Presentation on theme: "Soils Plant Material Maintenance. Soil Soil is the top layer of the Earth’s crust. Millions of years to make Being lost at a rate of 5.2 tons/acre/year."— Presentation transcript:
In undisturbed soils organic matter helps bind soil particles into larger aggregates.
Soil Horizons and the Soil Profile: O – Thin layer of decomposing organic matter. A – Primarily composed of inorganic materials (sands, silts, and clays) it is also normally rich in organic matter. This horizon has a characteristic dark color. E – Not present in all soils and not pictured in the illustration to the left. B – Zone of accumulation where materials that have leached from the surface mix with soil particles from the lower parent material. C – Composed of partially weathered parent material.
Water-holding Capacity Soils with a large percentage of micropores have a high water-holding capacity - clay Soils with a larger percentage of macropores over micropores have a lower water-holding capacity - sand
Gravitational Water Water that drains from the macropores under the force of gravity after a rain/irrigation event.
Field Capacity A soil is said to be at field capacity immediately after the gravitational water has drained away. Water that remains held in the micropores is called capillary water. available unavailable
Permanent Wilting Point When available water is depleted, and no additional water is added, plants may reach the permanent wilting point.
Soil Texture Determined by the percentages of sand, silt, and clay a soil contains. Textural triangle.
Loam Soils Ideal balance of 3 particles Results in high fertility and good water retention Drains well Desired for gardening
Organic Matter (OM) Generally only present in very small quantities; 5% or less. Most OM in the form of humus: stable, decomposed plant and animal life. In sandy soils - increases water and nutrient holding capacity. In clay soils - improves drainage, air movement, and helps form aggregates.
Cation-Exchange Capacity Capacity of a soil to attract and hold nutrients on the surface of soil particles. Soil and organic matter have negative charges. Nutrients have positive charge, so are attracted to the negative charges. Clay soils and soils high in organic matter have higher CEC rates.
pH Scale Measures the acidity/alkalinity. pH affects the nutrient availability in the soil. Ranges from 0 to 14. pH of 7 is neutral. Less than 7 is acidic. More than 7 is alkaline. pH of 6 is 10 times more acidic than 7 pH. pH of 5 is 100 times more acidic than 7 pH.
Nutrient availability and pH At certain pH levels, some micronutrients become unavailable to the plant. They become chemically bound to the soil particles. pH level of 6.5-7.0 is the optimal range for most micronutrients. Iron is commonly deficient due to high pH soil.
Adjusting pH levels Low pH soils (acidic) Add lime High pH soils (alkaline) Very difficult to lower pH on large scale Add sulfur Add organic amendments Oak leaves, sphagnum moss, pine needles
Mychorrhizal Fungi A symbiotic relationship between plant roots and fungi. The fungi help roots absorb water and nutrients. The roots provide the fungi with food (sugar). Most plants growing in “undisturbed” soils have mychorrhizal fungi growing in association with their roots.