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- W2126352169 abstract "SUMMARYThe accumulation of clay and organic material, forming argillans and organans, is poorly understood and is at least not a subject of general agreement. Electron scanning and microprobe show striking features. The argillans, having Si, Al and Fe, are clearly layered and seldom cracked. The organans do not contain Si, but either Al only, or Al and Fe, are not layered, but are composed of discrete very small bodies, stacked at random. They have a strong polygonal cracking pattern, indicating a shrinking process.The morphology of argillans seems inconsistent with a flocculation process, which would give a porous structure with much water, so that the strong layering is obviously due to a slow deposition of layer silicates out of a dispersed phase.The organans are formed by deposition of gel-like organo-metallic compounds and evaporation of the solvation water, causing a strong shrinking." @default.
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- W2126352169 date "1980-12-01" @default.
- W2126352169 modified "2023-09-26" @default.
- W2126352169 title "Morphology, composition and genesis of argillans and organans in soils" @default.
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- W2126352169 doi "https://doi.org/10.1111/j.1365-2818.1980.tb04154.x" @default.
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