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Experimental research on pore size distribution and soil-water characteristic curve of red clay after treatment with ionic soil stabilizer

机译:离子型土壤稳定剂处理后红黏土孔径分布及水土特性曲线试验研究

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Change in the thickness of water film of red clay particles is an important factor to produce geological disasters and geological environmental damage. In order to reduce the thickness of water film, Ionic Soil Stabilizer (ISS) is used to treat with red clay. F-Sorb3400 made in China and Soil Moisture Equipment made in U.S. A were used to test specific surface area, pore size distribution and soil-water char- acteristic curve at 0-500kPa matric suction respectively. The results show that the particle density increases, the specific surface area decreases, the cumulative pore volume and average pore size diameter decrease, dehydration rate slows and the thickness of water film thins after treatment with Ionic Soil stabilizer, thereby the geological engineering disasters caused by the changes of thickness of water film of red clay particle can be effectively inhibited.
机译:红粘土颗粒水膜厚度的变化是引起地质灾害和地质环境破坏的重要因素。为了减少水膜的厚度,使用离子土壤稳定剂(ISS)来处理红粘土。使用中国制造的F-Sorb3400和美国制造的土壤湿度设备分别测试了0-500kPa基质吸力下的比表面积,孔径分布和土壤-水特征曲线。结果表明,离子土壤稳定剂处理后,颗粒密度增加,比表面积减小,累积孔体积和平均孔径减小,脱水速率减慢,水膜厚度变薄,造成地质工程灾害。可以有效抑制红黏土颗粒水膜厚度的变化。

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