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首页> 外文期刊>Geothermal Energy Science >Reservoir characterization of the Upper Jurassic geothermal target formations (Molasse Basin, Germany): role of thermofacies as exploration tool
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Reservoir characterization of the Upper Jurassic geothermal target formations (Molasse Basin, Germany): role of thermofacies as exploration tool

机译:上侏罗统地热目标地层的储层特征(德国莫拉塞盆地):热相作为勘探工具的作用

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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.
机译: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,以生产为导向的储层表征具有很高的经济意义。露头类比研究通过确定岩相相关的热物理参数和岩石物理参数来实现储层物性预测。碳酸盐岩地层的热相分类有助于识别非均质性和生产区。水力传导率主要受构造构造和岩溶作用控制,而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。必须对在烘干后的样品上确​​定的物理参数进行校正,将储层转移模型应用于水饱和的储层条件。为了验证这些计算出的参数,使用了模拟储层温度和压力条件的热三轴单元,并在高温条件下进行了量热法和热导率测量。此外,从1600 m深的研究钻探和4850 m(总垂直深度,测得深度:6020 m)深井中提取的岩心和切削材料用于验证储层物性预测。在储层条件下,由于岩石基质的热膨胀,导致渗透率降低了2-3个数量级。对于致密的碳酸盐,基质渗透率是可控的。热物理基质参数是密度控制的。密度通常随深度而增加,尤其是随着白云石含量的增加而增加。因此,导热系数增加;但是,主导因素温度也会降低热导率。比热容通常随着深度和温度的增加而增加。基于露头和钻井数据的岩相相关的特征描述和储层物性预测表明,这种方法是地热储层勘探和运营的有力工具。

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