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Projected soil organic carbon loss in response to climate warming and soil water content in a loess watershed
Carbon Balance and Management ( IF 3.8 ) Pub Date : 2021-08-16 , DOI: 10.1186/s13021-021-00187-2 Fubo Zhao 1 , Yiping Wu 1 , Jinyu Hui 1 , Bellie Sivakumar 2 , Xianyong Meng 3 , Shuguang Liu 4
Carbon Balance and Management ( IF 3.8 ) Pub Date : 2021-08-16 , DOI: 10.1186/s13021-021-00187-2 Fubo Zhao 1 , Yiping Wu 1 , Jinyu Hui 1 , Bellie Sivakumar 2 , Xianyong Meng 3 , Shuguang Liu 4
Affiliation
Soil organic carbon (SOC) plays a crucial role in the global carbon cycle and terrestrial ecosystem functions. It is widely known that climate change and soil water content (SWC) could influence the SOC dynamics; however, there are still debates about how climate change, especially climate warming, and SWC impact SOC. We investigated the spatiotemporal changes in SOC and its responses to climate warming and root-zone SWC change using the coupled hydro-biogeochemical model (SWAT-DayCent) and climate scenarios data derived under the three Representative Concentration Pathways (RCPs2.6, 4.5, and 8.5) from five downscaled Global Climate Models (GCMs) in a typical loess watershed––the Jinghe River Basin (JRB) on the Chinese Loess Plateau. The air temperature would increase significantly during the future period (2017–2099), while the annual precipitation would increase by 2.0–13.1% relative to the baseline period (1976–2016), indicating a warmer and wetter future in the JRB. Driven by the precipitation variation, the root-zone SWC would also increase (by up to 27.9% relative to the baseline under RCP4.5); however, the SOC was projected to decrease significantly under the future warming climate. The combined effects of climate warming and SWC change could more reasonably explain the SOC loss, and this formed hump-shaped response surfaces between SOC loss and warming-SWC interactions under both RCP2.6 and 8.5, which can help explain diverse warming effects on SOC with changing SWC. The study showed a significant potential carbon source under the future warmer and wetter climate in the JRB, and the SOC loss was largely controlled by future climate warming and the root-zone SWC as well. The hump-shaped responses of the SOC loss to climate warming and SWC change demonstrated that the SWC could mediate the warming effects on SOC loss, but this mediation largely depended on the SWC changing magnitude (drier or wetter soil conditions). This mediation mechanism about the effect of SWC on SOC would be valuable for enhancing soil carbon sequestration in a warming climate on the Loess Plateau.
更新日期：2021-08-16
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