首页> 外文OA文献 >CO2 and Rn degassing from the natural analog of Campo de Calatrava (Spain): Implications for monitoring of CO2 storage sites
【2h】

CO2 and Rn degassing from the natural analog of Campo de Calatrava (Spain): Implications for monitoring of CO2 storage sites

机译:从Campo de Calatrava(西班牙)的天然类似物中脱除CO2和Rn:对监测CO2储存场所的意义

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Natural analogs offer a valuable opportunity to investigate the long-term impacts associated with thepotential leakage in geological storage of CO2.Degassing of CO2and radon isotopes (222Rn?220Rn) from soil, gas vents and thermal water dischargeswas investigated in the natural analog of Campo de Calatrava Volcanic Field (CCVF; Central Spain) todetermine the CO2?Rn relationships and to assess the role of CO2as carrier gas for radon. Furthermore,radon measurements to discriminate between shallow and deep gas sources were evaluated under theperspective of their applicability in monitoring programs of carbon storage projects.CO2flux as high as 5000 g m?2d?1and222Rn activities up to 430 kBq m?3were measured;220Rn activi-ties were one order of magnitude lower than those of222Rn. The222Rn/220Rn ratios were used to constrainthe source of the Campo de Calatrava soil gases since a positive correlation between radon isotopic ratiosand CO2fluxes was observed. Thus, in agreement with previous studies, our results indicate a deepmantle-related origin of CO2for both free and soil gases, suggesting that carbon dioxide is an efficientcarrier for Rn. Furthermore, it was ascertained that the increase of222Rn in the soil gases was likely pro-duced by two main processes: (i) direct transport by a carrier gas, i.e., CO2and (ii) generation at shallowlevel due to the presence of relatively high concentrations of dissolved U and Ra in the thermal aquiferof Campo de Calatrava.The diffuse CO2soil flux and radon isotopic surveys carried out in the Campo de Calatrava VolcanicFields can also be applicable to geochemical monitoring programs in CCS (Carbon Capture and Storage)areas as these parameters are useful to: (i) constrain CO2leakages once detected and (ii) monitor both theevolution of the leakages and the effectiveness of subsequent remediation activities. These measurementscan also conveniently be used to detect diffuse leakages.
机译:天然类似物为研究与CO2地质存储中的潜在泄漏有关的长期影响提供了宝贵的机会。在Campo de的天然类似物中研究了从土壤,气体排放口和热水排放中脱除CO2和ra同位素(222Rn?220Rn)的气体卡拉特拉瓦火山场(CCVF;西班牙中部)确定CO2?Rn关系并评估CO2作为ra的载气的作用。此外,还根据rad气测量方法在区分碳储藏项目监测计划中的适用性,对rad气测量方法进行了区分。测量了高至5000 gm?2d?1和222Rn的430Rbqm?3的CO2流量; 220Rn的活性。连接比222Rn低一个数量级。 222Rn / 220Rn比值用于限制Campo de Calatrava土壤气体的来源,因为观察到ra同位素比值与CO2流量之间呈正相关。因此,与先前的研究一致,我们的结果表明游离气体和土壤气体均与深幔有关的二氧化碳起源,表明二氧化碳是Rn的有效载体。此外,已确定土壤气体中222Rn的增加可能是由两个主要过程引起的:(i)通过载气直接运输,即产生CO2;(ii)由于存在相对较高的浓度而在较浅的水平上产生在Campo de Calatrava火山场中进行的弥散性CO2土壤通量和survey同位素测量也可应用于CCS(碳捕获和存储)区域的地球化学监测程序,因为这些参数是有助于:(i)一旦发现二氧化碳泄漏就加以遏制,(ii)监测泄漏的演变以及后续补救活动的有效性。这些测量值也可以方便地用于检测扩散泄漏。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号