Dynamics of grassland carbon sequestration and its coupling relation with hydrothermal factor of Inner Mongolia
文献类型：期刊论文
| 作者 | Zhou, Wei2,4; Yang, Han2; Zhou, Liang3,4; Chen, Yizhao1; Huang, Lu2; Ju, Weimin5 |
| 刊名 | ECOLOGICAL INDICATORS
 |
| 出版日期 | 2018-12-01 |
| 卷号 | 95页码:1-11 |
| 关键词 | Net ecosystem productivity Carbon sink Coupling relation Precipitation differential Targeted management |
| ISSN号 | 1470-160X |
| DOI | 10.1016/j.ecolind.2018.07.008 |
| 通讯作者 | Zhou, Liang(zhouw866@163.com) |
| 英文摘要 | Grassland carbon (C) sink/source evaluation is important to terrestrial ecosystem C cycling research. In this paper, boreal ecosystem productivity simulator (BEPS) model was used to simulate the net ecosystem productivity (NEP) of Inner Mongolia (IM) from 1982 to 2008. The coupling relation between NEP and climate factors was then explored. Results showed that the mean annual value of grassland NEP is 12.2 gC/m(2)/yr, and regions with NEP of > 0 (C sink) accounts for 73.2% of the total grassland area of IM. Additionally, the total C sequestration reaches 0.35 Pg C yearly. NEP was positively correlated with precipitation (R = 0.31), and the positive correlation percentage accounted for 90% of total grassland area. But NEP was negative correlated with temperature (R = -0.11), and the negative correlation percentage was 72% of case. And the partial correlation coefficient between NEP and precipitation and between NEP and temperature was 0.30 and -0.06 respectively. Meanwhile, the monthly NEP of the grassland is obviously lagging behind the precipitation and temperature, and the lag time is both three months. We defined a precipitation differential (PD) parameter to explore the coupling relation between grassland NEP and precipitation. Generally, areas with positive PD are typically a C sinks (72% of the grassland area of IM). However, regions with negative PD are likely a C source (28% of case). The obtained mean PD value of IM is 18 mm, indicating that IM is a C sink. Further analysis showed that 69% of regions have positive PD and positive NEP, and 20% of regions have negative PD and negative NEP. This result confirmed that precipitation deficit restrains C sequestration. However, the rest of 11% of regions was sensitive area of carbon sink and carbon source transition. Among 8% of the regions (with negative PD but positive NEP) have insufficient precipitation, although other conditions (i.e., ecological restoration program) are favorable to C sink. Moreover, 3% of the regions (with positive PD but negative NEP) have sufficient precipitation, but have negative NEP because of inappropriate management or low temperature. Thus, appropriate measures that can convert a C source to a C sink are necessary. This paper can serve as a reference for policy makers for the efficient targeted implementation of ecological engineering. |
| WOS关键词 | NET PRIMARY PRODUCTIVITY ; PROCESS MODEL ; SOIL CARBON ; TERRESTRIAL ECOSYSTEMS ; INTERANNUAL VARIATION ; TEMPERATE GRASSLANDS ; DIOXIDE EXCHANGE ; NORTHERN CHINA ; LAND-SURFACE ; FLUXES |
| 资助项目 | National Nature Science Fund, China[41501575] ; National Nature Science Fund, China[41701227] ; National Nature Science Fund, China[51508056] ; basic science and advanced technology Fund of Chongqing Scientific Council, China[cstc2016jcyjA1540] ; Scientific and Technological Research Program of Chongqing Municipal Education Commission, China[KJ1705114] |
| WOS研究方向 | Biodiversity & Conservation ; Environmental Sciences & Ecology |
| 语种 | 英语 |
| WOS记录号 | WOS:000456907400001 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | National Nature Science Fund, China ; basic science and advanced technology Fund of Chongqing Scientific Council, China ; Scientific and Technological Research Program of Chongqing Municipal Education Commission, China |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/49871]  |
| 专题 | 中国科学院地理科学与资源研究所 |
| 通讯作者 | Zhou, Liang |
| 作者单位 | 1.Nanjing Forestry Univ, Coll Biol & Environm, Nanjing 210037, Jiangsu, Peoples R China 2.Chongqing Jiaotong Univ, Dept Geog & Land & Resources, Coll Architecture & Urban Planning, Chongqing 400074, Peoples R China 3.Lanzhou Jiaotong Univ, Coll Surveying & Geog, AnNing East Rd, Lanzhou 730070, Gansu, Peoples R China 4.Chinese Acad Sci, State Key Lab Resources & Environm Informat Syst, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China 5.Nanjing Univ, Int Inst Earth Syst Sci, Nanjing 210093, Jiangsu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhou, Wei,Yang, Han,Zhou, Liang,et al. Dynamics of grassland carbon sequestration and its coupling relation with hydrothermal factor of Inner Mongolia[J]. ECOLOGICAL INDICATORS,2018,95:1-11. |
| APA | Zhou, Wei,Yang, Han,Zhou, Liang,Chen, Yizhao,Huang, Lu,&Ju, Weimin.(2018).Dynamics of grassland carbon sequestration and its coupling relation with hydrothermal factor of Inner Mongolia.ECOLOGICAL INDICATORS,95,1-11. |
| MLA | Zhou, Wei,et al."Dynamics of grassland carbon sequestration and its coupling relation with hydrothermal factor of Inner Mongolia".ECOLOGICAL INDICATORS 95(2018):1-11. |
入库方式： OAI收割
来源：地理科学与资源研究所
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