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浅论马鞍山地区的膨胀土
引用本文:简河清. 浅论马鞍山地区的膨胀土[J]. 世界地质, 1998, 17(3): 83-85
作者姓名:简河清
作者单位:安徽省马鞍山市建筑设计院!马鞍山,243000
摘    要:
膨胀土由于粘土矿物含量较多,在一定气候条件下其体积随含水量的增加而膨胀,随含水一的减少而收缩,以膨胀土为地基的低层建筑物常常成群开裂,笔者首次报道了马鞍山地区的膨胀土,并对该区膨胀土的分布,成因,评价方法和防治措施等提出了初步看法。

关 键 词:膨胀土 粘土矿物 含水量 地基

The Swelling Soil in Ma'anshan Area, Anhui Province
Jian Heqing. The Swelling Soil in Ma'anshan Area, Anhui Province[J]. Global Geology, 1998, 17(3): 83-85
Authors:Jian Heqing
Abstract:
The swelling soil is a kind of soil that consists of clay minerals, and it ischaracteristic of that the volume of soil will expand as the water content up; the volume ofsoil will contract as the water content down. Row upon row of low buildings that stand onit are usually splitting open. This article reports the swelling soil in Ma'anshan first, andproposes a tentative idea of swelling soil in Ma'anshan on its distribution, cause offormation, appraising way and measure of prevention and control.
Keywords:swelling soil  clay minerals  water content
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