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Prediction of Soil Formation as a Function of Age Using the Percolation Theory Approach

2018

Recent modeling and comparison with field results showed that soil formation by chemical weathering, either from bedrock or unconsolidated material, is limited largely by solute transport. Chemical weathering rates are proportional to solute velocities. Nonreactive solute transport described by non-Gaussian transport theory appears compatible with soil formation rates. This change in understanding opens new possibilities for predicting soil production and depth across orders of magnitude of time scales. Percolation theory for modeling the evolution of soil depth and production was applied to new and published data for alpine and Mediterranean soils. The first goal was to check whether the e…

010504 meteorology & atmospheric sciencesSoil production functionSoil texturesoil depthSoil modeling percolation theory chemical weathering soil depth alpine mediterraneanmediterraneanWeatheringSoil science01 natural sciencespercolation theorychemical weathering2300 General Environmental Science910 Geography & travellcsh:Environmental sciences0105 earth and related environmental sciencesGeneral Environmental Sciencelcsh:GE1-350geographygeography.geographical_feature_categorysoil modelingBedrockalpineTree throw04 agricultural and veterinary sciences10122 Institute of GeographySettore AGR/14 - PedologiaSoil water040103 agronomy & agricultureErosion0401 agriculture forestry and fisheriesEnvironmental scienceBioturbation
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