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石羊河流域产水服务供需时空变化及驱动因子 被引量:3
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作者 夏鸿华 杨林山 +3 位作者 冯起 苏迎庆 邹星怡 贺王含 《中国沙漠》 CSCD 北大核心 2024年第6期87-99,共13页
开展流域产水服务供需匹配关系的研究对促进区域水资源科学利用及生态环境可持续发展具有重要意义。选取石羊河流域为研究区,基于1990、2000、2010、2020年遥感影像、站点监测及再分析产品数据,采用InVEST模型、用水需求估算、供需指数... 开展流域产水服务供需匹配关系的研究对促进区域水资源科学利用及生态环境可持续发展具有重要意义。选取石羊河流域为研究区,基于1990、2000、2010、2020年遥感影像、站点监测及再分析产品数据,采用InVEST模型、用水需求估算、供需指数及地理探测器等方法综合分析1990—2020年石羊河流域产水服务供需现状及演变特征。结果表明:(1)1990—2020年,石羊河流域产水服务供给量空间上呈现西南高东北低的分布特征,1990年产水量最低(16.55×10^(8) m^(3)),2010年最高(19.37×10^(8) m^(3))。产水服务贡献率最高的为林地及草地。(2)流域产水服务需求量整体呈现西南高东北低的空间分布特征,1990年产水服务需求量最高(20.39×10^(8) m^(3)),2020年最低(17.78×10^(8) m^(3)),耕地是流域用水服务需求量最高的土地利用类型。(3)流域西南部山地产水服务供需匹配程度较高,石羊河干支流流经区次之,而流域东北及东部地区产水服务供需匹配程度较低。研究区内供需指数两极分化明显,区域内水资源供需空间分配极度不均。时间上产水服务匹配状况有逐步好转的迹象,2020年流域产水服务的供需匹配程度有明显提高。(4)地理探测器结果表明,10种因子中影响流域产水量空间分异的最大因子是年降水量,同时,各驱动因子的交互作用解释力均大于单一因子,存在双因子增强及非线性增强两种组合形式。因此,未来亟须加强流域气候变化适应性管理政策的调整,统筹流域水资源综合管理。 展开更多
关键词 产水量 供需关系 时空格局 InVEST模型 石羊河流域
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Compounding effects of human activities and climatic changes on coexistence of oasis-desert ecosystems:Prioritizing resilient decision-making for a riskier world 被引量:1
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作者 XinWei Yin Wei Liu +11 位作者 Meng Zhu JuTao Zhang Qi Feng Haiyang Xi linshan yang Tuo Han WenJu Cheng YingQing Su BaiTing Zhang YuanYuan Xue ZeXia Chen LingGe Wang 《Research in Cold and Arid Regions》 CSCD 2023年第5期219-229,共11页
Water-salt balance is critical for the stable coexistence of salt-affected and groundwater-fed oasis-desert ecosystems. Yet, a comprehensive investigation of how soil salinization and groundwater degradation threaten ... Water-salt balance is critical for the stable coexistence of salt-affected and groundwater-fed oasis-desert ecosystems. Yet, a comprehensive investigation of how soil salinization and groundwater degradation threaten the coexistence of oasis-desert ecosystems is still scarce, especially under the compounding effects of human activities and climatic changes. Here, we assessed the impacts of irrigated agriculture on hydrological regimes in oasisdesert systems, investigated the spatio-temporal variations of soil salinization in irrigated cropland, and evaluated the implications of the interplays of soil salinization and groundwater degradation on the coexistence of oasis-desert ecosystems in northwestern China, based on meaningful modelling approaches and comprehensive measurements over 1995–2020. The results showed that the irrigation return flow coefficient decreased sharply from 0.21 ± 0.09 in the traditional irrigation period to 0.09 ± 0.01 in the water-saving irrigation period. The continuous drop in groundwater tables and significant degradation of groundwater quality are occurring throughout this watershed. The eco-environmental flows are reaching to their limit with watershed closures(i.e.,the drainage from the oasis region into the desert region is being weakened or even eliminated), although these progressions were largely hidden by regional precipitation and streamflow variability. The process of salt migration and accumulation across different landscapes in oasis-desert system is being reshaped, and soil salinization in water-saving agricultural irrigated lands is accelerating with a regional average annual growth rate of18%. The vegetation in this watershed is degrading, and anthropogenic disturbance accelerates this trend. Our results highlight that environmental stress adaptation strategies must account for resilience maintenance to avoid accelerating catastrophic transitions in oasis-desert ecosystems. Determining the optimal oasis scales and formulating the best irrigation management plans are effective and resilient decision-making ways to maintain the coexistence relationship of oasis-desert ecosystem in drylands. 展开更多
关键词 Oasis-desert ecosystems Hydrological regimes Soil salinization Vegetation dynamics Resilient decision-making
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