中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Environmental implications of agricultural abandonment on Fe cycling: Insight from iron forms and stable isotope composition in karst soil, southwest China

文献类型:期刊论文

作者Zhang, Qian2; Han, Guilin1; Liu, Man1; Zhang, Shitong1; Wang, Lingqing2; Zhu, Guangyou3
刊名ENVIRONMENTAL RESEARCH
出版日期2022-12-01
卷号215页码:9
关键词Fe forms Fe isotopes Agricultural abandonment Karst soils Land-use change
ISSN号0013-9351
DOI10.1016/j.envres.2022.114377
通讯作者Han, Guilin(hanguilin@cugb.edu.cn)
英文摘要Land-use change influences the fate of nutrient elements, including iron (Fe), and then threaten soil security. In this study, Fe forms and stable isotope composition (delta Fe-56) in soils were investigated to identify the variations in the processes of Fe cycling during agricultural abandonment in a karst region of Southwest China. Soil delta Fe-56 compositions varied from -0.05 parts per thousand-0.02 parts per thousand in croplands, 0.05 parts per thousand-0.12 parts per thousand in abandoned croplands, to 0.30 parts per thousand-0.80 parts per thousand in the native vegetation lands. In the croplands, Fe oxidation-precipitation process is considered as the main contributor to Fe migration and isotope fractionation, leading to a relatively enrichment of heavier Fe isotope in deeper soil layer. In the abandoned croplands and native vegetation lands, Fe isotope in the organicrich layer (0-10 cm) was significantly lighter than that in subsurface layer (20-30 cm), mainly due to the recovery of soil organic carbon (SOC) and macro-aggregate after cropland abandonment. Moreover, the eluviation process mainly caused a decrease in soil Fe contents and enrichment of heavy Fe isotope in deeper soils (below 40 cm). The positive correlation between oxidized Fe and SOC contents suggested the accumulation of mobile Fe in soils after agricultural abandonment, which is beneficial for Fe uptake and assimilation by plants. This study suggests that agricultural abandonment significantly reduce soil Fe leaching loss and improve plant Fe supply by SOC accumulation in surface soil, which gives an environmental implication for the management of soil nutrients.
WOS关键词ORGANIC-MATTER ; PADDY SOILS ; FRACTIONATION ; PEDOGENESIS ; DISSOLUTION ; REDUCTION ; EVOLUTION ; OXIDATION ; SEDIMENTS ; TERRAIN
资助项目National Natural Science Foundation of China[42203011] ; National Natural Science Foundation of China[41661144029] ; National Natural Science Foundation of China[41325010]
WOS研究方向Environmental Sciences & Ecology ; Public, Environmental & Occupational Health
语种英语
WOS记录号WOS:000892427600006
出版者ACADEMIC PRESS INC ELSEVIER SCIENCE
资助机构National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/187888]  
专题中国科学院地理科学与资源研究所
通讯作者Han, Guilin
作者单位1.China Univ Geosci Beijing, Inst Earth Sci, Beijing 100083, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
3.Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
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GB/T 7714
Zhang, Qian,Han, Guilin,Liu, Man,et al. Environmental implications of agricultural abandonment on Fe cycling: Insight from iron forms and stable isotope composition in karst soil, southwest China[J]. ENVIRONMENTAL RESEARCH,2022,215:9.
APA Zhang, Qian,Han, Guilin,Liu, Man,Zhang, Shitong,Wang, Lingqing,&Zhu, Guangyou.(2022).Environmental implications of agricultural abandonment on Fe cycling: Insight from iron forms and stable isotope composition in karst soil, southwest China.ENVIRONMENTAL RESEARCH,215,9.
MLA Zhang, Qian,et al."Environmental implications of agricultural abandonment on Fe cycling: Insight from iron forms and stable isotope composition in karst soil, southwest China".ENVIRONMENTAL RESEARCH 215(2022):9.

入库方式: OAI收割

来源:地理科学与资源研究所

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