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DOI: 10.1371/journal.pone.0103720
论文题名:
Influence of Residue and Nitrogen Fertilizer Additions on Carbon Mineralization in Soils with Different Texture and Cropping Histories
作者: Xianni Chen; Xudong Wang; Matt Liebman; Michel Cavigelli; Michelle Wander
刊名: PLOS ONE
ISSN: 1932-6203
出版年: 2014
发表日期: 2014-7-31
卷: 9, 期:7
语种: 英语
英文关键词: Agricultural soil science ; Fertilizers ; Carbon dioxide ; Clay mineralogy ; Particulates ; Agricultural methods ; Carbon sequestration ; Agriculture
英文摘要: To improve our ability to predict SOC mineralization response to residue and N additions in soils with different inherent and dynamic organic matter properties, a 330-day incubation was conducted using samples from two long-term experiments (clay loam Mollisols in Iowa [IAsoil] and silt loam Ultisols in Maryland [MDsoil]) comparing conventional grain systems (Conv) amended with inorganic fertilizers with 3 yr (Med) and longer (Long), more diverse cropping systems amended with manure. A double exponential model was used to estimate the size (Ca, Cs) and decay rates (ka, ks) of active and slow C pools which we compared with total particulate organic matter (POM) and occluded-POM (OPOM). The high-SOC IAsoil containing highly active smectite clays maintained smaller labile pools and higher decay rates than the low-SOC MDsoil containing semi-active kaolinitic clays. Net SOC loss was greater (2.6 g kg−1; 8.6%) from the IAsoil than the MDsoil (0.9 g kg−1, 6.3%); fractions and coefficients suggest losses were principally from IAsoil’s resistant pool. Cropping history did not alter SOC pool size or decay rates in IAsoil where rotation-based differences in OPOM-C were small. In MDsoil, use of diversified rotations and manure increased ka by 32% and ks by 46% compared to Conv; differences mirrored in POM- and OPOM-C contents. Residue addition prompted greater increases in Ca (340% vs 230%) and Cs (38% vs 21%) and decreases in ka (58% vs 9%) in IAsoil than MDsoil. Reduced losses of SOC from residue-amended MDsoil were associated with increased OPOM-C. Nitrogen addition dampened CO2-C release. Clay type and C saturation dominated the IAsoil’s response to external inputs and made labile and stable fractions more vulnerable to decay. Trends in OPOM suggest aggregate protection influences C turnover in the low active MDsoil. Clay charge and OPOM-C contents were better predictors of soil C dynamics than clay or POM-C contents.
URL: http://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0103720&type=printable
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/19830
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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作者单位: College of Resources and Environment, Northwest A&F University, Yangling, Shaanxi, PR China;College of Resources and Environment, Northwest A&F University, Yangling, Shaanxi, PR China;Department of Agronomy, Agronomy Hall, Iowa State University, Ames, Iowa, United States of America;Sustainable Agricultural Systems Lab, Agricultural Research Center, Beltsville, Maryland, United States of America;Department of NRES, University of Illinois, Urbana-Champaign, Illinois, United States of America

Recommended Citation:
Xianni Chen,Xudong Wang,Matt Liebman,et al. Influence of Residue and Nitrogen Fertilizer Additions on Carbon Mineralization in Soils with Different Texture and Cropping Histories[J]. PLOS ONE,2014-01-01,9(7)
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