0.15)} = \dfrac{\pi\times40\times400}{\ln(1333.3)} = \dfrac{50{,}265}{7.195}\approx6987\ \dfrac{\text{m}^3}{\text{day}} \)

Answer: \(Q\approx6987\ \dfrac{\text{m}^3}{\text{day}}\).

Example 3 — Transmissivity from Confined Well Test

Given: A confined aquifer of thickness \(b=20\ \text{m}\) has hydraulic conductivity \(K=15\ \text{m/day}\). Find the transmissivity.

Solution:

\( T = Kb = 15\times20 = 300\ \dfrac{\text{m}^2}{\text{day}} \)

Answer: \(T=300\ \dfrac{\text{m}^2}{\text{day}}\).

Unconfined well with cone of depression during pumping Ground surface Static water table Impermeable base Pumped level H h R (radius of influence)

Fig. 3.1 — Unconfined well under steady pumping: the cone of depression forms between the static water table and the pumped level in the well, extending out to the radius of influence R.

Q1. Darcy's law is valid only for:
Darcy's law assumes laminar pore flow; at high velocities through gravel or fractured rock, flow becomes turbulent and the linear Darcy relationship breaks down.
Q2. In the confined well discharge formula, the driving term is proportional to:
In a confined aquifer, the aquifer thickness stays fully saturated regardless of pumping (only pressure/piezometric head drops), so the discharge equation uses the linear head difference (H−h), unlike the squared term for unconfined wells.
Q3. The Theis equation, unlike the Thiem equation, is used to analyse:
The Theis equation models how drawdown evolves with time before steady state is reached, incorporating the storage coefficient S — the Thiem equation only applies once the cone of depression has stabilised.
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4. Quality Control of Water Supplies
Physical/Chemical/Biological Characteristics · Hardness · Breakpoint Chlorination
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4.1 Physical Characteristics

ParameterUnitPermissible (IS 10500)DesirableTest Method
TurbidityNTU5 NTU<1 NTUNephelometer; Jackson turbidimeter
ColourHazen units15 HU5 HUVisual comparison; spectrophotometer
Taste & OdourTON (threshold)Unobjectionable—Dilution-to-threshold method
Temperature°C10–25°C (max 45°C)10–20°CThermometer
Total Dissolved Solids (TDS)mg/L500 mg/L—Gravimetric (105°C evaporation)

4.2 Chemical Characteristics

ParameterPermissible Limit (IS 10500:2012)Health Effect if Exceeded
pH6.5 – 8.5Corrosion (<6.5); scaling (>8.5)
Total Hardness300 mg/L (max 600)Scale in pipes/boilers; soap wastage; not harmful directly
Fluoride1.0 mg/L (max 1.5)Dental fluorosis >1.5; skeletal fluorosis >3–6
Nitrate (as NO₃)45 mg/LMethaemoglobinaemia (blue baby syndrome) in infants
Arsenic0.01 mg/LSkin cancer, arsenicosis (chronic); WHO 0.01 mg/L
Iron0.3 mg/LStaining, taste; no direct health effect at low levels
Chloride250 mg/L (max 1000)Salty taste; corrosion of pipes
Chlorine (residual)0.2 mg/L (min)Below → bacterial growth; above 0.5 → taste/odour
Sulphate200 mg/L (max 400)Laxative effect; concrete attack
Lead0.01 mg/LNeurotoxin; cumulative; children most vulnerable

4.3 Biological Characteristics

Coliform organisms (with E. coli as the specific index organism) serve as indicator bacteria for faecal contamination — their presence signals a risk of pathogenic contamination even though coliforms themselves are mostly harmless. IS 10500 requires zero coliforms in 100 mL of treated water. The Most Probable Number (MPN) method uses statistical inference from multiple-dilution tube tests to estimate the coliform count, while the Membrane Filter (MF) technique physically filters a sample and counts colonies grown on selective media directly.

4.4 Hardness of Water

Temporary hardness (from calcium and magnesium bicarbonates) can be removed simply by boiling, which drives off CO₂ and precipitates the carbonates. Permanent hardness (from sulphates and chlorides of calcium and magnesium) survives boiling and requires chemical softening. Both are conventionally expressed as an equivalent concentration of CaCO₃, allowing different hardness-causing ions to be compared on a common scale. The Langelier Saturation Index compares actual pH to the theoretical saturation pH to indicate whether water tends to deposit scale or corrode pipes.

4.5 Chlorine Demand and Breakpoint Chlorination

As chlorine dose increases from zero, it first reacts with ammonia present in the water to form chloramines (combined residual), and the measured residual rises slowly. Beyond a certain dose, the chloramines are oxidised and destroyed, and the residual actually dips — this is the breakpoint. Beyond the breakpoint, any further chlorine added remains as free residual chlorine, rising linearly with dose. Operating beyond the breakpoint ensures the required free residual (minimum 0.2 mg/L) reaches the consumer's tap.

💡 IS 10500:2012 Key Limits: Turbidity ≤ 5 NTU; TDS ≤ 500 mg/L; Hardness ≤ 300 mg/L; pH 6.5–8.5; Fluoride ≤ 1.0 mg/L; Nitrate ≤ 45 mg/L; Arsenic ≤ 0.01 mg/L; Coliforms = 0 per 100 mL (treated water). Memorise these for GATE.

4.6 Water Quality Index (WQI)

A Water Quality Index condenses several individual water-quality parameters into a single dimensionless number, giving a quick overall rating of a source's suitability (e.g. "excellent", "good", "poor"). It is computed as a weighted aggregation of the sub-index values of each parameter.

  1. Select parameters (e.g. pH, DO, BOD, turbidity, nitrate, total coliform, hardness).
  2. Assign weights \(w_i\): each parameter's unit weight is inversely proportional to its permissible standard \(S_i\), i.e. \(w_i = \dfrac{k}{S_i}\), normalised so \(\sum w_i = 1\).
  3. Compute quality rating (sub-index) \(q_i = 100\,\dfrac{V_i - V_0}{S_i - V_0}\), where \(V_i\) = observed value, \(V_0\) = ideal value (0 for most, 7 for pH, 14.6 mg/L for DO).
  4. Aggregate: \( WQI = \dfrac{\sum w_i\,q_i}{\sum w_i} \) (weighted arithmetic index; NSF-WQI uses a similar 0–100 scale where higher = better).

A rising WQI on the NSF scale means better water; on the weighted-arithmetic scale used by many Indian studies a lower value means better quality — always note which convention is in use.

Hardness as CaCO₃ Equivalent

Hardness (as CaCO₃) = ion concentration (mg/L) \(\times \dfrac{50}{\text{eq. wt of ion}}\)

\(Ca^{2+}\): eq. wt = 20; \(Mg^{2+}\): eq. wt = 12; \(HCO_3^-\): eq. wt = 61

Langelier Saturation Index

\( LSI = pH_{actual} - pH_s \)

LSI > 0 → scaling; LSI < 0 → corrosive; LSI = 0 → stable

Breakpoint Chlorination

Chlorine demand = chlorine added − residual chlorine

Breakpoint dose \(\approx 7.6\times\)(NH₃-N concentration)

Example 1 — Total Hardness as CaCO₃

Given: A water sample has \(Ca^{2+}=40\ \text{mg/L}\) and \(Mg^{2+}=12\ \text{mg/L}\). Find the total hardness as CaCO₃.

Solution:

\( \text{Ca hardness} = 40\dfrac{\times50}{20} = 100\ \text{mg/L as CaCO}_3 \)

\( \text{Mg hardness} = 12\dfrac{\times50}{12} = 50\ \text{mg/L as CaCO}_3 \)

Answer: Total hardness \(= 100+50 = 150\ \text{mg/L as CaCO}_3\).

Example 2 — Breakpoint Chlorine Dose

Given: Raw water has an ammonia-nitrogen concentration of \(0.5\ \text{mg/L}\). Estimate the breakpoint chlorine dose.

Solution:

\( \text{Breakpoint dose} \approx 7.6\times0.5 = 3.8\ \text{mg/L} \)

Answer: Approximately \(3.8\ \text{mg/L}\) of chlorine must be dosed to reach breakpoint, after which a free residual can be maintained.

Example 3 — Langelier Index Interpretation

Given: A water sample has \(pH_{actual}=8.2\) and calculated saturation \(pH_s=7.6\). Interpret the water's tendency.

Solution:

\( LSI = 8.2-7.6 = +0.6 \)

Answer: Since \(LSI>0\), the water has a scaling tendency (will tend to deposit CaCO₃ scale in pipes rather than corrode them).

