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Oscar Edward Meinzer (November 28, 1876 – June 14, 1948) was an American hydrogeologist who has been called the "father of modern groundwater hydrology". [ 2 ] [ 4 ] [ 3 ] He was awarded the William Bowie Medal in 1943.
Hydrology in Practice has been described by CRC Press as "likely to be the course text for every undergraduate/MSc hydrology course in the UK". [3]The book has been reviewed by the Quarterly Journal of the Royal Meteorological Society, [4] the Journal of the American Water Resources Association, [5] the Hydrological Sciences Journal, [6] and the Journal of Hydrology, [7] along with being cited ...
Groundwater engineering, another name for hydrogeology, is a branch of engineering which is concerned with groundwater movement and design of wells, pumps, and drains. [1] The main concerns in groundwater engineering include groundwater contamination , conservation of supplies, and water quality .
According to Groundwater, by Freeze and Cherry (1979), specific storage, [m −1], of a saturated aquifer is defined as the volume of water that a unit volume of the aquifer releases from storage under a unit decline in hydraulic head.
Herman Bouwer (1927–2013) was a hydrological scientist [1] who worked in groundwater hydrology and water resources management, with a specialization in the area of Managed Aquifer Recharge (MAR). He was born in the Netherlands and moved to the United States in 1952 to study for his PhD at Cornell University .
The energy balance of groundwater flow can be applied to flow of groundwater to subsurface drains. [2] The computer program EnDrain [3] compares the outcome of the traditional drain spacing equation, based on Darcy's law together with the continuity equation (i.e. conservation of mass), with the solution obtained by the energy balance and it can be seen that drain spacings are wider in the ...
Groundwater is water that is found underground in cracks and spaces in the soil, sand and rocks. Where water has filled these spaces is the phreatic (also called) saturated zone. Groundwater is stored in and moves slowly (compared to surface runoff in temperate conditions and watercourses) through layers or zones of soil, sand and rocks: aquifers.
It is commonly used in both hydrology and soil sciences. The infiltration capacity is defined as the maximum rate of infiltration. It is most often measured in meters per day but can also be measured in other units of distance over time if necessary. [1] The infiltration capacity decreases as the soil moisture content of soils surface layers ...
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