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THE EFFECTS OF URBANIZATION ONGROUNDWATER IN BEIJING

机译:北京城市化非地下水的影响

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Groundwater supplies 70% of Beijing’s water requirements (Beijing Municipal Water Conservancy Bureau, 2002). Thernimpact of urbanization on groundwater supply includes changes in impervious cover, sources of recharge, surface-water runoff,rnevapotranspiration, and municipal water demand. Research at the University of Texas at Austin indicates that the network ofrnwastewater systems, septic tanks, storm sewers, and lawn irrigation acts as an urban “karst” that supplies additional recharge to therngroundwater balance (Garcia-Fresca, 2004). At the same time, the increase in impervious cover that accompanies urban sprawl andrnmigration to the suburbs decreases evapotranspiration and increases storm runoff. Urbanization in Beijing is analyzed throughrnremotely sensed high-to-moderate resolution datasets, population censuses, administrative boundary maps, and highway constructionrnstatistics. Areas of urban growth are categorized using the Anderson (Anderson et. Al., 1974) classification scheme that analyzes landusernand land-cover. Estimates of impervious area are obtained from urban growth analysis and are used to obtain curve numbers forrnestimating storm runoff. Data on precipitation, irrigation, evapotranspiration, and surface-water runoff are obtained to estimaternrecharge and runoff. The results may indicate that the increase in impervious cover increases surface-water runoff while the increasernin urban irrigation and underground karst results in greater recharge to the groundwater. The results have implications for World Bankrnpolicies that advocate urbanization as a water resources management strategy for the sustainable development of water in rural andrnurban areas. Results of this study are to be obtained during on-site research to be conducted in Beijing during the summer of 2006rnpending approval and funding by the U.S. National Science Foundation’s East Asia and Pacific Summer Institute.
机译:地下水满足了北京70%的用水需求(北京市水利局,2002年)。城市化对地下水供应的影响包括不透水覆盖率,补给源,地表水径流,蒸发蒸腾量和市政用水需求的变化。德克萨斯大学奥斯汀分校的研究表明,废水系统,化粪池,雨水管道和草坪灌溉的网络是城市的“喀斯特”地带,为地下水平衡提供了补充(Garcia-Fresca,2004)。同时,随着城市蔓延和向郊区移民的增加,防渗层的增加减少了蒸散量并增加了暴雨径流。通过遥感的中高分辨率数据集,人口普查,行政边界图和公路建设统计数据,对北京的城市化进行了分析。使用分析土地使用者和土地覆盖的安德森(Anderson等人,1974年)分类方案对城市增长区域进行分类。不透水面积的估计是通过城市增长分析获得的,并用于获得加强暴雨径流的曲线数。获得有关降水,灌溉,蒸散和地表水径流量的数据,以估算补给量和径流量。结果可能表明,不透水覆盖的增加增加了地表水径流,而城市灌溉和地下岩溶的增加导致了对地下水的补给。这些结果对倡导城市化作为农村和城市地区水资源可持续发展的水资源管理战略的世界银行政策具有重要意义。这项研究的结果将在2006年夏季在北京进行的现场研究中获得,这需要美国国家科学基金会的东亚和太平洋夏季研究所的批准和资助。

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