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Monitor-wells material

The term aquifer is used to denote an extensive region of saturated material. There are many types of aquifers. The primary distinction between types involves the boundaries that define the aquifer. An unconfined aquifer, also known as a phraetic or water table aquifer, is assumed to have an upper boundary of saturated soil at a pressure of zero gauge, or atmospheric pressure. A confined aquifer has a low permeabiUty upper boundary that maintains the interstitial water within the aquifer at pressures greater than atmospheric. For both types of aquifers, the lower boundary is frequendy a low permeabihty soil or rock formation. Further distinctions exist. An artesian aquifer is a confined aquifer for which the interstitial water pressure is sufficient to allow the aquifer water entering the monitoring well to rise above the local ground surface. Figure 1 identifies the primary types of aquifers. [Pg.401]

Periodic monitoring points should include extraction, injection, and monitoring points. When sampling injection wells, the injection system should be shut down for approximately 24 h to allow ambient conditions to be reestablished. Monitoring wells should be purged and sampled according to standard procedures. Extracted fluid material (pumped water) can be sampled by the same procedures as collecting a surface water sample. [Pg.287]

Exploration for LNAPL beneath the main portion of the refinery commenced in October 1984 2-in. monitoring wells were initially installed followed by 4-in. test wells in areas of known occurrence. A one-pump recovery system was subsequently designed and installed in the less permeable material encountered beneath this area. The first well was activated in June 1987. [Pg.374]

Answer 16.4 The leachate monitored by the piezometers located in the pit revealed that a threat to local groundwater exists. (What are the concentrations of the various ions ) A plume of leachate entering the local groundwater is observed in the direction of the water level gradient. Contamination is noticeable at a distance of how far (use the scale of the maps) The mentioned observation that metals found in the leachate do not show up in the monitoring wells is explainable by adsorption on clay material in the soil. However, this means that a hallow of metals is formed in the soil and it may reach local groundwater in the future. Therefore, metals observed in the leachate should be measured periodically in the monitoring wells. [Pg.436]

In January, 1976, the Environmental Protection Agency (17, 18) reported that radioactive material migrated from a surface burial facility and extended to the surrounding environment for several hundred feet from its original site. Radioactive material was detected in surface soil samples, in soil cores, in sediments from deep monitoring wells, and in sediments from intermittent streams which drained the burial sites. Again, whenever possible, if carcinogenic material cannot be rendered harmless, it should be disposed of by incineration. [Pg.205]

Drilling. Common drill rigs available for monitor-well installation include cable tool, air rotary, mud rotary, reverse rotary, and hollow-stem auger. The cable tool rig repeatedly lifts and drops a drill bit, drill stem, drilling jars, and rope socket. The drill bit crushes hard rock or loosens unconsolidated material and mixes the loosened particles with water to form a slurry or sludge. The sludge is removed at intervals by a sand pump or a bailer. [Pg.166]

Barcelona, M.J. Gibb, J.P. Millar, R.A. "A Guide to the Selection of Materials for Monitor Well Construction and Ground Water Sampling " Illinois Water Survey Champaign, Illinois 1983 p. 39. [Pg.170]

Later, it was proposed to use redox potential for monitoring the materials of the primary circuit of PWRs as well [7]. [Pg.151]

Sorption/Desorption of Soluble Petroleum Constituents by Materials Used in Monitoring Wells... [Pg.32]


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Monitoring wells

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