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机构地区:[1]山西农业大学资源环境学院,山西太谷030801
出 处:《水土保持学报》2003年第6期85-88,91,共5页Journal of Soil and Water Conservation
基 金:国家自然科学基金(40071077);教育部科技重点项目(00149)资助
摘 要:矿区水土流失是一种典型的人为加速侵蚀,存在着明显不同于原地貌的侵蚀特征:井工开采引起的地表塌陷,使地表变形、坡度加大、侵蚀加重,对地下水质也造成污染;露天开采排出的大量松散堆积物,由于地表严重压实和非均匀沉降,促使径流大量汇集,引起崩塌、滑坡、泥石流等地质灾害,同时增加了入河泥沙量,造成河道淤积、行洪困难。本文沦述了采矿塌陷地、煤矸石山、排土场的水土流失特征,采矿对新增入河泥沙的影响,探讨了国内外矿区水土流失的防治所采用的工程措施和生物措施、动态监测水土流失的模型,以及今后尚需研究的内容。Soil and water loss is a kind of typical man-made accumulated erosion in mining area, whose erosion characteristics is distinctly different from previous landforms; ground subsidence resulting from pit-mining not only makes ground deform,slope steep and erosion degree serious, but has underground water quality polluted; Due to condensed surface and uneven subsidence, loose pile waste discharged by open-cast mining, prompts runoff to converge and leads to collapse and slope slide and debris flow etc, at the same time, increases mud and sand entering river making river course deposited and. making flood discharged difficultly. This paper elaborated characteristics of soil and water loss of subsidence and solid waste materials and its effect on sand entering river, discussed home and broad control measures including engineering measures and biological measures and dynamic monitoring model of soil and water loss, and research contents in future.
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