Zhou Hui-Ping, Gao Chao
International Institute for Earth System Science, Nanjing University, Nanjing 210093, China.
Huan Jing Ke Xue. 2008 Oct;29(10):2696-702.
Agricultural non-point phosphorus (P) pollution is an important cause of eutrophication in many freshwater systems. Identifying areas that at high risk for P loss to surface water in watershed and concentrating management efforts on these minimal portions of lands are better measures than implementing general strategies over a broad area. A modified version of P index was used to assess P loss risk and identify critical source areas in Chaohu watershed at a regional scale. Soil P sorption index and degree of P sorption saturation were introduced as source factors to show the inherent ability of P transport in soil-water interface. Distance from sources to Chaohu Lake was also considered as a new transport factor to show the influence from sources to final receiving water. The ranking schemes were modified according to available data and scale of study area. The soil P sorption indexes show mild spatial variations in watershed. However, the values are relative low which implies higher loss risk. Distinct spatial variations are found in the degree of soil P sorption saturation. More than 40% of the watershed is saturated over 25% by P. The results show prominent spatial variations of non-point P pollution risk index in Chaohu watershed. Highest risk areas, take up about 5% of the watershed, spread near the downstream parts of main rivers to Chaohu Lake. These should be regarded as critical source areas to be treated in priority. It indicates that P index is a rapid and simple tool to identify critical source areas of non-point P pollution at the regional scale and it enables managers to implement best management practice (BMPs) in a high priority to minimize P loss to sensitive watercourses.
农业面源磷污染是许多淡水系统富营养化的重要原因。识别流域内磷流失到地表水风险高的区域,并将管理工作集中在这些最小面积的土地上,比在大面积实施一般策略更好。采用改良版的磷指数来评估巢湖流域区域尺度上的磷流失风险并识别关键源区。引入土壤磷吸附指数和磷吸附饱和度作为源因素,以表明土壤-水界面磷迁移的内在能力。源区到巢湖的距离也被视为一个新的迁移因素,以显示源区对最终受纳水体的影响。根据现有数据和研究区域的尺度对分级方案进行了修改。流域内土壤磷吸附指数呈现温和的空间变化。然而,其值相对较低,这意味着流失风险较高。土壤磷吸附饱和度存在明显的空间变化。超过40%的流域磷饱和度超过25%。结果表明巢湖流域面源磷污染风险指数存在显著的空间变化。高风险区域约占流域面积的5%,分布在主要河流下游靠近巢湖的部分。这些区域应被视为优先治理的关键源区。这表明磷指数是在区域尺度上识别面源磷污染关键源区的快速简便工具,它能使管理者高度优先地实施最佳管理措施(BMPs),以最大限度减少磷向敏感水道的流失。