Impacts of vegetation restoration strategies on soil organic carbon and nitrogen dynamics in a karst area, southwest China

被引:75
作者
Xiao, Kongcao [1 ,3 ]
He, Tieguang [2 ]
Chen, Hao [1 ,3 ]
Peng, Wanxia [1 ,3 ]
Song, Tongqing [1 ,3 ]
Wang, Kelin [1 ,3 ]
Li, Dejun [1 ,3 ]
机构
[1] Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agro Ecol Proc Subtrop Reg, Changsha 410125, Hunan, Peoples R China
[2] Guangxi Acad Agr Sci, Agr Resources & Environm Res Inst, Nanning 530007, Guangxi, Peoples R China
[3] Chinese Acad Sci, Inst Subtrop Agr, Huanjiang Observat & Res Stn Karst Ecosyst, Huangjiang 547100, Guangxi, Peoples R China
基金
中国国家自然科学基金;
关键词
Accumulation; Cropland abandonment; Karst region; Soil organic matter; Spontaneous regeneration; Tree plantation; LAND-USE; SECONDARY FORESTS; CENTRAL AMAZONIA; CLIMATE-CHANGE; SEQUESTRATION; ACCUMULATION; MATTER; STOCKS; DECOMPOSITION; METAANALYSIS;
D O I
10.1016/j.ecoleng.2017.01.037
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Soil carbon (C) sequestration through cropland conversion has been regarded as a major strategy to absorb atmospheric CO2 and thus mitigate global warming, but much uncertainty still exists in terms of restoration strategies. In this study, soil C and nitrogen (N) were measured 13 years after cropland conversion in a karst area, southwest China. Four restoration strategies were included, i.e., (i) restoration with an economic tree species Toona sinensis (TS), (ii) restoration with Guimu-1 hybrid elephant grass (GG), (iii) restoration with a combination of Zenia insignis and Guimu-1 hybrid elephant grass (ZG), and iv) spontaneous regeneration (SR). Cropland under maize-soybean rotation (CR) was used as reference and the space-for-time substitution approach was adopted to evaluate soil C and N stock (0-15 cm) change. Soil C stocks in TS and SR were elevated by 40% and 50%, respectively, relative to CR, while those in GG and ZG were not significantly changed. Soil N stocks in GG were not significantly changed, but stocks in TS, ZG and SR were enhanced by 130%, 81% and 117%, respectively, relative to CR. Significant correlation was found between soil C and N stock changes with rate of relative N stock change greater than that of C stock change. Similar to soil N stock, nitrate concentration, net nitrification rate and 615N values in TS, ZG and SR were greater than those in GG or CR. Stepwise multiple linear regression indicated that exchangeable calcium was the soil variable mainly responsible for the dynamics of both soil C and N. Our results indicate that plantation with economic tree species and spontaneous regeneration are likely equally effective in soil C sequestration. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:247 / 254
页数:8
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