Storyboard

The three primary components of soil are sand, silt, and clay. While sand and silt grains are relatively spherical, clay particles resemble small flakes or plates. There is also a significant difference in their sizes: sand grains are just a fraction of a millimeter, silt grains are on the order of microns, and clay particles are even smaller, measuring just a few microns.



This variation in particle sizes has a significant impact on the soil's ability to compact. For instance, clay can fill the spaces between sand and silt grains, influencing the different degrees of compaction that can be achieved in the soil.

>Model

ID:(362, 'ky')

Description

The three primary components of soil are sand, silt, and clay. While sand and silt grains are relatively spherical, clay particles resemble small flakes or plates. There is also a significant difference in their sizes: sand grains are just a fraction of a millimeter, silt grains are on the order of microns, and clay particles are even smaller, measuring just a few microns. This variation in particle sizes has a significant impact on the soil's ability to compact. For instance, clay can fill the spaces between sand and silt grains, influencing the different degrees of compaction that can be achieved in the soil.

ID:(362, 0)