soil
DESCRIPTION
SOIL. What is soil?. The loose covering of broken rock particles and decaying organic matter (humus) covering bedrock. Why is soil important?. Grow food Wood for building Plants provide oxygen Filter pollutants. How is soil created?. Rock is chemically and physically weathered. - PowerPoint PPT PresentationTRANSCRIPT
SOIL
What is soil?
• The loose covering of broken rock particles and decaying organic matter (humus) covering bedrock.
Why is soil important?
• Grow food• Wood for building• Plants provide oxygen• Filter pollutants
How is soil created?• Rock is chemically and
physically weathered.• Bacteria, fungi, lichens, &
insects live in weathered rock.
• These organisms die and add nutrients to weathered rock.
• As soil builds, larger organisms can move in and colonize.
• Takes 100’s of years to create a few cm of soil.
What is a soil profile?• Vertical sequence of soil
layers (horizons).• O Horizon- vegetation/ leaf
litter on top of soil• A Horizon- dark-colored thin
layer; rich in organic matter; humus
• B Horizon- thick layer of subsoil; may be red or brown; clay based soil
• C Horizon- contains weathered parent rock; larger particles of rock; no organic matter
• R Horizon- unaltered parent bedrock
O horizon
R horizon
TYPES OF SOIL
• Polar soil– Form at high
elevations & high altitudes
– No distinct horizons- soil too thin
– Under top few inches of soil, ground is permanently frozen- PERMAFROST.
• Temperate soils– Vary depending on
rainfall & type of vegetation
– Tropical Grasslands- very thick, rich, humus
– Forests- thinner, less fertile clay soil
– Prairies- less rain, so soil not as thick, but still fertile.
• Desert soils– Very thin A horizon– Very little organic
matter– High in minerals– Soil is usually light
colored and coarse textured.
• Tropical soils– Intensely weathered
due to high precipitation and temp.
– Very little humus & very few nutrients
– High concentrations of iron- when oxidizes causes characteristic red color.
SOIL TEXTURES• Size of particles determines
– Water holding capacity– How compacted soil is– Ability to support plant
• Sand- larger particles• Silt- smaller particles• Clay- smallest particles• Loam- equal mix of sand, silt,
and clay
SOIL CONSERVATION
• Soil is easily eroded.• Methods to prevent
erosion include:
Contour Farming- plowing along slope instead of up and down it. Furrows btwn rows of crops collect water.
•Terracing- series of platforms are built into slopes. Effective with steep slopes, slows water flow.
•Shelter Belts- rows of trees planted along outer edges of s creating a windbreak to prevent wind erosion.
Strip-Cropping- Farmers plow so that plowed strips are separated by planted strips. Roots of planted strips hold soil in place.
• Reduce Grazing Permits
• Put up fencing– Animals cannot
compact and destroy plants