Results 341 to 350 of about 222,658 (358)
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Hydrobiologia, 1988
The chloride content of the groundwater increases towards Lake Torrens. Major enrichment occurs on the playa and is caused by evaporation from the capillary zone. The chloride is sea derived via cyclic aeolian transport.
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The chloride content of the groundwater increases towards Lake Torrens. Major enrichment occurs on the playa and is caused by evaporation from the capillary zone. The chloride is sea derived via cyclic aeolian transport.
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Microfiltration of cheese brine
Journal of Dairy Research, 1983SUMMARYA new technique is described for the microfiltration of cheese brine. Soft cheese brine with viable counts/ml of up to 1·2 × 106bacteria and 2·2 × 104yeasts and moulds was filtered using a pleated tangential flow filtration cartridge of 0·2 εm pore size membrane. This filtration resulted in a 3–4 orders of magnitude reduction of bacteria and the
Gerald B. Tanny, Uzi Merin, Salli Gordin
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Injection of dilute brine and crude oil/brine/rock interactions
2002Sensitivity of oil recovery to injection brine composition has been reported for a variety of circumstances including trends of increased recovery of crude oil with decrease in salinity. Absolute permeabilities of sandstones to synthetic reservoir brines and dilutions of these brines show little sensitivity to salinity when the initial brine and ...
Norman R. Morrow, Guo-Qing Tang
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SPRAY EVAPORATION OF BRINE SOLUTIONS
Multiphase, 2006The spray evaporation of brine solutions, for the purpose of salt production, was studied. The water evaporation rate was studied for different climatic conditions, namely relative humidity, air temperature and wind speed, and brine properties like temperature and salt concentration. Two different situations were highlighted: warm brines at about 70oC,
F. Rocha, J. Prior, L. Matos, M. Pinho
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Hydrochemical Characterization of Brines and Identification of Brine Contamination in Aquifersa
Groundwater, 1988ABSTRACTHydrochemical investigations of aquifer contamination by brine are usually approached using conventional graphical methods (i.e. Stiff, Piper, and Schoeller diagrams). While these methods may be used successfully to identify brine in distinction from other contaminants (e.g., road deicing agents) in ground water, they are unsuccessful in ...
Yoram Eckstein, Stephanie A. Novak
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Brine Preparation and Treatment
2005This chapter considers the preparation of brine from solid salt and the design and operation of each of the major units in a brine purification system. The discussion begins with the sources of electrolysis salts (both sodium and potassium chlorides; both natural and refined) and the methods of handling and storing them and then dissolving them to ...
Tilak V. Bommaraju +2 more
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1993
Hot springs, brines, anaerobic waters, temporary ponds, tide pools, frigid water, and other extreme conditions are recurring in the biosphere. They are accompanied by characteristic ecosystems composed of adapted organisms. Often occurring in small volumes as natural microcosms (Duke 1967; Ganning and Wulff 1970), these ecosystems can be readily ...
Howard T. Odum, Robert J. Beyers
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Hot springs, brines, anaerobic waters, temporary ponds, tide pools, frigid water, and other extreme conditions are recurring in the biosphere. They are accompanied by characteristic ecosystems composed of adapted organisms. Often occurring in small volumes as natural microcosms (Duke 1967; Ganning and Wulff 1970), these ecosystems can be readily ...
Howard T. Odum, Robert J. Beyers
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Proceedings of the Royal Society of Edinburgh, 1888
AbstractThe composition of the ice produced in saline solutions, and more particularly in sea-water, has frequently been the object of investigation and of dispute. It might be thought that to a question of whether ice so formed does or does not contain salt, experiment would at once give a decisive answer.
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AbstractThe composition of the ice produced in saline solutions, and more particularly in sea-water, has frequently been the object of investigation and of dispute. It might be thought that to a question of whether ice so formed does or does not contain salt, experiment would at once give a decisive answer.
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International Geology Review, 1968
This type of subsurface water contains more solutes than solvent and is found only at depths exceeding 1000–3000 m, where it exists at high pressures and temperatures, in the form of a dark heavy liquor in rocks ranging in age from Lower Cambrian to Upper Jurassic.
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This type of subsurface water contains more solutes than solvent and is found only at depths exceeding 1000–3000 m, where it exists at high pressures and temperatures, in the form of a dark heavy liquor in rocks ranging in age from Lower Cambrian to Upper Jurassic.
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