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    流域水循环观测与水资源可持续利用研究−以赣南禾丰盆地为例

    From water cycle observation to sustainable management: A case study of the Hefeng Basin, Southern Jiangxi

    • 摘要:
      研究目的 长江流域中游水资源时空分布不均,时常发生的自然水旱灾害、旱涝急转、自然湿地退化等水资源问题制约了区域国土空间优化与绿色可持续发展。
      研究方法 本文基于水循环与水平衡理论,选取水文地质边界清晰的典型产汇流盆地构建水循环野外观测站网,包括大气降雨观测、河流水文站、地下水监测井、地下水环境分层监测井等,基于定量观测数据开展流域地表水与地下水资源量评价。
      研究结果 赣南禾丰盆地受向斜构造控制整体呈椭圆形向西北倾斜展开,地层主体由石炭系−泥盆系碎屑岩、灰岩和燕山期岩浆岩围限。地下水流向呈“向心状”由边缘往盆地中心地势低洼处汇聚径流,沿禾丰河汇集朝西北方向排泄流出盆地。基于2020年度水循环观测数据开展流域地表水−地下水资源量评价及水平衡分析,结果显示,禾丰盆地浅层地下水天然补给资源量为2277.86×104 m3/a,开发利用程度约17.97%;地表水资源量为 8611.45×104 m3,开发利用程度约15.18%。结合盆地内近20年用水结构分析,农业种植用水占比超过70%,居民生活用水占比逐年提高至11.50%。
      结论 赣南禾丰盆地水资源量总体丰富,区域水资源总量显著大于年度用水总量,水资源可持续发展态势良好。用水需水方面,建议通过采取措施降低农业用水总量;供水结构方面,建议通过地下水应急供水水源地等措施,增强水资源跨时空配置调蓄能力,提高区域应急供水保障能力。值得借鉴的是,流域水循环观测与水平衡研究是区域水资源管理的重要基础性工作,为水资源约束区域绿色可持续发展提供重要科学依据。此外,为应对水资源时空分布不均及局部区域的应急水旱灾害,科学提高区内调水供水能力和优化用水结构。

       

      Abstract:
      This paper is the result of hydrogeological survey engineering.
      Objective The spatial and temporal distribution of water resources is uneven in the Yangtze River Basin, resulting in lots of problems including floods and droughts disasters, and degradation of natural wetlands, which restrict reginal land space optimization and sustainable development.
      Methods In this paper, based on the water balance theory, a water cycle monitoring network was constructed through a typical case study with clear hydrogeological boundaries. This water cycle monitoring network consisted of regional atmospheric precipitation, river runoff, cross-sectional flow, groundwater replenishment and drainage, and multilevel groundwater monitoring wells, thereby the integrated evaluation of surface water- groundwater was carried out based on the observation data.
      Results The Hefeng Basin, a typical oval-shaped basin inclined to the northwest, is a karst basin enclosed by clastic rock, limestone and magmatic rock. Groundwater flow direction is in a centripetal-shaped from the margin of the basin to the central low-lying area, and flows out of the basin along the Hefeng River to the northwest. The evaluation of surface water-groundwater resources and water balance analysis was conducted based on observation data from water cycle monitoring network at the year of 2020. The results show that the shallow groundwater resources was 2277.86×104 m3/a, and the degree of development and utilization at local was about 17.97%; comparing to the surface-water resources 8611.45×104 m3, and the degree of development and utilization about 15.18%. Combined with the analysis of water utilization structure in the basin in the past 20 years, the proportion of water used for agricultural planting exceeded 70%, and the proportion of domestic water used by residents increased to 11.50%.
      Conclusions The Hefeng Basin as a typical catchment in south China, is generally abundant in water resources, ensure sustainable development with the total regional water resources significantly exceeding the annual water consumption. In terms of water usage, it is recommended to measures to reduce total agricultural water consumption. Regarding the water supply, initiatives such as establishing emergency groundwater supply sources should be adopted to enhance the capacity for water resources allocation, thereby improving regional water supply security. It can be learned that, the water cycle monitoring network and water balance analysis are vital to local water resource management, which provide scientific guidelines for green and sustainable development especially in water-constrained cities. Furthermore, cope with emergency flood and drought disasters due to the uneven distribution of water resources, it is advisable to improve the capacity of water supply and optimize the water utilization structure in the region.

       

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