The process by which the upper layers of a soil become more acidic due to the depletion of iron and aluminium compounds, clay minerals, and humus by…
| 单词 | θ5316 |
| 释义 | the world > the earth > structure of the earth > formation of features > soil formation > [noun] > forming specific type of soil (8) podzolization1922 The process by which the upper layers of a soil become more acidic due to the depletion of iron and aluminium compounds, clay minerals, and humus by… solodization1925 the formation of a solod by the leaching of salts from a solonetz. podzolizing1927 The action or process that causes podzolization; by which a soil becomes more podzolic. Usually attributive. illuviation1928 The deposition of salts or colloids in a soil horizon from percolating water which has removed them from another, generally superior, horizon. salinization1928 The accumulation of salts in the soil. solonization1934 The formation of a solonetzic soil by the leaching of salts from a solonchak. overconsolidation1936 Consolidation to an excessive degree; spec. the consolidation of soil to a greater degree than could have been produced by the present pressure of… saprolitization1970 the process of formation of saprolite. |
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