1 / 38

HOMEWORK: BRING SOME SOIL FROM YOUR HOME.

HOMEWORK: BRING SOME SOIL FROM YOUR HOME. CHAPTER 5.2 SOIL. Characteristics of Soil Soil Composition Soil Texture Soil Structure. What is Soil?. Regolith = small pieces of weathered rock. MOON. EARTH. MARS. Soil Composition = what it’s made of. Soil Composition

dinh
Télécharger la présentation

HOMEWORK: BRING SOME SOIL FROM YOUR HOME.

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. HOMEWORK: BRING SOME SOIL FROM YOUR HOME.

  2. CHAPTER 5.2 SOIL • Characteristics of Soil • Soil Composition • Soil Texture • Soil Structure

  3. What is Soil? Regolith = small pieces of weathered rock MOON EARTH MARS

  4. Soil Composition = what it’s made of

  5. Soil Composition Different compositions of soils: HIGH % Organic Matter LOW % Organic Matter

  6. Soil Composition Different compositions of soils: HIGH % Air & Water LOW % Air & Water

  7. Soil Texture = proportions of different particle sizes • U.S. Dept of Agriculture – categories based on amounts of clay, silt and sand. • Soil-Texture Diagram (pg 134 Figure 11) • Loam has equal parts clay, silt and sand. • Loam is best for plant growth.

  8. Soil-Texture Diagram 60% Clay; 10% Silt; 30% Sand 0 100 90 10 20 80 70 30 Clay 60 40 % Silt % Clay Silty Clay 50 50 Sandy Clay 40 60 Silty Clay Loam Clay Loam Sandy Clay Loam 70 30 20 80 Silty Loam Sandy Loam Silt Loamy Sand 90 10 Sand 0 100 % Sand 100 90 80 70 60 50 40 30 20 10 0

  9. Soil Structure To clump or not to clump.

  10. Soil Formation Parent Material = source of minerals in soil. Time = how long it took to form the soil. Climate = did it form in dry or wet areas, under hot or cold temperatures, etc. Organisms = what types of organisms are living or dead in the soil. Slope = the angle of the land on which the soil forms.

  11. Parent Material Who’s the mama? Pg. 135 Figure 12 • Residual soil = forms on bedrock • formed on top of the parent material • Transported soil = forms unconsolidated soil • moved from parent material to another location.

  12. Parent Material How did mama affect it? • Affects rate of weathering and rate of soil formation • Unconsolidated deposits are already weathered some, so they provide more surface area for chemical weathering. • Affects the soil’s fertility • More plant material can grow – more organic matter – better fertility.

  13. Time How long did it take to form? • The longer it takes to form, the thicker it becomes. • As time passes, weathering can reduce the influence of the parent material.

  14. Climate How did and does “neighborhood” affect soils? • Has greatest affect on soil formation. • Temperature changes affect rate, depth, and type of weathering. • Example: hot, wet climate produces a thick layer of chemically weathered soil. • Example: cold, dry climate produces a thin layer of chemical weathered soil.

  15. Climate How did and does “neighborhood” affect soils? • Precipitation influences soil fertility. • Climate affects what types and how many animals and plants can live on the soil. • Climate can cause similar soils to be produced from different parent materials .

  16. Organisms How does the “family” affect soil? • Some soils named based on plants living in them. • Prairie soil, tundra soil, forest soil, etc. • Plants are main source of organic matter. • Protozoans decompose organic matter in soil. • Burrowing animals stir, pack and move soil.

  17. Slope Soils on the edge? • Slope varies greatly from location to location. • The steeper the slope, the faster the erosion and the less water can soak in. • Steep slopes have thin layers of soils or none at all. • Flat slopes have thick layers of soils.

  18. Slope Soils on the edge? • The direction a slope faces can affect soils. • South-facing slopes receive more sunlight so are warmer and dryer. • North-facing slopes receive less sunlight so are colder and wetter. • All of these factors work together to affect the formation of soils.

  19. Soil Formation – Summary

  20. SOIL PROFILES = shows soil layers and composition of a section of earth. • A Horizon • “topsoil” • loose, partly decayed organic matter • mineral matter mixed with organic matter • insects, fungi, worms, microorganisms

  21. SOIL PROFILES = shows soil layers and composition of a section of earth. • B Horizon • “subsoil” • fine clay washed out of Horizon A • sometimes packed into “hardpan” soil • lower limit of plant roots and burrowing animals.

  22. SOIL PROFILES = shows soil layers and composition of a section of earth. • C Horizon • partially weathered parent material • still resembles the parent material

  23. SOIL PROFILES = shows soil layers and composition of a section of earth. • Rock • parent material • unweathered

  24. SOIL TYPES PEDAL Three common types of soil: PEDOCAL FER LATERITE

  25. SOIL TYPES: Pedalfer • Temperate areas receiving > 63 cm/yr • Rutherford County, NC • B Horizon has lots of iron oxide and aluminum clay. • Red or brown color

  26. SOIL TYPES: Pedocal • Areas with grasses and brush vegetation. • Western USA • B Horizon has lots of iron oxide and aluminum clay. • Red or brown color

  27. SOIL TYPES: Laterite • Hot, wet tropical areas. • Deeper than other soils. • When dry, becomes very hard and almost waterproof. • Used in brick-making. Pg 139 Fig 15 • Red or orange color

  28. SOIL TYPES: Laterite (cont.) • Makes up much of the soil in rainforests. • Plants decompose so rapidly in the rainforest there is no organic matter in laterite. • Not fertile.

  29. SOIL TYPES: Laterite (cont.)

  30. SOIL EROSION How WATER erodes soil… IMPACT erosion is a physical effect of water on soil. When falling water hits soil it creates a tiny explosion that tosses soil into the air and displaces it.

  31. SOIL EROSION How WATER erodes soil… This is an erosion bed. It is used to test the affects of running water on different types of soil. Here is the bed BEFORE the water is released. FLOWING water picks up particles of soil and carries them with it. This results in a deposition of soil from its original location to another location downstream. Here is the bed AFTER the water is released.

  32. SOIL EROSION Rates of erosion… • In the past soil erodes more slowly than it does today because more land was covered by plants.

  33. SOIL EROSION Rates of erosion… • Human activities that remove natural vegetation have greatly accelerated erosion.

  34. SOIL EROSION Rates of erosion… • Before humans, rivers carried 9 trillion kg of sediment to the oceans each year.

  35. SOIL EROSION Rates of erosion… • Today rivers carry about 24 trillion kg of sediment to the oceans each year!

  36. SOIL EROSION Rates of erosion… • Excessive erosion causes excessive sediment deposition in rivers.

  37. SOIL EROSION Rates of erosion… • Wind can also carry displace large amounts of soil if the land becomes dry from a severe drought. 1930’s Dust Bowl

  38. SOIL EROSION Controlling erosion… Terracing Windbreaks Landscaping Crop Rotation Erosion Walls and Fences

More Related