Understanding the texture triangle to analyze the soil profile
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Time to read 4 min
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Time to read 4 min
Summary
Soil profile is the foundation of any successful crop. Understanding soil texture allows you to adapt planting, watering, and amendments. An essential tool for this is the soil texture triangle. This agronomic graphic tool precisely defines a soil's textural category based on its proportions of sand, silt, and clay. But what exactly is it used for? How do you read and use it? And what information does it provide about different soil types? Find the answers in this article, along with helpful links to our other guides on clay, silt, and sandy soils.
The soil texture triangle was developed in the 1930s by researchers at the USDA (United States Department of Agriculture) as part of the formalization of early modern agronomic classifications. Their goal was to provide a simple graphical tool for describing and comparing the physical structure of soils based on their proportions of sand, silt, and clay. By combining these three data points, a point can be located within a specific zone corresponding to a textural class: silty-clay, sandy-silty, clay-sandy, etc. This tool has since become an international standard, used by research institutes, agronomists, and experienced gardeners. This method is used by INRAE (the French National Research Institute for Agriculture, Food and Environment) and the French Soil Geoportal.
This triangle allows us to:
A good understanding of the triangle is therefore essential for any gardening or sustainable agriculture approach.
The triangle is composed of three axes:
To read the triangle:
Example: 60% sand, 25% silt, 15% clay → sandy-silty soil.
A simplified version of this tool is integrated into the analysis results of Pouryère to make reading easier for you.
Here is a summary table combining the average proportions, advantages and disadvantages of the main textural classes derived from the texture triangle:
| Textural class | % Sand | % Lemon | % Clay | Main advantages | Major drawbacks |
|---|---|---|---|---|---|
| Sandy soil | > 65% | < 20% | < 15% | Lightweight, easy to work with, good drainage | Poor in nutrients, low water retention |
| Loamy soil | 20-30% | > 40% | < 20% | Fertile, easy to loosen, retains water well | Sensitive to surface impact and erosion |
| Clay soil | < 20% | < 40% | > 40% | Very rich, high water retention capacity | Compact, sticky when wet, hard when dry |
| Balanced (firm) soil | 30-40% | 30-40% | 20-30% | Good compromise between retention, aeration, fertility | Rare in the wild, requires careful maintenance |
| Sandy-loamy soil | 40-60% | 20-40% | < 20% | Easy to work with, good infiltration | Risk of subsidence if poorly managed |
| Clay-loam soil | 20-30% | 30-50% | 20-40% | Fertile, good growing conditions, suitable for many crops | Difficult drainage, frequent compaction |
| Sandy-clay soil | 40-60% | < 20% | 20-40% | Good drainage, fairly stable | Less fertile, requires regular feeding. |
This classification helps you anticipate the specific needs of your soil and adjust your farming practices.
Once the texture is determined, you can adjust your practices:
Here are some methods to determine the texture of your soil, detailed step by step:
At Pouryère, a complete agronomic analysis (organic matter, pH , nutrients) includes characterizing your soil texture. To do this, order our agronomic analysis kit .