Soil carbon storage along a 46-year revegetation chronosequence in a desert area of northern China
文献类型：期刊论文
| 作者 | Chen, Yong-Le1,2; Zhang, Zhi-Shan1; Zhao, Yang1; Hu, Yi-Gang1; Zhang, Ding-Hai3 |
| 刊名 | GEODERMA
 |
| 出版日期 | 2018-09-01 |
| 卷号 | 325页码:28-36 |
| 关键词 | Soil inorganic carbon Root-derived carbon Deep soil carbon Recovery time Tengger Desert |
| ISSN号 | 0016-7061 |
| DOI | 10.1016/j.geoderma.2018.03.024 |
| 通讯作者 | Zhang, Zhi-Shan(zszhang@lzb.ac.cn) |
| 英文摘要 | Soil contains the majority of terrestrial carbon; however, most studies only focus on soil organic carbon (SOC) in the first meter or even shallower layers, and soil inorganic carbon (SIC) and root-derived carbon (RDC) are often overlooked. Here, we investigated the distribution of soil carbon at a depth of 0-3.0 m over a 46-year revegetation chronosequence on moving sand dunes and evaluated the potential influence of soil water content on soil carbon. The SOC density increased significantly along the 0-3.0 m profile, and showed a faster increasing rate in shallow layer (0-0.4 m) than that of the deep layers below 0.4 m. Although the SIC density did not increase significantly, it accounted for > 65% of the total soil carbon in shallow layer and at least 82% in deep layer. The live and dead RDC increased significantly over the chronosequence in both shallow and deep layers. The RDC accounted for a small amount of the total soil carbon at an average of 3.19%. The SOC was closely linked with live RDC in both the shallow and deep layers. The soil water content was only positively correlated with the SOC in the shallow layer. The SOC storage in the shallow layer required 57.4 years to reach the level at the natural vegetation site, whereas the storage in the deep layers required > 100 years. Our results indicated that soil carbon accumulation is a slow process in both shallow and deep layers after revegetation, and the most notable increase in soil carbon was accounted by SOC. We suggest that SOC, SIC and RDC should be considered when assessing the effects of revegetation on soil carbon in water-limited ecosystems. |
| 收录类别 | SCI |
| WOS关键词 | TENGGER DESERT ; INORGANIC CARBON ; ORGANIC-CARBON ; NORTHWESTERN CHINA ; CLIMATE-CHANGE ; AFFORESTATION ; VEGETATION ; ROOTS ; ECOSYSTEM ; MOISTURE |
| WOS研究方向 | Agriculture |
| WOS类目 | Soil Science |
| 语种 | 英语 |
| WOS记录号 | WOS:000432499000004 |
| 出版者 | ELSEVIER SCIENCE BV |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2557817 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Zhang, Zhi-Shan |
| 作者单位 | 1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Shapotou Desert Res & Expt Stn, Lanzhou 730000, Gansu, Peoples R China 2.Shenzhen Univ, Coll Life Sci & Oceanog, Shenzhen 518060, Peoples R China 3.Gansu Agr Univ, Coll Nat Sci, Lanzhou 730070, Gansu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chen, Yong-Le,Zhang, Zhi-Shan,Zhao, Yang,et al. Soil carbon storage along a 46-year revegetation chronosequence in a desert area of northern China[J]. GEODERMA,2018,325:28-36. |
| APA | Chen, Yong-Le,Zhang, Zhi-Shan,Zhao, Yang,Hu, Yi-Gang,&Zhang, Ding-Hai.(2018).Soil carbon storage along a 46-year revegetation chronosequence in a desert area of northern China.GEODERMA,325,28-36. |
| MLA | Chen, Yong-Le,et al."Soil carbon storage along a 46-year revegetation chronosequence in a desert area of northern China".GEODERMA 325(2018):28-36. |
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来源：寒区旱区环境与工程研究所
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