Reservoir characterization of the Upper Jurassic geothermal target formations (Molasse Basin, Germany): role of thermofacies as exploration tool

S. Homuth, A. Götz, I. Sass
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引用次数: 30

Abstract

Abstract. The Upper Jurassic carbonates of the southern German Molasse Basin are the target of numerous geothermal combined heat and power production projects since the year 2000. A production-orientated reservoir characterization is therefore of high economic interest. Outcrop analogue studies enable reservoir property prediction by determination and correlation of lithofacies-related thermo- and petrophysical parameters. A thermofacies classification of the carbonate formations serves to identify heterogeneities and production zones. The hydraulic conductivity is mainly controlled by tectonic structures and karstification, whilst the type and grade of karstification is facies related. The rock permeability has only a minor effect on the reservoir's sustainability. Physical parameters determined on oven-dried samples have to be corrected, applying reservoir transfer models to water-saturated reservoir conditions. To validate these calculated parameters, a Thermo-Triaxial-Cell simulating the temperature and pressure conditions of the reservoir is used and calorimetric and thermal conductivity measurements under elevated temperature conditions are performed. Additionally, core and cutting material from a 1600 m deep research drilling and a 4850 m (total vertical depth, measured depth: 6020 m) deep well is used to validate the reservoir property predictions. Under reservoir conditions a decrease in permeability of 2–3 magnitudes is observed due to the thermal expansion of the rock matrix. For tight carbonates the matrix permeability is temperature-controlled; the thermophysical matrix parameters are density-controlled. Density increases typically with depth and especially with higher dolomite content. Therefore, thermal conductivity increases; however the dominant factor temperature also decreases the thermal conductivity. Specific heat capacity typically increases with increasing depth and temperature. The lithofacies-related characterization and prediction of reservoir properties based on outcrop and drilling data demonstrates that this approach is a powerful tool for exploration and operation of geothermal reservoirs.
德国Molasse盆地上侏罗统地热目标层储层特征:热相作为勘探工具的作用
摘要自2000年以来,德国南部Molasse盆地的上侏罗统碳酸盐岩是众多地热热电联产项目的目标。因此,以生产为导向的油藏特征具有很高的经济效益。露头模拟研究可以通过确定和对比与岩相有关的热物性和岩石物性参数来预测储层性质。碳酸盐岩地层的热相分类有助于识别非均质性和产层。导流性主要受构造和岩溶作用的控制,岩溶作用的类型和等级与相有关。岩石渗透率对储层的可持续性影响很小。在烘箱干燥样品上确定的物理参数必须进行校正,将储层转移模型应用于水饱和的储层条件。为了验证这些计算参数,使用了模拟储层温度和压力条件的thermal - triaxial - cell,并进行了高温条件下的量热和导热测量。此外,从1600米深的研究钻井和4850米(总垂直深度,测量深度:6020米)深井中提取的岩心和切削材料用于验证储层属性预测。在储层条件下,由于岩石基质的热膨胀,渗透率降低了2-3个数量级。对于致密碳酸盐,基质渗透率是温控的;热物理矩阵参数是密度控制的。密度通常随着深度的增加而增加,尤其是白云石含量的增加。因此,导热系数增大;然而,主导因素温度也降低了导热系数。比热容通常随着深度和温度的增加而增加。基于露头和钻井资料的岩相表征和储层物性预测表明,该方法是地热储层勘探和开发的有力工具。
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来源期刊
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审稿时长
39 weeks
期刊介绍: Geothermal Energy is a peer-reviewed fully open access journal published under the SpringerOpen brand. It focuses on fundamental and applied research needed to deploy technologies for developing and integrating geothermal energy as one key element in the future energy portfolio. Contributions include geological, geophysical, and geochemical studies; exploration of geothermal fields; reservoir characterization and modeling; development of productivity-enhancing methods; and approaches to achieve robust and economic plant operation. Geothermal Energy serves to examine the interaction of individual system components while taking the whole process into account, from the development of the reservoir to the economic provision of geothermal energy.
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