What is the groundwater discharge?
groundwater discharge is the movement of water from the area of saturated soil. Rainwater penetrates into the ground and moves down the soil until saturated zones are reached, called aquifer. Here the holes and gaps in the soil and rock are filled with water called groundwater. The upper part of this saturated zone is called the water surface.
The water moves to the collectors in places called the area of groundwater charging and moves from the collectors to discharge groundwater in places called discharge points. While the drainage of groundwater usually refers to water leaving the aquifers in the soil, sometimes this term is also used to reference to water moving perverse. In both cases, a unit of measurement of groundwater flow that is usually used by cubic meters per second (m3/s) is usually used. The discharge of groundwater occurs when water penetrates from the Aquifers of the gauge, streams and lakes. Water can also leak from the ground to wetlands and marshes. In areas where the water level is near the top of the ground can be undergroundThe water is usually released by the action of growing plants when they pump water from the collectors and release it into the air as a moisture. Near the ocean, groundwater discharges can be discovered directly into the sea and in this case it is called groundwater discharge in groundwater.
well -created wells can create artificial discharge points for groundwater. When the water is pumped from the well, the water level in the ground that surrounds the well is reduced. This creates a zone called the cone of depression. Groundwater then tends to flow towards the well and provide additional water that can be pumped. In this way, groundwater sources are particularly important in dry areas that have small precipitation and strong Reliance on Wells as a water source.
groundwater flow is an important part of the water cycle. While underground springs may exist, the vast majority of underground waters occupies gaps and pores in the ground and flowsA little bit, as if the water could flow through the sponge. In the permeable rock, under the right circumstances, groundwater can quite far in short spaces. In other areas, groundwater can be stored for years in long -term collectors before it comes again as groundwater discharge.