Abstract
In nature, forest vegetation and soil have evolved as coupled ecosystems over a long period of time by natural succession in a place. Some abandoned croplands have also been afforested so long ago that some of their original characteristics have changed. These soils are also considered as forest soils. Forest soils have some characteristics different from agricultural soils. Forest soils include usually porous, aggregated, well-differentiated soils with plenty of organic matter, often forming a forest floor on the surface soil, and high biotic activity. Most present-day agricultural soils developed under forest in the past. The upper part of many of these soils have changed significantly due to prolonged cropping practices, but their subsoils still bear the signs of a past forest vegetation. Soil properties have a bearing on selecting tree species for plantation forestry. Tree species by occupancy in a soil for long period have an effect on the soil. Some tree species may be used for the improvement of degraded lands. Forests are efficient nutrient recyclers. Very dense forests may develop in relatively poorly fertile soils due to this nutrient recycling. Nutrients recycle within the system several times and the same nutrient atom performs the same physiological functions each time. During nutrient recycling nutrients are taken up, some proportion is retained in biomass, some proportion is returned to the soil as litter, and nutrients are released by decomposition of litter materials. Too fast and too slow nutrient recycling are both undesirable in the context of soil fertility restoration and plant nutrition. Forests are also efficient carbon sequesters. Forest and forest soil management can be used for climate change mitigation.
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Osman, K.T. (2013). Forest Soils. In: Soils. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-5663-2_14
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