Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.catena.2022.106735 |
Coupling of soil carbon and nitrogen dynamics in drylands under climate change | |
Han, Yaowen; Jia, Yufu; Wang, Guoan; Tan, Qiqi; Liu, Xuejun; Chen, Chongjuan | |
通讯作者 | Wang, GA |
来源期刊 | CATENA
![]() |
ISSN | 0341-8162 |
EISSN | 1872-6887 |
出版年 | 2023 |
卷号 | 221 |
英文摘要 | Climate change is predicted to be more dramatic in arid regions. Soil carbon (C) and nitrogen (N) dynamics maintain various functions in terrestrial ecosystems. It has been suggested that soil C and N dynamics are bio-logically coupled due to the strict proportions of C and N in organisms. However, whether dramatic climate change in drylands would break this coupling remained largely unknown. Given that climate change could occur over short distances in mountainous terrain, this study conducted a soil sampling across an altitude transect in Tianshan Mountains, China, which are the largest mountain system in drylands across the world. To avoid the disturbance of the influence of slope aspect, we therefore collected soil samples on the sunny and shady slopes of Tianshan Mountains. Our results showed that soil C and N concentrations and C:N ratio all increased with increasing altitude on the sunny slope and their changes were affected by temperature, soil sand content and precipitation. For the shady slope, soil C and N concentrations and C:N ratio all first increased then decreased along the altitude gradient. Soil pH, precipitation, temperature and soil sand content influenced soil C and N dynamics at altitude below 2650 m; soil pH and soil sand content affected soil C and N dynamics at altitude above 2650 m. These results indicated that soil C and N dynamics on the sunny and shady slopes both kept coupled under the condition of changing altitude. Furthermore, although the altitudinal patterns of soil C and N dynamics on the sunny and shady slopes were different, the correlations between soil C and N concentrations on these two slopes both were significant with a correlation coefficient of about 0.9. Hence, this study suggested that the coupling of soil C and N dynamics in drylands would still exist under climate change. |
英文关键词 | Global change Altitude Temperature Precipitation Soil stoichiometry |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000891889900001 |
WOS关键词 | ORGANIC-CARBON ; NUTRIENT CONCENTRATIONS ; TERRESTRIAL ECOSYSTEMS ; BIOGEOCHEMICAL CYCLES ; STOICHIOMETRY ; RESPONSES ; SEQUESTRATION ; DEPOSITION ; SLOPE ; WATER |
WOS类目 | Geosciences, Multidisciplinary ; Soil Science ; Water Resources |
WOS研究方向 | Geology ; Agriculture ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/395658 |
推荐引用方式 GB/T 7714 | Han, Yaowen,Jia, Yufu,Wang, Guoan,et al. Coupling of soil carbon and nitrogen dynamics in drylands under climate change[J],2023,221. |
APA | Han, Yaowen,Jia, Yufu,Wang, Guoan,Tan, Qiqi,Liu, Xuejun,&Chen, Chongjuan.(2023).Coupling of soil carbon and nitrogen dynamics in drylands under climate change.CATENA,221. |
MLA | Han, Yaowen,et al."Coupling of soil carbon and nitrogen dynamics in drylands under climate change".CATENA 221(2023). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。