Lecture 1-Soil Mass Volume-Relationships

Lecture 1-Soil Mass - LECTURE 1 SOIL AS A POROUS MEDIUM Soils as a porous medium Solids Liquids and Gaseous Phases The soil as a porous medium

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LECTURE 1 SOIL AS A POROUS MEDIUM
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Soils as a porous medium
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Solids, Liquids, and Gaseous Phases The soil as a porous medium consists of three phases that are dynamic and interrelated in composition. A mineral soil can consist of the following composition : a) Solid phase constitutes the soil matrix (clay minerals, organic matter) 50% b) Liquid phase, consists of soil water and dissolved substances (soil solution) 25%
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The Gaseous Phase The gaseous phase or soil atmosphere Soil variables are bulk density, water content, and gaseous content. The soil matrix controls the form, quantity,and distribution of the liquid and gaseous phases . N 2 % O 2 % CO 2 % Air 79 20.97 0.03 Soil 79.20 20.60 0.20
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5 Volume Fractions of the 3 phases a) Total porosity f = V f /V t = [V a +V w ]/V t b) Air filled porosity f a = V a /V t c) Water filled porosity θ v = V w /V t d) Water saturation s = V w /V f Therefore total porosity is equal to : f = f a + θ v Volume fraction of solids equals: 1 – f = [ ρ b / ρ s ] = V s /V t
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6 Mass, Volume, Relationships Relationship between: Porosity Bulk Density and Particle Density
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This note was uploaded on 10/26/2011 for the course SOS 6932 taught by Professor Kizza during the Summer '11 term at University of Florida.

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Lecture 1-Soil Mass - LECTURE 1 SOIL AS A POROUS MEDIUM Soils as a porous medium Solids Liquids and Gaseous Phases The soil as a porous medium

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