Curriculum 03

Soil Science

The living foundation beneath your feet — what soil is, how it works, how to improve it

Section I — Foundation

Chapter 2: Soil Texture — Sand, Silt, and Clay

Why this matters: Soil texture is the single most fundamental physical property of your soil — and unlike pH or nutrient levels, you cannot change it. Understanding texture tells you how your soil drains, how it holds water, how it compacts, how it behaves when wet and dry, and what plants will thrive in it. Every management decision flows from knowing your soil's texture.

2.1 The Three Mineral Particles

All soil mineral particles are classified by size. The relative proportion of sand, silt, and clay defines texture.

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PARTICLE SIZE COMPARISON

From: 2.1 The Three Mineral Particles

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig01.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig01.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig01.png" alt="PARTICLE SIZE COMPARISON"></figure>


2.2 The Soil Texture Triangle

The texture triangle classifies soils based on percentages of sand, silt, and clay.

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SOIL TEXTURE TRIANGLE

From: 2.2 The Soil Texture Triangle

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig02.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig02.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig02.png" alt="SOIL TEXTURE TRIANGLE"></figure>


2.3 The Ribbon Test — Identifying Texture by Hand

You don't need a laboratory to determine soil texture. The ribbon test is accurate enough for practical decision-making.

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RIBBON TEST PROCEDURE

From: 2.3 The Ribbon Test — Identifying Texture by Hand

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig03.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig03.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig03.png" alt="RIBBON TEST PROCEDURE"></figure>


2.4 Sand — Properties and Management

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SAND CHARACTERISTICS

From: 2.4 Sand — Properties and Management

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig04.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig04.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig04.png" alt="SAND CHARACTERISTICS"></figure>


2.5 Clay — Properties and Management

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CLAY CHARACTERISTICS

From: 2.5 Clay — Properties and Management

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig05.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig05.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig05.png" alt="CLAY CHARACTERISTICS"></figure>


2.6 Silt — Properties and Management

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SILT CHARACTERISTICS

From: 2.6 Silt — Properties and Management

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig06.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig06.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig06.png" alt="SILT CHARACTERISTICS"></figure>


2.7 Loam — The Ideal

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LOAM: balanced mixture of sand, silt, and clay

From: 2.7 Loam — The Ideal

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig07.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig07.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig07.png" alt="LOAM: balanced mixture of sand, silt, and clay"></figure>


2.8 Amending Texture vs Working With It

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CAN YOU CHANGE SOIL TEXTURE?

From: 2.8 Amending Texture vs Working With It

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig08.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig08.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig08.png" alt="CAN YOU CHANGE SOIL TEXTURE?"></figure>


Chapter Summary

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TEXTURE = relative amounts of sand, silt, clay

From: Chapter Summary

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig09.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig09.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig09.png" alt="TEXTURE = relative amounts of sand, silt, clay"></figure>

📝 Interactive Quiz
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Part A — True or False

1. Sand particles are the largest of the three main particle sizes

2. Clay particles are the smallest and have the highest surface area

3. Silt particles are intermediate in size between sand and clay

4. Sandy soils have high water-holding capacity

5. Clay soils drain slowly and hold nutrients well

6. Loam is a soil with roughly equal proportions of sand, silt, and clay

7. The ribbon test measures soil pH

8. A 2-inch ribbon in the ribbon test indicates a high clay content

9. Sandy soils warm up faster in spring than clay soils

10. Silty soils are prone to surface crusting and poor infiltration

11. Soil texture can be changed by adding amendments over time

12. The USDA soil texture triangle is used to classify soils

13. Clay soils are described as 'heavy' soils

14. Sandy soils are described as 'light' soils

15. Loam is generally considered the ideal soil texture for most crops

16. Adding sand to clay soil is the best way to improve drainage

17. Gritty feel indicates high sand content in soil

18. Smooth silky feel indicates high clay content in soil

19. The jar test separates soil particles by settling speed

20. Texas black clay soils are called Vertisols and shrink and crack when dry

Part B — Short Answer

1. Describe the three main soil particle sizes and their properties.

2. What is the ribbon test and how do you perform it?

3. What is the jar test and what does it reveal?

4. Why is clay soil difficult to work but good at holding nutrients?

5. Why do sandy soils need more frequent irrigation and fertilization?

6. What is loam and why is it considered ideal?

7. Why does adding sand to clay usually make things worse, not better?

8. Describe the water-holding capacity and drainage characteristics of clay vs sand.

9. What are Vertisols and where are they common in Texas?

10. How does soil texture affect root development?

Part C — Fill in the Blank

1. Sand particles range from to __________ mm in diameter.

2. Clay particles are smaller than mm.

3. The test involves making a rope of moist soil and measuring how long it extends before breaking.

4. Soil with roughly equal sand, silt, and clay that feels gritty but also somewhat sticky is called .

5. Clay soils are called soils because they are harder to till.

6. Sandy soils are called soils because they are easier to till.

7. The USDA soil classification tool using particle percentages is the texture .

8. Texas black clay soils that shrink and crack when dry are classified as .

9. In the jar test, settles first (within minutes), then silt, then clay on top.

10. Sandy soils have (high/low) cation exchange capacity because sand has little surface area.

Part D — Practical Exercises

Complete in the field. Check each off as you go.

1. Ribbon Test Practice: Collect soil from 5 different spots on your property. Wet each sample to plasticine consistency. Form a ribbon between thumb and forefinger. Measure ribbon length before breaking. Record clay estimate.

2. Jar Test: Half-fill a clear jar with soil from each of 3 locations. Add water to 2/3 full. Shake vigorously. Let settle for 24+ hours. Photograph and measure each layer. Calculate % sand, silt, clay.

3. Feel Test Sequence: Collect soil, add water until ribbon-able. Describe: gritty (sand), silky (silt), sticky/plastic (clay). Rate each property 1-5. This is how USDA field soil scientists work.

4. Drainage Test: Dig a 12-inch hole. Fill with water. Record time to drain. Do this in clay soil and sandy soil areas. Which drains faster? What does this mean for plant selection?

5. Amendment Effect: Add compost to a clay-heavy area and a sandy area. After one growing season, repeat the ribbon and jar tests. How has texture-related behavior changed? (Note: texture itself doesn't change, but structure does.)

0 / 40 answered correctly

Practice Exercises

  1. You squeeze moist soil and it forms a 2.5-inch ribbon that feels moderately sticky with no gritty feel. What texture class is this?
  2. A neighbor tells you to add sand to your clay garden bed to improve drainage. Why is this advice problematic?
  3. Why does clay hold far more nutrients per gram than sand, even though both are mineral particles?
  4. You have sandy soil in East Texas. List three specific management practices to improve it without changing its fundamental texture.
  5. After a rainstorm, your vegetable bed has a hard gray crust on the surface and seedlings can't push through. What texture is likely dominant and what should you do to prevent this?
  6. What creates aggregate structure in loam soil, and why does tillage destroy it?

Next Chapter → Soil Structure — Aggregates, Pores, and Tilth


Connections to Other Topics

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→ C03 Ch01: What is Soil — soil components overview

From: Connections to Other Topics

Image file: ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig10.png

Save image as ../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig10.png in this folder, then replace this block with:
<figure><img src="../../../images/s01-foundation/c03-soil-science/ch02/c03-soil-science_ch02_soil_texture_fig10.png" alt="→ C03 Ch01: What is Soil — soil components overview"></figure>

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