3. Soil Texture Determination through Feel Method.pdf

MARJORIE JEAN E. TAO
Agriculturist II
Soil Physics Section
Laboratory Services Division
BUREAU OF SOILS AND WATER MANAGEMENT
Soil Texture Determination
(Feel Method)
- refers to the proportion of sand, silt
and clay sized particles that make up
the mineral fraction of the soil
- influences almost every aspects of soil
use both agriculture and engineering
applications and even how natural
ecosystem functions
This PhotoThis Photo by Unknown Author is licensed under CC BY-SA
SOIL TEXTURE
Soil Separate
Particle Size
Grades
(Millimeters)
Very coarse sand 2.0 – 1.0
Coarse sand 1.0 – 0.5
Medium sand 0.5 – 0.25
Fine sand 0.25 – 0.10
Very fine sand 0.10 – 0.05
Silt 0.05 – 0.002
Clay Less than 0.002
SOIL TEXTURE
Sand
- Feels gritty
Silt
-feels like flour (dry)
-feels smooth (wet)
Clay
- hard and brittle (dry)
-feels sticky (wet)
SOIL TEXTURE
Coarse-textured soils
52-100% sand
Medium-textured soils
Even distribution of clay
and sand
Fine-textured soils
at least 35-40 % or more
clay
GUIDE TO SOIL TEXTURE
BY FEEL METHOD
GUIDE TO SOIL TEXTURE BY FEEL METHOD
3. Soil Texture Determination through Feel Method.pdf
3. Soil Texture Determination through Feel Method.pdf
3. Soil Texture Determination through Feel Method.pdf
3. Soil Texture Determination through Feel Method.pdf
3. Soil Texture Determination through Feel Method.pdf
3. Soil Texture Determination through Feel Method.pdf
3. Soil Texture Determination through Feel Method.pdf
Coarse-textured soils
-Low water holding capacity
-High water infiltration rates
-High potential for leaching
-Low nutrient retention
GUIDE TO SOIL TEXTURE
BY FEEL METHOD
Fine-textured soils
-Slower water infiltration rates
-Remains wet longer
-High nutrient retention
GUIDE TO SOIL TEXTURE
BY FEEL METHOD
Medium-textured soils
-Sufficient water infiltration
-Good water holding capacity and
nutrient retention
GUIDE TO SOIL TEXTURE
BY FEEL METHOD
• By feel and sight observation
o Sand – gritty
o Silt - smooth or silky
o Clay - smooth and exhibits stickiness and plasticity
FACTORS AFFECTING FEEL METHOD
FACTORS AFFECTING FEEL METHOD
• Composition of the soil
o Clay Mineralogy - montmorillonitic and kaolinitic clay
o Organic matter content - lowers plasticity
o Mica content - lubricating effect of platy minerals of silt
and sand
o Salt content - crystallization of salt
Modified from S.J. Thien. 1979. A flow diagram for teaching texture by feel analysis. Journal of
Agronomic Education. 8:54-55.
https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/edu/?cid=nrcs142p2_054311 date retrieved:
August 28, 2022
Moebius-Clune, B.N., D.J. Moebius-Clune, B.K. Gugino, O.J. Idowu, R.R. Schindelbeck, A.J.
Ristow, H.M. van Es, J.E. Thies, H.A. Shayler, M.B. McBride, K.S.M Kurtz, D.W. Wolfe, and G.S.
Abawi, 2016. Comprehensive Assessment of Soil Health – The Cornell Framework,Edition 3.2,
Cornell University, Geneva, NY.
USDA-NCS. 1987. Soil Mechanics Level I. Module 3 – USDA Textural Classification.
REFERENCES
Thank you for your attention!
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3. Soil Texture Determination through Feel Method.pdf

  • 1. MARJORIE JEAN E. TAO Agriculturist II Soil Physics Section Laboratory Services Division BUREAU OF SOILS AND WATER MANAGEMENT Soil Texture Determination (Feel Method)
  • 2. - refers to the proportion of sand, silt and clay sized particles that make up the mineral fraction of the soil - influences almost every aspects of soil use both agriculture and engineering applications and even how natural ecosystem functions This PhotoThis Photo by Unknown Author is licensed under CC BY-SA SOIL TEXTURE
  • 3. Soil Separate Particle Size Grades (Millimeters) Very coarse sand 2.0 – 1.0 Coarse sand 1.0 – 0.5 Medium sand 0.5 – 0.25 Fine sand 0.25 – 0.10 Very fine sand 0.10 – 0.05 Silt 0.05 – 0.002 Clay Less than 0.002 SOIL TEXTURE
  • 4. Sand - Feels gritty Silt -feels like flour (dry) -feels smooth (wet) Clay - hard and brittle (dry) -feels sticky (wet) SOIL TEXTURE
  • 5. Coarse-textured soils 52-100% sand Medium-textured soils Even distribution of clay and sand Fine-textured soils at least 35-40 % or more clay GUIDE TO SOIL TEXTURE BY FEEL METHOD
  • 6. GUIDE TO SOIL TEXTURE BY FEEL METHOD
  • 14. Coarse-textured soils -Low water holding capacity -High water infiltration rates -High potential for leaching -Low nutrient retention GUIDE TO SOIL TEXTURE BY FEEL METHOD
  • 15. Fine-textured soils -Slower water infiltration rates -Remains wet longer -High nutrient retention GUIDE TO SOIL TEXTURE BY FEEL METHOD
  • 16. Medium-textured soils -Sufficient water infiltration -Good water holding capacity and nutrient retention GUIDE TO SOIL TEXTURE BY FEEL METHOD
  • 17. • By feel and sight observation o Sand – gritty o Silt - smooth or silky o Clay - smooth and exhibits stickiness and plasticity FACTORS AFFECTING FEEL METHOD
  • 18. FACTORS AFFECTING FEEL METHOD • Composition of the soil o Clay Mineralogy - montmorillonitic and kaolinitic clay o Organic matter content - lowers plasticity o Mica content - lubricating effect of platy minerals of silt and sand o Salt content - crystallization of salt
  • 19. Modified from S.J. Thien. 1979. A flow diagram for teaching texture by feel analysis. Journal of Agronomic Education. 8:54-55. https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/edu/?cid=nrcs142p2_054311 date retrieved: August 28, 2022 Moebius-Clune, B.N., D.J. Moebius-Clune, B.K. Gugino, O.J. Idowu, R.R. Schindelbeck, A.J. Ristow, H.M. van Es, J.E. Thies, H.A. Shayler, M.B. McBride, K.S.M Kurtz, D.W. Wolfe, and G.S. Abawi, 2016. Comprehensive Assessment of Soil Health – The Cornell Framework,Edition 3.2, Cornell University, Geneva, NY. USDA-NCS. 1987. Soil Mechanics Level I. Module 3 – USDA Textural Classification. REFERENCES
  • 20. Thank you for your attention!