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- W65203492 abstract "Studies made on dispersion of bentonite, a highly colloidal clay, in turbid waters containing more or less dissolved mineral matter show that under easily controlled conditions coagulation of clay suspension takes place, to form a readily filtered floe that effectively clears up turbidity originally present. Moreover apparent volume of this floe measured by use of Imhoff cone is considerably greater than that produced with alum of equal weight and precipitated under optimum conditions. It is further observed that certain bentonites have zeolitic properties i.e., they undergo a base exchange with waters carrying calcium salts and thus produce a definite softening effect. This paper covers main features of an investigation made on a Utah clay. Schroeder, Stone and Sanford (1) of United States Geological Survey define bentonite as a bedded plastic clay which swells greatly on wetting. Ladoo (2) says the name bentonite has been applied to a group of clay-like minerals characterized by an alkaline or alkaline earth content of five to ten per cent, fine grain size, high adsorptive powers, and usually very strong colloidal properties. Davis and Vacher (3) assign to it more or less definite composition of crystalline clay-like minerals montmorillonite and beidellite in both colloidal and crystalline form. Ross and Shannon (4) consider it to be a rock composed essentially of a crystalline clay-like mineral formed by devitrification and chemical alteration of a glassy, igneous material, usually a tuff or volcanic ash, and often containing accessory crystal grains of feldspar, biotite and quartz. The average composition of 8 bentonites from different sources as shown by their data is given in Table I." @default.
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- W65203492 date "1937-04-01" @default.
- W65203492 modified "2023-09-24" @default.
- W65203492 title "The Use of Bentonite as a Coagulant in Water Treatment" @default.
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- W65203492 doi "https://doi.org/10.1002/j.1551-8833.1937.tb20975.x" @default.
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