Ce diaporama a bien été signalé.
Nous utilisons votre profil LinkedIn et vos données d’activité pour vous proposer des publicités personnalisées et pertinentes. Vous pouvez changer vos préférences de publicités à tout moment.
 
<ul><li>Soil is the loose covering of broken rock particles and decaying organic matter, called humus, overlying the bedro...
<ul><li>Soil contains approximately  </li></ul><ul><li>45 % mineral </li></ul><ul><li>25 % water </li></ul><ul><li>25 % ai...
<ul><li>1.  Parent Rock is the original rock which is broken down. The parent rock contributes the type of minerals found ...
<ul><li>Climate may be the strongest factor effecting climate.  </li></ul><ul><li>Temperature and precipitation will deter...
<ul><li>The primary source of organic matter in soil is plants, but animals also contribute.  When organic matter is decom...
<ul><li>The actions of microorganisms like fungi and bacteria and animals such as earthworms and moles, mix and move the s...
<ul><li>The slope of the land can influence the moisture and erosion of soil. </li></ul><ul><li>Steep slopes are often poo...
<ul><li>In contrast, poorly drained low lying areas can be thick and dark It can be too wet and also have a lack of oxygen...
<ul><li>It takes 100 years to form 1 inch of soil.  The longer a soil has been forming, the thicker it becomes and the les...
<ul><li>The vertical differences, which become more pronounced as time passes, divide into zones or layers known as horizo...
<ul><li>There are 3 major divisions in the soil profile. The top is the A layer. High organic matter and humus are found h...
<ul><li>Soil layer B is enriched with clay minerals. Many subsoils have a zone of accumulation consisting of soluble miner...
<ul><li>Layer C is directly above the parent rock or bedrock. This layer contains weathered parent material and no organic...
Prochain SlideShare
Chargement dans…5
×

Soil Is The Geologist S Word For Dirt

2 578 vues

Publié le

  • Soyez le premier à commenter

Soil Is The Geologist S Word For Dirt

  1. 2. <ul><li>Soil is the loose covering of broken rock particles and decaying organic matter, called humus, overlying the bedrock of Earth’s surface. </li></ul>
  2. 3. <ul><li>Soil contains approximately </li></ul><ul><li>45 % mineral </li></ul><ul><li>25 % water </li></ul><ul><li>25 % air </li></ul><ul><li>5 % organic matter </li></ul>
  3. 4. <ul><li>1. Parent Rock is the original rock which is broken down. The parent rock contributes the type of minerals found in the soil . </li></ul>
  4. 5. <ul><li>Climate may be the strongest factor effecting climate. </li></ul><ul><li>Temperature and precipitation will determine whether chemical or mechanical weathering will take place. Along with the type of plant and animal life present. </li></ul>
  5. 6. <ul><li>The primary source of organic matter in soil is plants, but animals also contribute. When organic matter is decomposed important nutrients are supplied to the soil. </li></ul>
  6. 7. <ul><li>The actions of microorganisms like fungi and bacteria and animals such as earthworms and moles, mix and move the soil and add to the enrichment process of forming the soil. </li></ul>
  7. 8. <ul><li>The slope of the land can influence the moisture and erosion of soil. </li></ul><ul><li>Steep slopes are often poorly developed because water is being run off and with no plant growth the erosion process quickens </li></ul>
  8. 9. <ul><li>In contrast, poorly drained low lying areas can be thick and dark It can be too wet and also have a lack of oxygen develop into a fertile soil. </li></ul>
  9. 10. <ul><li>It takes 100 years to form 1 inch of soil. The longer a soil has been forming, the thicker it becomes and the less it resembles the parent material. </li></ul>
  10. 11. <ul><li>The vertical differences, which become more pronounced as time passes, divide into zones or layers known as horizons. </li></ul><ul><li>This is called the soil profile. </li></ul>
  11. 12. <ul><li>There are 3 major divisions in the soil profile. The top is the A layer. High organic matter and humus are found here. </li></ul>
  12. 13. <ul><li>Soil layer B is enriched with clay minerals. Many subsoils have a zone of accumulation consisting of soluble minerals that have been leached or washed out from the topsoil. They can be red or brown in color as a result of the presence of iron oxides. </li></ul>
  13. 14. <ul><li>Layer C is directly above the parent rock or bedrock. This layer contains weathered parent material and no organic material. </li></ul>

×