Transmissibility (\( T \)) is a measure of how easily groundwater can flow through an aquifer. It is the product of the aquifer's permeability (\( K \)) and the thickness of the aquifer (\( d \)).
Step 1: Definition of Transmissibility and Permeability
- Permeability (\( K \)) is a property of the aquifer material that measures its ability to transmit water. - Transmissibility (\( T \)) is a measure of the ability of the aquifer to transmit water over a unit width and is related to both the permeability and the thickness of the aquifer.
Step 2: Relationship between Transmissibility and Permeability
The relationship between transmissibility (\( T \)), permeability (\( K \)), and aquifer thickness (\( d \)) is given by: \[ T = Kd \] This equation tells us that transmissibility is directly proportional to both the permeability and the thickness of the aquifer.
Final Answer: \[ \boxed{\text{(A) } T = Kd} \]
| Process | Description |
| (i) Straining | P: Removes only particles in the water large enough to get caught in the pores of the filter |
| (ii) Sedimentation | Q: Larger and heavier particles do not follow the fluid streamline around the sand grain and settle on the grain |
| (iii) Interception | R: Particles that do follow the streamline, but are too large and are caught because they brush up against the sand grains |
| (iv) Diffusion | S: Very small particles are experiencing Brownian motion and may collide with the sand grains by chance |