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一个世纪以来人类活动引起的环境变化以及营养物和土地利用在维多利亚湖集水区富营养化中的综合作用。

A century of human-induced environmental changes and the combined roles of nutrients and land use in Lake Victoria catchment on eutrophication.

机构信息

Department of Thematic Studies-Environmental Change, Linköping University, Linköping, Sweden; Department of Geology, University of Nairobi, P.O. Box 30197, Nairobi, Kenya.

Department of Thematic Studies-Environmental Change, Linköping University, Linköping, Sweden.

出版信息

Sci Total Environ. 2022 Aug 20;835:155425. doi: 10.1016/j.scitotenv.2022.155425. Epub 2022 Apr 27.

Abstract

Lake Victoria, a lifeline for millions of people in East Africa, is affected by anthropogenic activities resulting in eutrophication and impacting the aquatic life and water quality. Therefore, understanding the ongoing changes in the catchment is critical for its restoration. In this context, catchment and lake sediments are important archives in tracing nutrient inputs and their dominant sources to establish causality with human activities and productivity shifts. In this study, we determine the 1) changes in concentrations of total organic carbon (TOC), black carbon (BC), total nitrogen (TN), C/N ratio, and phosphorous (P) fractions in catchment sediments and the open lake, 2) distribution of diatom population in the lake, and 3) land use and land cover changes in the catchment. The distribution of TOC, BC, TN, C/N, and P correlate while showing spatial and temporal variations. In particular, the steady increase in BC confirms atmospheric inputs from anthropogenic activities in the catchment. However, lake sediments show more variations than catchment-derived sediments in geochemical trends. Notably, the catchment has undergone dramatic land use changes since the 1960s (post-independence). This change is most evident in satellite records from 1985 to 2014, which indicate accelerated human activities. For example, urban growth (666-1022%) and agricultural expansion (23-48%) increased sharply at the expense of a decline in forest cover, grassland, and woodlands in the catchment. Cities like Kisumu and Homa Bay expanded, coinciding with rapid population growth and urbanization. Consequently, nutrient inputs have increased since the 1960s, and this change corresponds with the divergence of diatom communities in the lake. In addition, the transition to Nitzschia and cyanobacteria mark increasing cultural eutrophication in the lake. The geochemical trends and statistical data support our inference(s) and provide insights into urban development and agriculture practices, which propelled increased nutrients from the catchment and productivity shifts in the lake.

摘要

维多利亚湖是东非数百万人的生命线,受到人为活动的影响,导致富营养化,从而影响水生生物和水质。因此,了解集水区的持续变化对于其恢复至关重要。在这种情况下,集水区和湖泊沉积物是追踪养分输入及其主要来源的重要档案,以确定与人类活动和生产力变化的因果关系。在这项研究中,我们确定了:1)集水区沉积物和开阔湖中的总有机碳(TOC)、黑碳(BC)、总氮(TN)、C/N 比和磷(P)分数的变化;2)湖中硅藻种群的分布;3)集水区的土地利用和土地覆盖变化。TOC、BC、TN、C/N 和 P 的分布相关,同时表现出时空变化。特别是,BC 的稳定增加证实了集水区人为活动的大气输入。然而,与集水区衍生沉积物相比,湖泊沉积物在地球化学趋势上表现出更多的变化。值得注意的是,自 20 世纪 60 年代(独立后)以来,集水区经历了剧烈的土地利用变化。从 1985 年到 2014 年的卫星记录中可以明显看出这种变化,这表明人类活动加速。例如,城市增长(666-1022%)和农业扩张(23-48%)急剧增加,而森林、草原和林地在集水区的覆盖率下降。基苏木和霍马湾等城市扩张,与人口快速增长和城市化相吻合。因此,自 20 世纪 60 年代以来,养分输入增加,这一变化与湖泊中硅藻群落的分歧相对应。此外,向菱形藻属和蓝藻的转变标志着湖泊中文化富营养化的增加。地球化学趋势和统计数据支持我们的推断,并提供了对城市发展和农业实践的深入了解,这些实践推动了集水区养分的增加和湖泊生产力的变化。

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