Sand, Silt and Clay Soil Classification Diagram

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Alden, Andrew. "Sand, Silt and Clay Soil Classification Diagram." ThoughtCo, Feb. 5, 2017, thoughtco.com/soil-classification-diagram-1441203. Alden, Andrew. (2017, February 5). Sand, Silt and Clay Soil Classification Diagram. Retrieved from https://www.thoughtco.com/soil-classification-diagram-1441203 Alden, Andrew. "Sand, Silt and Clay Soil Classification Diagram." ThoughtCo. https://www.thoughtco.com/soil-classification-diagram-1441203 (accessed September 26, 2017).
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Soil Classification Ternary Diagram

Sand-silt-clay diagram
Click the graph to see a larger version. (c) Andrew Alden, licensed to About.com (fair use policy)

This diagram is used to translate a sediment's proportion of the three different classes of grain size -- sand, silt and clay -- into a soil description. To the geologist, sand is material with grain sizes between 2 millimeters and 1/16th millimeter, silt is 1/16th to 1/256th millimeter, and clay is everything smaller than that (they are divisions of the Wentworth scale). This is not a universal standard; soil scientists and government agencies and different countries all have slightly different soil classification systems; keep that in mind if you go deeper into this subject.

Without a microscope, these soil particle sizes are impossible to measure directly so sediment testers determine the coarse fractions by separating the size grades with precision sieves and weighing them. For the smaller particles they use tests based on how fast the different sized grains settle in a column of water. A simple home test of particle size uses a quart jar, water and measurements with a metric ruler. Either way, the tests result in a set of percentages called a particle size distribution.

Soils Based on Particle Sizes

There are several different ways to interpret a particle size distribution, depending on your purpose. This graph, specified by the U.S. Department of Agriculture, is used to turn the percentages into a soil description. Other graphs are used to classify a sediment purely as a sediment (for instance as ballfield dirt) or as the ingredients of a sedimentary rock.

Loam is generally considered the ideal soil: equal amounts of sand and silt size with a lesser amount of clay. Sand gives soil volume and porosity; silt gives it resilience; clay provides nutrients and strength while retaining water. Too much sand makes a soil loose and sterile; too much silt makes it mucky; too much clay makes it impenetrable whether wet or dry.

How To Use This Soil Diagram

To use this ternary or triangular diagram, take the percentages of sand, silt and clay and measure them off against the tick marks. Each corner represents 100 percent of the grain size it's labeled with, and the opposite face of the diagram represents zero percent of that grain size. So with a sand content of 50 percent, you would draw the diagonal line halfway across the triangle from the "Sand" corner, where the 50 percent tick is marked. Do the same with the silt or the clay percentage, and where the two lines meet automatically shows where the third component would be plotted. That spot, representing the three percentages, takes the name of the space it's sitting in.

With a good idea of a soil's consistency, as shown by this graph, you can talk knowledgeably to a professional at a garden shop or a plant nursery regarding your soil needs

. And a familiarity with ternary diagrams can help you understand igneous rock classification and many other geological subjects.

Format
mla apa chicago
Your Citation
Alden, Andrew. "Sand, Silt and Clay Soil Classification Diagram." ThoughtCo, Feb. 5, 2017, thoughtco.com/soil-classification-diagram-1441203. Alden, Andrew. (2017, February 5). Sand, Silt and Clay Soil Classification Diagram. Retrieved from https://www.thoughtco.com/soil-classification-diagram-1441203 Alden, Andrew. "Sand, Silt and Clay Soil Classification Diagram." ThoughtCo. https://www.thoughtco.com/soil-classification-diagram-1441203 (accessed September 26, 2017).