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GEOLOGICAL CONSIDERATIONS FOR CO_2 SEQUESTRATION IN A CRATONIC BASIN: AN ASSESSMENT OF OPTIONS IN THE ILLINOIS BASIN, USA

机译:CRATONIC盆地CO_2封存的地质考虑:美国伊利诺伊州山谷的选择评估

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The distribution, characteristics, and potential viability of geological carbon sequestration options in the Illinois Basin are being assessed through a Regional Sequestration Partnership funded by the U.S. Department of Energy (DOE) and co-funded by state government, industry, and non-governmental organizations. The Illinois Basin is a cratonic basin covering most of the state of Illinois and parts of western Indiana and western Kentucky in the Midwestern United States. Major uneconomic coal resources, oil reservoirs potentially amenable to enhanced oil recovery (EOR), and deep, brine-filled sandstone reservoirs are all present in the basin as potential carbon dioxide sinks. Illinois, in fact, contains the largest bituminous coal resource of any U.S. state. Peak Illinois oil production occurred more than 50 years ago, indicative of a highly mature resource base, yet perhaps 60 percent of assessed original-oil-in-place remains unrecovered. Illinois ranks second in the U.S. in natural gas storage capacity, thus enhancing geological understanding of brine-filled reservoirs and their seals. Assessments of geological carbon dioxide sinks have emphasized the possible economic return from adsorption on deep, uneconomic coals with release of coalbed methane and from EOR with ultimate abandonment of carbon dioxide in the reservoir. Saline reservoir injection yields no economic product but may have greater storage capacity and greater certainty of containment than in coals or oil reservoirs. Over 120 years of mining activity has largely been concentrated around Basin margins leaving large areas over the deep central and southeastern parts of the Basin unlikely to be mined. Major coals in these areas occur at about 365 m (1,200 ft) in depth. Integrated assessment of geological sequestration opportunities using Geographic Information Systems (GIS) suggests potential areas where two or more carbon sinks may be vertically stacked. Depth and temperature will determine the applicability of miscible versus immiscible EOR technologies applicable to Illinois Basin oil reservoirs, and the overlap of oil and coal sinks will define sequestration fairways coincident with hydrocarbon recovery potential. Extensive past drilling will help define these fairways, yet each data point also represents a potential leakage point, particularly with respect to the condition of oil well casing and cement (current and future). Therefore, considerations of economic return and sink integrity in the Illinois Basin may favor delivery of carbon dioxide to locations where hydrocarbons can be recovered with ultimate storage taking place in the Mt. Simon Sandstone or similar saline reservoirs beneath the same location. Hydrocarbon recovery would offset the cost of surface infrastructure (pipelines, compression, metering, etc.), injection would take place where drilling and surface operations are already familiar to the general public, and the condition of hundreds of oil wells in a field following EOR would not become a long-term integrity issue.
机译:通过由美国能源部(DOE)资助的区域封存伙伴关系进行评估,通过由美国能源部(DOE)和国家政府,行业和非政府组织共同资助的区域封存伙伴关系来评估伊利诺伊州盆地的分布,特征和潜在可行性。伊利诺伊州盆地是一个覆盖大部分伊利诺伊州伊利诺伊州和印第安纳州西部和西部肯塔基州西部的地区的大部分裂缝盆地。主要不经济的煤炭资源,漏油储存器可能适用于增强的采油(EOR),深水填充的砂岩储层全部都存在于盆地中作为潜在的二氧化碳水槽。事实上,伊利诺伊州含有任何美国国家的最大烟煤资源。伊利诺伊州的峰值产量超过50年前发生,指示高度成熟的资源基础,但也许60%的评估原油就机仍未恢复。伊利诺伊州在美国的第二次跻身天然气储存能力,从而提高了对盐水储存器及其密封件的地质理解。地质二氧化碳水槽的评估强调了从煤层甲烷的深度,不合经济煤中吸附的可能经济回报,并从储层中的终极放弃二氧化碳。盐水储层注射产生不含经济产品,但可能具有更大的储存能力和遏制力的确定性而不是在煤或储物液中。超过120年的采矿活动主要集中在盆地边距周围,留下大面积的盆地中央和东南部地区,不太可能开采。这些区域的主要煤深度为约365米(1,200英尺)深度。使用地理信息系统(GIS)综合评估地质隔离机会(GIS)表明了两个或更多个碳汇可以垂直堆叠的潜在区域。深度和温度将决定可混溶的适用性与适用于伊利诺伊州盆地油藏的不加态EOR技术,而油和煤水槽的重叠将定义与碳氢化合物恢复潜力重合的封存球道。广泛的过去钻探将有助于定义这些球道,但每个数据点也代表潜在的泄漏点,特别是关于油井套管和水泥(电流和未来)的条件。因此,伊利诺伊州盆地的经济回报和汇总性的介绍可以赞成将二氧化碳输送到碳氢化合物可以用最终储存在Mt中的终极储存中恢复。同一位置下面的类似盐水储存器。碳氢化合物回收将抵消表面基础设施的成本(管道,压缩,计量等),喷射将发生钻井和表面操作在通用公众上已经熟悉的地方,以及eOR之后的野外井中的数百个油井的条件不会成为一个长期的诚信问题。

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