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Settleable solids; first-stage BOD

Short answer

Settleable solids measured via Imhoff cone (1L, 1hr settling, read mL/L); non-settleable = total suspended solids minus settleable solids. First-stage BOD derivation: dL/dt = -KL, integrating gives Lₜ = Le^(-Kt). BOD exerted yₜ = L(1-e^(-Kt)) = L(1-10^(-kt)) where k=K/2.303. Temperature correction: K_T = K₂₀(1.047)^(T-20).

Describe the practical approach of determining settleable and non-settleable solids. Also, derive an expression for first-stage BOD.

Practical approach to determine solids

1. Total solids (TS): a measured volume (100 mL) of well-mixed sample is evaporated in a pre-weighed dish on a water bath and dried at 103-105°C to constant weight. TS = (final − empty weight) / volume.

2. Suspended and dissolved solids: another sample is filtered through a weighed glass fibre filter. The dried residue on the filter is the suspended solids (SS); TDS=TS−SSTDS = TS - SS.

3. Volatile and fixed solids: the dried residue is ignited in a muffle furnace at 550°C. The weight lost is the volatile (organic) solids; the ash remaining is the fixed (inorganic) solids.

4. Settleable solids: 1 litre of mixed sample is poured into an Imhoff cone and left undisturbed for 1 hour (after 45 min, the sides are gently stirred). The volume of sludge settled in the tip is read in mL/L. (The gravimetric way: settleable solids = SS of the raw sample − SS of the clear supernatant left after 1 h of settling.)

5. Non-settleable solids: the SS of the supernatant after 1 hour of settling, which are mainly colloids and fine particles; i.e.

Non-settleable solids=Total suspended solids−Settleable solids\text{Non-settleable solids} = \text{Total suspended solids} - \text{Settleable solids}

Derivation of first-stage BOD expression

The first stage (carbonaceous) BOD is the oxygen used to oxidise organic carbon. It is a first order reaction: the rate of oxidation at any time is proportional to the organic matter still remaining (not yet oxidised).

Let LtL_t be the oxygen equivalent of organic matter remaining at time tt and KK the rate constant (day⁻¹).

dLtdt=−K Lt\frac{dL_t}{dt}=-K\,L_t

Separate variables and integrate between t=0t=0 (Lt=LL_t=L, the ultimate first-stage BOD) and time tt:

∫LLtdLtLt=−K∫0tdt ⇒ ln⁡LtL=−Kt\int_{L}^{L_t}\frac{dL_t}{L_t}=-K\int_0^t dt\ \Rightarrow\ \ln\frac{L_t}{L}=-Kt Lt=L e−Kt=L⋅10−kt(k=K/2.303)L_t=L\,e^{-Kt}=L\cdot10^{-k t}\quad(k=K/2.303)

BOD exerted up to time tt is the amount used up:

yt=L−Lt=L(1−e−Kt)=L(1−10−kt)y_t = L - L_t = L\left(1-e^{-Kt}\right)=L\left(1-10^{-kt}\right)

For example, with k=0.1k=0.1/day, BOD5=0.68LBOD_5=0.68L. The rate constant depends on temperature as KT=K20(1.047)T−20K_T=K_{20}(1.047)^{T-20}.

✓ Answer checked by Claude Opus 5.5 (high effort)

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