Breakpoint chlorination curve showing chloramine formation, breakpoint dip, and free residual rise Chlorine dose → Residual Cl₂ Chloramine formation Breakpoint (chloramine destruction) Free residual Cl₂ (linear rise)

Fig. 4.1 — Breakpoint chlorination curve: residual rises as chloramines form, dips sharply at the breakpoint as they are destroyed, then rises linearly as free residual chlorine beyond the breakpoint.

Q1. As per IS 10500, the desirable pH range for drinking water is:
IS 10500 specifies pH 6.5–8.5; below 6.5 causes corrosion, above 8.5 causes scaling.
Q2. Temporary hardness in water is caused by:
Temporary hardness comes from bicarbonates and is removed by boiling (which drives off CO₂ and precipitates carbonate); permanent hardness (sulphates, chlorides) survives boiling.
Q3. At the breakpoint in breakpoint chlorination, the residual chlorine:
At the breakpoint, previously-formed chloramines are oxidised and destroyed by the additional chlorine dose, causing a temporary dip in measured residual before free residual chlorine begins to rise linearly with further dosing.
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5. Water Treatment & Distribution System
Aeration · Coagulation-Flocculation · Sedimentation · Filtration · Disinfection
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5.1 Water Treatment Plant Flow Sequence

A conventional water treatment plant treats raw water through a fixed sequence of unit processes: Screening & Intake → Aeration (optional) → Coagulation & Flocculation → Sedimentation → Filtration (rapid or slow sand) → Disinfection (chlorine) → Storage & Distribution. Each stage removes progressively finer contaminants, so a later stage functioning correctly depends on the earlier stages having done their job (e.g., filtration works best on already-flocculated, low-turbidity water).

5.2 Aeration

Aeration removes dissolved gases (CO₂, H₂S, volatile organics), oxidises dissolved iron and manganese (Fe²⁺→Fe³⁺, Mn²⁺→MnO₂) so they can be removed in the following sedimentation step, and reduces taste and odour. Spray aerators are simple and effective for taste/odour; cascade aerators (stepped weirs) increase dissolved oxygen and strip CO₂; diffused-air aerators bubble air through the water; packed-tower aerators use counter-current air flow and are the most efficient for volatile organic compound removal.

5.3 Coagulation and Flocculation

Coagulation destabilises negatively-charged colloidal particles (1–1000 nm) by adding a coagulant salt — alum is most common, optimally effective at pH 6.5–7.5 where its hydroxide floc is least soluble; ferric salts work better at low pH and low temperature than alum. A jar test determines the optimum coagulant dose and pH in the laboratory before full-scale dosing. Flocculation follows with gentle agitation to aggregate the destabilised micro-flocs into larger, settle-able macro-flocs, characterised by the velocity gradient × detention time product (Camp number).

5.4 Sedimentation Tanks

Sedimentation removes settle-able solids under gravity. The key design parameter is the overflow rate (surface loading rate) — any particle with a settling velocity exceeding the overflow rate is completely removed, regardless of tank depth (Hazen's theory), which is why plain sedimentation uses a lower overflow rate than coagulation-sedimentation (heavier, faster-settling flocs allow a higher rate). Stokes' law gives the theoretical settling velocity of a discrete spherical particle as a function of the density difference and particle diameter.

5.5 Filtration

ParameterSlow Sand Filter (SSF)Rapid Sand Filter (RSF)
Filtration rate0.1–0.4 m/hr (0.1–0.2 usual)4–12 m/hr (5 m/hr typical)
MediaSand (0.15–0.35 mm, UC<2)Sand (0.45–0.70 mm) on gravel
Schmutzdecke (biofilm)Critical; biological action; vitalNot present; purely physical
Turbidity of influent≤5 NTU (needs pre-treatment if higher)Can handle higher (after coagulation)
BackwashScraping and washing; 1–2 monthsBackwashing every 24–72 hrs (upward flow)
Area neededVery large (low rate)Much smaller
CostLow operating; high land costHigh capital (coagulation needed); lower land
Coliform removal98–99%Lower; relies on disinfection

The schmutzdecke — a biological film that grows on the SSF sand surface — is what actually does most of the purification in a slow sand filter (biological action, not just straining), which is why SSF achieves excellent coliform removal without any prior coagulation, unlike RSF which relies purely on physical straining and needs disinfection to finish the job.

5.6 Disinfection

Chlorination (gas Cl₂, hypochlorite solutions, or bleaching powder) is the most common disinfection method. Chick's law models disinfection as first-order die-off of organisms with time. The CT concept — concentration × contact time — captures the trade-off between disinfectant dose and required contact time to achieve a given level of pathogen inactivation, and is used to compare different disinfectants (chlorine, ozone, UV) on a common basis. Ozone and UV are powerful but leave no residual, so they are typically used together with a small chlorine dose to maintain protection throughout the distribution system.

💡 SSF rate = 0.1–0.4 m/hr; RSF = 4–12 m/hr. Alum optimal pH = 6.5–7.5. Overflow rate for plain sedimentation = 12,000–18,000 L/m²/day; after coagulation = 30,000–40,000. Chick's law: first-order die-off. These are classic question areas.

Flocculation Velocity Gradient

\( G = \sqrt{\dfrac{P}{\mu V}} \)

Camp number \(G\times t = 10^4\)–\(10^5\) for flocculation

Overflow Rate & Stokes' Law

\( q_s = \dfrac{Q}{A_s} \); particles with \(v_s>q_s\) fully removed

\( v_s = \dfrac{g(\rho_s-\rho_w)d^2}{18\mu} \)

Plain: 12,000–18,000 L/m²/day; Coagulated: 30,000–40,000

RSF Design (IS 4090)

Filtration rate: 5 m/hr (range 4–6); Sand depth: 600–900 mm

Backwash rate: 12–15 m/hr for 5–10 min; expansion 25–50%

Chick's Law (Disinfection Kinetics)

\( N = N_0\,e^{-kt} \)

CT = constant for a given log inactivation

Example 1 — Stokes' Law Settling Velocity

Given: A discrete particle of diameter \(d=0.05\ \text{mm}\), density \(\rho_s=2650\ \text{kg/m}^3\), settles in water (\(\rho_w=1000\ \text{kg/m}^3\), \(\mu=1.0\times10^{-3}\ \text{Pa·s}\)). Find the settling velocity.

Solution:

\( v_s = \dfrac{9.81\times(2650-1000)\times(0.05\times10^{-3})^2}{18\times1.0\times10^{-3}} = \dfrac{9.81\times1650\times2.5\times10^{-9}}{0.018} \)

\( v_s \approx \dfrac{4.05\times10^{-5}}{0.018} \approx 2.25\times10^{-3}\ \text{m/s} = 2.25\ \text{mm/s} \)

Answer: \(v_s\approx2.25\ \text{mm/s}\).

Example 2 — Sedimentation Tank Surface Area

Given: A plant treats \(Q=5000\ \dfrac{\text{m}^3}{\text{day}}\), designed at an overflow rate of \(q_s=15{,}000\ \dfrac{\text{L/m}^2}{\text{day}}\) (plain sedimentation). Find the required surface area.

Solution:

\( A_s = \dfrac{Q}{q_s} = 5{,}000{,}000\ \text{L/day} / 15{,}000\ \dfrac{\text{L/m}^2}{\text{day}} = 333.3\ \text{m}^2 \)

Answer: \(A_s\approx333\ \text{m}^2\).

Example 3 — Chick's Law Disinfection Time

Given: A disinfectant has rate constant \(k=0.5\ \text{min}^{-1}\). Find the time needed to reduce organism count to 1% of initial (99% inactivation).

Solution:

\( N/N_0 = 0.01 = e^{-kt} \Rightarrow t = \dfrac{\ln(100)}{0.5} = \dfrac{4.605}{0.5} = 9.21\ \text{min} \)

Answer: \(t\approx9.2\ \text{minutes}\) of contact time required.

Water treatment plant flow sequence from source through distribution Screening & Intake Aeration (optional) Coagulation & Floccu. Sediment- ation Filtration (RSF/SSF) Disinfect. & Distrib. Source (River/Lake/GW)

Fig. 5.1 — Water treatment plant flow sequence: Screening → Aeration → Coagulation/Flocculation → Sedimentation → Filtration → Disinfection → Distribution.

