College of Resources and Environment, Huazhong Agricultural University, Wuhan, China.
The University of Arizona, Tucson, USA.
J Environ Manage. 2023 Jul 1;337:117717. doi: 10.1016/j.jenvman.2023.117717. Epub 2023 Mar 21.
Soil erosion is a common form of land degradation. The Coupled Model Intercomparison Project Phase 6 (CMIP6) provides a scenario framework for global socio-economic development and climate change by combining Shared Socioeconomic Pathways (SSP) and Representative Concentration Pathways (RCP). The soil erosion estimation under global climate change and land-use change scenarios provided by CMIP6 is valuable for representing future changes and hotspots. This study estimated the future changes in soil erosion in the Three Gorges Reservoir (TGR) area, China, which has suffered severe soil loss over an extended period, and vegetation restoration projects have been conducted since 1999. The scenarios provided by SSP1-2.6, SSP2-4.5, and SSP5-8.5 were coupled with the scenarios of regional vegetation restoration projects to reflect future land use changes (LUC) and climate change. The results showed that future soil erosion from 2020 to 2100 in the TGR area will experience a non-significant decreasing trend (with trend slopes of -0.013, -0.020, and-0.006 in SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively, with p > 0.05). However, with the R factors calculated by different methods, this decreasing trend becomes either insignificant or a significant increasing trend. SSP1-2.6 will experience the lowest soil erosion in 2100 owing to the large amount of forest increase in this scenario. Furthermore, as estimates, the grain-for-green policy (GGP) will reduce 89353.47, 92737.73 and 42916.52 ton soil erosion per year in SSP1-2.6, SSP2-4.5 and SSP3-8.5 by 2100, respectively. In the future, the GGP will become increasingly important for controlling soil loss in the TGR area owing to the increasing precipitation in all scenarios, which increases the risk of soil loss.
土壤侵蚀是一种常见的土地退化形式。耦合模式比较计划第六阶段(CMIP6)通过结合共享社会经济途径(SSP)和代表性浓度途径(RCP),为全球社会经济发展和气候变化提供了一个情景框架。CMIP6 提供的全球气候变化和土地利用变化情景下的土壤侵蚀估计对于代表未来的变化和热点是有价值的。本研究估计了中国三峡库区(TGR)未来的土壤侵蚀变化情况,该地区长期以来遭受了严重的土壤流失,自 1999 年以来已经开展了植被恢复项目。将 SSP1-2.6、SSP2-4.5 和 SSP5-8.5 等情景与区域植被恢复项目的情景相结合,以反映未来的土地利用变化(LUC)和气候变化。结果表明,TGR 地区从 2020 年到 2100 年的未来土壤侵蚀将经历一个不显著的减少趋势(在 SSP1-2.6、SSP2-4.5 和 SSP5-8.5 中分别为-0.013、-0.020 和-0.006 的趋势斜率,p>0.05)。然而,由于不同方法计算的 R 因素,这一下降趋势要么不显著,要么呈显著上升趋势。由于该情景下森林增加量较大,SSP1-2.6 将在 2100 年经历最低的土壤侵蚀。此外,作为估计,退耕还林还草政策(GGP)将使 SSP1-2.6、SSP2-4.5 和 SSP3-8.5 中每年的土壤侵蚀减少 89353.47、92737.73 和 42916.52 吨,到 2100 年为止。在未来,由于所有情景下降水增加,土壤流失的风险增加,GGP 将在控制 TGR 地区土壤流失方面变得越来越重要。