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Basin ecosystem management in the upper Han River for the South to North Water Division Project, China

机译:中国南水北调工程汉江上游流域生态系统管理

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摘要

China implemented the South to North Water Division Project (SNWDP) in 2002, and the three-route (i.e., East, Middle, and West) Project is capable of transferring a total of 41.3 billion m3 of water annually from the water rich Yangtze River to the drought Northern China. The upper Han River basin is the water source area of the SNWDP’s Middle Route, thus its aquatic ecosystem and water quality is of great concern. Field surveys and estimated soil erosion concerned with morphological properties from digital terrain model and land use/land cover were conducted and water quality variables were examined in April and October 2006 respectively in order to determine the major eco-environmental consequences such as land use and soil erosion, water pollution and building of hydropower dams in the basin. Hydroclimatologic data from Ankang and Danjiangkou demonstrated temperature rise of 0.29°C/10 a, and significantly decreases of precipitation and runoff (78×108 m3/10 a) in the recent 30 years. The upper Han River catchment with an erosion intensity of 1980-4400 t/km2/yr, transported 3×108 t/yr of soils to the river, and 40% of the riparian zone in some sub catchment was cultivated though the entire basin had a vegetated coverage of 77%. Moreover, chemical oxygen demand (COD) and nitrogen were the major pollutants in the upper Han River with considerably increases in the past 40 years, which would be further exaggerated by dam construction and global warming. Ultimately, corresponding strategies including proper land use, water pollution control, ecologically sustainable management for hydropower station and establishment of eco-environmental monitoring network were introduced for maintaining a scientifically sound aquatic ecosystem and satisfactory water quality in the upper Han River for the interbasin water transfer project.
机译:中国于2002年实施了南水北调工程(SNWDP),三路工程(即东,中,西)每年可从富水的长江中输送总计413亿立方米的水到中国北方干旱。汉江上游流域是SNWDP中线的水源地,因此其水生生态系统和水质备受关注。通过数字地形模型和土地利用/土地覆盖进行了与形态特征有关的野外调查和估计的土壤侵蚀,并分别于2006年4月和2006年10月检查了水质变量,以确定主要的生态环境后果,例如土地利用和土壤流域水土流失,水污染和水坝建设。来自安康和丹江口的水文气候资料显示,近30年温度升高了0.29°C / 10 a,降水和径流明显减少(78×108 m3 / 10 a)。汉江上游流域的侵蚀强度为1980-4400吨/平方公里/年,向河道输送的土壤为3×108吨/年,尽管整个流域都有,但部分流域的河岸带仍被耕种了40%。植被覆盖率达77%。此外,化学需氧量(COD)和氮是汉江上游的主要污染物,在过去的40年中显着增加,由于大坝的建设和全球变暖,这将进一步加剧。最终,引入了相应的策略,包括适当的土地利用,水污染控制,水电站的生态可持续管理和建立生态环境监测网络,以维持汉江上游水系科学合理的水生生态系统和令人满意的水质,以实现跨流域调水。项目。

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    Li, Siyue; Zhang, Quanfa;

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  • 年度 2012
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