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Experimental supercritical CO_2 and water interactions with coal under simulated in situ conditions

机译:实验超临界CO_2和煤炭在原位条件下与煤的水相互作用

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Geological storage of CO_2 is a key component of emission reduction strategies. Options for geosequestration include injecting CO_2 into oil and gas fields (producing or depleted), deep saline formations and coal seams. We have investigated injection of CO_2 into coal using static batch experiments conducted under temperature and pressure conditions similar to the in situ formation conditions for the coal samples. Within a custom built batch reactor, sister sample coal cubes (15 mm) were immersed first in water only, and then a mixture of supercritical CO_2 and water (sCO_2-H_2O). The sCO_2-H_2O experiment fluid chemistry indicates significant mobilisation of metals due to dissolution of cleat and matrix mineral matter, as well as displacement of ion exchangeable metals. Minor minerals within coal can be major constituents within the reaction fluids analysed. SEM images have provided evidence of the dissolution of both cleat and matrix minerals, as well as coal swelling and contraction induced by CO_2 adsorption and desorption, respectively.
机译:CO_2的地质储存是减排策略的关键组成部分。 GeoseQuestration的选择包括将CO_2注入油气场(生产或耗尽),深盐形成和煤层。使用与煤样的温度和压力条件下的温度和压力条件下进行的静态批量实验,研究了将CO_2注射到煤中。在定制的批量反应器中,姐妹样品煤立方体(15 mm)仅在水中浸入水中,然后浸入超临界CO_2和水(SCO_2-H_2O)的混合物中。 SCO_2-H_2O实验流体化学表明由于夹层和基质矿物质溶解,以及离子可交换金属的位移,所述金属的显着动员。煤中的次要矿物质可以是分析的反应液中的主要成分。 SEM图像提供了夹层和基质矿物质溶解的证据,以及CO_2吸附和解吸诱导的煤溶胀和收缩。

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