Influence of extreme rainfall events on soil carbon release in the Loess Hilly Region, China

被引:4
|
作者
Sun, Yarong [1 ]
Liu, Chao [1 ]
Zhao, Min [1 ]
Liu, Le [2 ,3 ]
Liang, Siqi [2 ,3 ]
Wang, Yajuan [1 ]
Chen, Yunming [1 ,2 ,3 ,4 ]
机构
[1] Northwest A&F Univ, Inst Soil & Water Conservat, State key Lab Soil Eros & Dryland Farming Loess Pl, Yangling 712100, Peoples R China
[2] Chinese Acad Sci, Inst Soil & Water Conservat, Yangling 712100, Peoples R China
[3] Minist Water Resources, Yangling 712100, Peoples R China
[4] Inst Soil & Water Conservat, 26 Xinong Rd, Yangling 712100, Shaanxi, Peoples R China
关键词
Soil carbon release; Extreme rainfall; Soil temperature; Soil moisture; Soil depths; PRECIPITATION EVENTS; SEASONAL-VARIATIONS; CLIMATE EXTREMES; CO2; EFFLUX; RESPIRATION; PATTERNS; DESERT; MECHANISMS; RESPONSES; DIOXIDE;
D O I
10.1016/j.catena.2022.106652
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Projected increases in the frequency and magnitude of extreme rainfall events can profoundly impact terrestrial ecosystems. However, the response of soil carbon release (RS) at various depths to these events and associated regulatory processes has not been well-documented in small watersheds. We measured the mean CO2 concentration, soil moisture (SM), and soil temperature (ST) at depths of 10, 50, and 100 cm in situ before and after extreme rainfall events between June and September 2019, in a typical small watershed of the Loess Hilly Region, China. RS, calculated using Fick's first law in one dimension, revealed the relationships between RS and extreme rainfall events. During the study period, we screened four extreme rainfall events, of which three were used. The mean RS at 10, 50, and 100 cm soil depths after extreme rainfall (post-RS) were significantly higher than those before (pro-RS) (P < 0.05). Simultaneously, decreased ST at a depth of 10 cm and increased SM at a depth of 10 cm during periods of extreme rainfall contributed to decreased RS at a depth of 10 cm. By contrast, the RS at depths of 50 and 100 cm were enhanced during periods of extreme rainfall and peaked between days two and four after the extreme rainfall events due to the significant stimulating increase in SM (P < 0.05); the relative change in RS at 50 cm soil depth was the largest. Moreover, the RS values at three soil depths were changed by extreme rainfall events (with higher SM to RS), yet the R2 of the ST was lower after extreme rainfall. In addition, after extreme rainfall, the temperature sensitivity (Q10) increased at a depth of 10 cm, while it decreased at depths of 50 and 100 cm. These findings imply that more CO2 is released from deep soil in semi-arid shrubs under extreme rainfall events with sustained increase for 2-4 days. The results will help predict the impact of future climate change on regional carbon emissions and improve the accuracy of predictive model.
引用
收藏
页数:9
相关论文
共 50 条
  • [1] Rainstorm events increase risk of soil salinization in a loess hilly region of China
    Ke, Zengming
    Liu, Xiaoli
    Ma, Lihui
    Feng, Zhe
    Tu, Wen
    Dong, Qin'ge
    Jiao, Feng
    Wang, Zhanli
    AGRICULTURAL WATER MANAGEMENT, 2021, 256
  • [2] Rainfall erosion influenced by slope length in the hilly Loess region, China
    Cai, QG
    PROCEEDINGS OF THE 8TH INTERNATIONAL CONFERENCE OF RAINWATER CATCHMENT SYSTEMS, VOLS 1 AND 2: RAINWATER CATCHMENT FOR SURVIVAL, 1997, : 848 - 853
  • [3] Effects of rainfall intensity on sediment concentration in loess hilly region of China
    Liu X.
    Liu C.
    Dang S.
    Dili Xuebao/Acta Geographica Sinica, 2019, 74 (09): : 1723 - 1732
  • [4] Effect of Terraces and Rainfall on Water and Soil Loss in Pinus tabulaeformis Plantations in the Semiarid Loess Hilly Region of China
    Huang, Yue
    Wei, Wei
    Chen, Shengnan
    ECOHYDROLOGY, 2024, 17 (08)
  • [5] Soil quality indices and their application in the hilly loess plateau region of China
    Xu, MX
    Zhao, YG
    Liu, GB
    Argent, RM
    AUSTRALIAN JOURNAL OF SOIL RESEARCH, 2006, 44 (03): : 245 - 254
  • [6] Multiobjective Network Optimization for Soil Monitoring of the Loess Hilly Region in China
    Liu, Dianfeng
    Liu, Yaolin
    Wang, Mingze
    Zhao, Xiang
    DISCRETE DYNAMICS IN NATURE AND SOCIETY, 2014, 2014
  • [8] Influence of Vegetation Restoration on Topsoil Organic Carbon in a Small Catchment of the Loess Hilly Region, China
    Qin, Yunbin
    Xin, Zhongbao
    Yu, Xinxiao
    Xiao, Yuling
    PLOS ONE, 2014, 9 (06):
  • [9] Assessment indicators of soil quality in Loess gullied hilly region of China
    Zhang, Jianing
    Xu, Min
    Wu, Faqi
    Nature Environment and Pollution Technology, 2015, 14 (02) : 313 - 318
  • [10] Soil organic carbon sequestration and its stability after vegetation restoration in the Loess Hilly Region, China
    Xu, Hongwei
    Qu, Qing
    Wang, Minggang
    Li, Peng
    Li, Yuanze
    Xue, Sha
    Liu, Guobin
    LAND DEGRADATION & DEVELOPMENT, 2020, 31 (05) : 568 - 580