| 1. | The soil of this region is a non-leptic podzol.
|
| 2. | The podzols often occur on deep periglacial solifluction deposits down to.
|
| 3. | The soils were mostly podzol, combined with peat and gleysols.
|
| 4. | The most prevalent soil types in the region are podzol and cambisol.
|
| 5. | Podzol profile development is usual in well-drained situations.
|
| 6. | Unlike podzols proper, these soils have no continuous leached E horizon.
|
| 7. | Humic Podzols have a dark B horizon with a low iron content.
|
| 8. | Podzol and Stagnosol brown soils prevail as soil types.
|
| 9. | Brown podzolic and podzol profile developments are most common.
|
| 10. | In podzols, horizon virtually depleted of all soil constituents except quartz grains.
|
मोबाइल