中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Stable isotope fractionation provides information on carbon dynamics in soil aggregates subjected to different long-term fertilization practices

文献类型:期刊论文

作者Liu, Yi2,3; Hu, Cheng1; Hu, Wei4; Wang, Li2; Li, Zhiguo2; Pan, Junfeng2; Chen, Fang2
刊名SOIL & TILLAGE RESEARCH
出版日期2018-04-01
卷号177页码:54-60
ISSN号0167-1987
关键词Soil aggregate Stable isotope natural abundance Long-term fertilization
DOI10.1016/j.still.2017.11.016
英文摘要Stable carbon (C) isotopes provide valuable information to study C incorporation in soil aggregates. Different soil aggregate fractions have different concentrations of soil organic C (SOC), and changes in the abundance of soil C isotopes are closely linked to aggregate turnover. Soils from rice-wheat rotation fields in a long-term (31 years) experiment established in subtropical Central China were analyzed to improve knowledge of the influence of long-term fertilization (e.g. inorganic fertilizers) on the organic C isotope composition of different aggregate fractions. Aggregate-associated C levels and delta C-13 values (C-13 to C-12 ratios, relative to a standard) ranged from 19.0 to 23.1 g kg(-1), and from -24.8 to -23.00%, respectively, across all treatments. However, SOC concentrations and delta C-13 values were higher under treatments including inorganic fertilization than under the control (fertilizer-free, CK) treatment. In addition, delta C-13 values of micro-aggregates (< 0.25 mm) were higher than those of macro-aggregates (> 0.25 nun), i.e. the micro-aggregates (< 0.25 mm) exhibited C-13 enrichment. Analyses of C flows between aggregates of different size classes (modelled in a scheme) indicate that C generally flows from macro-aggregates to micro-aggregates (or remains with them as they become successively smaller), and treatments with mineral fertilizers retarded these flows, relative to rates under the CK treatment. The results show that analyses of the natural abundance of stable C isotopes can provide valuable information on biogeochemical processes related to C transformation in soil aggregates.
资助项目National Science Foundation of China ; Open Funding Project of the State Key Laboratory of Soil Erosion and Dryland Fanning on the Loess Plateau
WOS研究方向Agriculture
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000424073900006
源URL[http://202.127.146.157/handle/2RYDP1HH/3775]  
专题中国科学院武汉植物园
通讯作者Li, Zhiguo; Chen, Fang
作者单位1.Hubei Acad Agr Sci, Inst Plant Protect & Soil Fertilizer, Wuhan 430064, Hubei, Peoples R China
2.Chinese Acad Sci, Key Lab Aquat Bot & Watershed Ecol, Wuhan Bot Garden, Wuhan 430074, Hubei, Peoples R China
3.Chinese Acad Sci & Minist Water Resource, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Peoples R China
4.New Zealand Inst Plant & Food Res Ltd, Private Bag 4704, Christchurch 8140, New Zealand
推荐引用方式
GB/T 7714
Liu, Yi,Hu, Cheng,Hu, Wei,et al. Stable isotope fractionation provides information on carbon dynamics in soil aggregates subjected to different long-term fertilization practices[J]. SOIL & TILLAGE RESEARCH,2018,177:54-60.
APA Liu, Yi.,Hu, Cheng.,Hu, Wei.,Wang, Li.,Li, Zhiguo.,...&Chen, Fang.(2018).Stable isotope fractionation provides information on carbon dynamics in soil aggregates subjected to different long-term fertilization practices.SOIL & TILLAGE RESEARCH,177,54-60.
MLA Liu, Yi,et al."Stable isotope fractionation provides information on carbon dynamics in soil aggregates subjected to different long-term fertilization practices".SOIL & TILLAGE RESEARCH 177(2018):54-60.

入库方式: OAI收割

来源:武汉植物园

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