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Well water

M. W. Kemblowski and co-workers, "Fate and Transport of Residual Hydrocarbon in Ground Water A Case Study," Petroleum Hydrocarbons and Organic Chemicals in Ground Water Prevention, Detection, and Restoration, presented at the conference and exposition. National Water Well Association and American Petroleum Institute, Nov. 17—19, 1987. [Pg.173]

D. P. Hart and R. CouviUion, Earth-Coupled Heat Transfer, National Water Well Association, Dublin, Ohio, 1986. [Pg.174]

At the Taylor Road landfill (originally intended for the disposal of municipal refuse only), unknown quantities of hazardous wastes from industrial and residential sources were deposited. During the period when the landfill was active, soil and groundwater samples collected at the site were found to contain concentrations of volatile organic compounds and metals above acceptable safe drinking water standards. Analysis of samples collected from private drinking water wells indicated that contamination... [Pg.135]

Brenoel, M. and R.A. Brown. Remediation of a Leaking Underground Storage Tank with Enhanced Bioreclamation. In Proc. 5th National Symposium and Exposition on Aquifer Restoration and Groundwater Monitoring, National Water Well Association, Worthington, Ohio, 1985. pp. 527. [Pg.169]

Pipe used for low-pressure applications such as transporting air, steam, gas, water, oil, etc. Employed in machinery, buildings, sprinkler and irrigation systems, and water wells but not in utility distribution systems can transport fluids at elevated temperatures and pressures not subjected to external heat applications. Fabricated in standard diameters and wall thicknesses to ASTM specifications, its diameters range from Vs to 42 in. o.d. [Pg.140]

Procedure (iodometric method). Weigh out accurately about 5.0 g of the bleaching powder into a clean glass mortar. Add a little water, and rub the mixture to a smooth paste. Add a little more water, triturate with the pestle, allow the mixture to settle, and pour off the milky liquid into a 500 mL graduated flask. Grind the residue with a little more water, and repeat the operation until the whole of the sample has been transferred to the flask either in solution or in a state of very fine suspension, and the mortar washed quite clean. The flask is then filled to the mark with distilled water, well shaken, and 50.0 mL of the turbid liquid immediately withdrawn with a pipette. This is transferred to a 250 mL conical flask, 25 mL of water added, followed by 2 g of iodate-free potassium iodide (or 20 mL of a 10 per cent solution) and 10 mL of glacial acetic acid. Titrate the liberated iodine with standard 0.1M sodium thiosulphate. [Pg.397]

Groundwater samples collected over the last 10 years from monitoring and private water wells in the offpost area of RMA have provided data regarding the extent of diisopropyl methylphosphonate. The data indicate that diisopropyl methylphosphonate in the alluvial aquifer extends from the RMA northwest to the South Platte River. In the 1995 sampling event, diisopropyl methylphosphonate concentrations ranged from less than 0.392 g/L, the detection limit, to just over 600 g/L in this area. The highest reported concentrations were present upstream of the Peoria Street Treatment Plant. The lowest or non-... [Pg.120]

In 1996, chemical analyses of groundwater revealed the presence of DIMP in a 19.4 km2 area located north and northwest of RMA, and within 11 km of South Adams County Water and Sanitation District (SACWSD) municipal water wells supplying the city of Commerce City (Harding Lawson Associates 1996). [Pg.121]

In ATES (Aquifer Thermal Energy Storage) systems groundwater is used to carry the thermal energy into and out of an aquifer. For the connection to the aquifer water wells are used. However, these wells are normally designed with double functions, both as production and infiltration wells, see Figure 29. [Pg.155]

An aquifer is in practice defined to be a limited geological formation from which ground water can be pumped by using water wells. [Pg.161]

Figure 34. Flow of groundwater from an unconfined aquifer, drained by a river and by pumping from a water well... Figure 34. Flow of groundwater from an unconfined aquifer, drained by a river and by pumping from a water well...
Smith, S., Rock fracturing methods their development and use, Water Well J., February, 41-47, 1989. [Pg.665]

Williams, E.G., Contaminant containment by in situ polymerization, in Proc. Second National Symposium on Aquifer Restoration and Ground Water Monitoring, National Water Well Association, Worthington, OH, 1982. [Pg.665]

Motor fuels may be found in drinking water wells or rivers. [Pg.692]

Immiscible-phase separation Transformation Processes No Fluids (such as gasoline) that are immiscible in water are a significant consideration in near-surface contamination. Deep-well injection is limited to wastestreams that are soluble in water. Well blowout from gaseous carbon dioxide formation is an example of this process that is distinct to the deep-well environment. [Pg.793]

Scrivner, N.C., Bennet, K.E., Pease, R.A., Kopatsis, A., Sanders, S.J., Clark, D.M., and Rafal, M., Chemical fate of injected wastes, in Proc. Int. Symp. Subsurface Injection of Liquid Wastes, New Orleans, National Water Well Association, Dublin, OH, 1986, pp. 560-609. [Pg.850]

Mercer, J.W. C.R. Faust (1981). Groundwater modeling. National Water Well Association, Washington, DC. [Pg.63]

A pump with a 1 in. diameter suction line is used to pump water from an open hot water well at a rate of 15 gpm. The water temperature is 90°C, with a vapor pressure of 526 mmHg and density of 60 lbm/ft3. If the pump NPSH is 4 ft, what is the maximum distance above the level of the water in the well that the pump can be located and still operate properly ... [Pg.258]

Ke and Regier [71] have described a direct potentiometric determination of fluoride in seawater after extraction with 8-hydroxyquinoline. This procedure was applied to samples of seawater, fluoridated tap-water, well-water, and effluent from a phosphate reduction plant. Interfering metals, e.g., calcium, magnesium, iron, and aluminium were removed by extraction into a solution of 8-hydroxyquinoline in 2-butoxyethanol-chloroform after addition of glycine-sodium hydroxide buffer solution (pH 10.5 to 10.8). A buffer solution (sodium nitrate-l,2-diamino-cyclohexane-N,N,N. AT-tetra-acetic acid-acetic acid pH 5.5) was then added to adjust the total ionic strength and the fluoride ions were determined by means of a solid membrane fluoride-selective electrode (Orion, model 94-09). Results were in close agreement with and more reproducible than those obtained after distillation [72]. Omission of the extraction led to lower results. Four determinations can be made in one hour. [Pg.75]


See other pages where Well water is mentioned: [Pg.90]    [Pg.297]    [Pg.48]    [Pg.431]    [Pg.432]    [Pg.214]    [Pg.33]    [Pg.158]    [Pg.35]    [Pg.650]    [Pg.354]    [Pg.213]    [Pg.143]    [Pg.130]    [Pg.12]    [Pg.105]    [Pg.85]    [Pg.101]    [Pg.297]    [Pg.614]    [Pg.803]    [Pg.354]    [Pg.120]    [Pg.128]    [Pg.1342]   
See also in sourсe #XX -- [ Pg.311 ]

See also in sourсe #XX -- [ Pg.338 ]




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