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内部负荷调节华北半湿润区浅水湖入流浅湖的磷浓度:湖滨湿地和开阔水区的差异过程。

Internal loading regulates the phosphorus concentration in a diversion input shallow lake in the semi-humid region of North China: Differentiated processes in littoral wetland and open water areas.

机构信息

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academic of Sciences, No. 73 East Beijing Road, Nanjing 210008, China; School of Civil Engineering and Architecture, Xi 'an Technological University, Xi 'an 053000, China.

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academic of Sciences, No. 73 East Beijing Road, Nanjing 210008, China.

出版信息

Water Res. 2024 Jun 15;257:121680. doi: 10.1016/j.watres.2024.121680. Epub 2024 Apr 26.

Abstract

Diversion input lakes usually have a low catchment area/lake area ratio and pulsing pollution input. Various pollutants might accumulate in the lake continuously owing to the concentration effect under high evaporation but low precipitation over the entire area, typically for sedimentary cyclic elements such as phosphorus (P). However, the detailed transportation, sedimentation, and internal release mechanisms of P in the diversion input lakes remain unclear. This study conducted a year-long investigation of the littoral wetlands and open water areas of the shallow Lake Hengshui in the semi-humid region of North China. Results revealed that the average total P concentrations in the water and surficial sediment reached as high as 0.202 mg L and 878.21 mg kg in summer. The high water P levels in the lake were mainly regulated by the high internal P loading during summer and autumn, with the internal P loading being approximately nine times the external P loading. The littoral wetland area serves as a higher sedimentation sink and release source of P than the open water area. The concentrated P was continuously transported to the littoral wetland area through detritus burial, coprecipitation, and deposition of suspended particles. The release of P was mainly controlled by the dissolution of redox-sensitive Fe-P and Org-P at high temperatures and organic matter mineralization in the sediment, accompanied by the potential release capacity of apatite P (Ca-P). Future management of eutrophication and P levels in similar diversion input lakes should pay more attention to the high internal P loading in the sediment and the differentiated sedimentation and release processes in the littoral wetland and open water areas.

摘要

分流输入湖泊通常具有低集水区/湖泊面积比和脉冲污染输入。由于整个地区高蒸发但低降水的浓缩效应,各种污染物可能会在湖中不断积累,通常是磷 (P) 等沉积循环元素。然而,分流输入湖泊中 P 的详细迁移、沉积和内部释放机制仍不清楚。本研究对中国北方半湿润地区浅水衡水湖的湖滨湿地和开阔水区进行了为期一年的调查。结果表明,夏季湖水和表层沉积物中的总磷平均浓度高达 0.202mg/L 和 878.21mg/kg。湖泊中高的水体磷水平主要受夏季和秋季高内部磷负荷的调节,内部磷负荷约为外部磷负荷的九倍。湖滨湿地面积比开阔水区更能作为 P 的沉降汇和释放源。浓缩的 P 通过碎屑埋藏、共沉淀和悬浮颗粒的沉积不断输送到湖滨湿地。P 的释放主要受高温下氧化还原敏感的 Fe-P 和 Org-P 的溶解以及沉积物中有机质矿化的控制,同时还伴随着磷灰石 P (Ca-P) 的潜在释放能力。未来对类似分流输入湖泊富营养化和磷水平的管理应更加关注沉积物中的高内部磷负荷以及湖滨湿地和开阔水区的差异化沉积和释放过程。

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