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Characteristics of the evolution of groundwater flow field in Zhanjiang

Cai Li-xia

Open publisher page 4 citations

Abstract

After the groundwater in the middle and deep aquifers are exploited for nearly 50 years,regional depression cones in groundwater levels have formed.Groundwater in the shallow aquifers has not been exploited as the main water resources,as a result depression cones in water level are not encountered in these aquifer.The main factor affecting the groundwater flow field is the withdrawal rate of groundwater.The second factor is the exploitation manner and hydrogeology conditions in the area.

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What this paper is about

After the groundwater in the middle and deep aquifers are exploited for nearly 50 years,regional depression cones in groundwater levels have formed.Groundwater in the shallow aquifers has not been exploited as the main water resources,as a result depression cones in water level are not encountered in these aquifer.The main factor affecting the groundwater flow field is the withdrawal rate of groundwater.The second factor is the exploitation manner and hydrogeology conditions in the area.

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Available abstract

After the groundwater in the middle and deep aquifers are exploited for nearly 50 years,regional depression cones in groundwater levels have formed.Groundwater in the shallow aquifers has not been exploited as the main water resources,as a result depression cones in water level are not encountered in these aquifer.The main factor affecting the groundwater flow field is the withdrawal rate of groundwater.The second factor is the exploitation manner and hydrogeology conditions in the area.

Key concepts: Aquifer, Hydrogeology, Groundwater, Groundwater flow, Cone of depression, Geology, Hydrology (agriculture), Groundwater discharge

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