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[农业源头溪流中的空间磷截留]

[Spatial phosphorus retention in an agricultural headwater stream].

作者信息

Mao Zhanpo, Shan Baoqing, Yin Chengqing, Liu Huaiquan, Fang Yang, Wang Haibo, Bai Ying

机构信息

State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, CAS, Beijing 100085, China.

出版信息

Huan Jing Ke Xue. 2003 Nov;24(6):1-8.

Abstract

The spatial dynamics of phosphorus and suspended solids were investigated for two years in a 1.8 km agricultural headwater stream, located by Chaohu Lake, southeastern China. The stream form was greatly modified by human activities. The stream could be divided into 4 channelized reaches (1.3 km), a pond reach (0.15 km) and 3 estuary reaches (0.36 km). It was found that the retention of total phosphorus (TP), phosphate and total suspended solids (TSS) predominantly occurred in the pond reach and estuary reaches. TP, phosphate and TSS retained in the pond and estuary reaches accounted for more than 50% of those retained in whole stream. The retention mostly happened in the precipitation-runoff events and it was 10 to 27 times than that in baseflow. The results showed that channelized reaches were the most important source for pollutant release under either runoff or baseflow conditions, and it accounted for more than 90% of whole stream release. There was a high spatial variation of nutrient dynamics in different channelized reaches. The channelized reach directly discharging into the pond did always retain nutrients and TSS under base flow and runoff, whereas the other channelized reaches performed differently in different hydrological conditions. Stream forms, hydrological conditions, and nutrients characteristics controlled the high spatial variation of the nutrients and TSS in the stream, while the human practices would accelerate these spatial patterns.

摘要

在中国东南部巢湖附近一条1.8公里长的农业源头溪流中,对磷和悬浮固体的空间动态进行了为期两年的研究。溪流形态因人类活动而发生了很大改变。该溪流可分为4个渠化段(1.3公里)、1个池塘段(0.15公里)和3个河口段(0.36公里)。研究发现,总磷(TP)、磷酸盐和总悬浮固体(TSS)的截留主要发生在池塘段和河口段。池塘段和河口段截留的TP、磷酸盐和TSS占整个溪流截留量的50%以上。截留大多发生在降雨径流事件中,是基流情况下的10至27倍。结果表明,渠化段是径流或基流条件下污染物释放的最重要来源,占整个溪流释放量的90%以上。不同渠化段的养分动态存在很大的空间差异。直接排入池塘的渠化段在基流和径流情况下始终截留养分和TSS,而其他渠化段在不同水文条件下表现不同。溪流形态、水文条件和养分特征控制了溪流中养分和TSS的高空间变异性,而人类活动会加速这些空间格局。

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