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خاک لای

File:Windrow_of_windblown_glacial_silt,_NWT.jpg · Wikimedia Commons · See Wikimedia Commons

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خاک لای

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thumb|Windrow of windblown silt, Northwest Territories, Canada|right Silt is granular material of a size between sand and clay and composed mostly of broken grains of quartz. Silt may occur as a soil (often mixed with sand or clay) or as sediment mixed in suspension with water. Silt usually has a floury feel when dry, and lacks plasticity when wet. Silt can also be felt by the tongue as granular when placed on the front teeth (even when mixed with clay particles).

AI overview

Silt is a fine granular material made mostly of broken quartz grains, sized between sand and clay, that can occur as soil or suspended in water and feels floury when dry. It matters because understanding silt's properties—including how it behaves when wet or dry—is important for soil science, construction, water management, and other practical applications.

AI-generated from the Wikipedia summary — may contain errors.

Wikidata facts

Subclass of
sediment
Image
Watt1.jpg
Show 3 more facts
Commons category
Silt
different from
aleurite (sediment)
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