Department of Geology and Geophysics , University of Wyoming , 1000 E. University Avenue , Laramie , Wyoming 82071 , United States.
Physical and Computational Sciences Directorate , Pacific Northwest National Laboratory , P.O. Box 999, MS K8-98, Richland , Washington 99352 , United States.
Environ Sci Technol. 2018 Jun 19;52(12):7138-7148. doi: 10.1021/acs.est.8b00438. Epub 2018 Jun 6.
We explored the influence of a model organic ligand on mineral carbonation in nanoscale interfacial water films by conducting five time-resolved in situ X-ray diffraction (XRD) experiments at 50 °C. Forsterite was exposed to water-saturated supercritical carbon dioxide (90 bar) that had been equilibrated with 0-0.5 m citrate (CHO) solutions. The experimental results demonstrated that greater concentrations of citrate in the nanoscale interfacial water film promoted the precipitation of magnesite (MgCO) relative to nesquehonite (MgCO·3HO). At the highest concentrations tested, magnesite nucleation and growth were inhibited, lowering the carbonation rate constant from 9.1 × 10 to 3.6 × 10 s. These impacts of citrate were due to partial dehydration of Mg(aq) and the adsorption of citrate onto nuclei and magnesite surfaces. This type of information may be used to predict and tailor subsurface mineralization rates and pathways.
我们通过在 50°C 下进行五次时间分辨原位 X 射线衍射 (XRD) 实验,探索了模型有机配体对纳米尺度界面水膜中矿物碳化的影响。方镁石暴露于与 0-0.5m 柠檬酸盐 (CHO) 溶液平衡的水饱和超临界二氧化碳 (90 巴) 中。实验结果表明,纳米尺度界面水膜中柠檬酸浓度越高,相对于水菱镁矿 (MgCO·3HO),促进了菱镁矿 (MgCO) 的沉淀。在测试的最高浓度下,菱镁矿成核和生长受到抑制,使碳化速率常数从 9.1×10 降至 3.6×10 s。柠檬酸的这些影响是由于 Mg(aq) 的部分脱水和柠檬酸在核和菱镁矿表面的吸附。这种类型的信息可用于预测和调整地下成矿速率和途径。