SOILS How Do Soils Form Soils differ from

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SOILS

SOILS

How Do Soils Form? • Soils differ from one part of the world to

How Do Soils Form? • Soils differ from one part of the world to another • Differ because of where and how soil was formed • There are 5 major factors that control how a soil forms …CLORPT

CLORPT • 5 Formation Factors: Climate Organisms Relief Parent Material Time CLORPT for short!!!

CLORPT • 5 Formation Factors: Climate Organisms Relief Parent Material Time CLORPT for short!!!

CLIMATE • Temperature and moisture influence the speed of chemical reactions • This controls

CLIMATE • Temperature and moisture influence the speed of chemical reactions • This controls how fast rocks weather and dead organisms decompose • Temp. increase = weathering increase • Rain/water increase = weathering increase

ORGANISMS (Vegetation and Biology) • Plant roots spread out, animals burrow, and bacteria eat…

ORGANISMS (Vegetation and Biology) • Plant roots spread out, animals burrow, and bacteria eat… this speeds up the break down of soil particles • Roots give CO 2 and organic kjskjss acids that break down • Roots may physically break hjjjjjh rocks • Decomposers such as fungi, jhjjjjjjjjjj worm, and bacteria

RELIEF (Topography) • Shape and aspect (direction the land faces) makes a difference in

RELIEF (Topography) • Shape and aspect (direction the land faces) makes a difference in the how much the sunlight the soil gets and how much water it keeps • Steep slopes are more likely to erode and are unstable • Sun facing slopes show more development as they are warmer • Deeper soils form at the jjjjjjjj bottom of a hill due to water jjjjjjjjjjjjjj and gravity

PARENT MATERIAL • Every soil inherits traits from the material from which it formed…

PARENT MATERIAL • Every soil inherits traits from the material from which it formed… just like you! • EXAMPLES • Soils formed in limestone bedrock are high in calcium • Soils formed at the bottom of lakes are high in clay • Parent material can include – Transported Materials – Bedrock or Residual Materials – Organic Materials

TIME Older soils differ from younger soils Have had more time to develop More

TIME Older soils differ from younger soils Have had more time to develop More horizons Time does not always represent true chronological order • EXAMPLE • • • Old soil in Antarctica will show very little development and appear young • Young soil in a tropical area will show more development and appear older