English
| dc.contributor.author | Erzin, Y | |
| dc.contributor.author | Erol, O | |
| dc.date.accessioned | 2024-07-18T11:58:00Z | |
| dc.date.available | 2024-07-18T11:58:00Z | |
| dc.description.abstract | ELSEVIER SCIENCE BV | |
| dc.identifier.uri | http://akademikarsiv.cbu.edu.tr:4000/handle/123456789/7172 | |
| dc.language.iso | Article | |
| dc.publisher | 0013-7952 | |
| dc.subject | Soil suction is the most relevant soil parameter for characterization of the swell behavior. An attempt was made to predict swell pressures from soil suction measurements. In this study, Na-bentonite was mixed with kaolinite in the ratios of 5, 10, 15, 20 and 25% of dry kaolinite weight to obtain soils in a wide range of plasticity indices (i.e. 30, 50, 68, 84 and 97%). Suction measurements using thermocouple psychrometer technique were made on statically compacted specimens. The dependence of soil suction on water content, dry density and bentonite content was examined. Soil suction was correlated to the soil properties, namely, water content, plasticity index, dry density, cation exchange capacity and specific surface area using multiple regression analyses. The correlations revealed a simple regression equation for a quick prediction of soil suctions from easily determined soil properties. In order to investigate soil suction versus swell pressure behavior, the results of standard constant volume swell tests (ASTM, 1990) performed on statically compacted samples of these clay mixtures were used. A linear relationship was established between the logarithm soil suction and the swell pressure. It was also found that an experimental relationship which would directly relate the initial soil suction to the swell pressure can be established. (c) 2007 Elsevier B.V All rights reserved. | |
| dc.title | English | |
| dc.type | LIQUID LIMIT | |
| dc.type | SURFACE-AREA | |
| dc.type | SOILS | |
| dc.type | MINERALOGY | |
| dc.type | CLAYS |