Step 1: Use the formula for steady-state concentration in an airshed. \[ C = \frac{Q}{A \cdot H \cdot V} \] Where: \(C\) = steady-state concentration ($\mu g/m^3$)
\(Q\) = emission rate (20 kg/s)
\(A\) = area of the airshed (10 km × 10 km = \(100 \, {km}^2 = 10^8 \, {m}^2\))
\(H\) = mixing height (1200 m)
\(V\) = wind velocity (4 m/s)
Step 2: Convert emission rate to $\mu$ g/s. \[ Q = 20 \, {kg/s} = 20 \times 10^6 \, {g/s} = 20 \times 10^9 \, \mu{g/s} \] Step 3: Calculate the concentration. \[ C = \frac{20 \times 10^9}{10^8 \times 1200 \times 4} = \frac{20 \times 10^9}{4.8 \times 10^{11}} = 410 \, \mu{g/m}^3 \] Answer: The steady-state SO$_2$ concentration is 410 $\mu$g/m$^3$.
The figure below shows four profiles of the environmental lapse rate. Given that the dry adiabatic lapse rate is \( -10^\circ {C/km} \), the atmosphere is highly unstable for the profile:
Reciprocal levelling is performed for points P and Q by placing the same levelling instrument at A and B. The observations of staff readings are tabulated as below.
If the Reduced Level (RL) of P is 115.246 m, then the true RL of Q, in m, is _______ (rounded off to 3 decimal places)
The information of a mining project for a life of three years is given below:
Additional data: Applicable tax rate = 30%
Discount rate = 10%
Depreciation method: Straight line with zero salvage value
Data from a borehole log with collar elevation at 590 mRL are given below. Composite grade is calculated using cores of 5 m above and below the reference bench at 580 mRL. The composite grade, in %, is: