Based on soil type and storage density, sludge and clay soils of the loess areas,
the tertiary hill country and the floodplains are the best conditions for a deep
Rooting. Clay and especially sandy soils, as they are used for the soils of the pleistocene
Lowlands, but also characteristic of large parts of the mountain and hilly countries,
lower effective rooting depth. In the high and low bogs pleistoz
low groundwater flux levels act as a limiting factor. In the
Limit mountain and hilly countries, in the low mountains and in particular in the Alps
the present solid rock or even high skeleton content of periglazial rubble ceilings
physiological thoroughness.
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