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DOI10.1016/j.scitotenv.2018.12.243
Biogeochemistry of soil organic matter in agroecosystems & environmental implications
Ondrasek, Gabrijel1; Begic, Helena Bakic1; Zovko, Monika1; Filipovic, Lana1; Merino-Gergichevich, Cristian2; Savic, Radovan3; Rengel, Zed4
发表日期2019
ISSN0048-9697
EISSN1879-1026
卷号658页码:1559-1573
英文摘要

The biogeochemistry of soil organic matter (SOM), as a highly complex and dynamic soil property, is of vital importance for the health and ecological functioning of ecosystems, including managed and natural ones. Dominantly composed of carbon (C), SOM functions in global C cycling, including C sequestration and emission (e.g. soil respiration). Mediterranean agroecosystems especially, due to favourable climate conditions for mineralisation of SUM, are expected to go through enhanced SOM decomposition (i.e. C emission) under the ongoing global warming and related climatic change and variability (frequent heat waves, fires and extreme water disturbances). The relatively stable (humified) SOM components, especially in the organically-enriched topsoil layers, due to their specific physical chemistry (strongly charged interface) may have a significant role in biogeochemistry of charged (in)organic nutrients and/or contaminants such as toxic metal ions and persistent organic pollutants. The recent studies show that some natural vulnerabilities of Mediterranean regions (such as high risk of the erosion-driven processes) can increase movement of some hazardous pedospheric constituents (e.g. pesticides) to water bodies and/or into the air, thus influencing the whole ecosystem health. A majority of recent surveys confirm depletion of SUM and spatially variable distribution of metal contamination in the Mediterranean topsoils. Using the advanced geochemical prediction approaches in combination with the relevant soil databases, we characterised organo-mineral and organo-metal complexation and its effect on speciation and sorption of trace metals in karstified Mediterranean agroecosystems. Metal biogeochemistry was found to vary markedly under relatively constant pedosphere conditions, depending on organo-mineral soil components and pH, which may significantly impact metal mobility/availability in the soil-plant continuum. The knowledge of the SOM spatial distribution and dynamics and its interactions with other pedovariables is essential for sustainable management of SOM and control of contaminant mobility to avoid degradation processes in (agro)ecosystems. (C) 2018 Elsevier B.V. All rights reserved.


WOS研究方向Environmental Sciences & Ecology
来源期刊SCIENCE OF THE TOTAL ENVIRONMENT
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/95139
作者单位1.Univ Zagreb, Fac Agr, Zagreb, Croatia;
2.Univ La Frontera, Ctr Plant Soil Interact & Nat Resources Biotechno, Sci & Technol Bioresource Nucleus, Temuco, Chile;
3.Univ Novi Sad, Fac Agr, Novi Sad, Serbia;
4.Univ Western Australia, UWA Sch Agr & Environm, Perth, WA, Australia
推荐引用方式
GB/T 7714
Ondrasek, Gabrijel,Begic, Helena Bakic,Zovko, Monika,et al. Biogeochemistry of soil organic matter in agroecosystems & environmental implications[J],2019,658:1559-1573.
APA Ondrasek, Gabrijel.,Begic, Helena Bakic.,Zovko, Monika.,Filipovic, Lana.,Merino-Gergichevich, Cristian.,...&Rengel, Zed.(2019).Biogeochemistry of soil organic matter in agroecosystems & environmental implications.SCIENCE OF THE TOTAL ENVIRONMENT,658,1559-1573.
MLA Ondrasek, Gabrijel,et al."Biogeochemistry of soil organic matter in agroecosystems & environmental implications".SCIENCE OF THE TOTAL ENVIRONMENT 658(2019):1559-1573.
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