Abstract
In three samples of palygorskite, Fe3+ was found from Mossbauer data to occupy edge sites with relatively regular 6-coordination, and M(1) or M(2) sites in the interior of the chains. Data obtained on heating are compatible with a model of palygorskite dehydroxylate previously proposed by Preisinger (1963, in Clays and Clay Minerals, Proc. 10th Nat. Conf., Austin, Texas, 1961, pp 365-371). -D.F.B.
| Original language | English |
|---|---|
| Pages (from-to) | 226-232 |
| Number of pages | 7 |
| Journal | Clays and Clay Minerals |
| Volume | 29 |
| Issue number | 3 |
| DOIs | |
| State | Published - 1981 |
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