Soil properties mediate the freeze-thaw-related soil N2O and CO2 emissions from temperate grasslands | |
Wu, Xing; Li, Ting; Wang, Dongbo; Wang, Fangfang; Fu, Bojie; Liu, Guohua; Lv, Yihe | |
刊名 | CATENA |
2020-12 | |
卷号 | 195页码:1-16 |
关键词 | Soil properties Freeze-thaw cycles Nitrous oxide Carbon dioxide Temperate grassland |
ISSN号 | 0341-8162 |
英文摘要 | Freeze-thaw cycles (FTCs) may affect soil carbon (C) and nitrogen (N) cycling and thus stimulate greenhouse gas emissions in cold regions. However, the dynamics of these gases in response to FTCs, especially for N2O, vary substantially due to the differences in soil properties. We conducted an incubation study to investigate the effects of soil properties from different land cover types (arid steppe, AS; typical steppe, TS; meadow steppe, MS; and marshland, ML) on the N2O and CO2 emissions during three FTCs from temperate grasslands in Northeast China. Our results showed that the freeze-thaw-related soil N2O and CO2 emissions differ significantly among different land cover types. Significant increases in N2O emissions during FTCs were observed from the MS, ML, and TS soils, but not from AS soils, which indicated that threshold values of some key soil properties might exist triggering N2O pulse emissions during thawing. Furthermore, AS soil cores were amended with deionized water, glucose-C and NO3--N, respectively, to identify the crucial factors for N2O emissions during FTCs. The significantly increased N2O emissions from AS soils after amendments with water and/or nutrients confirmed that soil organic carbon (SOC), NO3- and water content might be the limiting factors influencing the N2O Semissions from AS soils during FTCs. In addition to soil substrates and moisture, our results suggest that the soil texture and bulk density significantly impact N2O and CO2 emissions during FTCs. Stepwise multiple regression analysis showed that TN coupled with the soil WFPS and sand content could explain 95% of the spatial variability in N2O fluxes, and 75% of the variations in CO2 fluxes were related to the SOC and clay contents. Thus, our results indicate that the interactions between soil properties and FTCs in various ecosystems are important for predicting regional and global greenhouse gas balances, especially in cold regions. |
内容类型 | 期刊论文 |
源URL | [http://ir.rcees.ac.cn/handle/311016/44455] |
专题 | 生态环境研究中心_城市与区域生态国家重点实验室 |
推荐引用方式 GB/T 7714 | Wu, Xing,Li, Ting,Wang, Dongbo,et al. Soil properties mediate the freeze-thaw-related soil N2O and CO2 emissions from temperate grasslands[J]. CATENA,2020,195:1-16. |
APA | Wu, Xing.,Li, Ting.,Wang, Dongbo.,Wang, Fangfang.,Fu, Bojie.,...&Lv, Yihe.(2020).Soil properties mediate the freeze-thaw-related soil N2O and CO2 emissions from temperate grasslands.CATENA,195,1-16. |
MLA | Wu, Xing,et al."Soil properties mediate the freeze-thaw-related soil N2O and CO2 emissions from temperate grasslands".CATENA 195(2020):1-16. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
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。
修改评论