Title: Physical Science Applications in Agriculture
1Physical Science Applications in Agriculture
- Unit
- Physical Science Systems
2Problem Area
- Agricultural Production Systems
3Testing Common Substances for pH
4Ever see limestone being applied on a growers
field?
- What is so important about this powdery
substance? - What does it do for the soil?
- Does the composition or type of limestone
(liquid, dry, palletized) make a difference in
its effectiveness?
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5Which plant looks healthier?
- Examine the pictures or actual plants that have
received different levels of fertilizer. - Which plant looks healthier?
- Which plant would produce better and more
product? - How much fertilizer do they apply to get optimum
growth of our vegetable plants? - Is there a way to determine this? How?
6Learning Objectives
- Define pH and discuss its role in plant
nutrition. - Explain how soils become acidic.
- Explain how soil pH is measured.
- Explain why lime is applied to acid soils.
- Discuss the effectiveness of lime on acidic soils.
7Terms
- Acid
- Calcium carbonate equivalent
- Cation
- Cation exchange capacity
- Lime requirement
- Percent base saturation
- pH scale
- Soil pH
8What is pH?
- Soil pH is the measure of acidity or alkalinity
of the soil.
9What is the pH scale?
- The pH scale is a fourteen point scale used to
measure pH. - A neutral pH is 7.0.
- A solution with a pH between zero and 6.9 is
considered acid. - A solution with a pH between 7.1 and 14.0 is
considered alkaline or base. - The scale is expressed in logarithmic terms.
- Each unit change in pH corresponds to a tenfold
change in acidity or alkalinity. - A pH of 6.0 is 10 times more acidic than a pH or
7.0.
10How does pH affect plant nutrition?
- The pH value of soil is important to
agriculturalists because certain nutrients become
unavailable to plants if the pH value is too high
or too low. - The amount of nutrients that are available is
dependent upon soil pH.
11How does pH affect plant nutrition?
12How do soils become acidic?
- pH is determined by the concentration of hydrogen
(H) ions and hydroxyl ions (OH-) in the soil
solution.
13How do soils become acidic?
- A sample of pure water has an equal number of H
and OH- and is neutral. - An acid is a substance that releases hydrogen
ions. - When saturated with H, a soil behaves as a weak
acid. - The more H held on the exchange complex, the
greater the soils acidity.
14Several factors influence soil pH.
- Soil organic matter is continuously being
decomposed by micro organisms into organic acids,
carbon dioxide, and water, forming carbonic acid.
- Carbonic acid reacts with Ca and Mg carbonates in
the soil to form more soluble bicarbonates, which
are leached away, leaving the soil more acid.
15Several factors influence soil pH.
- As water from rainfall passes through the soil,
basic nutrients such as calcium and magnesium are
leached. - They are replaced by acidic element including
aluminum, hydrogen, and manganese.
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16Several factors influence soil pH.
- Soils formed under forest vegetation tend to be
more acidic than those developed under
grasslands.
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17Several factors influence soil pH.
- Soils often become more acidic when crops are
harvested because bases are - removed.
- Legumes generally contain higher levels of bases
than grasses. - Legumes also release H ions into their
rhizosphere when actively fixing atmospheric N.
18Several factors influence soil pH.
- Nitrogen from fertilizer, organic matter, manure,
and legume N fixation produces acidity. - Nitrogen fertilization speeds up the rate at
which acidity develops. - At lower N rates, acidification rate is slow, but
is accelerated as N fertilizer rates increase.
19ACID AND ALKALINE SOILS
20How is soil pH measured?
- The two most commonly accepted methods of
measuring soil pH are indicator dyes and the pH
meter.
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21How is soil pH measured?
- Indicators are frequently used in the field to
make a rapid pH determination and must be used by
a trained hand to avoid major error.
- The more accurate and widely used method is the
pH meter used in soil testing laboratories.
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22Why is lime applied to acidic soils?
- Since various plants require different pH levels
for optimum growth, growers must attempt to
adjust soil pH to suit the crop or plant being
grown. - This involves the use of limestone to raise pH or
the use of alum to lower pH. - Lime requirement is the amount of agricultural
limestone needed to establish the desired pH
range.
23Why is lime applied to acidic soils?
- Soil pH is an excellent single indicator of soil
acidity, it does not determine lime requirement. - Lime requirement of a soil is not only related to
the pH but also to its buffer capacity or cation
exchange capacity. - Cation exchange capacity is the total number of
exchangeable cations, an ion with a positive
charge, a soil can adsorb. - The relative amount of the cation exchange
capacity filled with basic cations is called
percent base saturation. - Soil pH is a measure of the percent base
saturation.
24Why is lime applied to acidic soils?
- Lime replaces hydrogen and aluminum on the cation
exchange sites with calcium and changes hydrogen
ions to water.
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25Factors to figure how much lime is required
- the present pH
- the desired pH
- the cation exchange capacity of the soil
- the liming material to be used
www.hort.wisc.edu/.../soiltest/soiltest.htm
26The effectiveness of lime on soil.
- The effectiveness of lime depends on
- Purity
- Fineness
- Rate it dissolves
- Measured as the calcium carbonate equivalent
27What determines the effectiveness of lime on acid
soils?
- The neutralizing power of lime depends upon its
purity, measured as the calcium carbonate
equivalent. - Neutralizing values of all liming materials are
determined by comparing them to the neutralizing
value of pure claim carbonate. - Setting the neutralizing value of calcium
carbonate at 100, a value for other materials can
be assigned.
28What determines the effectiveness of lime on acid
soils?
- When a given quantity of lime is mixed with the
soil, its reaction rate and degree of reactivity
are affected by particle size. - Coarse live particles react more slowly and less
fully. - Fine lime particles react more rapidly and much
more completely. - Cost of lime increases with the fineness of
grind. - The goal is a material that requires a minimum of
grinding, yet contains enough fine material to
cause a rapid pH change.
29Other important factors determining the
effectiveness of lime
- Placement for maximum contact with the soil in
the tilled layer is essential. - Even when properly mixed with the soil, lime will
have little effect on pH if the soil is dry. - Moisture is essential for lime-soil reaction to
occur. - The full benefit of lime is not seen until the
second or third year after application. - Lime does not react with acidic soil very far
from the lime particle.
30Review/Summary
- What is pH and how does it affect plant
nutrition? - How do soils become acidic?
- How is soil pH measured?
- Why is lime applied to acidic soils?
- What determines the effectiveness of lime on acid
soils?