Q1. The optimal pH range for alum coagulation is:
At pH 6.5–7.5, aluminium hydroxide floc is least soluble and most effective at capturing colloidal particles; outside this range, coagulation efficiency drops sharply.
Q2. The schmutzdecke, critical to slow sand filter performance, is:
The schmutzdecke is a biological film that develops on top of the slow sand filter bed; its biological action (not just physical straining) is why SSF achieves excellent purification, including 98–99% coliform removal, without coagulation.
Q3. Rapid sand filters, compared to slow sand filters, have a filtration rate that is approximately:
RSF operates at 4–12 m/hr versus SSF's 0.1–0.4 m/hr — roughly 20–30 times faster — which is why RSF needs much less land but requires coagulation pre-treatment and more frequent backwashing.
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6. Design of Sewer
Sewerage Systems · Quantity of Sewage · Hydraulic Design · Appurtenances
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6.1 Sewerage Systems — Types

SystemDescriptionAdvantageUse
Separate systemTwo separate pipes: one for sewage, one for storm waterSmaller sewage treatment plant; no dilutionNew planned developments; most modern systems
Combined systemSingle pipe carries both sewage and storm waterLower initial cost; single networkOld cities; can cause overflow in heavy rain
Partially separateSome storm water (from roofs) enters sewerCompromise; reduces surchargeOlder cities modifying to separate

6.2 Quantity of Sewage

The Dry Weather Flow (DWF) is the sewage generated from domestic and industrial use with no rainfall contribution, typically taken as about 80% of the water supplied (the return-flow fraction). Since sewage flow fluctuates hour-to-hour just like water demand, sewers are sized for a peak factor applied to DWF — a higher factor (×3) for small lateral sewers where fluctuations are more pronounced, and a lower factor (×2) for large interceptor sewers where flows from many sources average out. Storm water quantity, where relevant, is estimated by the rational method using a runoff coefficient that reflects the catchment's imperviousness.

6.3 Sewer Hydraulics — Design

Sewers are designed using Manning's equation, exactly as for gravity water conduits, but with two specific velocity constraints unique to sewage: a minimum self-cleansing velocity (to prevent solids from settling and blocking the pipe) and a maximum velocity (to prevent erosion/abrasion of the sewer lining from suspended grit at excessive speeds). A subtlety of circular pipe hydraulics is that the maximum discharge does not occur when the pipe runs completely full, but at about 94% of full depth — because near the very top, a small increase in depth adds disproportionately more wetted perimeter (and hence friction) than flow area.

6.4 Hydraulic Elements — Circular Pipe

The ratio of actual discharge to full-pipe discharge (\(\dfrac{Q}{Q_{full}}\)) and actual velocity to full-pipe velocity (\(V/V_{full}\)) both vary non-monotonically with the depth ratio \(\dfrac{d}{D}\) — each reaching a maximum before the pipe is completely full. Sewers should be designed so the anticipated peak flow does not exceed \(Q_{max}\) (i.e., stays below \(\dfrac{d}{D}=0.94\)), ensuring the pipe never needs to run under pressure.

6.5 Sewer Appurtenances

AppurtenancePurposeSpacing / Size
ManholeAccess for inspection, cleaning, roddingEvery 30–50 m on straight; at every change of direction, dia, gradient; junction
Drop connectionHouse drain enters sewer at much higher elevationWhen incoming pipe invert is >0.6 m above sewer invert
Flushing tankPeriodic flushing of flat-gradient small sewersSelf-priming; at dead ends; automatic
Catch basinTrap grit and floating material from storm drainsAt road inlets; prevents grit entering sewer
Inverted siphonCarries sewage under an obstruction (road, river) under pressureVelocity ≥ 1.0 m/s to prevent deposition; minimum 2 barrels
Ventilation shaftReleases sewer gases; prevents septic conditionsAt every 150–300 m; at siphon ends
💡 Self-cleansing velocity = 0.75 m/s (IS). Max velocity = 3.0 m/s (erosion limit). Q_max for circular pipe = 1.08 × Q_full at d/D = 0.94. Manhole spacing: 30–50 m on straight runs. Inverted siphon velocity ≥ 1.0 m/s. These are core design facts.

Quantity of Sewage

\( Q_{sewage} = \dfrac{80}{100}\times Q_{water\ supply} \)

Peak factor: \(3\times DWF\) (small sewers); \(2\times DWF\) (interceptors)

Manning's Equation (Sewer)

\( V = \dfrac{1}{n}R^{2/3}S^{1/2} \), \( Q = \dfrac{A}{n}R^{2/3}S^{1/2} \)

n: RCC=0.013; glazed stoneware=0.011; PVC=0.009

Velocity Limits

\( V_{min} = 0.75\ \text{m/s} \) (self-cleansing, IS); \( V_{max} = 3.0\ \text{m/s} \) (erosion)

Circular Pipe Hydraulic Elements

\(Q_{max}\) at \(\dfrac{d}{D}=0.94\) (\(=1.08\,Q_{full}\)); \(V_{max}\) at \(\dfrac{d}{D}=0.81\)

Storm Water (Rational Method)

\( Q_{storm} = \dfrac{C\,I\,A}{360} \) (Q in m³/s, I in mm/hr, A in ha)

Example 1 — Design Sewage Flow

Given: A town's design water supply is \(200\ \text{lpcd}\) for a population of \(50{,}000\). Estimate the design (peak) sewage flow for a small sewer.

Solution:

\( Q_{water} = 200\times50{,}000 = 10{,}000{,}000\ \text{L/day} = 10{,}000\ \dfrac{\text{m}^3}{\text{day}} \)

\( DWF = 0.8\times10{,}000 = 8{,}000\ \dfrac{\text{m}^3}{\text{day}} \)

\( Q_{peak} = 3\times8{,}000 = 24{,}000\ \dfrac{\text{m}^3}{\text{day}} \)

Answer: Design peak sewage flow \(\approx24{,}000\ \dfrac{\text{m}^3}{\text{day}}\).

Example 2 — Manning's Velocity Check

Given: A RCC sewer (\(n=0.013\)) has hydraulic radius \(R=0.15\ \text{m}\) and slope \(S=0.002\). Check if the self-cleansing velocity is achieved.

Solution:

\( V = \dfrac{1}{0.013}\times0.15^{2/3}\times0.002^{1/2} = 76.9\times0.282\times0.0447\approx0.97\ \text{m/s} \)

Answer: \(V\approx0.97\ \text{m/s} > 0.75\ \text{m/s}\), so self-cleansing velocity is achieved and the pipe is safely below the 3.0 m/s erosion limit.

Example 3 — Storm Water by Rational Method

Given: A paved catchment of area \(A=8\ \text{ha}\), runoff coefficient \(C=0.9\), design rainfall intensity \(I=60\ \text{mm/hr}\). Find the storm water discharge.

Solution:

\( Q_{storm} = \dfrac{0.9\times60\times8}{360} = \dfrac{432}{360} = 1.2\ \dfrac{\text{m}^3}{\text{s}} \)

Answer: \(Q_{storm}=1.2\ \dfrac{\text{m}^3}{\text{s}}\).

Hydraulic elements of a circular sewer pipe showing Q/Qfull and V/Vfull curves against depth ratio d/D d Partial-depth flow section d/D → ↑ ratio Q/Q_full: peak 1.08 at d/D=0.94 V/V_full: peak at d/D=0.81

Fig. 6.1 — Hydraulic elements of a circular sewer pipe: Q_max occurs at 94% full depth (Q=1.08 Q_full); V_max occurs at 81% depth. Design so peak flow stays below Q_max.

Q1. In a circular sewer pipe, the maximum discharge occurs at:
Maximum discharge occurs at d/D=0.94, not when the pipe is completely full, because near the top a small depth increase adds more wetted perimeter (friction) than flow area — d/D=0.81 is where maximum velocity (not discharge) occurs.
Q2. The self-cleansing velocity recommended by IS codes for sewers is:
IS recommends a minimum self-cleansing velocity of 0.75 m/s (to prevent solids settling); 3.0 m/s is the upper limit to prevent erosion of the sewer lining.
Q3. Dry Weather Flow (DWF) sewage quantity is typically estimated as:
Not all supplied water becomes sewage (some is consumed, lost to evaporation, gardening, etc.); the standard return-flow fraction used for DWF estimation is 80% of water supply.
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7. Quality & Characteristics of Sewage
Composition · BOD Kinetics · Streeter-Phelps · SVI
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7.1 Composition of Domestic Sewage

Sewage is approximately 99.9% water and only 0.1% solids (dissolved, suspended, colloidal) — yet that tiny solid fraction is what makes sewage a pollutant, since it comprises organic matter, inorganic salts, and disease-causing microorganisms.

