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富营养化加剧导致浅水湖泊中 N/P 比值下降的因果关系。

Cause and effect of N/P ratio decline with eutrophication aggravation in shallow lakes.

机构信息

Center for Environment and Health in Water Source Area of South-to-North Water Diversion, School of Public Health and Management, Hubei University of Medicine, Shiyan 442000, PR China.

Key Laboratory of Algal Biology, State Key Laboratory of Freshwater Ecology and Biotechnology, Institute of Hydrobiology, the Chinese Academy of Sciences, 7# Donghu South Road, Wuhan 430072, PR China.

出版信息

Sci Total Environ. 2018 Jun 15;627:1294-1302. doi: 10.1016/j.scitotenv.2018.01.327. Epub 2018 Feb 7.

Abstract

To explore the relationship and cause and effect between eutrophication and the nitrogen (N)/phosphorus (P) ratio, samples from 38 lakes in Wuhan City, China, with differing degrees of eutrophication, were collected for nutrient levels and extracellular enzyme activities (EEA) in the water column from July 2011 to November 2011. The phosphorus fraction, abundance and potential denitrification rate (PDR) as well as community composition of nirS-type denitrifier in sediments of five typical lakes were further analyzed. A higher trophic level index (TSI) corresponded to a lower N/P ratio, which can be attributed to a loss of N and an increase in P. Specifically, in more eutrophic lakes, the enrichment of total organic carbon and all forms of P in sediments could fuel PDR by shaping community composition and increasing the abundance of nirS-type denitrifier as evidenced by correlation and redundancy analysis, ultimately resulting in a loss of N. Meanwhile, iron-bound phosphorus release induced by anoxia and the hydrolysis of organic P accounted for the observed increase of P in the water column. The lower N/P ratio facilitated the production of leucine aminopeptidase, which was unexpectedly induced by high P but not by low N. Similarly, alkaline phosphatase was induced by high N but not by low P. These findings indicate a mutual coupling and interplay between N and P cycling and confirm our hypothesis that P accumulation accelerates N loss in the process of eutrophication.

摘要

为了探究富营养化与氮磷比之间的关系和因果关系,于 2011 年 7 月至 11 月采集了中国武汉市 38 个不同富营养化程度的湖泊水样,分析了水体柱中营养水平和胞外酶活性(EEA)。此外,还进一步分析了五个典型湖泊沉积物中磷形态、丰度和潜在反硝化速率(PDR)以及nirS 型反硝化菌的群落组成。更高的营养水平指数(TSI)对应更低的 N/P 比,这可以归因于 N 的损失和 P 的增加。具体而言,在富营养化程度更高的湖泊中,沉积物中总有机碳和各种形式的 P 的富集可以通过塑造群落组成和增加 nirS 型反硝化菌的丰度来促进 PDR,这一点可以通过相关和冗余分析得到证明,最终导致 N 的损失。同时,缺氧引起的铁结合磷释放和有机磷的水解导致了水体柱中 P 的增加。较低的 N/P 比有利于亮氨酸氨肽酶的产生,这一现象出人意料地是由高 P 而不是低 N 诱导的。同样,碱性磷酸酶是由高 N 而不是低 P 诱导的。这些发现表明 N 和 P 循环之间存在相互耦合和相互作用,并证实了我们的假设,即富营养化过程中 P 的积累会加速 N 的损失。

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