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SOIL

SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

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Page 1: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

SOIL

Page 2: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Soil

composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Page 3: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Soil

classified according to percentage of sand, silt, and clay they contain.

Page 4: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Soil Particles

vary greatly in size sand is the largest silt - medium clay - smallest

Page 5: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Clay

particles hold moisture and plant food elements more effectively than larger particles.

Page 6: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Soil Profile

consists of 3 basic layers Topsoil – A horizon Subsoil – B horizon soil bedrock – C horizon

Page 7: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Topsoil

represents depth normally ploughed

Page 8: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Subsoil

deep rooting plants send roots down into subsoil

Page 9: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Sandy Soil

silt and clay make up less than 20% by weight

drain well little water holding capacity

Page 10: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Clayey Soil

must contain at least 30% clay

holds more moisture than is good for plants

poor drainage

Page 11: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Loamy Soil

most desirable soil equal parts sand, silt and

clay

Page 12: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Read page 49

Answer the questions

Page 13: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Answers pg 49

1. - B2. - B3. - B4. - C5. - C6. - D7. - C8. - A9. - D10. - A

Page 14: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Soil Improvement

Drainage – change soil structure

–add organic matter to encourage earth worms

Page 15: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Worms

their tunnels and castings result in better soil structure - aggregation - clinging together

Page 16: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Drainage

drainage tiles raise planting beds ditching between beds

Page 17: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Moisture retention

adding organic matter (o.m.) sources of o.m. animal manure green manure - crop grown and

plowed under to improve the soil

Page 18: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Sources of O.M.

peat moss sawdust mulches - compost or wood

chips

Page 19: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Mulches

placed on the surface to help retain moisture

reduce runoff and evaporation

reduce weeds

Page 20: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Moisture retention

irrigation

Page 21: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Fertilizing

fertilize according to soil test results

Page 22: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Read page 50 – Nutrient status

Answer all questions

Page 23: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Answers for page 50

1. They are required by plants in relatively large quantities.

2. They are only needed in small amounts. Too much could cause toxicity problems or nutrient imbalance.

3. Sandy soils allow water to percolate readily because of the large macropore space. The water takes dissolved nutrients with it. Clay soils do not drain easily so nutrients are retained.

4. Small clay particles means a much larger surface area than sand particles so therefore release more nutrients from that large surface area.

Page 24: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Nutritional deficiencies

show on leaves of plants Nitrogen - pale green leaves Phosphorus - purple color on

underside of leaves

Page 25: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Plant food and fertilizers

divided into two groups Major elements (macro) Nitrogen - N Phosphorus - P Potassium - K

Page 26: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

minor elements (micro)

Calcium - Ca Magnesium - mg Sulfur - S Iron - Fe

Page 27: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

minor elements (micro)

Manganese - Mn Boron - B Copper - Cu Zinc - Zn

Page 28: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Plant requirements

large amounts of major elements

relatively small amounts of minor elements

Page 29: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Soil tests

determine amount of elements needed for various plants.

Page 30: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Nitrogen generally purchased in one of four forms Nitrate of soda ammonium nitrate http://www.youtube.com/watch?v=Ekx84-T5GLk&feat

ure=related

Page 31: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Nitrogen

ammonium sulfate urea formaldehyde

Page 32: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Nitrogen has most noticeable effect on plants encourages above ground vegetative growth regulates use of other elements http://www.youtube.com/watch?v=N1AVE6-FcAI&feat

ure=related http://www.youtube.com/watch?v=m4YToXw724w&fe

ature=related http://www.youtube.com/watch?v=uYaTdC-dCYQ&fe

ature=relmfu

Page 33: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Too much N

lower disease resistance weaken stem because of

long soft growth lower fruit quality

Page 34: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Too much N

delay maturity increase winter damage to

plants

Page 35: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Not enough N

yellow or light green color stunted root and top growth

Page 36: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

N lost easily from soil

leaching - being filtered down through soil with water

not held by soil particles, dissolved in water

O.M. holds insoluble N for slow release

Page 37: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Don’t use excess N

quickly lost through leaching can damage plants

Page 38: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phosphorous

held tightly by soil particles not easily leached

Page 39: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phosphorous

effects plants in several ways

encourage cell division

Page 40: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phosphorous

flowers and seeds don’t form without it

hastens maturity, offsetting quick growth caused by N.

