soil physics
DESCRIPTION
Soil physics. Magnus Persson. What is soil?. You have 3 minutes to develop a group consensus definition. What is soil?. What’s the difference between soil and dirt? Dirt is what you find under your fingernails. Soil is what you find under your feet. - PowerPoint PPT PresentationTRANSCRIPT
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Soil physics
Magnus Persson
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What is soil?
You have 3 minutes to develop a group consensus definition
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What is soil?
What’s the difference between soil and dirt? Dirt is what you find under your fingernails. Soil is what you find under your feet.
Soil is a complex mixture of organic and inorganic compounds
Definition, Soil Science Glossary, SSSA
(i) The unconsolidated mineral or organic material on the immediate surface of the earth that serves as a natural medium for the growth of land plants.
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Why soil science?
Geology, the soil material Agriculture, soil-plant interaction Engineering, soil mechanics Hydrology, soil-water interaction
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Soil science disciplines
Pedology (the study of soils in their natural environment)
Pedogenesis (how soils are created) soil morphology (attributes of the soil within the
various soil horizons) soil classification (taxonomy)
Soil fertility Hydrogeology Soil physics Soil chemistry Soil biology
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Soil taxonomyO1 Undecomposed litterO Horizon
Organic PlantResidues O2 Partly decomposed debris
A1 Zone of humus accumulation
A2 Zone of strongest leaching
A HorizonZone ofeluviaiton(leaching) A3 Transition to B horizon
B1 Transition to A horizon
B2 Zone of strongest depositionSol
um, T
rue
Soi
l
B HorizonZone ofilluviation(deposition) B3 Transition to C horizonR
egol
ith,
Wea
ther
ed M
ater
ial
C HorizonParent Material
C Unconsolidated rock
R Layer - Bedrock R Consolidated rock
A soil horizon is a specific layer in the soil parallel to the soil surface and possesses physical characteristics which differ from the layers above and beneath.
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Soil taxonomy
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Soil taxonomy
Food and Agriculture Organization of the United Nations (FAO)
United States Department of Agriculture (USDA)
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The Hydrological cycle
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Unsaturated and saturated zones
The unsaturated zone lies between the soil surface and groundwater
table The soil pores are not completely filled with
water Mainly vertical water movement
The saturated zone All pores are completely filled with water Exists in aquifers Mainly horizontal water movement
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Soil properties
Soil properties depends on Formation processes Parent material Climate/time Texture Structure
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Particle sizeThe size of the mineral soil particles determines the soil texture
Is determined using sieving and sedimentation
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Soil textural classes
Soil textural classes according to USDA
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Soil structureDescribes how individual soil granules clump or bind together and aggregate and arrangement of soil pores between them.
The five major classes of structure seen in soils are; platy, prismatic, columnar, granular, and blocky. There are also structureless soils.
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Soil structure
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Specific surface
The specific surface is the total surface area per unit of mass or bulk volume. Generally it increases with decreasing particle size. It also depends on the particle shapeSoil type Specific surface (m2
g-1)
Sand <10
Sandy loam 5-20
Clay >25
Organic matter 500-800
Bentonite 100-200
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Soil water
Soils can contain water. Water is retained in the soil by capillary or adsorptive forces
O--
H+
H+Remember that the water molecule is a dipole
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Definition
A soil sample of volume V The same sample with each phase ‘packed’ together. V denotes volume and M mass.
Vair, Mair
Vwater, Mwater
Vsolid, Msolid
b = Msolid/V (bulk density) 1.2-1.7 g/cm3
s = Msolid/Vsolid (particle density) 2.65 g/cm3
v = Vwater/V (volumetric water content)
g = Mwater/Msolid (gravimetric water content)
n = (Vwater + Vair)/V (porosity) 0.2 – 0.7 m3/m3
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Exercise
How do you convert g to v?
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Water content With all pores completely filled with
water, you have saturated conditions θs. If you let a saturated sample drain until
drainage stops you have field capacity θfc. When there is so little water that a plant
can not suck any water you have the wilting point θwp
Effective porosity θs- θfc Plant available water θfc- θwp Soil moisture deficit (θfc- θwp)*root depth
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Water content
Some examples of field capacity and wilting points for different soil textures
Textural class Wilting point (m3/m3)
Field capacity (m3/m3)
Clay 0.25 0.40
Silt 0.15 0.35
Loam 0.10 0.30
Sand 0.05 0.10
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Surface tension
2·R·cos R
2·r
P1
P2
z
Due to surface tension water can be held at negative pressure in capillary tubes. (P1<P2 = Patm)
The smaller the diameter of the tube, the higher capillary rise.
An useful analogy is that the soil can be considered to act like a bundle of capillary tubes with different diameters (representing the range of pore sizes)
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pF curveThe soil moisture potential, or soil water suction, is sometimes given in pF = log(-pressure in cm H2O).
The water retention curve, soil moisture characteristic, or pF curve, is the relationship between the water content, θ, and the soil water potential, ψ. This curve is characteristic for different types of soil
(1 bar = 100 kPa = 1000 cm H2O)
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pF curve
mnrs
r ))(1()(
Several different models describing the pF curves exist, one of the most commonly used was developed by van Genuchten in 1980
where θs and θr are the saturated and residual water content, respectively, α, n, and m are empirical soil specific parameters
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HysteresisWetting and drying curves are different
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Soil water potential
The total potential consists of the moisture potential (synonyms; pore water tension, soil water suction) and the elevation potential, z.
Normally the groundwater surface is used as a reference level (z = 0)
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Water movement
Water movement is driven by total potential gradients
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Pedotransfer functionA pedotransfer function is a predictive function of certain soil properties from other more available, easily, routinely, or cheaply measured properties.
For example, the ROSETTA model estimates the soil water retention curve from soil texture.
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Literature and links
http://www.ars.usda.gov/Services/docs.htm?docid=15992 (models for download)
https://www.soils.org/sssagloss/ (glossary of soil science terms)
http://www.fao.org/docrep/W8594E/w8594e00.HTM (soil taxonomy FAO)
http://soils.usda.gov/technical/classification/taxonomy/ (soil taxonomy USDA)
http://wwwbrr.cr.usgs.gov/projects/GW_Unsat/Unsat_Zone_Book/index.html (online textbook)