Longer-term monitoring of a degrading sodic lake: landscape level impacts of hydrological regime changes and restoration interventions (SE Hungary)

IF 1.9 4区 农林科学 Q3 ENVIRONMENTAL SCIENCES Arid Land Research and Management Pub Date : 2023-01-06 DOI:10.1080/15324982.2022.2161970
Zsuzsanna Ladányi, K. Balog, T. Tóth, G. Barna
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引用次数: 1

Abstract

Abstract The diminishing number, extent and degradation of soda lakes were reported from the lowland area of the Carpathian Basin in the past two decades due to anthropogenic impact and climate change. This study provides a detailed spatio-temporal assessment of a degrading alkaline sodic lake ecosystem (13.5 ha) in Southeast Hungary. It discusses the results of spatially detailed topsoil and vegetation surveys from 2009 and 2018 to understand the changes among the current natural and anthropogenic conditions to support a future possible ecological water management. Habitat mapping and laboratory measurement of EC2.5, soda and calcium carbonate content from 199 topsoil samples provided the basis for the assessment. In 2009 the degradation of the naturalness was observed according to the vegetation survey, and the topsoil parameters reflected steppification, leaching and desalinization. Between 2009 and 2018 the loss in extent of Puccinellia swards and the spread of salt meadow species along the channel continued due to the changing salt content. According to the 2018 snapshot of the topsoil, higher salt (from 0.7 to 1.3 mS/cm) and soda content (from 0.08 to 0.12%), furthermore decreasing CaCO3 content (from 25.89 to 20.08%) were characteristic, meaning that there was a changing water and salt regime in the lakebed. The past decade was partly favourable in the point that humid years could rehabilitate the natural conditions in certain parts of the lakebed, but they did not prove to be enough to sustain this alkaline sodic lake.
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退化盐湖的长期监测:水文制度变化和恢复干预措施对景观水平的影响(匈牙利东南部)
摘要/ Abstract摘要:本文报道了近20年来喀尔巴阡盆地低洼地区由于人类活动和气候变化的影响,苏打湖的数量、范围和退化都在减少。本研究对匈牙利东南部一个退化的碱性盐碱湖生态系统(13.5 ha)进行了详细的时空评价。本文对2009年至2018年的空间详细表土和植被调查结果进行了讨论,以了解当前自然和人为条件的变化,为未来可能的生态水管理提供支持。199个表层土壤样品的EC2.5、苏打和碳酸钙含量的室内测量和生境测绘为评价提供了依据。2009年通过植被调查观察到自然度的退化,表层土壤参数反映了阶梯化、淋滤和脱盐。在2009年至2018年期间,由于含盐量的变化,普契利亚草地的面积减少和盐草甸物种沿河道的传播继续下去。根据2018年表层土壤的快照,湖床的盐含量(从0.7到1.3 mS/cm)和苏打含量(从0.08到0.12%)增加,CaCO3含量(从25.89到20.08%)减少,这意味着湖床的水盐状态发生了变化。过去的十年在一定程度上是有利的,因为潮湿的年份可以恢复湖床某些部分的自然条件,但它们不足以维持这个碱性钠质湖泊。
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来源期刊
Arid Land Research and Management
Arid Land Research and Management 环境科学-环境科学
CiteScore
3.80
自引率
7.10%
发文量
23
审稿时长
9 months
期刊介绍: Arid Land Research and Management, a cooperating journal of the International Union of Soil Sciences , is a common outlet and a valuable source of information for fundamental and applied research on soils affected by aridity. This journal covers land ecology, including flora and fauna, as well as soil chemistry, biology, physics, and other edaphic aspects. The journal emphasizes recovery of degraded lands and practical, appropriate uses of soils. Reports of biotechnological applications to land use and recovery are included. Full papers and short notes, as well as review articles and book and meeting reviews are published.
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