Integrating plant litter quality, soil organic matter stabilization, and the carbon saturation concept

被引:677
作者
Castellano, Michael J. [1 ]
Mueller, Kevin E. [2 ]
Olk, Daniel C. [3 ]
Sawyer, John E. [1 ]
Six, Johan [4 ]
机构
[1] Iowa State Univ, Dept Agron, Ames, IA 50011 USA
[2] ARS, USDA, Rangeland Resources Res Unit, Ft Collins, CO 80526 USA
[3] ARS, USDA, Natl Lab Agr & Environm, Ames, IA 50011 USA
[4] ETH, Swiss Fed Inst Technol, Dept Environm Syst Sci, CH-8092 Zurich, Switzerland
基金
美国农业部;
关键词
decomposition; litter; mineralization; nitrogen; residue; MICROBIAL CARBON; RESIDUE QUALITY; TILLAGE SYSTEMS; TEMPERATE SOILS; NITROGEN; DYNAMICS; DECOMPOSITION; C-13; MECHANISMS; FRACTIONS;
D O I
10.1111/gcb.12982
中图分类号
X176 [生物多样性保护];
学科分类号
083001 [环境科学];
摘要
Labile, 'high-quality', plant litters are hypothesized to promote soil organic matter (SOM) stabilization in mineral soil fractions that are physicochemically protected from rapid mineralization. However, the effect of litter quality on SOM stabilization is inconsistent. High-quality litters, characterized by high N concentrations, low C/N ratios, and low phenol/lignin concentrations, are not consistently stabilized in SOM with greater efficiency than 'low-quality' litters characterized by low N concentrations, high C/N ratios, and high phenol/lignin concentrations. Here, we attempt to resolve these inconsistent results by developing a new conceptual model that links litter quality to the soil C saturation concept. Our model builds on the Microbial Efficiency-Matrix Stabilization framework (Cotrufo et al., 2013) by suggesting the effect of litter quality on SOM stabilization is modulated by the extent of soil C saturation such that high-quality litters are not always stabilized in SOM with greater efficiency than low-quality litters.
引用
收藏
页码:3200 / 3209
页数:10
相关论文
共 77 条
[1]
Combining theory and experiment to understand effects of inorganic nitrogen on litter decomposition [J].
Ågren, GI ;
Bosatta, E ;
Magill, AH .
OECOLOGIA, 2001, 128 (01) :94-98
[2]
[Anonymous], 2008, J GEOPHYS RES BIOGEO
[3]
Beyaert RP, 2011, CAN J SOIL SCI, V91, P985, DOI [10.4141/CJSS2010-055, 10.4141/cjss2010-055]
[4]
13C and 15N stabilization dynamics in soil organic matter fractions during needle and fine root decomposition [J].
Bird, Jeffrey A. ;
Kleber, Markus ;
Torn, Margaret S. .
ORGANIC GEOCHEMISTRY, 2008, 39 (04) :465-477
[5]
Empirical evidence that soil carbon formation from plant inputs is positively related to microbial growth [J].
Bradford, Mark A. ;
Keiser, Ashley D. ;
Davies, Christian A. ;
Mersmann, Calley A. ;
Strickland, Michael S. .
BIOGEOCHEMISTRY, 2013, 113 (1-3) :271-281
[6]
A long-term nitrogen fertilizer gradient has little effect on soil organic matter in a high-intensity maize production system [J].
Brown, Kimberly H. ;
Bach, Elizabeth M. ;
Drijber, Rhae A. ;
Hofmockel, Kirsten S. ;
Jeske, Elizabeth S. ;
Sawyer, John E. ;
Castellano, Michael J. .
GLOBAL CHANGE BIOLOGY, 2014, 20 (04) :1339-1350
[7]
INFLUENCE OF FERTILIZER AND STRAW BALING ON SOIL ORGANIC-MATTER IN A THIN BLACK CHERNOZEM IN WESTERN CANADA [J].
CAMPBELL, CA ;
LAFOND, GP ;
ZENTNER, RP ;
BIEDERBECK, VO .
SOIL BIOLOGY & BIOCHEMISTRY, 1991, 23 (05) :443-446
[8]
Biochemical changes across a carbon saturation gradient: Lignin, cutin, and suberin decomposition and stabilization in fractionated carbon pools [J].
Carrington, Elizabeth M. ;
Hernes, Peter J. ;
Dyda, Rachael Y. ;
Plante, Alain F. ;
Six, Johan .
SOIL BIOLOGY & BIOCHEMISTRY, 2012, 47 :179-190
[9]
Linking Carbon Saturation Concepts to Nitrogen Saturation and Retention [J].
Castellano, Michael J. ;
Kaye, Jason P. ;
Lin, Henry ;
Schmidt, John P. .
ECOSYSTEMS, 2012, 15 (02) :175-187
[10]
Comparison of organic versus mineral resource effects on short-term aggregate carbon and nitrogen dynamics in a sandy soil versus a fine textured soil [J].
Chivenge, P. ;
Vanlauwe, B. ;
Gentile, R. ;
Six, J. .
AGRICULTURE ECOSYSTEMS & ENVIRONMENT, 2011, 140 (3-4) :361-371