首页> 外文会议>2010 International Conference on Management and Service Science >Effect of Soil and Water Loss on Water Eutrophication in Xiaojiang River Basin in Three Gorges Reservoir Region
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Effect of Soil and Water Loss on Water Eutrophication in Xiaojiang River Basin in Three Gorges Reservoir Region

机译:三峡库区小江流域水土流失对富营养化的影响。

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Soil and water loss is an important source of water eutrophication. In this study, soil erosion were measured in the four types of cultivated lands (Paddy land, Terraced farmland, Sloping farmlands <25º, and Sloping farmlands ≥ 25º) in Xiaojiang River basin, Chongqing of China. In addition, water qualities were investigated in 5 reaches of Xiaojiang River (Qukou, Yanglu, Gaoyang, Huangshi, and Shuangjiang) at various times (April, June, July, and November) in 2008. The results showed that (1) Soil and water loss was mainly result from sloping farmlands in Xiaojiang River Basin; (2) Soil and water loss made major contribution to eutrophication in Xiaojiang River. In the study area, the annual losses of TN and TP through soil and water loss from farmlands accounted for 45.7 % and 40.2% of the total TN and TP import of Xiaojiang, respectively; (3) TN and TP concentrations in Xiaojiang River were seriously exceeded the criteria of eutrophication at the sampling times; (4) The phenomenon of "water blooming" occurred in June 2008, one month early when the peak TN concentrations occurred. This may be attributed to interaction of other environmental factors, such as suitable hydrological conditions, temperature and light radiation; (5) TN and TP concentrations in Xiaojiang River were mostly controlled by both soil and water loss and the Yangtze River. And TP concentrations showed obviously seasonal variations. Our study demonstrates that nutrients losses from farmland can be effectively controlled by appropriated management practices, such as the shift of the sloping farmlands to terraced farmlands, proper application of fertilizers, and so on.
机译:水土流失是富营养化的重要来源。在这项研究中,对中国重庆小江流域的四种耕地类型(稻田,梯田,坡度小于25º的坡地和坡度≥25º的耕地)进行了土壤侵蚀测量。此外,在2008年的不同时间(4月,6月,7月和11月)对小江(曲口,洋鹿,高阳,黄石和双江)的5个河段进行了水质调查。结果表明:(1)土壤和土壤失水主要是由于小江流域的坡地耕作造成的。 (2)水土流失是小江富营养化的主要因素。在研究区,由于农田水土流失而造成的总氮和总磷的年损失分别占小江总氮和总磷进口的45.7%和40.2%。 (3)小江总氮和总磷浓度在采样时间严重超过富营养化标准; (4)“水华”现象发生在2008年6月,即TN浓度峰值出现的一个月前。这可能归因于其他环境因素的相互作用,例如适当的水文条件,温度和光辐射; (5)小江的总氮和总磷浓度主要受水土流失和长江的控制。总磷浓度表现出明显的季节性变化。我们的研究表明,可以通过适当的管理措施来有效控制农田的养分流失,例如将坡地转移到梯田,适当使用化肥等。

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