松辽流域地下水储存量及其可开采量

    Groundwater storage and its exploitable amount in Songliao basin

    • 摘要: 地下水是维持社会发展和生态安全的重要资源,地下水储存量评价是摸清水资源家底,服务生态文明建设的基础。在整理相关勘察和监测资料并概化含水层的基础上,采用体积法评价了松辽流域地下水储存量及其可开采量,分析了地下水储存量的控制性因素。结果显示:松辽流域浅层地下水总储存量为48734.66×108m3,其中平原区储存量40253.74×108m3、山间盆地477.21×108m3,河谷区1901.32×108m3,玄武岩区为1982.56×108m3,岩溶区73.15×108m3,基岩山区4046.68×108m3。主要平原中三江平原和兴凯湖平原地下水储存量模数相对较大。地下水主要为淡水,TDS≤1的地下水储存量为47162.97×108m3,占总储存量的96%以上。松辽流域平原区可开采储存量为818.97×108m3,其中年度可开采调节储存量为359.85×108m3,难以更新可开采储存量为459.12×108m3。地下水储存量主要受富水性和含水层厚度等水文地质条件的影响,水文地质条件的差异性造成地下水储存量的空间分布不均。地下水储存量评价为松辽流域水资源综合管理和生态保护提供基础数据,为自然资源综合调查与生态文明建设提供支撑。

       

      Abstract:  Groundwater is an important resource to maintain social development and ecological security. Groundwater storage assessment is the basis for identifying the quantity of water resources and serving the construction of ecological civilization. On the basis of sorting out the relevant survey and monitoring data and generalizing the aquifer, the volume method is used to evaluate the groundwater storage capacity and its exploitable capacity in Songliao Basin, and the controlling factors of groundwater storage capacity are analyzed. The results show that the total storage of shallow groundwater in Songliao basin is 48734.66×108m3, including 40253.74×108m3 in plain area, 477.21 ×108m3 in intermountain basin, 1901.32×108m3 in river valley, 1982.56×108m3 in basalt area, 73.15×108m3 in karst area, 4046.68×108m3 in bedrock mountainous area. Among the main plains, the modulus of groundwater storage in Sanjiang Plain and Xingkai Lake Plain is relatively large. The groundwater in Songliao Basin is mainly fresh water, and the storage capacity of groundwater with TDS ≤ 1 is 47162.97×108m3, accounting for more than 96% of the total storage. The exploitable storage in the plain area of Songliao Basin is 818.97×108m3, of which the annual exploitable regulated storage is 359.85×108m3, and the unrenewable exploitable storage is 459.12×108m3. Groundwater storage is mainly affected by hydrogeological conditions such as water abundance and aquifer thickness. The difference of hydrogeological conditions results in uneven spatial distribution of groundwater storage. The evaluation of groundwater storage provides basic data for the comprehensive management of water resources and ecological protection in Songliao Basin, and provides support for the comprehensive investigation of natural resources and the construction of ecological civilization.

       

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