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Soils NR 200

Soils NR 200. Unit 1. The Soils Around Us. What is soil?. Dictionary – The unconsolidated material that occupies the earth’s surface and supports plant life. Or perhaps: The link between the living and non-living. (The non-living supporting the living).

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Soils NR 200

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  1. Soils NR 200

  2. Unit 1 The Soils Around Us

  3. What is soil? • Dictionary – The unconsolidated material that occupies the earth’s surface and supports plant life. • Or perhaps: The link between the living and non-living. (The non-living supporting the living)

  4. I. Functions of Soil in our Human World A. Medium for plant growth B. Important component of the hydrological system C. Mother nature’s way of recycling organisms D. A sphere for living organisms ie macro and micro organisms E. Supporting foundations of our human made structures

  5. II. Four major components of soil.

  6. Minerals: 45% • Rocks that are broken down into particles that we call soil • Source of 13 of the 16 nutrients needed for plant growth.

  7. Air 20-30% 1) the roots need O2 for respiration 2) organisms need O2as well

  8. Soil Solution:water with dissolved minerals held in the soil particles.20-30%

  9. Organic matter 1) From once living organisms 2) Decaying and making their minerals available again 3) Improves water holding capacity 4) Humus is the longer lasting material that is responsible for this water holding ability, colloidal.

  10. III. Plant Requirements for Soil orWhat the soil needs to provide the plant to allow it to grow successfully

  11. A. Anchorage 1)Needed to allow the plant to have as many leaves positioned to accept sunlight 2)Keep plant in place to receive water and minerals

  12. B. Oxygen 1) Needed to allow for respiration 2) Needed for microorganisms to flourish

  13. C. Water 1)Almost all the water the plants need comes from the soil 2)Also important for the microbial action in the soil 3) Important for nutrient absorption

  14. Water continued: 4) pH: the degree of alkalinity or acidity of the soil solution or soil pH range - 1 – 7 – 14 a logarithmic relationship

  15. Soil pH is simply the measurement of the H+ ion

  16. D. Temperature moderation 1)The ability of the soil to insulate itself from the extreme hot and cold of the air above it. 2) Allows the roots to grow and an environment favorable to microorganisms

  17. E. Nutrients: 16 essential for plant growth 1)Only C,H and O are taken in by the plant from the atmosphere the other 13 are from the soil.N,P,K, Ca, Mg, S, Fe, Mn, Zn, Cu, B, Mo, and Cl? A few to watch Ni, Co, Na and Si? 2)Root hairs are the plant structure responsible for bring in the nutrients and water.

  18. 3) The elements must be brought into the plant via ionic solution that is, ions dissolved in solution. These ions go into solution from the colloids in the soil. Pg 25

  19. 3) The plant obtains these minerals by: a)Root interception -that is the root grows into a new area and captures the ionic solution. b) Mass flow – soil water with ions moves into contact with the root. c) Diffusion – ions move from areas of higher concentrations to areas of lower concentrations ie around roots.

  20. F. Free From Harmful Organisms

  21. IV. Soil Profile: Cross Section of the Soil Observed Vertically

  22. O- Organic layer i - undecomposed organic material a – organic material highly decomposed

  23. A- Topsoil:The Most Productive Soil 1) Best for nutrient holding, water capacity, micro-organisms 2) The most important soil profile for plant life 3) p – plowed or other cultivated disturbance (man made)

  24. E – An area where the greatest eluvation (removal of clay, iron and OM) occurs, resistant materials such as quartz, sand and silts remain usually light in color.

  25. B – Sub Soil or Zone of Accumulation, Illuviation - Usual Location of Hardpan m - cemented zone usually silicates or calcium g - strong gleying

  26. C – Parent material but broken down but not subject to the soil forming properties as the above solum (A&B) and not massive in structure as R R- Rock

  27. Soil Profile

  28. V. Soil texture isthe amount of sand, silt and clay in the soil. Sand: 2 - .05 mm Silt: .05 - .002 mm Clays: less than .002 mm

  29. VI. Soil structure is ……….the way these smaller aggregates form larger particles.

  30. Soil is the interaction of the lithosphere (rock), Atmosphere, Hydrosphere and the Biosphere (living organisms)

  31. With proper management and care our soils can produce a healthy bountiful harvest

  32. Uses of Soil 1) Agriculture 2) Non-Agriculture a) Recreation b) Foundations c) Waste disposal d) building materials 3) Land use of the future????

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