LO 3.3 - Texture Flashcards

- Definition of texture - Effect of texture on growing characteristics

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1
Q

Question

The particle sizes in different mineral soils influence the physical characteristics of soils.

How are the mineral particles in soil grouped?

Soil Texture

A

The mineral particles in soils can be grouped into classes by size.

  • Sand
  • Silt
  • Clay

Soil Texture

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2
Q

Question

Soil texture particle sizes are measured with an international classification.
What sizes are used for Pebbles, Sand, Silt and Clay?

Soil Texture

A

Slightly different systems are used in the UK and the US.

This is the international classification.

Soil Texture

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3
Q

Question

Soil texture is the term used to describe the proportion of different particle sizes (sands, silts and clays) in a soil.

How big in mm, is the largest particle size considered?

Soil Texture

A

The largest is 2mm
Any particles over 2 mm in diameter are stones/pebbles and are not considered to be part of the ‘fine earth’ component of the soil.

Soil Texture

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4
Q

Question

Laboratory assessment of soil texture.

What are 4 things you need to do?

Soil Texture

A
  • Remove the stones/pebbles with a 2 mm sieve
  • Remove the organic matter.
  • Put a measured amount in a litre cylinder with a dispersant solution.
  • Shake it.

The particles will settle according to size – sand first, then silt, then clay.

Soil Texture

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5
Q

Question

What is a Hydrometer?

Soil Texture

A

A hydrometer is an instrument for measuring the density of liquids.

Soil Texture

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6
Q

Question

How do you measure the density of soil using a Hydrometer?

Soil Texture

A
  • Use a hydrometer to measure the density of the liquid at 40 seconds and 2 hours.
  • This allows us to work out what percentage of the original sample was in each particle size group
  • We can plot those % figures on a textural triangle to determine the textural class of the soil.

Soil Texture

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7
Q

Question

Using this textural triangle, what are the textural classes of the following soils?

  1. 15% sand, 70% silt, 15% clay.
  2. 65% sand, 20% silt, 15% clay.
  3. 15% sand, 15% silt, 70% clay.
  4. 40% sand, 40% silt, 20% clay.
  5. 33% sand, 33% silt, 33% clay

Soil Texture

A

Textural class of the soils using the textural triangle.
1. Silt Loam
2. Sandy Loam
3. Clay
4. Loam
5. Clay Loam

Soil Texture

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8
Q

Question

What’s so important about Soil Texture?

Soil Texture

A

Soil texture is important because it affects:
* Drainage and water holding.
* Soil temperature.
* Fertility & leaching.
* Workability.
* Soil structure.

Soil Texture

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9
Q

Question

Describe what drainage and water holding is in Soil Texture?

Soil Texture

A
  • Sand particles are much bigger than clay particles.
  • This means that the gaps between particles are much larger in sand than in clay.
  • Water moves more easily through soils that have large pores, so sandy soils are free draining and clay soils are poorly drained.

Soil Texture

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10
Q

Question

How does texture affect soil temperature?

Soil Texture

A

Clay soils, which tend to be wetter, are slower to warm up in spring than lighter, sandy soils.

Soil Texture

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11
Q

Question

How does Soil texture affect fertility/leaching?

Soil Texture

A
  • Clay particles are negatively charged so they attract positively charged ions in the soil such as ammonium (NH4+), magnesium (Mg++), potassium (K+) and calcium (Ca++).
  • Note: the elements are ‘adsorbed’ by the clay particles.
  • Relatively large sand particles have no charge.

Soil Texture

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12
Q

Question

What is meant by Workability in Soil texture?

Soil Texture

A

Clay soils are often referred to as ‘heavy’ and sandy soils as ‘light’.
* This refers to the power required to cultivate them, not to the actual weight of the soil.
* Clay soils are naturally sticky and tend to form clods, so they are more difficult to cultivate than sandy soils which are not sticky.

Soil Texture

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