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Chou,Eugster和Boctor等曾利用fo_2和f_(HCl)缓冲技术分别研究了磁铁矿和赤铁矿在超临界HCl-H_2O流体中的溶解度,Crerar等测定了黄铁矿+磁黄铁矿+磁铁矿组合在酸性NaCl热水溶液中的溶解度。这些工作是目前地球化学界流行的假说——铁在热液中成铁氯络合物运移的主要实验依据。根据地质学、矿物学和地球化学的研究已知,NaCl是热
Chou, Eugster and Boctor et al. Have studied the solubility of magnetite and hematite in supercritical HCl-H 2 O fluids respectively using fo_2 and f_ (HCl) buffer technologies. Crerar et al. Determined the pyrite + pyrrhotite + Solubility of magnetite combinations in acidic NaCl hot aqueous solution. These works are the current epidemic hypothesis of geochemistry - the main experimental basis for iron transport into FeCl3 in hydrothermal solution. It is known from the studies of geology, mineralogy and geochemistry that NaCl is hot