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contributor authorNatalie M. Soule
contributor authorSusan E. Burns
date accessioned2017-05-08T21:27:13Z
date available2017-05-08T21:27:13Z
date copyrightApril 2001
date issued2001
identifier other%28asce%291090-0241%282001%29127%3A4%28363%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/52032
description abstractThis study quantified the effects of four quaternary ammonium cations (TMA, DTMA, HDTMA, and BTEA) on the mechanical properties of a modified Wyoming bentonite. TMA, DTMA, and HDTMA are organic cations with alkyl chains of lengths 1, 10, and 16 carbons, while BTEA has a benzyl ring attached. Substitution of the organic cations onto the bentonite surfaces altered the soil's behavior by: (1) reducing the soil's specific gravity, with the specific gravity decreasing linearly as the size of the exchanged organic cation was increased; (2) dramatically reducing the soil's liquid limit (from 458% for the unmodified bentonite to 52–65% for the organoclays); (3) reducing the compressibility of the clays (from a compression index of 5.5 for the unmodified bentonite to compression indices of 0.47–0.59 for the organoclays); (4) reducing the swell potential (
publisherAmerican Society of Civil Engineers
titleEffects of Organic Cation Structure on Behavior of Organobentonites
typeJournal Paper
journal volume127
journal issue4
journal titleJournal of Geotechnical and Geoenvironmental Engineering
identifier doi10.1061/(ASCE)1090-0241(2001)127:4(363)
treeJournal of Geotechnical and Geoenvironmental Engineering:;2001:;Volume ( 127 ):;issue: 004
contenttypeFulltext


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