Secondary Silicates as a Barrier to Carbon Capture and Storage in Deccan Basalt  

作　　者：Amit KUMAR J.P. SHRIVASTAVA 

机构地区：[1]Department of Geology,University of Delhi,Delhi 110007,India

出　　处：《Acta Geologica Sinica(English Edition)》2020年第3期861-876,共16页地质学报（英文版）

基　　金：financial support in the form of a Project Grant (IS-STAC/CO2-SR-79/10/G)

摘　　要：Investigating the immobilization of CO2,previous basalt-water-CO2 interaction studies revealed the formation of carbonates over a short period,but with the extensive formation of secondary silicates(SS).The mechanisms involved in these processes remain unresolved,so the present study was undertaken to understand secondary mineral formation mechanisms.XRPD and Rietveld refinement data for neo-formed minerals show a drastic decrease in the Ca-O bond length,with the calcite structure degenerating after 80 h(hours).However,SEM images and EDS data revealed that a longer interaction time resulted in the formation of chlorite and smectite,adjacent to basalt grains which prevent basaltwater-CO2 interaction to form carbonates,thus restricting carbonate formation.As a result of this,the CO2 mineralization rate is initially high(till 80 h),but it later reduces drastically.It is evident that,for such temperature-controlled transformations,low temperature is conducive to minimizing SS surface coating at the time of mineral carbonation.

关 键 词：basalt-water-CO2 interaction carbon capture and storage CO2 mineralization leachate chemistry normalized mass loss secondary silicates 

分 类 号：P618.13[天文地球—矿床学]