黄河三角洲潜在碳封存区域二氧化碳环境背景基线特征分析OACSTPCD
Characteristics analysis of CO2 environmental background baseline for potential carbon sequestration sites in Yellow River Delta
大规模封存CO2 可能会发生泄漏并侵入浅地表造成环境影响.由于自然过程复杂变化,准确地掌握基线数值和分布对于近地表泄漏监测控制至关重要.采用移动设备沿预定路径进行流动现场监测和采样实验室测试分析结合的方法,对黄河三角洲潜在碳封存区域的大气、土壤气体组分、CO2 浓度进行监测分析,以确定基线值和分布.研究结果表明:①流动监测方法的CO2 浓度在3 个不同层位的监测图中均显示出与固定监测点连续监测数据的一致性,呈现了监测区域CO2 浓度周期性波动的特征,同时,δ13 CCO2 与CO2 和O2 含量之间的关系显著,验证了流动监测方法的有效性;②查明了2 条环境背景基线,第一条是δ13 CCO2 和δ13 COC基线值,土壤δ13 CCO2 值为-14.35‰~-20.95‰,大气δ13 CCO2值为-16.92‰~-19.89‰,土壤δ13 COC值为-20.59‰~-24.79‰,这些数据反映了温带气候下土壤生物活动产生的C同位素值范围,第二条是大气与土壤CO2 浓度基线,大气CO2 浓度范围为219.20~416.4 ppm,土壤 30 cm深度的CO2 浓度范围为 1 002.793~14 808.13 ppm,土壤 50 cm深度的CO2 浓度范围为1 497.26~19 658.59 ppm.研究通过确定黄河三角洲潜在封存场所浅地表环境CO2 浓度和同位素基线值,为未来实施大规模CO2 封存后的地面监测提供了对照基准和监测方案参考.
The large-scale sequestration of CO2 may result in leakage,which could intrude into the shallow sub-surface and cause environmental impacts.Due to the complex changes of natural processes,accurately determi-ning baseline values and distributions is crucial for monitoring and controlling near-surface leakage.This study utilized portable devices along scheduled path to conduct mobile and field monitoring and sampling laboratory test,and monitored and analyzed atmospheric and soil gas components and CO2 concentrations at potential sequestration sites in Yellow River Delta to determine baseline values and distributions.The results indicate that:①in the mo-nitoring maps of three different layers,CO2 concentration data from the portable monitoring method are consistent with the continuous monitoring data from the fixed monitoring points,indicating the periodic fluctuation character-istics of the monitored CO2 concentration.Additionally,the statistically significant relationship between δ13 CCO2 and CO2 and O2 content confirms the reliability of the portable monitoring method.② Two environmental back-ground baseline values are established.The first is δ13 CCO2 and δ13 COC baseline,with the soil δ13 CCO2 isotope val-ues of-14.35‰~-20.95‰,atmospheric δ13 CCO2 values of-16.92‰~-19.89‰,and soil δ13 COC values of-20.59‰~-24.79‰.These values revealed the range of carbon isotope values produced by biological activity in temperate climates.The second is atmospheric and soil CO2 concentration baseline,with the atmospheric CO2 concentration of 219.20~416.4 ppm,soil CO2 concentrations at 30 cm depth of 1 002.793~14 808.13 ppm,and soil CO2 concentrations at 50 cm depth of 1 497.26~19 658.59 ppm.The environmental CO2 concentration and isotope baseline of shallow surface in potential carbon sequestration sites of Yellow River Delta were confirmed in this research,providing reference benchmarks and monitoring scheme recommendations for future surface moni-toring after large-scale CO2 sequestration.
汪心雯;朱宇通;李采;郭朝斌;张保建;何庆成;杨利超
中国地质科学院,北京 100037||中国地质大学(北京),北京 100083||自然资源部碳封存与地质储能工程技术创新中心,北京 100037中国地质科学院,北京 100037||自然资源部碳封存与地质储能工程技术创新中心,北京 100037中国地质科学院,北京 100037||自然资源部碳封存与地质储能工程技术创新中心,北京 100037中国地质科学院,北京 100037||自然资源部碳封存与地质储能工程技术创新中心,北京 100037中国地质科学院,北京 100037||自然资源部碳封存与地质储能工程技术创新中心,北京 100037中国地质科学院,北京 100037||自然资源部碳封存与地质储能工程技术创新中心,北京 100037中国地质科学院,北京 100037||自然资源部碳封存与地质储能工程技术创新中心,北京 100037
地质学
黄河三角洲二氧化碳地质封存泄漏环境背景基线流动监测
Yellow River Deltacarbon dioxide geological sequestrationleakageenvironmental background baselineportable monitoring
《中国地质调查》 2024 (4)
17-25,9
中国地质调查局"重点地区地质碳汇与碳封存资源调查评价(编号:DD20230119)"、国家自然科学基金"CO2大规模封存泄漏规律及其与水土环境互馈机制研究(编号:U2344226)"及中国地质科学院基本科研业务费"自然资源部碳封存与地质储能工程技术创新中心建设与运行(编号:JKY202413)"项目联合资助.
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