Soil Structure - Soil Physics - Lecture Slides, Slides of Soil Physics

Soil physics is the study of soil physical properties and processes. It is applied to management and prediction under natural and managed ecosystems. (Wikipedia). Keywords in this lecture are: Soil Structure, Soil Strength, Classificaiton of Structure Granular, Blocky, Platy, Prismatic, Columnar, Drivers of Structure, Fragmentation Systems, Sphere Packing

Typology: Slides

2012/2013

Uploaded on 12/31/2013

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Outline
Announcements
Where were we?
Soil Structure (particles)
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Outline

  • Announcements
  • Where were we?
  • Soil Structure (particles)

Where were we?

Soil strength

Soil structure

Specifically, most soil structure exists because of cohesiondocsity.com

Classification of structure:

Platy Blocky Crumb Granular Columnar Prismatic Angular Subangular …

Granular

Classification of structure: Blocky

Classification of structure: Prismatic

Classification of structure: Columnar

Figure & Ground

Why soil structure (particles)?

Particles & Pores

Figure and Ground

Dual networks Triangular & honeycomb

Dual networks Voronoi & Delaunay

Structure implies not random

This might be a preferential arrangement

Based on chance, you shouldn’t find lots of this: Clay should hang out with the other particles, too.

Why do clay quasicrystals

(and other non-random structures)

form?

Drivers of structure (particles)

Gravity: if it can’t stand, it will fall Stability: if it’s not stable, it will soon change

Climate, life, parent material

Water, heat, roots: different ways energy disturbs the soil, shaking it into a more stable configuration

Fragmentation systems

When an aggregate is dropped, there is usually a power-law distribution of pieces:

d f

N r r

This is characteristic of fragmentation systems. It implies that larger pieces are easier to break than smaller pieces.

r

N

( r

log ( r )

log

[ N

( r

)]

slope = – df

Causes / consequences of hierarchical structure

  • Small structures tend to be denser than large structures
  • Small structures are more stable than large structures
  • Bonds within and between small structures are stronger than bonds within and between large structures
  • Spaces (pores) between large structures are bigger than those between small structures

In soil, these structures are called aggregates

Aggregate properties

  • Size, shape, distribution
  • Strength versus physical forces
  • Strength versus chemical forces

Fragmentation Dry sieving Rupture

Wet sieving

Granular structure

Eventually, physicists try to treat everything as spheres…