Abstract
Research was conducted to evaluate Fe transformations in a hydrosequence of Oxisols from the Central Plateau of Brazil. The best-drained member of the hydrosequence of soils selected for the study classifies as an Anionic Acrustox (Dark-Red Latosol). Differences in color and iron oxide mineralogy of soils in this hydrosequence are the result of the preferential reduction of hematite over Al-substituted goethite in the presence of a seasonally high water table. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 1114-1118 |
| Number of pages | 5 |
| Journal | Soil Science Society of America Journal |
| Volume | 53 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1989 |
All Science Journal Classification (ASJC) codes
- Soil Science
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