Page 41: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phosphorous

encourage root growth makes K more available increase disease resistance improves quality of grain,

roots and fruit crops

Page 42: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phosphorous

container plants can be damaged by excess P

increases soluble salt content of medium

causes dehydration of roots

Page 43: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phosphorous

Insufficient P purple color on underside of

leaf reduced flower fruit and seed

production

Page 44: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Insufficient P

susceptibility to cold injury susceptibility to plant

diseases poor quality fruit and seeds

Page 45: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Potassium

modifies both fast, soft growth of N and early maturity of P

is essential

Page 46: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Potassium

increase disease resistance encourages healthy root

systems essential for starch formation

Page 47: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Potassium

development of chlorophyll efficient use of CO2

Page 48: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Insufficient K

leaves appear dry and scorched with irregular yellow areas on the surface

Page 49: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces
Page 50: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

NutrientsNutrient Why plants need this

nutrientNitrogen Used to make proteins and encourages leaf

growth. Important in the process of photosynthesis.

Potassium Important in the processes of photosynthesis and respiration and with flowering and fruit growth.

Sulfur Used in the production of chlorophyll and needed in many proteins.

Boron Involved in the production of proteins and growth hormones and found in some enzymes.

Copper Occurs in some enzymes concerned with respiration.

Page 51: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Iron Needed to make chlorophyll and occurs in some enzymes

involved in respiration.Carbon Used in the processes of

photosynthesis, respiration and transpiration.

Oxygen Used in the processes of photosynthesis, respiration and transpiration.

Phosphorus Important in the production of flowers and fruit and in the process of photosynthesis.

Calciumhttp://www.youtube.com/watch?v=UpsmJaHFH1g

Occurs in the cell walls and required for the development of stem and root tips.

Magnesium Used in the production of chlorophyll.

Page 52: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Molybdenum Used in the chemical reaction to make nitrogen available in the soil from nitrates.

Manganese Aids in the production of chlorophyll and occurs in some enzymes.

Cobalt Present in some enzymes and required in some growth processes.

Hydrogen Used in the processes of photosynthesis, respiration and transpiration.

Zinc Important in controlling plant growth.

Page 53: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Lime

CaCO3- Calcium Carbonate acts as a plant food affects soil acidity soil acidity affects availability of

plant food elements

Page 54: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Lime

furnishes Calcium

Page 55: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

pH

measure of acidity or alkalinity

pH scale - runs from 0 - 14 most plants grow best from

5.6-7.0

Page 56: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

pH

7.0 is neutral pH of 7 or above is alkaline

or basic pH below 7 is acidic

Page 57: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

pH

as numbers decrease, solution becomes more acidic.

As numbers increase, solution becomes more basic or alkaline

Page 58: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

pH

if soil is too acidic, lime is added to raise the pH

if soil is too alkaline, sulfur is added

Page 59: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Above ground environment temperature some plants prefer cool

weather some plants prefer warm

weather

Page 60: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Temperature

there are temperatures above and below which plants stop growth

generally, plant growth rate increases as temps increase up to about 90 degrees

Page 61: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Light

must be present before plants can manufacture food

plants vary in light requirement

effects flowering

Page 62: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Photoperiodism

response to different periods of day and night in terms of growth and maturity

Page 63: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Photoperiodism

short day plants chrysanthemum and

Christmas Cactus bloom when days are short

and nights are long

Page 64: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Photoperiodism

long day plants lettuce and radishes bloom when days are long

and nights are short

Page 65: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Photoperiodism

day length indifferent do not depend on length of

light or darkness African Violet and tomato

Page 66: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Phototropism

plants appear to grow towards the sun or light source

Page 67: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Humidity

moisture level of the air most plants grow best in 40-

80% relative humidity (R.H.) Relative Humidity

Page 68: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Humidity

too high humidity may cause the spread of fungus diseases

Page 69: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Plant diseases and Insects reduce production lower fruit and vegetable

quality

Page 70: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Gases and Air Particles

CO2 is vital to plants for Photosynthesis

Air pollutants can cause damage

Page 71: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Air Pollutants

Sulfur Dioxide - SO2 - from burning coal

Carbon Monoxide - CO - exhaust from cars

Page 72: SOIL. Soil n composed of sand, silt, and clay, organic matter, living organisms, and pore spaces

Carbon Monoxide

reduces plant growth can kill plants