1984
DOI: 10.1007/bf01711765
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Strength of gypsum-clay soils and its variation during the leaching of salts

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Cited by 11 publications
(3 citation statements)
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“…The reason for this behavior can be deduced from the behavior of internal friction angle (ø) where the mineral friction increases simultaneously with increasing gypsum content due to the high coefficient of friction of the gypsum particles, however the porosity of the gypsum-soil increases with increasing gypsum content leading to a reduction in (ø) which affects the shear strength. [13]. Fig.…”
Section: Laboratory Testsmentioning
confidence: 99%
“…The reason for this behavior can be deduced from the behavior of internal friction angle (ø) where the mineral friction increases simultaneously with increasing gypsum content due to the high coefficient of friction of the gypsum particles, however the porosity of the gypsum-soil increases with increasing gypsum content leading to a reduction in (ø) which affects the shear strength. [13]. Fig.…”
Section: Laboratory Testsmentioning
confidence: 99%
“…The improvement is greater for sample S 3 where v = 27 %. This may be attributed to the presence of gypsum fragments within these soils, whose crystallization structures have extremely strong structural bonds, but are very brittle and are irreversibly destroyed by mechanical action during the loading stage (Petrukhin and Arakelyan 1985;AlQaissy 1989).…”
Section: Compression Testmentioning
confidence: 99%
“…Leaching of clayey soil in triaxial cell is a very difficult task because of high labor outlay and lengthy nature of this process (Petrukhin and Arakelyan 1984). This process is relatively easier for short samples such as oedometer or direct shear samples.…”
Section: Test Constrainsmentioning
confidence: 99%