Ground water
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This document defines groundwater as water present beneath the Earth's surface, within soil pores and fractures in rock formations. An aquifer is a unit of rock or sediment that yields usable water. The water table marks the depth where pores and fractures become fully saturated. Groundwater is extracted via wells for agriculture, municipal, and industrial uses. Its study is called hydrogeology. Springs form when aquifers fill to the point of overflowing onto land. Pumping a well creates a cone of depression in the water table or pressure levels around the well. The size of this cone depends on factors like the pumping rate, aquifer properties, storage, and thickness.
Ground water
- 1. GROUND WATER
- 2. DEFINITION: • Groundwater (or ground water) is the water present beneath Earth's surface in soil pore spaces and in the fractures of rock formations. • A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. • The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table.
- 5. USES: • Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. • The study of the distribution and movement of groundwater is hydrogeology, also called GROUNDWATER HYDROLOGY. • Groundwater is often cheaper, more convenient and less vulnerable to pollution than surface water.
- 8. SPRINGS: • A spring is the result of an aquifer being filled to the point that the water overflows onto the land surface. • They range in size from intermittent seeps, which flow only after much rain, to huge pools flowing hundreds of millions of gallons daily. • Types of springs: • Seepage or filtration spring. The term seep refers to springs with small flow rates in which the source water has filtered through permeable earth. • Fracture springs, discharge from faults, joints, or fissures in the earth, in which springs have followed a natural course of voids or weaknesses in the bedrock.
- 10. CONE OF DEPRESSION: • A cone of depression occurs in an aquifer when groundwater is pumped from a well. In an unconfined aquifer (water table), this is an actual depression of the water levels. • In confined aquifers (artesian), the cone of depression is a reduction in the pressure head surrounding the pumped well.
- 12. DIFFERENCE: • The size and shape (slope) of the cone of depression depends on many factors. The pumping rate in the well will affect the size of the cone. • Also, the type of aquifer material, such as whether the aquifer is , sand,silt, fractured rocksetc., also will affect how far the cone extends. • The amount of water in storage and the thickness of the aquifer also will determine the size and shape of the cone of depression.
- 13. • As a well is pumped, the cone of depression will extend out and will continue to expand in a radial fashion until a point of equilibrium occurs. • This usually is when the amount of water released from storage equals the rate of pumping. This also can occur when recharge to the aquifer equals the amount of water being pumped.