How can groundwater depletion affect streams and water quality?
How can groundwater depletion affect streams and water quality?
Some consequences of aquifer depletion include: Lower lake levels or—in extreme cases—intermittent or totally dry perennial streams. These effects can harm aquatic and riparian plants and animals that depend on regular surface flows. Land subsidence and sinkhole formation in areas of heavy withdrawal.
Which of the following factors does not influence the level of the water table?
The correct option is (c) pollution. Pollution is not the factor affecting the level of water table as pollution can contaminate the water and make it unsuitable for commercial use or industrial use but it does not decreases or increases the level of water table.
How can we reduce ground water level?
Ways to Protect and Conserve Groundwater
- Go Native. Use native plants in your landscape.
- Reduce Chemical Use.
- Manage Waste.
- Don’t Let It Run.
- Fix the Drip.
- Wash Smarter.
- Water Wisely.
- Reduce, Reuse, and Recycle.
What are the suggestions to increase water level?
1)Construct percolation tanks, which improves the ground water and recharges the wells and bore wells around the tanks and also attracts the migratotry birds . 2)Construct small tanks in the fields, which helps in percolation and increase the ground water level and also helps the live stock for drinking water.
Do you support the water business in your locality Why?
Answer: No, I don’t support the water business in my locality. Because in my locality there is no water problem. So, it is completely unnecessary to make a water business in my locality.
Why is the ground water level decreasing?
Groundwater depletion most commonly occurs because of the frequent pumping of water from the ground. We pump the water more quickly than it can renew itself, leading to a dangerous shortage in the groundwater supply.
What happens if water flows through a permeable soil layer and reaches a clay layer?
What most likely happens if water flows through a permeable soil layer and reaches a clay layer? It dries up.
Why is permeable soil best for plants that need a lot of drainage Brainly?
A soil possessing an enhanced quality to transfer water is known as permeable soil. Hence, there would be more drainage in the soil with enhanced permeability. Permeable soil loses more water as compared to the impermeable ones. Hence, choosing permeable soil would be best for plants that require a lot of drainage.
Which is the saturated zone quizlet?
Unsaturated zone: The area between the soil-water belt and the water table where pore spaces are not saturated with water. Saturated zone: The zone of rock below and including the water table where pore spaces are completely filled with water.
Where is the saturated zone located?
The phreatic zone, or zone of saturation, is the part of an aquifer, below the water table, in which relatively all pores and fractures are saturated with water. Above the water table is the vadose zone. The phreatic zone size, color, and depth may fluctuate with changes of season, and during wet and dry periods.
Which is a saturated zone?
The saturated zone, a zone in which all the pores and rock fractures are filled with water, underlies the unsaturated zone. The top of the saturated zone is called the water table (Diagram 1). The water table may be just below or hundreds of feet below the land surface.
What do we call the boundary between the unsaturated and saturated zone?
The boundary between the saturated and unsaturated zones is called the water table. 1. The water table rises or falls depending on how much water has recently seeped into the ground or how much groundwater is pumped out of wells.
Which of the following has the highest permeability?
Gravel
What is it called when groundwater comes to the surface?
The locations where water moves laterally are called “aquifers”. Groundwater returns to the surface through these aquifers (arrows), which empty into lakes, rivers, and the oceans. Under special circumstances, groundwater can even flow upward in artesian wells.