Siliceous deposits formed from geothermal water I. The major constituents and the existing states of iron and aluminium

Takushi Yokoyama, Yumi Sato, Yonezo Maeda, Toshikazu Tarutani, Ryuichi Itoi

研究成果: Contribution to journalArticle査読

44 被引用数 (Scopus)

抄録

In the deposition of siliceous material from geothermal water, a relationship between chemical compositions of geothermal waters and siliceous deposits was investigated. The results indicated that iron and aluminium were concentrated into these siliceous deposits. For the chemical state of the iron in the deposits, some oxides and oxyhydroxides, sulfide and amorphous iron silicate were identified by powder X-ray diffraction and 37Fe Mossbauer spectroscopy. For the aluminium, two states were detected by 27A1 MAS NMR: 6-coordinate aluminium (such as aluminium hydroxide) and 4-coordinate aluminium substituting a Si atom site in the deposit. In some deposit samples, both 4- and 6-coordinate aluminium were detected, but in others only the former was found.

本文言語英語
ページ(範囲)375-384
ページ数10
ジャーナルGEOCHEMICAL JOURNAL
27
6
DOI
出版ステータス出版済み - 1993

All Science Journal Classification (ASJC) codes

  • 地球物理学
  • 地球化学および岩石学

フィンガープリント

「Siliceous deposits formed from geothermal water I. The major constituents and the existing states of iron and aluminium」の研究トピックを掘り下げます。これらがまとまってユニークなフィンガープリントを構成します。

引用スタイル