In a study of silica dissolution from diatoms, the rate coefficient (K) h -1 of raw diatom cells was estimated as 4 to 5 times smaller than that of the acid-digested siliceous skeletons. The dissolution rate coefficient at early stage (K1) can be predicted as a function of temperature (T ~ In K1 = a
โฆ LIBER โฆ
Silica Dissolution and Overgrowth of Fossil Diatoms
โ Scribed by Naja Mikkelsen
- Book ID
- 115511085
- Publisher
- Bioone
- Year
- 1977
- Tongue
- English
- Weight
- 248 KB
- Volume
- 23
- Category
- Article
- ISSN
- 0026-2803
- DOI
- 10.2307/1485336
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