how many moles of nacl are required to prepar
1.2 M NaCl means that there are 1.2 moles of NaCl per 1...
When you over pump an aquifer the result can be the spreading of contamination or even land subsidence. … When a well is over pumped, water is withdrawn faster than it is coming in and the water level in the well drops dramatically as the geology around the well drains.
When water is pumped out of a well that causes the water table around a well to drop, the initial feature formed is called the. cone of depression.
Some of the negative effects of ground-water depletion include increased pumping costs, deterioration of water quality, reduction of water in streams and lakes, or land subsidence. Such effects, while variable, happen to some degree with any ground-water use.
Overpumping groundwater can cause water tables to fall, as is happening in California, which means that some wells will no longer reach water. … And when aquifers are overpumped, they can collapse, forever reducing their capacity to store water.
A groundwater shortage keeps additional water from flowing into lakes, rivers and seas. This means that over time, less water will enter as the existing surface water continues to evaporate. As the water becomes less deep, it will affect everything in that particular region, including fish and wildlife.
Saltwater_______ occurs if groundwater wells are overpumped along coastlines. … When groundwater is overpumped, subsidence of the land may occur.
When groundwater is overpumped, subsidence of the land may occur. In areas with unconsolidated sediments, compaction occurs, whereas in areas of solid bedrock, ____ in the rock develop, in order to accommodate for the change in surface elevation. Select geologic settings where springs commonly occur.
The water moves from an area where water enters the aquifer (a recharge zone) to an area where water exits the aquifer (a discharge zone). The slope of the water table, or potentiometric surface, which is termed the hydraulic gradient, will dictate t he direction of groundwater flow.
Why has groundwater use increased over time? The principal reason for the increase of groundwater use is the increasing population. Urbanization and pollution have both contributed to an increase in the use of groundwater. Polluted rivers, lakes, and springs are no longer viable sources of groundwater.
Increase in population. Increase in agriculture. Less rainfall.
Ground water depletion is due to drying of wells, reduction od precipitation, over use in irrigating for agriculture and land subsidence.
The water table is an underground boundary between the soil surface and the area where groundwater saturates spaces between sediments and cracks in rock. … Springs are formed where the water table naturally meets the land surface, causing groundwater to flow from the surface and eventually into a stream, river, or lake.
Droughts, seasonal variations in rainfall, and pumping affect the height of the under groundwater levels. If a well is pumped at a faster rate than the aquifer around it is recharged by precipitation or other underground flow, then water levels in the well can be lowered.
Various factors responsible for the depletion of water table are:
Overdraft occurs when, over a period of years, more water is pumped from a groundwater basin than is replaced from all sources – such as rainfall, irrigation water, streams fed by mountain runoff and intentional recharge.
The advantages of withdrawing groundwater include water for drinking and irrigation; availability and locality; low cost, no evaporation losses; and it is renewable. Disadvantages include aquifer depletion from over pumping, subsidence, pollution, saltwater intrusion, and reduced water flow.
Ways to Protect and Conserve Groundwater
Some human activities, such as pumping water into the ground for oil and gas extraction, can cause an aquifer to hold too much ground water. Too much ground water discharge to streams can lead to erosion and alter the balance of aquatic plant and animal species.
Pollution in groundwater aquifers has made many of these wells unfit for consumption. Over-exploitation of ground water lowers water tables, which may damage wetlands, cause ground subsidence, and induce salt-water intrusion in coastal aquifers. Rivers and streams have long been used for discharging the waters.
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