Answer:
Sediments in and below a dewatered area of an aquifer become compacted because: A) Water pressure drops and the pore spaces are closed
Step-by-step explanation:
Porosity and specific yield are the aquifer most important properties. Specific yield is responsible of giving its capacity to release the water in the pores and transmit the flow with no stress effort. When an aquifer area is dewatered, its pressure drops, and sediments used to clog pore spaces, making them to close.