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• W3146363542 abstract "从中立温泉形成的五件铁的沉积物样品被分析决定他们是否由微分热分析(DTA ) 由硅石，含水的氧化铁或铁硅酸盐的混合物组成了，红外线(红外) 光谱学，粉末 X 光检查衍射(XRD ) ，和 57Fe M ? ssbauer 光谱学。存款的 Si/Fe 原子比率从 0.25 ～ 0.45 ，并且是比 hisingerite (12 ) 的那些小的，但是显然硅质的 ferrihydrite (0.250.5 ) 关门到那些。Si 被证实从在 IR 系列上拉长颤动频率的 Si-O 表现为 monomeric 或 oligomeric 硅酸盐。从 DTA 的结果判定，开始在加热以后生产的矿物质，和在拉长颤动频率和 Si/Fe 原子比率的 Si-O 之间的一种关系由 Henmi 等建议了它。(1981 ) ，在这研究的所有沉积物被结束是有低、高的 Si/Fe 原子比率的各种各样的硅质的 ferrihydrites 的混合物。而且由比较热泉水的化学性质，硅质的 ferrihydrite 的形成条件也被讨论。" @default.
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• W3146363542 date "2013-01-01" @default.
• W3146363542 modified "2023-09-27" @default.
• W3146363542 title "A study on the interaction between ferric ion and silicic acid in hydrosphere： Si-containing ferruginous deposits formed in neutral hot spring waters" @default.
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