一种基于三维地质模型的深部咸水层碳封存储量评估方法

By constructing a three-dimensional geological model and modeling lithofacies and porosity, the uncertainty in assessing carbon sequestration reserves in deep saline aquifers was resolved, enabling more accurate assessment of carbon sequestration reserves and site selection recommendations.

CN116664787BActive Publication Date: 2026-07-17CENT SOUTH UNIV

Patent Information

Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
CENT SOUTH UNIV
Filing Date
2023-05-26
Publication Date
2026-07-17

AI Technical Summary

Technical Problem

Existing technologies are insufficient to accurately assess the carbon sequestration reserves in deep saline aquifers. Traditional methods cannot effectively reflect the spatial distribution and heterogeneity of lithofacies and geological properties, resulting in high uncertainty in assessment results.

Method used

A three-dimensional geological model was used to calculate the carbon sequestration of deep saline aquifers by constructing a stratigraphic potential field, modeling lithofacies under strata-controlled constraints, and modeling geological properties in situ under facies-controlled constraints, combined with the volumetric method.

Benefits of technology

It improves the accuracy and reliability of carbon sequestration assessment in deep saline aquifers, accurately reflects the spatial distribution of lithofacies and porosity, and provides reasonable suggestions for carbon sequestration site selection.

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Abstract

本发明涉及深部咸水层碳封存储量评估技术领域,具体公开了一种基于三维地质模型的深部咸水层碳封存储量评估方法,包括以下步骤:S01:地层位势场构建:采用三维地质隐式建模方法对地层界线点及其对应的属性进行空间插值,建立同一沉积序列的整合地层的地层位势场;S02:层控约束条件下的岩相建模,以岩相为空间插值的主变量,地层位势场作为次级变量,通过考察主变量与次级变量之间的相关性来提升岩相插值结果的准确性;S03:相控约束条件下的地质属性同位协同随机建模:在岩相模型约束下模拟储层中孔隙度等属性的空间分布,来确定封存条件较好的深部咸水层;S04:深部咸水层碳封存储量估算,即采用容积法计算深部咸水层的碳封存储量。
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