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SOIL! SOIL: Particles of minerals, organic matter (plant and animal), water, and air; that is found on most surfaces of the land. It takes 100+ years to.

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Presentation on theme: "SOIL! SOIL: Particles of minerals, organic matter (plant and animal), water, and air; that is found on most surfaces of the land. It takes 100+ years to."— Presentation transcript:

1 SOIL! SOIL: Particles of minerals, organic matter (plant and animal), water, and air; that is found on most surfaces of the land. It takes 100+ years to form 1-inch of topsoil

2 Soil Basics

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4 Why do we study soils? Agriculture Engineering Construction
Conservation Exploration/Mining Natural History Biodiversity

5 Basic Soil Facts An average soil sample is made up of minerals, water, air, and organic matter. A renewable resource- forms at rate of ~1 in in a 100 years Plant roots loosen the soil, allowing oxygen to penetrate. Plant Roots also hold soil together to prevent erosion.

6 Fertilizers Make plants grow faster- increase crop yields.
Key Macronutrients: N,P,K Too much- causes soil acidification= stunts growth and/or kills plant. Results in crop reduction.

7 Soil Horizons Weathered rock mixed with organic material (humus), mineral nutrients, microorganisms, water and air form soil. Soil horizons O horizon: organic material/surface litter “HUMUS” A horizon:”topsoil” layer; most productive layer; Some HUMUS - B horizon: subsoil; minerals present here C horizon/ parent material: lower subsoil and Bedrock

8 Why Humus is Important? How humus improves soil conditions:
Provides nutrients/fertility for plants and soil organisms Helps topsoil hold water (water-holding capacity) Improves habitats for soil organisms Improves buffering capacity, which stabilizes pH Prevents erosion Improves porosity

9 Soil Textures Soils have varying amounts of:
Clay – finest particles of rocks and minerals Silt – fine particles of rock Sand – medium-sized particles Relative amounts of these materials determine soil texture

10 Chemical Properties of Soil
Cation Exchange Capacity Cation: + charged mineral ions. Cation exchange capacity (CEC)- nutrient holding capacity. It’s a function of the type and amount of CLAY particles present. Clay and Organic Matter (HUMUS) have HIGH CEC Soils with HIGH CEC = HIGH PRODUCTIVITY

11 High CEC soil retain the fertilizer and pesticides; Leaching occurs with low CEC (sandy soils)

12 Three Key test to KNOW for my TEST and APES TEST
PHYSICAL TESTS Soil texture by measurement- use soil triangle. Soil by texture- ribbon test. Color of soil CHEMICAL TESTS Nitrogen level 2.Phosphorus level 3. pH

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14 Soil texture by measurement

15 Soil Triangle Provides a percent (%) composition of sediments that compose a soil Loam soil has EQUAL parts of Sand, Silt, Clay. It’s ideal for most plants.

16 Soil Triangle Example: 50% sand 20% clay 30% silt
The percentage of sediments in the soil triangle must equal 100%

17 Soil Texture Determines porosity, permeability and structure of soil
Porosity: space between soil particles. Depends on the soil texture. Permeability: rate at which water and air move from upper to lower soil layers. Clay has a low permeability. Structure: way in which soil particles are organized and clumped together pH: determines plants’ ability to take up nutrients from soil

18 Soil Lab Part II- DAY 2

19 Using the Soil Triangle
You will record your measurements for each layer of sediment- Amt clay, silt, etc. Recall clay will be at the top, followed by silt, then sand. Calculate the %: Volume of X/ 25 x 100 Ex: silt= 15/25 x 100= 60% Repeat with clay and sand.

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21 Soil Triangle Example: 50% sand 20% clay 30% silt
The percentage of sediments in the soil triangle must equal 100%

22 Animated Soil Triangle

23 What do the test tell you about your soil?
Did the ribbon test match your soil by measurement results? If not, why? Consider the texture, porosity & permeability? CEC? Recall combo of clay and humus= High CEC and High productivity Level of nutrients? What would you need to do to this soil to improve it?


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