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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Chemical-mechanical coupling observed for depleted oil reservoirs subjected to long-term CO2-exposure - A case study of the Werkendam natural CO2 analogue field
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Chemical-mechanical coupling observed for depleted oil reservoirs subjected to long-term CO2-exposure - A case study of the Werkendam natural CO2 analogue field

机译:长期暴露于CO2的贫油油藏观察到的化学-机械耦合-以Werkendam天然CO2类似物领域为例

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Geological storage of CO2 is one of the most promising technologies to rapidly reduce anthropogenic emissions of carbon dioxide. In order to ensure storage integrity, it is important to understand the effect of long-term CO2/brine/rock interactions on the mechanical behaviour of a storage complex. As most of these reactions are too slow to reproduce on laboratory timescales, we studied a natural CO2 analogue reservoir (the Rot Fringe Sandstone, Werkendam field, the Netherlands; 125-135 Ma of CO2-exposure) and its unreacted counterpart. We focused on CO2-induced mineralogical and porosity-permeability changes, and their effect on mechanical behaviour of both intact rock and simulated fault gouge. Overall, CO2-exposure did not lead to drastic mineralogical changes. The CO2-exposed material shows a stronger dependence of permeability on porosity, which is attributed to differences in diagenesis (closed-system diagenesis and hydrocarbon emplacement) taking place before CO2 charging. The limited extent or reaction was in part the result of bitumen coatings protecting specific mineral phases from reaction. In local, mm-sized zones displaying significant anhydrite cement dissolution, enhanced porosity was observed. For most of the reservoir the long-term mechanical behaviour after CO2-exposure could be described by the behaviour of the unreacted sandstone, while these more 'porous' zones had a lower rock strength. In addition, CO2-exposure did not affect the fault friction behaviour, and slip is expected to result in stable sliding. Simple stress path calculations predict that reservoir failure due to depletion and injection is unlikely, even for the 'porous' zones, nor will fault reactivation occur for realistic injection scenarios. (c) 2015 Elsevier B.V. All rights reserved.
机译:二氧化碳的地质封存是迅速减少人为排放二氧化碳的最有希望的技术之一。为了确保存储完整性,重要的是要了解长期的CO2 /盐水/岩石相互作用对存储设备的机械性能的影响。由于这些反应中的大多数反应太慢而无法在实验室时间尺度上重现,因此我们研究了天然二氧化碳类似物储层(荷兰Werkendam油田的Rot Fringe砂岩;二氧化碳暴露量为125-135 Ma)及其未反应的对应物。我们重点研究了二氧化碳引起的矿物学和孔隙度-渗透率变化,以及它们对完整岩石和模拟断层泥的力学行为的影响。总体而言,二氧化碳暴露并未导致剧烈的矿物学变化。暴露于CO2的材料显示出渗透率对孔隙度的依赖性更大,这归因于在注入CO2之前发生的成岩作用(封闭系统成岩作用和碳氢化合物沉积)的差异。有限的程度或反应部分是由于沥青涂层保护了特定矿物相免于反应的结果。在局部毫米大小的区域显示出明显的硬石膏水泥溶解,观察到孔隙率增加。对于大多数储层,CO 2暴露后的长期力学行为可以用未反应的砂岩的行为来描述,而这些“多孔”区域的岩石强度较低。此外,接触二氧化碳不会影响断层摩擦性能,预计打滑会导致稳定的滑动。简单的应力路径计算可以预测,即使对于“多孔”区域,由于耗尽和注入造成的储层破坏也不可能发生,对于实际的注入情况也不会发生断层活化。 (c)2015 Elsevier B.V.保留所有权利。

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