温室气体
环境科学
碳足迹
铀
溶解
浸出(土壤学)
二氧化碳
碳捕获和储存(时间表)
环境工程
环境化学
土壤科学
地质学
气候变化
化学
材料科学
工程类
土壤水分
化学工程
冶金
有机化学
海洋学
作者
Yun Yang,Jinsong ZUO,Wenjie Qiu,Jichun Wu,Weimin Que,Genmao ZHOU,Zhengbang LIU,Jianfeng Wu
标识
DOI:10.1111/1755-6724.15058
摘要
Abstract Under the new development philosophy of carbon peaking and carbon neutrality, CO 2 and O 2 in situ leaching (ISL) has been identified as a promising technique for uranium mining in China, not only because it solves carbon dioxide utilization and sequestration, but it also alleviates the environmental burden. However, significant challenges exist in assessment of CO 2 footprint and water‐rock interactions, due to complex geochemical processes. Herein this study conducts a three‐dimensional, multicomponent reactive transport model (RTM) of a field‐scale CO 2 and O 2 ISL process at a typical sandstone‐hosted uranium deposit in Songliao Basin, China. Numerical simulations are performed to provide new insight into quantitative interpretation of the greenhouse gas (CO 2 ) footprint and environmental impact (SO 4 2 – ) of the CO 2 and O 2 ISL, considering the potential chemical reaction network for uranium recovery at the field scale. RTM results demonstrate that the fate of the CO 2 could be summarized as injected CO 2 dissolution, dissolved CO 2 mineralization and storage of CO 2 as a gas phase during the CO 2 and O 2 ISL process. Furthermore, compared to acid ISL, CO 2 and O 2 ISL has a potentially smaller environmental footprint, with 20% of SO 4 2– concentration in the aquifer. The findings improve our fundamental understanding of carbon utilization in a long‐term CO 2 and O 2 ISL system and provide important environmental implications when considering complex geochemical processes.
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