用于二氧化碳地质封存的布鲁姆溪深盐含水层的综合岩石物理评估和岩石物理建模

Fuels Pub Date : 2024-02-06 DOI:10.3390/fuels5010004
Prasad Pothana, Ghoulem Ifrene, Kegang Ling
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引用次数: 0

摘要

煤炭和碳氢化合物等化石燃料是导致全球变暖的主要因素,也是包括二氧化碳在内的全球温室气体排放的主要原因。在深盐水层中封存二氧化碳被认为是减少二氧化碳排放和实现气候目标的最实用、最有前途的方法之一。北达科他州工业委员会(NDIC)最近批准了北达科他州威利斯顿盆地第四个碳捕集与封存项目的 VI 级许可,该项目将在 Broom Creek 地层进行二氧化碳地质封存。目前的研究旨在对 Broom Creek 深盐储层进行全面的岩石物理特征描述和岩石物理建模,以揭示矿物学分布并了解整个地层的岩石物理和弹性特性变化。这项研究利用地球物理测井记录、常规岩心分析和高级岩心分析来评估 Broom Creek 地层。经 X 射线衍射结果校准的多矿物岩石物理分析表明,该地层主要由高孔隙度的洁净砂岩和低孔隙度的白云岩、无水石膏和粉砂/粘土层组成。该地层显示出不同的孔隙度,最高可达 0.3,克林肯贝格空气渗透率最高可达 ∼ 2600 mD。根据阿奇方程,地层水电阻率在 150 °F 时约为 0.055 欧姆-米,相当于大约 63,000 ppm 的氯化钠盐度,这与之前的数据一致。清洁砂岩岩层样本中的孔喉分布主要位于宏观-超宏观尺度。然而,无水石膏和白云石的存在阻碍了孔隙度和孔喉尺寸。通过开发岩石物理模板,实现了对有效弹性特性的准确预测。干岩模量采用希尔平均法建模,饱和模量采用贝里曼自洽法建模。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Integrated Petrophysical Evaluation and Rock Physics Modeling of Broom Creek Deep Saline Aquifer for Geological CO2 Storage
Fossil fuels, such as coal and hydrocarbons, are major drivers of global warming and are primarily responsible for worldwide greenhouse gas emissions, including carbon dioxide CO2. The storage of CO2 in deep saline reservoirs is acknowledged as one of the top practical and promising methods to reduce CO2 emissions and meet climate goals. The North Dakota Industrial Commission (NDIC) recently approved the fourth Class VI permit for a carbon capture and storage project in the Williston basin of North Dakota for the geological CO2 storage in the Broom Creek formation. The current research aimed to conduct a comprehensive petrophysical characterization and rock physics modeling of the Broom Creek deep saline reservoir to unravel the mineralogical distribution and to understand the variations in petrophysical and elastic properties across the formation. This study utilized geophysical well logs, routine core analysis, and advanced core analysis to evaluate the Broom Creek formation. Multimineral petrophysical analysis calibrated with X-ray diffraction results reveals that this formation primarily comprises highly porous clean sandstone intervals with low-porosity interspersed with dolomite, anhydrite, and silt/clay layers. The formation exhibits varying porosities up to 0.3 and Klinkenberg air permeabilities up to ∼2600 mD. The formation water resistivity using Archie’s equation is approximately 0.055 ohm-m at 150 °F, corresponding to around 63,000 ppm NaCl salinity, which is consistent with prior data. The pore throat distribution in the samples from clean sandstone intervals is primarily situated in the macro-mega scales. However, the presence of anhydrite and dolomite impedes both porosity and pore throat sizes. The accurate prediction of effective elastic properties was achieved by developing a rock physics template. Dry rock moduli were modeled using Hill’s average, while Berryman’s self-consistent scheme was employed for modeling saturated moduli.
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