ParameterTypical RangeSignificance
BOD₅ (5-day BOD at 20°C)150–300 mg/LOrganic pollution indicator; O₂ demand for biodegradation
COD (Chemical Oxygen Demand)250–600 mg/LTotal oxidisable matter (biodegradable + non-biodeg.); COD > BOD always
Suspended Solids (SS)100–350 mg/LSettles; causes sludge; reduces clarity
Dissolved Oxygen (DO)0–1 mg/L (septic)Low/zero DO → anaerobic decomposition; H₂S odour
pH6.5–8.0 (fresh); acidic when septicControls biological treatment
Nitrogen (total)20–85 mg/L as NNutrient; causes eutrophication; TKN + NO₃-N
Phosphorus4–15 mg/L as PNutrient for algae; eutrophication
Coliforms (MPN)10⁶–10⁹/100 mLPathogen indicator; faecal contamination

7.2 BOD — Biochemical Oxygen Demand

BOD measures the oxygen consumed by microorganisms as they biodegrade organic matter, following approximately first-order kinetics — the remaining unoxidised BOD decays exponentially with time. Since the standard 5-day test only captures a fraction of the total (ultimate) oxygen demand, the ratio \(\dfrac{BOD_5}{BOD_u}\) is typically 0.65–0.75 for domestic sewage. COD, which oxidises both biodegradable and non-biodegradable matter chemically, is always higher than BOD₅; a COD/BOD₅ ratio above about 2.5 signals a significant non-biodegradable fraction, a red flag for biological treatment feasibility.

7.3 Dissolved Oxygen and the Streeter-Phelps Equation

When sewage (with its high BOD, low DO) is discharged into a river, dissolved oxygen initially falls as bacteria consume it to oxidise the organic load faster than re-aeration from the atmosphere can replenish it — reaching a minimum at the critical point — then recovers downstream as the BOD load is progressively consumed and re-aeration begins to dominate. The Streeter-Phelps equation models this "oxygen sag curve" as the combined effect of two competing first-order processes: deoxygenation (BOD exertion) and re-aeration.

7.4 Sludge Volume Index (SVI)

SVI measures how well activated sludge settles — a sludge with good settleability (SVI 80–120 mL/g) compacts efficiently in the secondary clarifier, while a "bulking" sludge (SVI >200 mL/g), often caused by filamentous bacteria outcompeting floc-formers, settles poorly and can be washed out of the clarifier, degrading effluent quality. The related Food-to-Microorganism (F/M) ratio expresses the organic loading rate per unit of active biomass, and is a key operational control parameter distinguishing extended aeration (low F/M) from conventional activated sludge (higher F/M) plants.

💡 BOD₅/BOD_u ≈ 0.65–0.75; k_d at 20°C ≈ 0.23/day (base-e). DO_sat at 20°C = 9.08 mg/L. Good SVI = 80–120 mL/g; bulking > 200 mL/g. Streeter-Phelps critical point (minimum DO) is a classic GATE numerical.

First-Order BOD Kinetics

\( BOD_t = L_0(1-e^{-k_d t}) \)

Temperature correction: \( k_d(T) = k_d(20^\circ C)\times\theta^{T-20} \), \(\theta=1.047\)

Streeter-Phelps Oxygen Sag

\( D_t = \dfrac{k_d L_0}{k_r-k_d}\left(e^{-k_d t}-e^{-k_r t}\right)+D_0 e^{-k_r t} \)

Critical Point (Minimum DO)

\( t_c = \dfrac{1}{k_r-k_d}\ln\!\left[\dfrac{k_r}{k_d}\left(1-\dfrac{D_0(k_r-k_d)}{k_d L_0}\right)\right] \)

\( D_c = \dfrac{k_d}{k_r}L_0\,e^{-k_d t_c} \)

Sludge Volume Index

\( SVI = \dfrac{\text{settled sludge volume (mL/L)}}{\text{MLSS (mg/L)}}\times1000 \)

\( \dfrac{F}{M} = \dfrac{\text{BOD input}}{MLVSS\times\text{aeration volume}} \)

Example 1 — Ultimate BOD from 5-Day Test

Given: A sewage sample has \(BOD_5=180\ \text{mg/L}\), \(k_d=0.23\ \text{day}^{-1}\) (base-e). Find the ultimate BOD.

Solution:

\( 180 = L_0(1-e^{-0.23\times5}) = L_0(1-e^{-1.15}) = L_0(1-0.3166) = 0.6834\,L_0 \)

\( L_0 = \dfrac{180}{0.6834} \approx 263.4\ \text{mg/L} \)

Answer: \(L_0\approx263\ \text{mg/L}\).

Example 2 — Sludge Volume Index

Given: A 1-litre sample of mixed liquor with MLSS = 3000 mg/L settles to a volume of 300 mL after 30 minutes. Find the SVI and classify the sludge.

Solution:

\( SVI = \dfrac{300}{3000}\times1000 = 100\ \text{mL/g} \)

Answer: \(SVI=100\ \text{mL/g}\) — within the 80–120 mL/g range, indicating good-settling sludge.

Example 3 — Temperature-Corrected Deoxygenation Rate

Given: \(k_d\) at 20°C is \(0.23\ \text{day}^{-1}\). Find \(k_d\) at 25°C (\(\theta=1.047\)).

Solution:

\( k_d(25) = 0.23\times1.047^{5} = 0.23\times1.258 \approx 0.289\ \text{day}^{-1} \)

Answer: \(k_d(25^\circ C)\approx0.289\ \text{day}^{-1}\) — higher temperature speeds up biodegradation.

Streeter-Phelps dissolved oxygen sag curve downstream of a sewage outfall Distance / Time downstream → DO DO saturation Sewage outfall D_c (max deficit) at t_c Degradation zone → → Recovery zone

Fig. 7.1 — Streeter-Phelps DO sag curve: dissolved oxygen falls below saturation after the sewage outfall, reaching a minimum at the critical point t_c, then recovers as re-aeration overtakes deoxygenation downstream.

Q1. COD is always ______ BOD₅ for the same sewage sample.
COD chemically oxidises both biodegradable and non-biodegradable organic matter, so it always equals or exceeds BOD₅, which only captures biological oxidation within 5 days.
Q2. In the Streeter-Phelps oxygen sag curve, the critical point represents:
The critical point occurs where deoxygenation rate equals re-aeration rate (dD/dt=0), giving the minimum DO / maximum oxygen deficit downstream of the discharge — the most ecologically vulnerable point.
Q3. An activated sludge sample with SVI > 200 mL/g indicates:
SVI above 200 mL/g signals bulking sludge, commonly caused by filamentous organisms outcompeting normal floc-formers — this settles poorly and can wash out of the secondary clarifier, degrading effluent quality.
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8. Disposing of Sewage Effluents
Land Disposal · River Dilution · Septic Tanks · Irrigation Standards
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8.1 Land Disposal Methods

MethodDescriptionBOD RemovalBest for
Irrigation (Land treatment)Sewage applied to agricultural land; plants uptake nutrients85–95%Nutrient-rich effluent; agriculture
Rapid infiltrationHigh rate loading in basins; percolates through soil90–99%Recharge of groundwater
Overland flowSheet flow over grass terraces; collected in drain80–90%Slow-draining soils
Subsurface applicationTile drains or absorption trenches90–99%Small installations; septic tanks

8.2 Dilution and Self-Purification in Rivers

Discharging sewage into a flowing river relies on dilution — mixing with the much larger river flow — combined with the river's natural self-purification capacity. IS 2306 requires a minimum dilution of 1:20 (one part sewage to twenty parts river flow) for pathogenic safety, and separately requires that the outfall not push river DO below 4 mg/L. Self-purification itself proceeds through five simultaneous mechanisms: physical dilution and sedimentation, biological oxidation of organics by aerobic bacteria, photo-oxidation of pathogens by sunlight, and atmospheric re-aeration restoring dissolved oxygen.

8.3 Septic Tank Design

A septic tank is a two-stage (anaerobic digestion + clarification) underground unit used for individual dwellings not connected to a public sewer. IS 2470 specifies a minimum capacity of 1000 litres for 1–5 users, with 180 litres added for each additional user beyond 5 — sized for a minimum 24-hour liquid detention time. The tank's effluent, still containing significant pathogens and nutrients, must be followed by a soak pit or absorption trench for subsurface percolation, and accumulated sludge requires periodic desludging every 1–3 years.

8.4 Wastewater Irrigation Standards

Treated wastewater reused for irrigation must meet standards that depend on the crop and exposure risk: unrestricted irrigation (including food crops eaten raw) requires the strictest limits, while restricted irrigation (non-food crops) permits higher BOD and coliform levels since human exposure is lower. Separately, CPCB sets discharge standards for effluent released to land or inland surface water, which are generally less strict than the unrestricted-irrigation reuse standards since dilution and further natural attenuation are assumed in the receiving environment.

