This process is known as podzolization and is particularly intense in boreal and cool temperate forests that are mainly constituted by coniferous pines whose litterfall is rich in phenolic compounds and fulvic acid.
2.
During the 1930s, soil formation was explained in terms of loosely conceived processes, such as " podzolization, " " laterization, " and " calcification . " These were presumed to be unique processes responsible for the observed common properties of the soils of a region.
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