To determine the hydraulic conductivity of the aquifer, we need to use the relationship between transmissivity, hydraulic conductivity, and aquifer thickness.
- Transmissivity (T): The rate at which water is transmitted through a unit width of an aquifer under a unit hydraulic gradient. It is measured in m$^2$/day or ft$^2$/day.
- Hydraulic Conductivity (K): A measure of the ability of a porous medium (such as soil or rock) to transmit water. It is measured in m/day or ft/day.
- Aquifer Thickness (b): The saturated thickness of the aquifer, measured in meters or feet.
The relationship between these parameters is given by:
\[ T = K \times b \]
Where:
- T is Transmissivity
- K is Hydraulic Conductivity
- b is Aquifer Thickness
\( T = 650 \text{ m}^2/\text{day} \)
\( b = 10 \text{ m} \)
We need to rearrange the formula to solve for K: \[ K = \frac{T}{b} \] Substituting the given values: \[ K = \frac{650 \text{ m}^2/\text{day}}{10 \text{ m}} = 65 \text{ m/day} \]
The hydraulic conductivity of the aquifer is 65 m/day.
In the context of the effect of drainage density on the run-off generation and the hydrograph at the catchment outlet, all other factors remaining the same, pick one or more CORRECT statement(s):