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采煤沉陷区地裂缝对土壤含水率的影响

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为了探究地裂缝对深层土壤含水率的影响,以陕北某煤炭基地煤矿区为研究对象,利用统计分析方法分析动态地裂缝和边缘地裂缝对浅层(0。1~0。3 m)和深层(0。5~6。0 m)土壤含水率的影响,并基于克里金插值法解析土壤含水率的时空变化规律。研究结果表明:①竖直方向上,深度为0~2。0 m时,动态地裂缝区和边缘地裂缝区的土壤含水率均低于未扰动区的值;深度为 2。0~6。0 m时,各区土壤含水率差异不明显,表明地裂缝对土壤含水率的影响深度约为 0~2。0 m,即地裂缝对浅层土壤含水率的影响较大,对更深层土壤含水率的影响相对较小。②水平方向上,动态地裂缝区土壤含水率整体低于闭合区,而 1 年边缘裂缝区土壤含水率整体高于 2 年边缘裂缝区,表明地裂缝会对土壤含水率的空间分布产生较大影响。综合来看,地表塌陷与地裂缝的出现改变了土壤的结构状态,加速了土壤水分的蒸发,降低了土壤持水性。
Influence of ground fissures on deep soil moisture content in coal mining subsidence area
In order to explore the influence of ground fissures on the moisture content of deep soil,a coal mining area located in a coal base in northern Shaanxi was taken as the research object.Statistical analysis methods were used to analyze the influence of dynamic ground fissures and marginal ground fissures on shallow(0.1-0.3 m)and deep(0.5-6.0 m)soil moisture content,and the temporal and spatial variation law of soil moisture content was analyzed based on the Kriging interpolation method.The results showed that:①In the vertical direction,when the depth was 0-2.0 m,the soil moisture content in the dynamic and marginal ground fissure areas was lower than that in the undisturbed area.When the depth was 2.0-6.0 m,there was no signifi-cant difference in soil moisture content among different areas,indicating that the influence of ground fissures on soil moisture content was about 0-2.0 m deep.The influence of ground fissures on the moisture content of shallow soil was greater,and the influence on deeper the moisture content of deeper soil was relatively smaller.②In the horizontal direction,the overall soil moisture content in the dynamic ground fissure area was lower than that in the closed area,while the soil moisture content in the 1-year marginal fissure area was higher than that in the 2-year edge fissure area,indicating that ground fissures have a signifi-cant impact on the spatial distribution of soil moisture.Overall,surface subsidence and the appearance of ground fissures have changed the structural state of soil,accelerated the evaporation of soil moisture,and reduced soil water holding capacity.

coal mining subsidence areasoil moisture contentmarginal ground fissuredynamic ground fissure

高云飞、张凯、杜坤、赵乐、吴凤箫

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国能神东煤炭集团有限责任公司,陕西 榆林 719300

中国矿业大学(北京) 化学与环境工程学院,北京 100083

采煤沉陷区 土壤含水率 边缘地裂缝 动态地裂缝

国家自然科学基金神东集团科技创新项目新疆人才引进计划(2020)

42177037202016000041

2024

天津师范大学学报(自然科学版)
天津师范大学

天津师范大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.311
ISSN:1671-1114
年,卷(期):2024.44(1)
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