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    基于分布式参数模型的地热资源评价方法研究——以牛驼镇地热田为例

    Evaluation method of geothermal resource based on distributed parameter model: A case study of Niutuozhen geothermal field

    • 摘要:
      研究目的 随着中国地热田勘查程度不断提升,全井段测温数据、测井数据不断涌现,如何保留单个数据的代表性,采用合理方法对有限参数进行扩展,体现地质参数在三维空间分布的连续性、渐变性和非均质性,是提高地热资源评价精度亟待解决的问题。三维地质建模技术为高效处理这些数据提供了解决方案。开展基于分布式参数模型的地热资源评价方法研究对于提高地热资源评价的自动化水平和精度具有重要意义。
      研究方法 采用三维地质建模技术刻画了研究区的地质结构,采用离散光滑插值方法对研究区测温数据进行离散,采用序贯高斯模拟方法对研究区的空隙率数据进行离散,分别将密度和比热容与温度进行相关分析。基于以上分布式参数模型,以有限单元格作为评价单元,开展地热资源评价。
      研究结果 分别构建了研究区的三维地质模型,温度场模型,空隙率模型,密度模型和比热容模型,采用热储法评价得到各单元格的地热资源储量,共600余万个数据。通过模型的数据提取功能,提取了不同区域、不同深度范围内热储中储存的热量,得到地热资源的水平和垂向分布规律。
      结论 基于分布式参数模型的地热资源评价可以直观展示资源的空间分布特征,相比集中参数而言可以显著提高评价精度。模型可以根据需求提取特定空间范围内的热储参数统计规律和资源储量,可以用于指导三维空间的开发区划、主力目标层的定位、地热钻井孔位论证与施工方案制定、经济效益分析以及地热资源管理。

       

      Abstract:
      This paper is the result of geothermal exploration engineering.
      Objective With the continuous improvement of the exploration level of geothermal fields in China, more and more temperature measurement data and logging data are emerging. How to retain the representativeness of individual data, adopt reasonable methods to extend the limited parameters, and reflect the continuity, gradation, and heterogeneity of geological parameters in the three-dimensional spatial distribution are urgent problems to be solved for improving the accuracy of geothermal resource evaluation. The three-dimensional geological modeling technology provides a solution for efficiently processing these data. The research on the evaluation method of geothermal resources based on distributed parameter models is of great significance for improving the automation level and accuracy of geothermal resource evaluation.
      Methods The geological structure of the study area was characterized by the three-dimensional geological modeling technology. The temperature measurement data in the study area were discretized by the discrete smooth interpolation method, and the porosity data in the study area were discretized by the sequential Gaussian simulation method. The density and specific heat capacity were correlated with temperature respectively. Based on the above distributed parameter models, the geothermal resource evaluation was carried out with finite cells as evaluation units.
      Results Three-dimensional geological models, temperature field models, porosity models, density models, and specific heat capacity models of the study area were constructed. The geothermal resource reserves of each cell were evaluated by the heat reservoir method, and a total of more than 6 million data were obtained. Through the data extraction function of the model, the heat stored in the heat reservoirs in different regions and at different depths was extracted, and the horizontal and vertical distribution laws of geothermal resources were obtained.
      Conclusions The geothermal resource evaluation based on distributed parameter models can intuitively display the spatial distribution characteristics of resources. Compared with centralized parameters, it can significantly improve the evaluation accuracy. The model can extract the statistical laws and resource reserves of heat reservoir parameters within a specific spatial range, and can be used to guide the delineation of development zones in three-dimensional space, the positioning of main target layers, the argumentation and construction of geothermal drilling well positions, economic benefit analysis, and geothermal resource management.

       

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