groundwater

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Related to Pore water: Pore water pressure

groundwater

Water below the earth's surface, saturating soil and rock at the level of the water table and below. It supplies approximately 35 percent of the drinking water in the country and, as such, is a source of much concern for the Environmental Protection Agency. If one purchases a property with contaminants, and those contaminants have leached into the groundwater, then remediation will usually be required before development can proceed.

References in periodicals archive ?
A few data points showed apparent positive Ce anomaly caused by a negative La anomaly (as defined by Bau & Dulski 1996), and one data point from the Nostolepis body scale showed a real positive Ce anomaly, likely reflecting pore water anoxia present in most of the depositional settings.
malinverniana, pore water nitrate was very high compared with values measured in Dutch and Norwegian Isoetes stands (Table 1) and values reported for isoetid lakes in Spain (Catalan et al.
This is very similar to the behavior of 4% agarose at 10 mm/min cross-head speed and should also be caused by the leakage of pore water at the higher stresses reached.
If mixed soil type consist of low bearing capacity, in the slope model maximum pore water pressure could be observed
1999) reported that well-structured soil which allowed preferential flow was associated with a small ratio of 'mobile' water to total pore water ([[theta].
Regardless of depth, investigations of diagenesis must take into account the conditions during and right after deposirion, which determine the types and amounts of primary porosity and the chemistry of the pore water that may or may not have been buried with the sediments/rocks.
If the effect of excess pore water pressure is not considered in the determination of the yield acceleration as is in the existing methods, the yield acceleration does not change from the initial value as is shown in the same figure for [D.
Besides enhancing vegetation growth, paper sludge also minimizes erosion of the tailings caused by winter and water, reduces acid generation and runoff, and lowers metal concentrations in vegetation and pore water.
Surface and pore water pH were studied at Peat Bay Wetlands, located at the Savannah River Site.
At the boiling point of water, 212 [degrees] F (100 [degrees] C), this pore water expands as a gas (steam), and can explode a pot if it can not escape.