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监测二氧化碳地质封存:一种新方法。

Monitoring geological storage of CO: a new approach.

作者信息

Fawad Manzar, Mondol Nazmul Haque

机构信息

Department of Geosciences, University of Oslo, Oslo, Norway.

Norwegian Geotechnical Institute (NGI), Oslo, Norway.

出版信息

Sci Rep. 2021 Mar 15;11(1):5942. doi: 10.1038/s41598-021-85346-8.

Abstract

Geological CO storage can be employed to reduce greenhouse gas emissions to the atmosphere. Depleted oil and gas reservoirs, deep saline aquifers, and coal beds are considered to be viable subsurface CO storage options. Remote monitoring is essential for observing CO plume migration and potential leak detection during and after injection. Leak detection is probably the main risk, though overall monitoring for the plume boundaries and verification of stored volumes are also necessary. There are many effective remote CO monitoring techniques with various benefits and limitations. We suggest a new approach using a combination of repeated seismic and electromagnetic surveys to delineate CO plume and estimate the gas saturation in a saline reservoir during the lifetime of a storage site. This study deals with the CO plume delineation and saturation estimation using a combination of seismic and electromagnetic or controlled-source electromagnetic (EM/CSEM) synthetic data. We assumed two scenarios over a period of 40 years; Case 1 was modeled assuming both seismic and EM repeated surveys were acquired, whereas, in Case 2, repeated EM surveys were taken with only before injection (baseline) 3D seismic data available. Our results show that monitoring the CO plume in terms of extent and saturation is possible both by (i) using a repeated seismic and electromagnetic, and (ii) using a baseline seismic in combination with repeated electromagnetic data. Due to the nature of the seismic and EM techniques, spatial coverage from the reservoir's base to the surface makes it possible to detect the CO plume's lateral and vertical migration. However, the CSEM low resolution and depth uncertainties are some limitations that need consideration. These results also have implications for monitoring oil production-especially with water flooding, hydrocarbon exploration, and freshwater aquifer identification.

摘要

地质二氧化碳封存可用于减少向大气排放的温室气体。枯竭的油气藏、深层盐水层和煤层被认为是可行的地下二氧化碳封存选择。在注入期间及之后,远程监测对于观测二氧化碳羽流迁移和潜在泄漏检测至关重要。泄漏检测可能是主要风险,不过对羽流边界进行全面监测以及核实封存体积也很有必要。有许多有效的远程二氧化碳监测技术,各有其优点和局限性。我们建议采用一种新方法,即结合重复地震和电磁勘探来描绘二氧化碳羽流,并在一个封存场地的使用期内估算盐水层中的气体饱和度。本研究利用地震和电磁或可控源电磁(EM/CSEM)合成数据的组合来处理二氧化碳羽流描绘和饱和度估算问题。我们假设了40年期间的两种情况;情况1的建模假设同时获取了地震和电磁重复勘探数据,而在情况2中,仅利用注入前(基线)的三维地震数据进行重复电磁勘探。我们的结果表明,(i)通过使用重复地震和电磁数据,以及(ii)通过结合基线地震数据与重复电磁数据,都能够在范围和饱和度方面对二氧化碳羽流进行监测。由于地震和电磁技术的特性,从储层底部到地表的空间覆盖范围使得检测二氧化碳羽流的横向和纵向迁移成为可能。然而,可控源电磁的低分辨率和深度不确定性是一些需要考虑的局限性。这些结果对于监测石油生产(特别是注水开采时)、烃类勘探和淡水含水层识别也具有重要意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/db14/7960710/5e2ec54198cf/41598_2021_85346_Fig1_HTML.jpg

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