Bifalgorithm post · Introduction to soil science · Poorly Crystalline Silicate, Oxide, and Organic Colloids

Poorly Crystalline

Poorly Crystalline (Introduction to soil science · Poorly Crystalline Silicate, Oxide, and Organic Colloids) — "Poorly crystalline silicates are silicon-oxygen…

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Poorly crystalline silicates
They are silicon-oxygen minerals.
They have short-range order rather than extensive repeating crystal patterns.
They commonly form from volcanic ash.
Examples include allophane and imogolite.
Allophane
Imogolite
These minerals have sphere- or tube-shaped structures.
They retain substantial water.
They have significant pH-dependent charge.
These properties contribute to the fertility of volcanic-ash soils.

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Poorly Crystalline

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Introduction to soil science

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"Poorly crystalline silicates are silicon-oxygen minerals with short-range order rather than extensive repeating crystal patterns. They commonly form from volcanic ash and include allophane and imogolite, which have sphere- or tube-shaped structures. These minerals retain substantial water and have significant pH-dependent charge, contributing to the fertility of volcanic-ash soils."

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