浸出(土壤学)
土(古典元素)
溶解二氧化硅
石英
降水
杂质
矿物学
嗜石者
材料科学
地质学
环境化学
溶解
化学
冶金
土壤水分
玄武岩
地球化学
有机化学
部分熔融
土壤科学
气象学
物理化学
数学物理
物理
作者
Masahiko Bessho,Yasuhiro Fukunaka,Hiromu Kusuda,Takashi Nishiyama
出处
期刊:Energy & Fuels
[American Chemical Society]
日期:2009-07-16
卷期号:23 (8): 4160-4165
被引量:27
摘要
A refining processing of high-purity silica from biogenic diatomaceous earth is newly proposed to exploit the steady and stable resource to the solar-power generation industry. The specimens collected from various representative diatomaceous earth deposits, including both marine and freshwater origin, were chemically analyzed. Trace element distribution in diatomaceous earth was influenced by the biotope habitat of diatoms, when compared to that in quartz of igneous origin. Al, K, and Fe were mainly terrestrially derived, while Si and B were from diatom shells. B content in diatomaceous earth specimens from lacustrine sources was less than that in marine origin. Diatomaceous earth was then dissolved into caustic alkaline solution. With a decreasing pH value, amorphous silica precipitated with impurities. Al and Fe were concentrated in silica precipitated in the pH range of 12.5−10.5, while B was more soluble than silica at pH less than 9. Silica can be precipitated in the pH range of 10.5−9.0, followed by acid leaching to reduce Al and Fe content. A simple chemical operation consisting of extraction, precipitation, and acid leaching has been proposed. Repetition of chemical processing 3 times provides more than 5 N silica from diatomaceous earth samples from freshwater-source rocks.
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