Silt


Summary

Silt is granular material between sand and clay, mostly broken quartz grains, roughly 4 to 63 microns, and floury with no plasticity when wet. It loses strength when wetted and can liquefy in earthquakes, so silty soils need geotechnical review before bearing or compaction assumptions are made.


Cols

Image

Silt.jpg


Terminology

Composition and production

Raw materials

Grades and types

Properties

Physical

Mechanical

Standards

Test methods

Uses in buildings

Building elements

Pros and cons

Pros

Cons

Sources