💡 IS 2306 minimum river dilution = 1:20. Septic tank minimum capacity (IS 2470) = 1000 L for 1–5 users, +180 L per extra user. CPCB discharge standard: BOD ≤ 30 mg/L, SS ≤ 100 mg/L for inland surface water. These specific numbers are frequently tested.

Dilution Factor

\( D = \dfrac{Q_{river}+Q_{sewage}}{Q_{sewage}} \)

IS 2306: minimum dilution 1:20 for pathogenic safety

Septic Tank Capacity (IS 2470)

1–5 users: 1000 L; each additional user: +180 L

Detention time \(\ge24\ \text{hr}\); L:B:D = 2:1:1 to 4:1:1

Discharge / Reuse Standards

Unrestricted irrigation: BOD ≤10, SS ≤20, Coliforms ≤1000/100mL

CPCB inland surface water: BOD ≤30, SS ≤100, pH 5.5–9

Example 1 — River Dilution Factor

Given: A river carries \(Q_{river}=8\ \dfrac{\text{m}^3}{\text{s}}\), and sewage of \(Q_{sewage}=0.3\ \dfrac{\text{m}^3}{\text{s}}\) is discharged into it. Check whether the IS 2306 minimum dilution requirement is met.

Solution:

\( D = \dfrac{8+0.3}{0.3} = \dfrac{8.3}{0.3} \approx 27.7 \)

Answer: Dilution ratio \(\approx1:27.7\), which exceeds the IS 2306 minimum of 1:20 — the discharge is acceptable on the dilution criterion.

Example 2 — Septic Tank Capacity

Given: A household of 8 people needs a septic tank. Find the minimum required capacity per IS 2470.

Solution:

First 5 users: 1000 L. Additional users: \(8-5=3\), so \(3\times180 = 540\ \text{L}\)

\( \text{Total} = 1000+540 = 1540\ \text{L} \)

Answer: Minimum capacity \(=1540\ \text{litres}\).

Example 3 — Checking DO Impact of Discharge

Given: A river with DO = 7 mg/L receives a sewage discharge that is estimated to reduce river DO by 2.5 mg/L at the critical point. Check compliance with IS 2306's DO requirement.

Solution:

Resulting DO \(= 7-2.5 = 4.5\ \text{mg/L}\)

Answer: Since \(4.5\ \text{mg/L} > 4\ \text{mg/L}\) (the IS 2306 minimum), the discharge is acceptable, though only with a small margin — any additional loading would risk non-compliance.

Septic tank cross-section with two-stage anaerobic digestion and clarification, followed by a soak pit Chamber 1 (anaerobic digestion, sludge settles) Chamber 2 (clarification, final settling) Sludge Inlet To soak pit Soak pit (percolation)

Fig. 8.1 — Septic tank cross-section: two-stage chamber (anaerobic digestion and settling, then clarification) followed by a soak pit for subsurface percolation of the effluent.

Q1. As per IS 2306, the minimum dilution required for pathogenic safety when discharging sewage into a river is:
IS 2306 requires a minimum dilution of 1 part sewage to 20 parts river flow for pathogenic safety, in addition to the separate requirement that river DO not fall below 4 mg/L.
Q2. Per IS 2470, the minimum septic tank capacity for 1–5 users is:
IS 2470 sets a minimum of 1000 litres for 1–5 users, adding 180 litres for each additional user beyond 5, with a minimum 24-hour liquid detention time.
Q3. Self-purification of a river receiving sewage includes all of the following EXCEPT:
Self-purification mechanisms are dilution (of the existing discharge with river flow), sedimentation, aerobic oxidation, photo-oxidation, and re-aeration — adding more sewage would only worsen pollution, not purify it.
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9. Treatment of Sewage
Levels of Treatment · Activated Sludge · Trickling Filter · WSP · Sludge Management
○ Not Started

9.1 Levels of Sewage Treatment

LevelProcessesBOD RemovalSS Removal
PreliminaryScreening, grit removal, comminution5–10%5–10%
PrimaryPlain sedimentation; skimming of floatables25–40%50–70%
Secondary (biological)Activated sludge; trickling filter; waste stabilisation pond80–95%80–95%
Tertiary (advanced)Nutrient removal (N, P); MF/UF; RO; disinfection>95%>95%

9.2 Activated Sludge Process (ASP)

In the ASP, raw sewage first passes through a primary clarifier, then enters an aeration tank where it is mixed with a suspension of active microorganisms (activated sludge) and aerated by blowers, allowing the biomass to metabolise the dissolved and suspended organic matter. The mixture then flows to a secondary clarifier, where the biomass settles out — most of it is returned to the aeration tank as Return Activated Sludge (RAS) to maintain the required biomass concentration, while the excess (Waste Activated Sludge, WAS) is removed to control sludge age.

9.3 Trickling Filter (Biological Filter)

A trickling filter passes sewage over a fixed bed of media (crushed stone or plastic) on which a biological slime layer grows, oxidising organic matter as the liquid trickles through. Unlike the ASP's suspended-growth biomass, the trickling filter is an attached-growth system. Design uses empirical formulae such as the NRC formula, which relates BOD removal efficiency to organic loading and a recirculation factor — recirculating part of the effluent improves distribution and wetting of the media and dilutes strong influent.

9.4 Waste Stabilisation Ponds (WSP)

Pond TypeDODepthHRTRemoval
Anaerobic pondZero2–5 m5–30 days50–70% BOD
Facultative pondAerobic top; anaerobic bottom1–2 m5–30 days70–90% BOD
Maturation pondAerobic throughout0.5–1.5 m5–10 daysPathogen removal (log reduction)

WSPs form a natural treatment train — anaerobic ponds handle the heaviest organic load first, facultative ponds provide the bulk of BOD removal through a combined aerobic-anaerobic mechanism, and maturation ponds (fully aerobic, shallow, sunlit) focus specifically on pathogen die-off before final discharge.

9.5 Sludge Treatment and Management

Sludge removed from primary and secondary clarifiers must itself be treated before disposal: thickening concentrates it, digestion (anaerobic, in two stages — hydrolysis/acidogenesis then methanogenesis) stabilises it and produces biogas, dewatering reduces its volume for handling, and final disposal is via agricultural land application, landfill, or incineration.

9.6 Industrial Effluent Treatment (ETP)

Industrial wastewater often needs additional steps beyond a conventional municipal sewage train — equalization to smooth out flow and load variability, neutralization to bring pH into a biologically tolerable range, and specific tertiary steps (activated carbon, UV/ozone) tailored to the industry's particular contaminants. Zero Liquid Discharge (ZLD) is mandated by CPCB/MoEF for water-intensive, high-pollution-load industries such as textile, distillery, and paper mills.

💡 ASP: MLSS = 2000–4000 mg/L; SRT = 5–15 days; HRT = 4–8 hours. SSF filtration rate = 0.1–0.4 m/hr; RSF = 4–12 m/hr. Biogas from anaerobic digestion: 60–70% CH₄. SVI = volume of sludge (mL/L) × 1000 / MLSS. These are perennial GATE questions.

ASP Design Parameters

MLSS: 2000–4000 mg/L; \(MLVSS=0.7\text{–}0.8\times MLSS\)

SRT: 5–15 days (conventional); HRT: 4–8 hours

\(\dfrac{F}{M} = \dfrac{BOD_{in}}{MLVSS\times HRT}\): 0.2–0.5 kg BOD/kg MLVSS/day

NRC Formula (Trickling Filter)

\( E = \dfrac{1}{1+0.4432\sqrt{BOD/(VF)}} \)

\( F = \dfrac{1+R}{(1+R/10)^2} \) (R = recirculation ratio)

Anaerobic Digestion

Biogas: 60–70% CH₄, 30–40% CO₂

Gas production: 0.5–1.0 m³/kg VS destroyed; SRT 20–30 days (mesophilic, 35°C)

Example 1 — F/M Ratio for ASP

Given: BOD load entering an aeration tank is \(500\ \text{kg/day}\); MLVSS \(=2500\ \text{mg/L}\); aeration tank volume \(=1000\ \text{m}^3\). Find the F/M ratio.

Solution:

Biomass mass \(= MLVSS\times V = 2500\times10^{-3}\ \text{kg/m}^3\times1000\ \text{m}^3 = 2500\ \text{kg}\)

\( \dfrac{F}{M} = \dfrac{500}{2500} = 0.2\ \text{kg BOD/kg MLVSS/day} \)

Answer: \(\dfrac{F}{M}=0.2\), at the lower end of the conventional ASP range.

Example 2 — Trickling Filter Recirculation Factor

Given: A trickling filter operates at recirculation ratio \(R=2\). Find the recirculation factor F.

