长江流域资源与环境 >> 2017, Vol. 26 >> Issue (04): 606-614.doi: 10.11870/cjlyzyyhj201704014
闵敏1,2, 林晨2,3, 熊俊峰2,4, 沈春竹3, 金志丰3, 马荣华2, 许金朵2
MIN Min1,2, LIN Chen2,3, XIONG Jun-feng2,4, SHEN Chun-zhu3, JIN Zhi-feng3, MA Rong-hua2, XU Jin-duo2
摘要: 综合星地协同技术手段,定量化表征1990年以来洪泽湖流域非点源颗粒态磷负荷的时空变化特征,并差别化地探讨其与流域土地利用变化的响应关系,厘清二者的作用机制,为实现非点源磷污染的有效管控提供科技支撑。主要结论包括:(1)近20年,颗粒态磷负荷呈现“下降-上升-下降”的波动状态,1990~1996年呈下降趋势,1998~2006年保持平稳增长状态,2008年后快速下降;(2)颗粒态磷单位负荷空间差异明显,高值区集中分布在淮河支流流域(3.88 t/km2/a),低值区则主要分布在汴河流域(0.57 t/km2/a);(3)不同土地利用模式下平均颗粒态磷负荷由高到低依次为:多种地类混合的淮河支流流域(681.84 t/a)、城镇化快速增长的高松河流域(317.65 t/a)、农用地主导的维桥河流域(185.73 t/a)、湿地保护区的汴河流域(121.09 t/a)。林地、湿地等用地类型能显著减少颗粒态磷污染物的流失量,农用地和建设用地则会加剧颗粒态面源磷污染。
中图分类号:
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