Potential impacts of climate change on soil properties

Q4 Agricultural and Biological Sciences
G. Gelybó, E. Tóth, C. Farkas, Á. Horel, I. Kasa, Z. Bakacsi
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引用次数: 40

Abstract

Climate change is expected to have a vigorous impact on soils and ecosystems due to elevated temperature and changes in precipitation (amount and frequency), thereby altering biogeochemical and hydrological cycles. Several phenomena associated with climate change and anthropogenic activity affect soils indirectly via ecosystem functioning (such as higher atmospheric CO2 concentration and N deposition). Continuous interactions between climate and soils determine the transformation and transport processes. Long-term gradual changes in abiotic environmental factors alter naturally occurring soil forming processes by modifying the soil water regime, mineral composition evolution, and the rate of organic matter formation and degradation. The resulting physical and chemical soil properties play a fundamental role in the productivity and environmental quality of cultivated land, so it is crucial to evaluate the potential outcomes of climate change and soil interactions. This paper attempts to review the underlying long-term processes influenced by different aspects of climate change. When considering major soil forming factors (climate, parent material, living organisms, topography), especially climate, we put special attention to soil physical properties (soil structure and texture, and consequential changes in soil hydrothermal regime), soil chemical properties (e.g. cation exchange capacity, soil organic matter content as influenced by changes in environmental conditions) and soil degradation as a result of longterm soil physicochemical transformations. The temperate region, specifically the Carpathian Basin as a heterogeneous territory consisting of different climatic and soil zones from continental to mountainous, is used as an example to present potential changes and to assess the effect of climate change on soils. The altered physicochemical and biological properties of soils require accentuated scientific attention, particularly with respect to significant feedback processes to climate and soil services such as food security.
气候变化对土壤性质的潜在影响
由于气温升高和降水(数量和频率)的变化,预计气候变化将对土壤和生态系统产生强烈影响,从而改变生物地球化学和水文循环。与气候变化和人类活动相关的一些现象通过生态系统功能间接影响土壤(如大气二氧化碳浓度升高和氮沉降)。气候和土壤之间的持续相互作用决定了土壤的转化和运移过程。非生物环境因子的长期渐进变化通过改变土壤水分状况、矿物组成演变以及有机质形成和降解的速度来改变自然发生的土壤形成过程。由此产生的土壤理化性质对耕地的生产力和环境质量起着至关重要的作用,因此评估气候变化和土壤相互作用的潜在结果至关重要。本文试图回顾受气候变化不同方面影响的潜在长期过程。在考虑主要的土壤形成因素(气候、母质、生物、地形),特别是气候时,我们特别关注土壤的物理性质(土壤结构和质地,以及相应的土壤热液制度的变化)、土壤化学性质(如阳离子交换容量、受环境条件变化影响的土壤有机质含量)和土壤长期物理化学转化导致的土壤退化。温带地区,特别是喀尔巴阡盆地,作为一个由从大陆到山地的不同气候和土壤带组成的异质领土,被用作展示潜在变化和评估气候变化对土壤影响的例子。土壤物理化学和生物特性的改变需要加强科学关注,特别是在气候和土壤服务(如粮食安全)的重要反馈过程方面。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Agrokemia es Talajtan
Agrokemia es Talajtan Agricultural and Biological Sciences-Soil Science
CiteScore
0.40
自引率
0.00%
发文量
17
期刊介绍: The journal publishes original papers with English summaries, reports on conferences, book reviews, contributed by Hungarian and foreign authors in the field of soil science, agricultural chemistry, soil microbiology and soil biochemistry.Papers and reviews only in Hungarian.
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