Solution:

\( F = \dfrac{1+2}{(1+2/10)^2} = \dfrac{3}{1.44} \approx 2.08 \)

Answer: \(F\approx2.08\), which increases the effective BOD removal efficiency in the NRC formula compared to no recirculation (\(R=0\), \(F=1\)).

Example 3 — Biogas Production

Given: An anaerobic digester destroys \(2000\ \text{kg}\) of volatile solids per day, with a gas yield of \(0.75\ \text{m}^3\) per kg VS destroyed. Estimate the daily biogas volume and methane volume.

Solution:

Biogas \(=2000\times0.75=1500\ \dfrac{\text{m}^3}{\text{day}}\)

Methane (at 65% average) \(=1500\times0.65=975\ \dfrac{\text{m}^3}{\text{day}}\)

Answer: Total biogas \(\approx1500\ \dfrac{\text{m}^3}{\text{day}}\), of which \(\approx975\ \dfrac{\text{m}^3}{\text{day}}\) is methane.

Activated sludge process flow diagram with return and waste activated sludge Primary Clarifier Aeration Tank (biomass + air) Secondary Clarifier Effluent Return Activated Sludge (RAS) Waste Sludge (WAS)

Fig. 9.1 — Activated Sludge Process: raw sewage → Primary clarifier → Aeration tank (biomass + air) → Secondary clarifier → treated effluent; RAS maintains MLSS in the aeration tank, WAS controls sludge age.

Q1. Return Activated Sludge (RAS) in an ASP serves to:
RAS recycles settled biomass from the secondary clarifier back to the aeration tank, sustaining the active microorganism population needed to treat incoming sewage.
Q2. The trickling filter is best described as a:
In a trickling filter, biomass grows as a fixed film on the media surface (attached growth), unlike the ASP where biomass is suspended in the mixed liquor (suspended growth).
Q3. In waste stabilisation pond systems, pathogen removal is primarily achieved in the:
Maturation ponds are shallow, fully aerobic, and sunlit — conditions that maximise UV-driven photo-oxidation of pathogens — making them the final, dedicated pathogen-removal stage in a WSP train.
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10. Air & Sound (Noise) Pollution
Pollutants · Control Devices · Gaussian Plume · Noise Standards
○ Not Started

10.1 Composition of Clean Air & Major Pollutants

Clean, dry air is roughly 78% nitrogen, 21% oxygen, 0.93% argon, and 0.04% CO₂ (rising steadily), with trace gases making up the remainder. Anthropogenic activity adds a further set of pollutants — particulate matter (PM₁₀, PM₂.₅), SO₂, NOx, CO, ozone (secondary, formed photochemically), lead, and volatile organic compounds — each with its own dominant source (combustion, vehicles, industry) and health/environmental effect.

PollutantPrimary SourceHealth EffectNAAQS Limit (24-hr)
Particulate Matter (PM₁₀)Dust, construction, vehicles, industriesRespiratory disease; PM₂.₅ reaches alveoli100 µg/m³ (PM₁₀); 60 µg/m³ (PM₂.₅)
SO₂Combustion of S-containing coal; power plants; refineriesAcid rain (H₂SO₄); respiratory irritant80 µg/m³ (24-hr; annual 50)
NO₂ / NOxHigh-temperature combustion; vehiclesSmog; acid rain (HNO₃); lung damage80 µg/m³
COIncomplete combustion; vehiclesBinds haemoglobin (COHb); asphyxiation2 mg/m³ (8-hr)
Ozone (O₃)Photochemical reaction (NOx + VOC + sunlight)Lung irritant; eye irritation; crop damage100 µg/m³ (8-hr)
Lead (Pb)Leaded fuel (now banned); battery industry; smeltersNeurotoxin; cognitive impairment0.5 µg/m³ (24-hr)
VOCs / HydrocarbonsVehicles; evaporation; industrial solventsPrecursor to photochemical smog—
CO₂ / CH₄Fossil fuels; agriculture; wasteGreenhouse effect; climate changeNo NAAQS (GHG)

10.2 Effects of Air Pollution

  • Health: Respiratory diseases (asthma, COPD, lung cancer), cardiovascular disease, neurological damage (lead, Hg)
  • Vegetation: Leaf burn (SO₂, O₃, HF); stunted growth; reduced yield
  • Visibility: Smog, haze, reduced visibility (PM, aerosols)
  • Materials: Corrosion of metals (SO₂); building stone damage (acid rain dissolves CaCO₃)
  • Climate: Greenhouse effect (CO₂, CH₄, N₂O, CFCs); ozone depletion (CFCs); acid rain (SO₂, NOx)

10.3 Air Pollution Control Devices

Particulate control devices span a range of efficiency and cost. Gravity settling chambers and cyclone separators remove only the coarser fraction cheaply. Fabric filters (baghouses) and electrostatic precipitators (ESPs) achieve very high efficiency down to sub-micron particle sizes — ESPs use a corona discharge to charge particles electrostatically before collecting them on oppositely-charged plates. Wet scrubbers additionally remove gaseous pollutants (SO₂, HCl) alongside particulates by direct contact with a liquid spray.

10.4 Atmospheric Dispersion — Gaussian Plume Model

The Gaussian plume model predicts the ground-level concentration of a pollutant downwind of a stack, assuming the plume spreads in a Gaussian (bell-curve) distribution both horizontally and vertically as it travels downwind. The dispersion coefficients \(\sigma_y\) and \(\sigma_z\) grow with downwind distance and depend on atmospheric stability — more unstable conditions (strong solar heating, low wind) disperse the plume faster and reduce peak ground-level concentration, while stable conditions (clear nights, low wind) trap the plume and can produce higher ground-level concentrations closer to the source.

10.5 Pasquill-Gifford Stability Classes

ClassStabilityConditionDispersion
AExtremely unstableStrong insolation, low wind (<2 m/s)Rapid, wide dispersion
BUnstableModerate insolationGood dispersion
CSlightly unstableSlight insolationModerate
DNeutralOvercast or windy (>6 m/s)Average; most common
ESlightly stableClear night, moderate windPoor dispersion
FStableClear night, low windVery poor; fumigation possible

10.6 Noise Pollution

Sound pressure level is expressed on a logarithmic decibel scale referenced to the threshold of human hearing. Because decibels are logarithmic, sound levels from multiple sources cannot simply be added arithmetically — combining two equal sources only raises the level by 3 dB, not doubling it, since a 3 dB increase already represents a doubling of sound energy. The equivalent sound level \(L_{eq}\) is the single steady-level value that carries the same total sound energy as the actual, fluctuating noise over the measurement period, and is the standard metric used in noise regulations.

10.7 Noise Standards and Health Effects

ZoneDay (6am–10pm) dB(A)Night (10pm–6am) dB(A)
Industrial7570
Commercial6555
Residential5545
Silence zone (hospitals, schools)5040

Prolonged exposure above 85 dB carries a risk of permanent hearing damage (NIPTS — Noise-Induced Permanent Threshold Shift), which characteristically shows up first as a notch at 4000 Hz in an audiogram — a distinctive diagnostic signature of occupational noise exposure rather than age-related hearing loss.

💡 NAAQS: PM₁₀ ≤100, PM₂.₅ ≤60, SO₂ ≤80, NO₂ ≤80 µg/m³. Two equal sound sources → L+3dB (not 2L). CPCB residential: day 55, night 45 dB(A). 4000 Hz notch = NIPTS signature. Stability class A (most unstable) to F (most stable).

Gaussian Plume — Ground Level, Centreline

\( C(x,0,0) = \dfrac{Q}{\pi\sigma_y\sigma_z U}\exp\!\left(\dfrac{-H^2}{2\sigma_z^2}\right) \)

Q=emission rate; U=wind speed; H=effective stack height

Sound Pressure Level

\( L = 20\log_{10}(\dfrac{P}{P_{ref}}) \), \(P_{ref}=20\ \mu\text{Pa}\)

Addition: \( L_{total} = 10\log_{10}\!\left(\Sigma10^{L_i/10}\right) \); two equal sources: \(L+3\ \text{dB}\)

Equivalent Sound Level

\( L_{eq} = 10\log_{10}\!\left[\dfrac{1}{T}\int_0^T\left(\dfrac{P}{P_{ref}}\right)^2dt\right] \)

Example 1 — Decibel Addition

Given: Two machines each produce a sound level of \(80\ \text{dB}\) individually. Find the combined sound level when both operate together.

Solution:

\( L_{total} = 10\log_{10}(10^{8}+10^{8}) = 10\log_{10}(2\times10^8) = 10\times8.301 = 83.01\ \text{dB} \)

Answer: \(L_{total}\approx83\ \text{dB}\) (i.e., \(80+3\ \text{dB}\)), NOT \(160\ \text{dB}\).

