Centre d'Applications et de Recherches en Télédétection, Département de géomatique appliquée, Université de Sherbrooke, 2500 boulevard de l'Université, Sherbrooke, Québec J1K 2R1, Canada; Quebec Centre for Biodiversity Science, 1205 Dr. Penfield Avenue, Montréal, Québec H3A 1B1, Canada.
Centre d'Applications et de Recherches en Télédétection, Département de géomatique appliquée, Université de Sherbrooke, 2500 boulevard de l'Université, Sherbrooke, Québec J1K 2R1, Canada; Quebec Centre for Biodiversity Science, 1205 Dr. Penfield Avenue, Montréal, Québec H3A 1B1, Canada.
Sci Total Environ. 2020 Jun 10;720:137477. doi: 10.1016/j.scitotenv.2020.137477. Epub 2020 Feb 24.
In order to control severe soil erosion, large-scale ecological restoration programs (ERPs) were undertaken, which greatly increased vegetation cover in the Chinese Loess Plateau. Although this has generated positive impacts on soil erosion reduction, the conflicts between water supply and the ERPs in the Loess Plateau remain debatable. The impacts of ERPs and climate change on soil erosion and water supply in the future received little attention. Therefore, the objective of this study is to analyze the potential impacts of ERPs on soil erosion and water yield by 2050 in northern Shaanxi, the Chinese Loess Plateau. Soil erosion and water yield were modelled for 2050 based on land use and land cover (LULC) retrospective datasets and downscaled climate scenarios. We designed three 2050 conservation scenarios (protection, business as usual (BAU), and No LULC change) and compared them to the 2015 baseline. The results indicate that soil erosion under the protection and BAU scenarios showed similar decreasing trends compared with the 2015 baseline. The water yield decreased for all three scenarios: by 28% (No LULC change scenario), 29% (BAU scenario), and 37% (protection scenario), indicating that climate change and ecological restoration are likely to place substantial pressures on water by 2050. Considering the water scarcity and climate scenarios in this region, stabilization of the vegetation cover at the 2015 levels may best support soil and water conservation in the future in northern Shaanxi. This study is expected to provide insights for decision-making to develop optimal soil and water conservation strategies in the semi-arid environment in China.
为了控制严重的土壤侵蚀,中国黄土高原实施了大规模的生态恢复计划(ERPs),大大增加了植被覆盖。尽管这对减少土壤侵蚀产生了积极影响,但黄土高原供水与 ERPs 之间的冲突仍存在争议。ERPs 和气候变化对未来土壤侵蚀和供水的影响受到的关注较少。因此,本研究的目的是分析陕北(中国黄土高原)未来 ERPs 对土壤侵蚀和产水量的潜在影响。基于土地利用和土地覆盖(LULC)回溯数据集和降尺度气候情景,对 2050 年的土壤侵蚀和产水量进行了建模。我们设计了三个 2050 年的保护情景(保护、照常营业(BAU)和 LULC 不变),并将其与 2015 年基准进行了比较。结果表明,保护和 BAU 情景下的土壤侵蚀与 2015 年基准相比呈现出相似的减少趋势。所有三个情景下的产水量都有所减少:LULC 不变情景减少 28%,BAU 情景减少 29%,保护情景减少 37%,这表明气候变化和生态恢复可能会在 2050 年对水产生巨大压力。考虑到该地区的水资源短缺和气候情景,将植被覆盖稳定在 2015 年的水平可能是未来陕北地区水土保持的最佳选择。本研究有望为制定中国半干旱地区最佳水土保持策略提供决策参考。