Greenhouse gas released from the deep permafrost in the northern Qinghai-Tibetan Plateau
文献类型：期刊论文
| 作者 | Mu, Cuicui1,2,3; Li, Lili1; Wu, Xiaodong2; Zhang, Feng1; Jia, Lin1; Zhao, Qian1; Zhang, Tingjun1 |
| 刊名 | SCIENTIFIC REPORTS
 |
| 出版日期 | 2018-03-09 |
| 卷号 | 8页码:9 |
| ISSN号 | 2045-2322 |
| DOI | 10.1038/s41598-018-22530-3 |
| 通讯作者 | Wu, Xiaodong(wxd565@163.com) |
| 英文摘要 | Deep carbon pool in permafrost regions is an important component of the global terrestrial carbon cycle. However, the greenhouse gas production from deep permafrost soils is not well understood. Here, using soils collected from 5-m deep permafrost cores from meadow and wet meadow on the northern Qinghai-Tibetan Plateau (QTP), we investigated the effects of temperature on CO2 and N2O production under aerobic incubations and CH4 production under anaerobic incubations. After a 35-day incubation, the CO2, N2O and CH4 production at -2 degrees C to 10 degrees C were 0.44 similar to 2.12 mg C-CO2/g soil C, 0.0027 similar to 0.097 mg N-N2O/g soil N, and 0.14 similar to 5.88 mu g C-CH4/g soil C, respectively. Greenhouse gas production in deep permafrost is related to the C: N ratio and stable isotopes of soil organic carbon (SOC), whereas depth plays a less important role. The temperature sensitivity (Q(10)) values of the CO2, N2O and CH4 production were 1.67-4.15, 3.26-5.60 and 5.22-10.85, without significant differences among different depths. These results indicated that climate warming likely has similar effects on gas production in deep permafrost and surface soils. Our results suggest that greenhouse gas emissions from both the deep permafrost and surface soils to the air will increase under future climate change. |
| 收录类别 | SCI |
| WOS关键词 | SOIL ORGANIC-MATTER ; ACTIVE-LAYER ; TEMPERATURE SENSITIVITY ; METHANE PRODUCTION ; CARBON RELEASE ; NITROGEN ; REGIONS ; CHINA ; MOUNTAIN ; CO2 |
| WOS研究方向 | Science & Technology - Other Topics |
| WOS类目 | Multidisciplinary Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000427015200002 |
| 出版者 | NATURE PUBLISHING GROUP |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2558114 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Wu, Xiaodong |
| 作者单位 | 1.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China 2.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resource, State Key Lab Cryospher Sci, Cryosphere Res Stn Qinghai Tibetan Plateau, Lanzhou 730000, Gansu, Peoples R China 3.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resource, State Key Lab Frozen Soil Engn, Lanzhou 730000, Gansu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Mu, Cuicui,Li, Lili,Wu, Xiaodong,et al. Greenhouse gas released from the deep permafrost in the northern Qinghai-Tibetan Plateau[J]. SCIENTIFIC REPORTS,2018,8:9. |
| APA | Mu, Cuicui.,Li, Lili.,Wu, Xiaodong.,Zhang, Feng.,Jia, Lin.,...&Zhang, Tingjun.(2018).Greenhouse gas released from the deep permafrost in the northern Qinghai-Tibetan Plateau.SCIENTIFIC REPORTS,8,9. |
| MLA | Mu, Cuicui,et al."Greenhouse gas released from the deep permafrost in the northern Qinghai-Tibetan Plateau".SCIENTIFIC REPORTS 8(2018):9. |
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来源：寒区旱区环境与工程研究所
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