Answer:
The correct option is;
A. Recharges freshwater aquifers
Explanation:
Sedimentary deposits or formations of rock material with sufficient porosity for water retention are known as aquifers
The episodic movement of water from land surfaces, following a storm or other unsaturated areas into a saturated zone is known as aquifer recharge
The natural source of freshwater aquifer recharge is therefore through rainfall or surface waters from wetlands.
Explanation:
The frictional resistance of the various pipes are given by the
K value in the table which may be used with the formula
hf = KQ2
to relate the magnitude of head loss hf in the pipeline
to the volumetric flow rate, Q. Water is drawn at the constant flow
rates from the network at nodes C and D. The static heads
(elevation + pressure head) at nodes B, C and D are 100m, 65m
and 61m respectively above the local datum. Calculate the
discharges at C and D and the water level in reservoir A. (The
data has been added to the diagram to aid the solution)
Use no more than 3 iterations and 3 significant figures.
Answer:
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I hope it's helpful!
Answer:
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