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V. Dokuchaev (Saint Petersburg, 1888)
V. Dokuchaev (Saint Petersburg, 1888)
Dokuchaev's soil-formation factors
Dokuchaev's soil-formation factors
V. Dokuchaev, 1898
V. Dokuchaev, 1898
Grave.
Grave.
Podzol
The picture is of a stagnic podzol in upland Wales, and shows the typical sequence of organic topsoil with leached grey-white subsoil with iron-rich h
The picture is of a stagnic podzol in upland Wales, and shows the typical sequence of organic topsoil with leached grey-white subsoil with iron-rich horizon below. This example has two weak ironpans.
The biome typically associated with Spodosols is coniferous forest.
The biome typically associated with Spodosols is coniferous forest.
Spodosols of the world
Spodosols of the world
A Podzol with a characteristic eluvial (bleached, ash-colored) horizon and intensely coloured illuvial horizons. The photo was taken in the Feldberg a
A Podzol with a characteristic eluvial (bleached, ash-colored) horizon and intensely coloured illuvial horizons. The photo was taken in the Feldberg area, Southern Black Forest, Germany.