Soil organic carbon dynamics following natural vegetation restoration: Evidence from stable carbon isotopes (delta C-13)
文献类型：期刊论文
| 作者 | Shangguan, Zhouping2; Tang, Zhuangsheng2; Wang, Kaibo1; Deng, Lei1,2 |
| 刊名 | AGRICULTURE ECOSYSTEMS & ENVIRONMENT
 |
| 出版日期 | 2016-04-01 |
| 卷号 | 221期号:2016页码:235-244 |
| 关键词 | Carbon Sequestration Carbon Isotopes Farmland Abandonment New Carbon Old Carbon Organic Carbon Decomposition The Loess Plateau |
| DOI | 10.1016/j.agee.2016.01.048 |
| 文献子类 | Article |
| 英文摘要 | Knowledge of soil carbon (C) dynamics following vegetation restoration is essential for evaluating carbon budgets and cycles at regional and global scales. In this study, we investigated the dynamics of soil organic carbon (OC) following farmland abandonment along with similar to 160 years of vegetation restoration on the Loess Plateau, China. Our specific objectives were to examine the variation of soil OC decomposition rates, to quantify the changes in the proportion of new and old soil OC, and to explore the factors controlling soil OC stock patterns. The results showed that the rate of new soil OC increase was higher in the early stage (similar to 10 years) after land-use change. The rate of new soil OC increase ranged from 109.17 to 41.88 g m(-2) year(-1) in the early (similar to 10 years) and later stages (similar to 160 years), respectively. It took about 30 years for the amount of new soil OC to reach the same level as old OC in the top 20 cm of soil following farmland abandonment. Also, soil OC decomposition rate was higher (decomposition rate constants = 0.04) in the early stage (similar to 10 years) and showed a non-significant difference after >30 years of vegetation restoration. Our results suggested that soil C/N is the most factor to effect on soil OC sequestration following vegetation restoration, and the proportions of new soil OC was mainly determined by fine roots, soil OC decomposition rate constants were mainly determined by soil silt content, and the rates of new soil OC increase were mainly determined by soil sand content that these observations were made out of considering many other soil properties. (C) 2016 Elsevier B.V. All rights reserved. |
| WOS关键词 | LAND-USE CHANGE ; LOESS PLATEAU ; MICROBIAL BIOMASS ; MATTER DYNAMICS ; AGGREGATE FRACTIONS ; NORTHWEST CHINA ; CLIMATE-CHANGE ; NITROGEN ; FOREST ; SEQUESTRATION |
| WOS研究方向 | Agriculture ; Environmental Sciences & Ecology |
| 语种 | 英语 |
| WOS记录号 | WOS:000373649100025 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5752]  |
| 专题 | 地球环境研究所_生态环境研究室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Shaanxi, Peoples R China 2.Northwest A&F Univ, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China |
| 推荐引用方式 GB/T 7714 | Shangguan, Zhouping,Tang, Zhuangsheng,Wang, Kaibo,et al. Soil organic carbon dynamics following natural vegetation restoration: Evidence from stable carbon isotopes (delta C-13)[J]. AGRICULTURE ECOSYSTEMS & ENVIRONMENT,2016,221(2016):235-244. |
| APA | Shangguan, Zhouping,Tang, Zhuangsheng,Wang, Kaibo,&Deng, Lei.(2016).Soil organic carbon dynamics following natural vegetation restoration: Evidence from stable carbon isotopes (delta C-13).AGRICULTURE ECOSYSTEMS & ENVIRONMENT,221(2016),235-244. |
| MLA | Shangguan, Zhouping,et al."Soil organic carbon dynamics following natural vegetation restoration: Evidence from stable carbon isotopes (delta C-13)".AGRICULTURE ECOSYSTEMS & ENVIRONMENT 221.2016(2016):235-244. |
入库方式： OAI收割
来源：地球环境研究所
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