抜粋
Imogolites were prepared with Ge/(Ge + Si) ratios of 0, 0.2, 0.5 and 1.0; the products are illustrated with electron micrographs. Products were similar to natural imogolites in their tubular morphology, electron diffraction patterns and DTA curves. Changes in tube dimensions and in IR absorption bands are discussed. -D.F.B.
| 元の言語 | 英語 |
|---|---|
| ページ（範囲） | 123-138 |
| ページ数 | 16 |
| ジャーナル | Clays & Clay Minerals |
| 巻 | 30 |
| 発行部数 | 2 |
| DOI | |
| 出版物ステータス | 出版済み - 1982 |
All Science Journal Classification (ASJC) codes
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth and Planetary Sciences (miscellaneous)
フィンガープリント Effects of substitution of germanium for silicon in imogolite.' の研究トピックを掘り下げます。これらはともに一意のフィンガープリントを構成します。
これを引用
Wada, S. I., & Wada, K. (1982). Effects of substitution of germanium for silicon in imogolite. Clays & Clay Minerals, 30(2), 123-138. https://doi.org/10.1346/ccmn.1982.0300206