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Introduction to Soils. By Rick Bandy, Resource Soil Scientist Natural Resources Conservation Service. Soil Forming Factors. Parent Material Climate Living Organisms Topography Time. Physical Properties of Soils. Soil Solids 1. Mineral Soil 2. Organic Matter Soil Pore Space 1. Air
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Introduction to Soils By Rick Bandy, Resource Soil Scientist Natural Resources Conservation Service
Soil Forming Factors • Parent Material • Climate • Living Organisms • Topography • Time
Physical Properties of Soils • Soil Solids • 1. Mineral Soil • 2. Organic Matter • Soil Pore Space • 1. Air • 2. Water
Organic Matter <5% <10% 33-50% 33-50%
Soil Minerals • Sand • Silt • Clay
Soil Minerals • Sand • - 2.0 to 0.05 mm diameter • - Individual particles visible to the eye • - Rounded or irregular shape • - Gives texture gritty feel • - Influences drainage and air movement
Soil Minerals • Silt • - 0.05 to .002 mm diameter • - Magnify 10 to 100 times to see particles • - Irregular shape • - Gives texture soft, slippery, floury feel • - Largely influences water holding capacity
Soil Minerals • Clay • - Less than .002 mm diameter • - Magnify 2,000 times to see particles • - Gives texture sticky, greasy feel • - Largely influences fertility, permeability, shrinking and swelling
Soil Textural Triangle A. Miller
Bulk Density of Mineral Soils • In the field one cubic centimeter of a • certain soil appears as below • If all the solids were compressed to • the bottom, the cube would look • like this: 1/2 PORE SPACES • 1.33 grams • SOILDS AND PORE SPACES • 1.33 grams • 1/2 SOLIDS • To calculate solid particle density: • Volume = 0.5 cc Weight = 1.33 grams • Solid particle density = Weight of solids/Volume of solids • Therefore • Solid particle density = 1.33/0.5 = 2.66g/cc • To calculate bulk density of the soil: • Volume = 1 cubic centimeter Weight = 1.33 grams • Bulk Density = Weight of soil/Volume of soil • Therefore • Bulk Density = 1.33/1 = 1.33 g/cc
Forms of water that are held in soils • Capillary Water • Soil Particle • Adsorbed Water
SOIL WATER DIAGRAM • AIR SPACES
Water Holding Capacity of Soils • SATURATION • FIELD CAPACITY • WILTING POINT • Solid Space • Pore Space • SATURATED SOIL • 40 g • 100 g • FIELD CAPACITY • 20 g • 100 g • Air • Air • WILTING POINT • 100 g • 10 g
Soil Moisture Characteristics of Individual Soil Particles • 0 Atm. • 1/3 Atm. • Soil Particle • 15 Atm 31 Atm • Available • Water • Capacity • (AWC) Gravitational Water • Bound Water Permanent Wilting Point Field Capacity Saturated Soil
SOIL MOISTURE CHARACTERISTICS AND TEXTURE FIELD CAPACITY AVAILABLE WATER UNAVAILABLE WATER WILTING POINT
AWC ADJUSTED FOR ROCKS AND SALT CONTENT IN SOILS 30 .22 .02 25 .20 .04 .18 .06 20 .16 70 .08 60 50 15 .14 40 .10 30 12 20 .12 .12 10 8 4 0 Percent Rock Fragments 0 .10 .14 .08 .16 Salt Content (EC) .06 .18 .04 .20 .02 .22 0
WATER TABLE CapillaryFringe Water Table
STRATIFIED SOILS Clay Sand
RESTRICTIVE LAYER Sandy Loam Clay
SOIL REACTION The degree of acidity or alkalinity of a soil, usually expressed as a pH value or by terms ranging from extremely acid to very strongly alkaline
Ranges found in soils pH scale Bleach 12 11 10 9 8 7 6 5 4 3 2 1 0 Milk of Magnesia Sodic soils Antacid tablets Calcareous soils Sea Water Pure water Humid region soils Natural rain Forest soils Beer, coffee Acid sulfate soils Vinegar Lemon Juice Battery acid
AFFECTS OF pH ON SOILS • Plant nutrient availability • Microbial populations • Types of Vegetation • Movement of nutrients and pollutants
Where to get soil information • Each County has a published soil survey that provides detailed soil maps. • The local NRCS office has copies of the published soil survey for that county. • Web Soil Survey is a web based tool where soil maps can be generated on-line. http://soils.usda.gov/survey/
Soil Forming Factors • Parent Material • Climate • Living Organisms • Topography • Time