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- Measurements of the depth below the ground surface of the water table, or its height above sea level, are a key dataset for understanding groundwater. Groundwater levels depend on aquifer properties, local geological conditions and a complex balance between recharge from rainfall, and discharges to rivers or pumped abstraction.
www2.bgs.ac.uk/groundwater/datainfo/levels/levels_data.htmlAccess to groundwater level data | British Geological Survey ...
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Groundwater levels depend on aquifer properties, local geological conditions and a complex balance between recharge from rainfall, and discharges to rivers or pumped abstraction. The data can be used to quantify resources, to understand the flow of groundwater and to measure the impacts of abstraction.
The groundwater transmission and storage properties of geologic formations including aquifers and confining units can be described by three hydrogeologic terms: transmissivity, T; specific storage, Ss; and storativity, S. Transmissivity.
- William Woessner, Eileen Poeter
Apr 24, 2024 · Groundwater exists everywhere there is porosity. However, whether that groundwater is able to flow in significant quantities depends on the permeability. An aquifer is defined as a body of rock or unconsolidated sediment that has sufficient permeability to allow water to flow through it. Unconsolidated materials like gravel, sand, and even silt ...
Aug 19, 2022 · The amount of groundwater flow into the sewer system, and consequently, the effect on the groundwater table, depends on the permeability coefficient of the aquifer, the hydraulic gradient between the groundwater and sewer water level, and the size of the interface area.
- 19 August 2022
- 9, Issue5
Groundwater levels depend on aquifer properties, local geological conditions and a complex balance between recharge from rainfall, and discharges to rivers or pumped abstraction. The data can be used to quantify resources, to understand the flow of groundwater and to measure the impacts of abstraction.
Aug 26, 2021 · Using a superimposed GW–SW system and appropriately grouping the system parameters (as hydraulic and geometric), the experiment shows that the aquifer properties can dominate exchanging flux under certain conditions, e.g., at higher streambed conductance.
Oct 10, 2020 · The variation of groundwater levels varies and depends on the pumping from the wells, permeability, area of recharge and discharge, in effect impacting the increasing or declining water rates in wells that are extracted from aquifers.