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水流入和内生因素驱动了中国洱海生物元素缓冲能力的变化。

Water inflow and endogenous factors drove the changes in the buffering capacity of biogenic elements in Erhai Lake, China.

机构信息

Guangdong-Hong Kong Joint Laboratory for Water Security, Center for Water Research, Advanced Institute of Natural Sciences, Beijing Normal University at Zhuhai, Zhuhai 519087, China; College of Water Sciences, Beijing Normal University, Beijing 100875, China; Engineering Research Center of Ministry of Education on Groundwater Pollution Control and Remediation, Beijing 100875, China.

Guangdong-Hong Kong Joint Laboratory for Water Security, Center for Water Research, Advanced Institute of Natural Sciences, Beijing Normal University at Zhuhai, Zhuhai 519087, China; Engineering Research Center of Ministry of Education on Groundwater Pollution Control and Remediation, Beijing 100875, China.

出版信息

Sci Total Environ. 2022 Feb 1;806(Pt 1):150343. doi: 10.1016/j.scitotenv.2021.150343. Epub 2021 Sep 14.

Abstract

Buffering capacity could provide a comprehensive view to recognize the response between external loads and water quality and help address the significant challenges associated with the reduction of lake pollution. However, quantification of the dynamic change in the holistic buffering capacity of biogenic elements in lakes and its driving mechanisms has not been fully understood. Taking Erhai Lake in China as an example, this study quantified the long-term (2000-2019) dynamic changes in buffering capacity and revealed key driving forces for the changes in buffering capacity. The results showed that nitrogen buffering capacity (NBC) and organic buffering capacity (CODBC) decreased during the past 20 years, while phosphorus buffering capacity (PBC) did not change significantly. Endogenous factors are the main controlling factors of buffering capacity. Specifically, algal biomass drove the change in NBC (interpretation rate of 62.2%); the adsorption and sedimentation effects of sediments maintained the relative stability of PBC (56.30%) while algal biomass indirectly impacted the PBC (1.69% only) by affecting the redox environment of the sediments; and algae-derived organic matter and refractory organic matter accumulation dominated the change in CODBC (61.4% and 32.8%, respectively). Water inflow is another controlling factor for NBC and CODBC due to dilution of lake water. This study indicated that the accumulation of endogenous loads and a decrease in water inflow drove the decrease in the lake's buffering capacity (mainly NBC and CODBC), which could help explain why the decrease in external loads in Erhai Lake has not yet reversed the trend of water quality decline. Our study highlights the importance of comprehensive buffering capacity improvement instead of simple external load control to optimize lake environmental management. In the future, attention should be given to controlling endogenous loads, especially preventing algal blooms, and to optimizing hydrodynamic conditions to cope with the decrease in water inflow.

摘要

缓冲容量可以提供一个综合的视角来认识外部负荷与水质之间的响应,有助于应对与湖泊污染减少相关的重大挑战。然而,对于生物成因要素整体缓冲容量的动态变化及其驱动机制的量化尚未得到充分理解。以中国洱海为例,本研究量化了缓冲容量的长期(2000-2019 年)动态变化,并揭示了缓冲容量变化的关键驱动因素。结果表明,在过去的 20 年中,氮缓冲容量(NBC)和有机缓冲容量(CODBC)呈下降趋势,而磷缓冲容量(PBC)没有显著变化。内源性因素是缓冲容量的主要控制因素。具体来说,藻类生物量驱动 NBC 的变化(解释率为 62.2%);沉积物的吸附和沉降作用维持了 PBC 的相对稳定(占 56.30%),而藻类生物量通过影响沉积物的氧化还原环境间接影响 PBC(仅占 1.69%);藻类衍生的有机物和难降解有机物的积累主导了 CODBC 的变化(分别占 61.4%和 32.8%)。水流入是 NBC 和 CODBC 的另一个控制因素,因为它会稀释湖水。本研究表明,内源性负荷的积累和水流入的减少导致了湖泊缓冲容量的下降(主要是 NBC 和 CODBC),这可以解释为什么洱海外部负荷的减少尚未扭转水质下降的趋势。本研究强调了综合缓冲容量改善的重要性,而不是简单的外部负荷控制,以优化湖泊环境管理。未来应注意控制内源性负荷,特别是防止藻类大量繁殖,并优化水动力条件以应对水流入的减少。

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