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首页> 外文期刊>International Journal of Greenhouse Gas Control >Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates - Application in the area of the Celtic Sea and the Bay of Biscay
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Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates - Application in the area of the Celtic Sea and the Bay of Biscay

机译:杂质(氮和甲烷)对以沉积物为气态水合物的二氧化碳储存能力的影响-在凯尔特海和比斯开湾地区的应用

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摘要

Deep saline aquifers are the most important potential storage reservoirs for CO2 under supercritical conditions. Another option is the trapping of CO2 in deep-sea sediments at low temperature, either in liquid state or as gas hydrates. The Negative Buoyancy Zone (NBZ) and the Gas Hydrate Stability Zone (GHSZ) are used to calculate the theoretical storage volume. It depends essentially on the geothermal gradient and on the quality of the injected CO2. A sensitivity analysis shows that the storage volume in the Celtic Sea and the Bay of Biscay area is one order of magnitude lower if the injected fluid contains impurities like nitrogen or methane. Overall, the storage capacity in the French Exclusive Economic Zone (EEZ) exceeds 100 years of storage of the current French CO2 emissions from large point sources. The conservative estimate of the EEZ storage capacity is found to be higher than in the deep saline aquifers of the Paris Basin. Moreover, the CO2 storage capacity in this area is doubled when considering the zone beyond 200 miles from the shores. The implications of these results are potentially important for the long-term deployment strategy for CO2 storage in France and in Western Europe. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在超临界条件下,深层盐水是最重要的CO2潜在储集层。另一种选择是在低温下以液态或气态水合物形式将CO2捕集到深海沉积物中。负浮力区(NBZ)和天然气水合物稳定区(GHSZ)用于计算理论存储量。它主要取决于地热梯度和注入的二氧化碳的质量。敏感性分析表明,如果注入的流体包含诸如氮或甲烷之类的杂质,则在凯尔特海和比斯开湾地区的存储量要低一个数量级。总体而言,法国专属经济区(EEZ)的存储容量超过了法国目前从大型点源产生的CO2排放的存储时间100年。对EEZ储存能力的保守估计被发现高于巴黎盆地深层盐水含水层。此外,当考虑到距海岸200英里以外的区域时,该区域的二氧化碳存储量将增加一倍。这些结果的含义对于法国和西欧的二氧化碳封存的长期部署策略可能具有重要意义。 (C)2015 Elsevier Ltd.保留所有权利。

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