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    鲁西北地区地温场特征及地热资源可持续开发研究

    Characteristics of the geothermal field and sustainable exploitation of geothermal resources in northwest Shandong Province

    • 摘要: 本文聚焦鲁西北地区中低温水热型地热资源开发面临的地热井水位下降、回灌效率不足及热突破风险等核心问题,通过研究区域地质、地热钻井、地球物理勘探、地球化学测试及长期监测数据,运用热储法、数值模拟等技术,系统剖析了地温场特征、热储特性、地热流体地球化学规律,评估了资源潜力,并基于5个典型采灌工程数据优化了集约化开发井网方案。研究结果表明,区域大地热流背景较高,地温场受基底构造控制,存在"东高西低、凸起高、凹陷低"特征,地温梯度3.0 ℃/100 m~4.0 ℃/100 m,局部凸起区超4.0 ℃/100 m;主要热储层为新近纪馆陶组和古近纪东营组砂岩,热储温度54.4 ℃~85.9 ℃,馆陶组属高孔(22%~32%)高渗(平均596.3×10-3μm2)储层,东营组部分区域厚度达800 m,具备规模化开发条件;地热流体以Cl-Na型为主,结垢与腐蚀性弱至中等;区域资源储量丰富,馆陶组单井涌水量76.03m3/h~92.24m3/h,确定450 m为最优采灌井距,搭配交错排状井网与100%同层回灌模式,可将热储温度变化控制在0.5 ℃以内。研究揭示了"构造控热"核心机理,通过多工程实测与数值模拟融合量化井距、回灌参数对开发效果的影响,构建"地质认知-资源评价-技术优化-环境防控"全链条开发体系,为同类沉积盆地地热资源可持续开发提供可复制范式。

       

      Abstract: This paper focuses on the core issues in the development of medium-low temperature hydrothermal geothermal resources in northwestern Shandong, such as geothermal water level decline, insufficient reinjection efficiency, and risk of thermal breakthrough. Based on regional geological surveys, geothermal drilling, geophysical exploration, geochemical testing and long-term monitoring data, this study systematically analyzes the geothermal field characteristics, geothermal reservoir properties and geochemical evolution of geothermal fluids using the thermal reservoir method and numerical simulation, evaluates the resource potential, and optimizes the intensive development well pattern using data from five typical production-injection projects. The results indicate a regionally high terrestrial heat flow. The geothermal field, controlled by basement structures, exhibits a pattern of "higher in the east and lower in the west, and higher in uplifted areas than in depressions." Geothermal gradient ranges from 3.0 ℃/100 m to 4.0 ℃/100 m, exceeding 4.0 ℃/100 m in local uplift zones. The main thermal reservoirs are the sandstones of the Neogene Guantao Formation and the Paleogene Dongying Formation, with reservoir temperatures between 54.4 ℃ and 85.9 ℃. The Guantao Formation is a high-porosity (22% to 32%) and high-permeability (averaging 596.3×10-3μm2) reservoir. The Dongying Formation, with thicknesses up to 800 m in some areas, meets the conditions for large-scale development. The geothermal fluid is predominantly of the Cl-Na type, exhibiting weak to moderate scaling and corrosiveness. The region is rich in geothermal resources, with single-well water yields from the Guantao Formation ranging from 76.03 m3/h to 92.24 m3/h. An optimal production-injection well spacing of 450 m was determined. When combined with a staggered-row well network layout and 100% same-layer reinjection, the temperature variation within the thermal reservoir can be controlled within 0.5 ℃. This study elucidates the core mechanism of "structural control on heat distribution." By integrating multi-project field data with numerical simulation, it quantifies the impacts of well spacing and reinjection parameters on development efficiency. The research establishes a full-chain development framework encompassing "geological understanding→resource assessment→technical optimization→environmental impact prevention and control," providing a replicable model for the sustainable development of geothermal resources in similar sedimentary basins.

       

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