针对冷凝条件下的“锅盖效应”现象,设计了简易的水气迁移试验模拟装置,进行不同干密度的北京地区粉土的水气迁移试验.试验结果表明:不同土体干密度的试验中,均发生了明显的水气迁移导致的土体低温端含水量增大的现象;随着土体干密度的增大,土体中水气迁移的速率随之下降,土体含水量增大的现象被弱化.因此,提高粉质土的干密度,虽不能避免水气迁移的发生,但可作为一项防治“锅盖效应”的有效辅助措施.
Abstract
To study the “Potcover Effect” phenomenon, a simple test and its apparatus are designed. A series of moisture migration test were carried on Beijing soils in different dry density. The test results bear the following findings: the water content mounts up in every moisture migration test on soils in different dry density; when the void ratio of soil reduces, the speed of moisture migration slows down as well. As a result, increasing the dry density of soils can be an effective supplementary approach against the “Potcover Effect” phenomenon.
关键词
锅盖效应 /
粉土 /
温度 /
水气迁移 /
含水量 /
干密度
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Key words
Pot-cover Effect /
soils /
temperature /
moisture migration /
water content /
dry density
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参考文献
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脚注
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基金
国家重点基础研究发展计划(973计划)资助项目(2014CB047006);国家自然科学基金资助项目(51209002)
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