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Impact of land use change on groundwater quality in a typical karst watershed of southwest China: a case study of the Xiaojiang watershed, Yunnan Province

机译:西南典型喀斯特流域土地利用变化对地下水水质的影响-以云南省小江流域为例

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摘要

The impact of land-use change on the quality of groundwater in the Xiaotjiang watershed, China was assessed for the period 1982–2004. Groundwater samples were collected from 30 monitoring points across the watershed, and were representative of the various changes, determined by remote sensing and geographical information systems. The results indicate that 610 km2 (60% of the total watershed area) were subject to land-use change during the period. The most important changes were the conversion of 135 km2 of forested land to cultivated land, and 211 km2 of unused land to cultivated land. The main impact was ascribed to diffuse pollution from fertilizers applied to newly cultivated land, and from building development. Overall the groundwater pH value was significantly increased, as were the concentrations of ions $ {text{NH}}^{ + }_{4} $ , $ {text{SO}}^{{2 - }}_{4} $ , $ {text{NO}}^{ - }_{3} $ , $ {text{NO}}^{ - }_{2} $ , and Cl? in groundwater whilst the concentrations of Ca2+ and $ {text{HCO}}^{ - }_{3} $ declined. More precisely, in the regions where forested land and unused land were converted into cultivated land, the pH value and the concentrations of Mg2+, $ {text{NH}}^{ + }_{4} $ , $ {text{SO}}^{{2 - }}_{4} $ , $ {text{NO}}^{ - }_{3} $ , $ {text{NO}}^{ - }_{2} $ , Cl? increased whilst the concentrations of Ca2+ and $ {text{HCO}}^{ - }_{3} $ declined. However in the region where cultivated land was converted into construction land, the pH value and the concentrations of Ca2+, Mg2+, $ {text{NH}}^{ + }_{4} $ , $ {text{HCO}}^{ - }_{3} $ , $ {text{SO}}^{{2 - }}_{4} $ , $ {text{NO}}^{ - }_{3} $ , $ {text{NO}}^{ - }_{2} $ , Cl? increased.
机译:在1982-2004年期间,对中国小江流域土地利用变化对地下水质量的影响进行了评估。从流域的30个监测点收集了地下水样本,这些样本代表了各种变化,这些变化是由遥感和地理信息系统确定的。结果表明,在此期间,610 km2 (占流域总面积的60%)受到土地利用变化的影响。最重要的变化是将135 km2的林地转为耕地,将211 km2的未利用地转为耕地。主要影响归因于新耕地施肥和建筑开发造成的污染扩散。总体上,地下水的pH值显着增加,离子浓度$ {text {NH}} ^ {+} _ {4} $,$ {text {SO}} ^ {{2-}} _ {4}地下水中的$,$ {text {NO}} ^ {-} _ {3} $,$ {text {NO}} ^ {-} _ {2} $和Cl?,而Ca2 +的浓度和$ {text {HCO}} ^ {-} _ {3} $被拒绝。更准确地说,在林地和未利用土地被转换为耕地的区域中,pH值和Mg2 + 的浓度为$ {text {NH}} ^ {+} _ {4} $,$ { text {SO}} ^ {{{2-}} _ {4} $,$ {text {NO}} ^ {-} _ {3} $,$ {text {NO}} ^ {-} _ {2} $,Cl?增加,而Ca2 + 和$ {text {HCO}} ^ {-} _ {3} $的浓度下降。但是在耕地转化为建设用地的地区,pH值和Ca2 + ,Mg2 + 的浓度,$ {text {NH}} ^ {+} _ {4} $,$ {text {HCO}} ^ {-} _ {3} $,$ {text {SO}} ^ {{2-}} _ {4} $,$ {text {NO}} ^ {-} _ {3 } $,$ {text {NO}} ^ {-} _ {2} $,Cl?增加了。

著录项

  • 来源
    《Hydrogeology Journal》 |2008年第4期|727-735|共9页
  • 作者单位

    School of Geographical Sciences Southwest University No.2 Tiansheng Ave Chongqing 400715 China;

    School of Geographical Sciences Southwest University No.2 Tiansheng Ave Chongqing 400715 China;

    School of Geographical Sciences Southwest University No.2 Tiansheng Ave Chongqing 400715 China;

    Institute of Geology Investigation in Yunnan Province Kunming 650041 China;

    Institute of Geology Investigation in Yunnan Province Kunming 650041 China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Karst; Land-use change; Groundwater monitoring; Xiaojiang watershed; China;

    机译:岩溶;土地利用变化;地下​​水监测;小江流域;

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