Example 2 — Sound Pressure Level from Pressure

Given: A sound has a measured pressure of \(P=2\ \text{Pa}\). Find the SPL.

Solution:

\( L = 20\log_{10}(\dfrac{2}{20\times10^{-6}}) = 20\log_{10}(100{,}000) = 20\times5 = 100\ \text{dB} \)

Answer: \(L=100\ \text{dB}\).

Example 3 — Combining Three Unequal Sources

Given: Three sources produce \(70\ \text{dB}\), \(73\ \text{dB}\), and \(68\ \text{dB}\) individually. Find the combined level.

Solution:

\( L_{total} = 10\log_{10}(10^{7}+10^{7.3}+10^{6.8}) = 10\log_{10}(10{,}000{,}000+19{,}953{,}000+6{,}310{,}000) \)

\( = 10\log_{10}(36{,}263{,}000) \approx 10\times7.56 = 75.6\ \text{dB} \)

Answer: \(L_{total}\approx75.6\ \text{dB}\), dominated by (but higher than) the loudest individual source.

Gaussian plume dispersion from a stack showing horizontal and vertical spread growing with downwind distance Ground level Stack (H) Plume envelope (grows with distance) Ground-level conc. ↑ then ↓ with distance

Fig. 10.1 — Gaussian plume dispersion: the plume spreads horizontally and vertically as it travels downwind, following a Gaussian distribution at each cross-section; ground-level concentration first rises then falls with downwind distance.

Q1. Combining two equal 70 dB sound sources gives a combined level of:
Decibels are logarithmic; two equal sources add only 3 dB, not double the value, since 3 dB already represents a doubling of sound energy.
Q2. Which Pasquill-Gifford stability class corresponds to the most unstable atmosphere (fastest dispersion)?
Class A represents extremely unstable conditions (strong solar heating, low wind), giving the most rapid and widest plume dispersion; class F is the most stable, giving the poorest dispersion.
Q3. Electrostatic precipitators (ESPs) remove particulates by:
ESPs use a high-voltage corona discharge to electrically charge particles, which are then attracted to and collected on oppositely-charged plates — achieving 95–99.5% efficiency, even for sub-micron particles.
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11. Solid Waste Management
Classification · 3R Hierarchy · Disposal Methods · Sanitary Landfill Design
○ Not Started

11.1 Classification of Solid Wastes

TypeSourcesExamplesCharacteristics
Municipal Solid Waste (MSW)Household, commercial, institutionalFood waste, paper, plastic, glass, metalsMixed; 50–60% biodegradable in India
Industrial solid wasteFactories, power plantsFly ash, slag, packaging, process wasteMay contain hazardous substances
Biomedical wasteHospitals, labs, clinicsSharps, body fluids, infected materialHazardous; special handling (BMW Rules 2016)
Hazardous wasteChemical industries; EV batteriesSolvents, heavy metals, pesticidesToxic; special treatment and landfill (Hazardous Waste Rules)
Construction & demolition (C&D)Building demolition, excavationConcrete rubble, steel, brick, soilInert; large volume; recycling possible
E-wasteConsumer electronicsComputers, mobiles, batteriesContains heavy metals (Pb, Hg, Cd, Cr); E-waste Rules 2022

11.2 Municipal Solid Waste — Composition (India)

Typical Indian MSW is dominated by biodegradable organics (40–60%, mainly food waste), with the remainder split among inert material (dirt/ash, 15–20%), paper, plastic, glass, and metals. Per capita generation ranges 0.3–0.6 kg/person/day in urban India, and the calorific value is relatively low (1000–2500 kcal/kg) due to high moisture and inert content — a key constraint on waste-to-energy feasibility, since low calorific value waste needs supplementary fuel to sustain combustion.

11.3 Integrated Solid Waste Management (ISWM) — the 3R Hierarchy

ISWM follows a waste management hierarchy that prioritises interventions in order of environmental preference: Reduce waste generation at the source first (most effective, since it avoids the waste entirely); then Reuse items as-is; then Recycle materials that can't be reused directly; then Recover energy from residual waste that can't be recycled (RDF, waste-to-energy, biogas); and only Dispose (landfill) of what remains after all higher options are exhausted.

11.4 Disposal Methods

MethodDescriptionAdvantageDisadvantage
Open dumpingWaste thrown in open without treatmentNone (cheap short-term)Illegal; vermin, leachate, gas; prohibited under SWM Rules 2016
Sanitary landfillCompacted waste in lined cells; covered daily; leachate collected; gas managedAll waste types; low cost per tonneLand intensive; 30+ year liability
CompostingAerobic decomposition of organics; produces compostReduces waste; produces useful productNeeds source segregation; market for compost
VermicompostingWorms (Eisenia) decompose organicsHigh N compost; decentralisedSensitive to temperature; lower capacity
Incineration (WTE)Combustion at high temperature; energy recovered90%+ volume reduction; energyAir pollution; expensive; needs high calorific waste
BiomethanationAnaerobic digestion; biogas + compostEnergy + compost; closed systemNeeds organics segregation
Pyrolysis / GasificationThermal decomposition without airHandles mixed waste; energy rich productsComplex; expensive; emerging in India

11.5 Sanitary Landfill Design

A sanitary landfill has several essential engineered components: a liner system (HDPE geomembrane, often combined with compacted clay of low permeability) to prevent leachate from contaminating groundwater; a leachate collection system to capture and treat the polluted liquid draining through the waste; a gas collection system to capture landfill gas (roughly equal parts methane and CO₂) since accumulated gas is both a fire/explosion hazard and a potent greenhouse gas if released untreated; and daily cover to control odour, vectors, and windblown litter.

💡 3R hierarchy: Reduce > Reuse > Recycle > Recover energy > Dispose. Landfill gas ≈ 50% CH₄ + 50% CO₂. Liner: HDPE ≥1.5mm + compacted clay (K≤10⁻⁷ cm/s, 60cm). Daily cover minimum 15 cm. These are the most frequently tested landfill facts.

Leachate Generation

\( L = \dfrac{P\times A\times R_c}{1000} \) (m³/day)

P=precipitation (mm/day); A=area (m²); R_c=runoff coefficient (0.3–0.5, covered landfill)

Landfill Gas Generation

Gas: ~50% CH₄ + 50% CO₂

Generated: 1–5 m³/tonne refuse over 10–30 years

Liner Specification

HDPE geomembrane: 1.5 mm minimum

Compacted clay: \(K\le10^{-7}\ \text{cm/s}\), 60 cm thick

Example 1 — Leachate Generation Rate

Given: A covered landfill cell has area \(A=20{,}000\ \text{m}^2\), average daily precipitation \(P=8\ \text{mm/day}\), runoff coefficient \(R_c=0.4\). Find the leachate generation rate.

Solution:

\( L = \dfrac{8\times20{,}000\times0.4}{1000} = \dfrac{64{,}000}{1000} = 64\ \dfrac{\text{m}^3}{\text{day}} \)

Answer: \(L=64\ \dfrac{\text{m}^3}{\text{day}}\) of leachate must be collected and treated.

Example 2 — Landfill Gas Yield

Given: A landfill receives \(500\ \text{tonnes/day}\) of refuse, with an expected gas yield of \(3\ \text{m}^3\) per tonne over its generation life. Estimate the total lifetime gas volume from one day's waste.

Solution:

\( \text{Gas volume} = 500\times3 = 1500\ \text{m}^3 \) (total, released over 10–30 years)

Answer: \(\approx1500\ \text{m}^3\) of landfill gas will eventually be generated from one day's waste input.

Example 3 — Selecting a Disposal Method

Given: A city generates MSW that is 55% biodegradable food waste with low calorific value (1200 kcal/kg) after removing recyclables. Recommend a disposal method for the biodegradable fraction.

Solution: Low calorific value (well below the ~1500 kcal/kg threshold typically needed for self-sustaining incineration) makes waste-to-energy incineration inefficient without supplementary fuel. The high biodegradable fraction is well suited to biological treatment instead.

Answer: Composting or biomethanation (anaerobic digestion) is the more suitable choice, converting the biodegradable fraction into compost and/or biogas rather than attempting incineration.

Sanitary landfill cross-section showing liner system, leachate collection, gas collection and daily cover Native soil / subgrade Compacted clay (K≤10⁻⁷cm/s, 60cm) HDPE liner (≥1.5mm) Leachate pipe Compacted waste (cells) Daily cover (≥15 cm soil) Gas vent (~50% CH₄ + 50% CO₂)

Fig. 11.1 — Sanitary landfill cross-section: HDPE + compacted-clay composite liner and leachate collection at the base, compacted waste cells with daily cover, and gas vents releasing landfill gas.

