Nitrogen-fixing tree species modulate species richness effects on soil aggregate-associated organic carbon fractions

被引:4
|
作者
Ye, Yuqian [1 ]
Wang, Hui [1 ]
Luan, Junwei [2 ]
Ma, Jinhao [1 ,2 ]
Ming, Angang [3 ,4 ]
Niu, Baoliang [1 ]
Liu, Cuiju [1 ]
Freedman, Zac [5 ]
Wang, Jingxin [6 ]
Liu, Shirong [1 ]
机构
[1] Chinese Acad Forestry, Natl Forestry & Grassland Adm, Ecol & Nat Conservat Inst, Key Lab Forest Ecol & Environm, Beijing 100091, Peoples R China
[2] Int Ctr Bamboo & Rattan, Beijing Bamboo & Rattan Sci & Technol, Inst Resources & Environm, Key Lab Natl Forestry & Grassland Adm, Beijing 100102, Peoples R China
[3] Chinese Acad Forestry, Expt Ctr Trop Forestry, Pingxiang 532600, Peoples R China
[4] Guangxi Youyiguan Forest Ecosyst Res Stn, Pingxiang 532600, Peoples R China
[5] Univ Wisconsin Madison, Dept Soil Sci, Madison, WI 53706 USA
[6] West Virginia Univ, Div Forestry & Nat Resources, Morgantown, WV 26506 USA
基金
中国国家自然科学基金;
关键词
Tree species richness; N-fixing tree species; Aggregate-associated organic carbon; Soil carbon fraction; COMMUNITY COMPOSITION; FUNCTIONAL DIVERSITY; MATTER; STABILIZATION; SEQUESTRATION; PARTICULATE; PHOSPHORUS; STORAGE; STOCKS; POOLS;
D O I
10.1016/j.foreco.2023.121315
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Soil aggregation is an important mechanism shaping soil organic carbon (SOC) fractions, but the effects of tree species richness on soil aggregate-associated organic carbon fractions are poorly understood. In this study, a manipulative experiment was conducted to examine whether and how tree species richness (1, 2, 4 and 6) together with or without the presence of nitrogen (N)-fixing tree species affect soil aggregate-associated organic carbon. Soil aggregates were classified into four fractions: large macroaggregates (>2 mm), small macroaggregates (0.25-2 mm), microaggregates (0.053-0.25 mm), and silt and clay (<0.053 mm). And then large and small macroaggregates were further separated into coarse (c-iPOC), fine intra-aggregate particulate organic carbon (fiPOC) and mineral associated organic carbon (MAOC), and microaggregates were divided into f-iPOC and MAOC. We observed that the effects of tree species richness on soil aggregate-associated organic carbon fractions were depended on the presence or absence of N-fixing tree species. In the presence of N-fixing tree species, organic carbon contents of small macroaggregate, microaggregate and silt and clay fractions were increased across the gradient of tree species richness (+10.4%, +31.3% and + 26.7% from monocultures to 6-species mixture), and the similar responses occurred for c-iPOC within small macroaggregates (+42.9%) and f-iPOC within microaggregates (+50.0%). In the absence of N-fixing tree species, however, only f-iPOC within large macroaggregates (+60.0%) had a positive linear relationship with tree species richness. Structural equation modeling was then used to dissect the mechanism underlying the positive effects of tree species richness on the aggregate-associated organic carbon fractions, indicating either direct or indirect effects by increasing root length density. Our study highlights the important roles of N-fixing tree species in shaping tree species richness effects on soil aggregateassociated organic carbon fractions, and therefore, N-fixing tree species should be preferentially considered in mixed-species plantations to enhance long-term SOC stabilization.
引用
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页数:9
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