| Autor: |
FARMER, V. C., MEW, G., CLAYDEN, B., LEE, R. |
| Zdroj: |
Journal of Soil Science; 1984, Vol. 35 Issue 1, p99-102, 4p |
| Abstrakt: |
SUMMARY The gley podzols of the west coast of South Island, New Zealand, typically exhibit permanent waterlogging extending from the surface to depths of 1-3 m. Their formation is explained by a continuation of processes which give rise to Peaty Podzols with thin iron pan (Ironpan Stagnopodzols; Placaquods). Iron pans initially formed within the upper B horizon are breached by acidic reducing waters and reform at a succession of lower levels down to 3 m or more below the surface. [ABSTRACT FROM AUTHOR] |
| Databáze: |
Complementary Index |
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