Q1. In the 3R waste management hierarchy, the most preferred (top-priority) intervention is:
The waste hierarchy prioritises Reduce (avoiding waste generation entirely) above Reuse, Recycle, Recover energy, and Dispose (landfill), which is the last resort for residuals only.
Q2. Landfill gas is approximately composed of:
Landfill gas from anaerobic decomposition of buried waste is roughly half methane and half carbon dioxide, generated continuously over 10–30 years.
Q3. Open dumping of municipal solid waste is:
Open dumping (uncontrolled, untreated disposal) is explicitly prohibited under India's SWM Rules 2016 due to vermin, leachate contamination, and uncontrolled gas emission — sanitary landfill with engineered controls is the legally required alternative.
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12. Quick Revision
Key Formulae · Exam-Angle Summary · Mnemonics · Practice
○ Not Started

A. Key Formulae at a Glance

Peak Demand

\( MDD=1.8\times ADD \); \( MHD=2.7\times ADD \)

Kuichling Fire Demand

\( Q=3182\sqrt{P} \) (L/min, P in thousands)

Hazen-Williams

\( Q=0.2785\,C\,D^{2.63}S^{0.54} \)

Hardy-Cross Correction

\( \Delta Q=-\dfrac{\Sigma h_L}{n\Sigma|h_L/Q|} \)

Unconfined Well

\( Q=\dfrac{\pi K(H^2-h^2)}{\ln(R/r_w)} \)

Confined Well

\( Q=\dfrac{2\pi T(H-h)}{\ln(R/r_w)} \), \(T=Kb\)

Stokes' Settling Velocity

\( v_s=\dfrac{g(\rho_s-\rho_w)d^2}{18\mu} \)

Sewer Self-Cleansing

\( V_{min}=0.75\ \text{m/s} \), \(V_{max}=3.0\ \text{m/s}\)

First-Order BOD

\( BOD_t=L_0(1-e^{-k_d t}) \)

Streeter-Phelps DO Sag

\( D_t=\dfrac{k_dL_0}{k_r-k_d}(e^{-k_dt}-e^{-k_rt})+D_0e^{-k_rt} \)

Sludge Volume Index

\( SVI=\dfrac{\text{settled vol (mL/L)}}{MLSS(\text{mg/L})}\times1000 \)

Gaussian Plume (Centreline)

\( C(x,0,0)=\dfrac{Q}{\pi\sigma_y\sigma_zU}\exp\!\left(\dfrac{-H^2}{2\sigma_z^2}\right) \)

Decibel Addition

\( L_{total}=10\log_{10}(\Sigma10^{L_i/10}) \); equal sources: \(L+3\ \text{dB}\)

B. Exam-Angle Summary

ChapterGATE FocusESE FocusSSC JE Focus
Water demandPer capita values; peak factors; population methodsDetailed demand calculations; fire demand; design periodPer capita; MDD and MHD values
Conduits & distributionHazen-Williams numericals; Hardy-Cross conceptFull network analysis; storage designPipe materials; layout types
Ground water & wellsNumerical: unconfined/confined well equations; \(T=Kb\)Theis method; Thiem; test analysis; Sichardt RTypes of aquifers; formula recognition
Water qualityIS 10500 key limits; hardness types; BOD kinetics; Chick's lawJar test; coagulant chemistry; Langelier index; breakpoint ClIS 10500 key limits only
Water treatmentSSF vs RSF rates; sedimentation overflow rate; disinfection CTTank design calculations; filter media specs; G×t for flocculationSequence of treatment; types of filters
Sewer designManning eq; self-cleansing velocity; Q at d/D=0.94; sewer typesFull sewer design; storm water; rational methodManning equation; sewer materials; manhole spacing
Sewage qualityBOD-COD; Streeter-Phelps; DO sag; SVI; F/MFull river quality analysis; critical DO calculationsBOD definition; COD concept
Sewage disposalDilution factor; IS 2306; septic tank sizingLand disposal design; irrigation reuse standardsSeptic tank basics; disposal methods
Sewage treatmentASP design parameters; SRT; HRT; MLSS; biogas CH₄%Complete STP design; ETP; ZLD; NRC formula for TFTypes of treatment; primary vs secondary
Air & noise pollutionGaussian plume formula; NAAQS limits; stability classes; dB additionStack design; control device selection; photochemical smogPollutant sources and effects; NAAQS limits; noise zones
Solid waste3R hierarchy; sanitary landfill components; leachateLandfill design; gas collection; EIATypes of waste; disposal methods

C. Mnemonics & Memory Aids

💡 Water treatment sequence — "Screens Are Cleverly Set For Distribution": Screening → Aeration → Coagulation → Sedimentation → Filtration → Disinfection.
💡 IS 10500 "5-5-300" rule: Turbidity ≤5 NTU | TDS ≤500 mg/L | Hardness ≤300 mg/L | Fluoride ≤1.0 | Nitrate ≤45.
💡 Peak factors "1.8 and 2.7": MDD=1.8×ADD (Maximum Daily); MHD=2.7×ADD (Maximum Hourly).
💡 RSF vs SSF — "Rapid is Raw, Slow is Schmutzdecke": RSF needs coagulation and runs at 4–12 m/hr; SSF relies on its biological schmutzdecke and runs at 0.1–0.4 m/hr (~30× slower).
💡 Well equations — "UC for Unconfined, C for Confined": Unconfined Q∝(H²−h²); Confined Q∝(H−h) — squared vs linear.
💡 SVI — "80 to 120 good; above 200 bulking": the good-settling range versus filamentous bulking sludge.
💡 Noise zones (D–C–R–S) "75–65–55–50 day; 70–55–45–40 night": Industrial–Commercial–Residential–Silence zone.
💡 Air pollution control (increasing efficiency) — "Gravity Catches Some Big Elephants": Gravity chamber → Cyclone → Wet scrubber → Baghouse → ESP.
💡 Sewer self-cleansing "Walk, don't Sprint": minimum 0.75 m/s (must at least walk); maximum 3 m/s (must not sprint and erode the pipe).

Practice Questions

Q1. A city's average daily demand is \(20{,}000\ \dfrac{\text{m}^3}{\text{day}}\). Find the maximum daily demand and maximum hourly demand.

Show Answer
\(MDD=1.8\times20{,}000=36{,}000\ \dfrac{\text{m}^3}{\text{day}}\); \(MHD=2.7\times20{,}000=54{,}000\ \dfrac{\text{m}^3}{\text{day}}\)

Q2. An unconfined aquifer has \(K=30\ \text{m/day}\), \(H=20\ \text{m}\), \(h=12\ \text{m}\), \(R=250\ \text{m}\), \(r_w=0.1\ \text{m}\). Find the well discharge.

Show Answer
\( Q=\dfrac{\pi\times30\times(20^2-12^2)}{\ln(250/0.1)}=\dfrac{\pi\times30\times256}{\ln(2500)}=\dfrac{24{,}127}{7.824}\approx3083\ \dfrac{\text{m}^3}{\text{day}} \)

Q3. A water sample has \(BOD_5=200\ \text{mg/L}\) with \(k_d=0.23\ \text{day}^{-1}\). Find the ultimate BOD \(L_0\).

Show Answer
\( 200=L_0(1-e^{-1.15})=0.6834L_0 \Rightarrow L_0\approx292.7\ \text{mg/L} \)

Q4. A household with 10 members needs a septic tank sized per IS 2470. Find the minimum capacity.

Show Answer
1000 L (first 5) + 5×180 L (5 extra users) = 1000+900 = 1900 L

Q5. Three equal noise sources each produce 65 dB. Find the combined sound level.

Show Answer
\( L_{total}=10\log_{10}(3\times10^{6.5})=10\log_{10}(3{,}162{,}277\times3)\approx65+10\log_{10}(3)\approx65+4.77=69.77\ \text{dB} \)

Mini Quiz — Full Chapter Recap

Q1. As per IS 1172, the total design per capita water demand for urban India is approximately:
Total design demand for urban India is typically 170–200 lpcd, combining domestic (135 lpcd), industrial/commercial allowances, and losses.
Q2. The confined well discharge equation uses transmissivity \(T\), defined as:
Transmissivity T = K × b, the product of hydraulic conductivity and aquifer thickness — representing the aquifer's overall capacity to transmit water across its full saturated thickness.
Q3. The CPCB noise standard for a residential zone during the day (6am–10pm) is:
Residential zones are limited to 55 dB(A) during the day and 45 dB(A) at night; industrial zones allow up to 75 dB(A) day / 70 dB(A) night.
🎉 All Environmental Engineering topics mastered! Next: Surveying →