soil

17
SOIL

Upload: emlyn

Post on 24-Feb-2016

38 views

Category:

Documents


0 download

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 Presentation

TRANSCRIPT

Page 1: SOIL

SOIL

Page 2: SOIL

What is soil?

• The loose covering of broken rock particles and decaying organic matter (humus) covering bedrock.

Page 3: SOIL

Why is soil important?

• Grow food• Wood for building• Plants provide oxygen• Filter pollutants

Page 4: SOIL

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.

Page 5: 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

Page 6: SOIL

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.

Page 7: SOIL

• 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.

Page 8: SOIL

• Desert soils– Very thin A horizon– Very little organic

matter– High in minerals– Soil is usually light

colored and coarse textured.

Page 9: SOIL

• 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.

Page 10: SOIL

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

Page 11: SOIL
Page 12: SOIL

SOIL CONSERVATION

• Soil is easily eroded.• Methods to prevent

erosion include:

Page 13: SOIL

Contour Farming- plowing along slope instead of up and down it. Furrows btwn rows of crops collect water.

Page 14: SOIL

•Terracing- series of platforms are built into slopes. Effective with steep slopes, slows water flow.

Page 15: SOIL

•Shelter Belts- rows of trees planted along outer edges of s creating a windbreak to prevent wind erosion.

Page 16: SOIL

Strip-Cropping- Farmers plow so that plowed strips are separated by planted strips. Roots of planted strips hold soil in place.

Page 17: SOIL

• Reduce Grazing Permits

• Put up fencing– Animals cannot

compact and destroy plants