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Soil Organic Matter
A Lecture By
Mr .Allah Dad Khan
Soil Organic Matter=SOM
Is this a healthy soil? Is this a healthy field?
SOM
 Soil Organic matter
encompasses
all organic components
of a soil:
 Fresh residues
 Decomposing
organic
matter
 Stable organic
matter
 Living organisms
Soil Organic Matter
 Soil organic matter =
 all living organisms
(microorganisms,
earthworms, etc),
 fresh residues (old plant
roots, crop residues,
recently added manures),
 well-decomposed residues
(humus).
 The SOM content of
agricultural topsoil is usually in
the range of 1 to 6%.
 This amount is the result of all
additions and losses of SOM
that have occurred over the
years.
 Non-cultivated soils will have
SOM ranges between 3-10%
Citizen Science – Kansas State
Fresh Residues
 Up to 15% of organic
matter is fresh
residue (usually <10)
 Comprised mainly of
litter fall
 Many of the different types
of plant litter can be
recognized.
Decomposing Organic Matter
 Plant material is transformed
from one organic compound to
another mainly by organisms in
the soil
 Organisms create by-products,
wastes, and cell tissue
 Compounds released as waste
by one organisms can often be
used as food by another
Soil Organic
Matter =SOM
 SOM is labile* -it can
decline rapidly if the
soil environment
changes and renewable
-it can be replenished
by inputs of organic
material to the soil.
 * Labile = Constantly or readily
undergoing chemical, physical, or
biological change or breakdown;
unstable.
Adequate levels of SOM can be maintained with:
1. proper
fertilization,
2. crop
rotations, and
tillage
practices
3. Returning
crop residues
to the soil.
Factors Controlling SOM
 1) Kind of parent materials (texture
primarily), climate, slope, and
management practices that exist.
(Sandy = Low & Clay = High)
 2) Climate: PMs that have not lost their
nutrients from excessive rainfall
(leaching), and areas where
temperature and water are adequate
will have high SOM.
 3) Management practices that affect
crop biomass (yield and straw)
production (water, fertilizer, variety),
residue maintenance (equipment,
harvest), and litter (wind) will also
affect SOM content.
 4) As dry matter production increases,
SOM increases.
 5) However, only that which remains
after harvest along with root biomass
will influence long-term SOM content.
Established in 1876 the Morrow Plots are the oldest agronomic experiment fields
in the United States. They include the longest-term continuous corn plot in the
world. Located near the center of the University of Illinois' Urbana campus.
manure, lime and phosphorus (MLP)
Morrow Plots – Why the difference in SOM?
How is SOM
Measured?
SOM is usually measured in the
laboratory as organic carbon,
Soil organic matter is estimated
to contain 50% organic carbon
(varies from 40 to 70%) with
the rest of the SOM
comprising of other elements
(eg, 5% N, 0.5% P and 0.5% S).
A conversion to SOM from a
given organic carbon analysis
requires that the organic
carbon content be multiplied
by a factor of
2.00(1.00/0.50).
Thus, 2% SOM is about 1 %
organic carbon.
Testing for Soil Organic Carbon
UF/IFAS Extension Soil Testing Laboratory
Active Fraction
 10 to 30% of the soil
organic matter (active
fraction) is responsible
for maintaining soil
microorganisms.
 The active fraction of
organic matter is most
susceptible to soil
management practices.
(Inactive = humus)
ACTIVE
Adding Fresh OM
 In a soil which at
first has no readily
decomposable
materials, adding
fresh tissue under
favorable
conditions:
 1) immediately
starts rapid
multiplication of
bacteria, fungi,
and actinomycetes,
 2) which are soon
actively
decomposing the
fresh tissue.
ADDED
Fresh SOM
 as most readily
available energy
sources are used up,
microorganisms again
become relatively
inactive,
 leaving behind a dark
mixture usually
referred to as humus
– a stable organic
compound
Stable Organic Matter -Humus
 Thus, soil organic
compounds become
stabilized and resistant to
further changes by
microorganisms
 Stabilized organic matter
acts like a sponge and can
absorb six times its
weight in water
HUMUS
 Newly-formed humus=
 a) combination of
resistant materials from
the original plant tissue,
 b) compounds synthesized
as part of the
microorganisms' tissue
which remain as the
organisms die. (Fulvic and
Humic Acid)
 humus is mostly resistant
to further microbial
attack- N and P are
protected from ready
solubility
Leaf Humus
Function of Humus
 holds water and nutrients;
 sticks together & helps
establish and maintain a
strong crumb structure &
thus reduce soil erosion
 provides some nutrients
(N & P) as it is slowly
decayed by microbial
activity,
 Buffers effects of
pesticides
 humus decomposes at the
rate of 2.5% per year
 Creates good soil “ Tilth”
 Coates the sand, silt, clay
particles making them
dark and the darker the
color, the greater the
amount of soil humus
present.
Humus = High Medium
SOM Maintains soil “Tilth”
 aiding
infiltration of
air and water
 promoting
water
retention
 reducing
erosion
BMI
SOM = SOIL
HEALTH
 Measuring SOM is one step in
assessing overall soil quality
or soil health -
 measuring various key
attributes of soil organic
matter quantity and quality
will give an indication of the
health of the soil.
 Or Look at the state of the
soil organisms in the soil.
 Or look at how well the soil
“Holds Together”.
“If your soil clods can't pass the water
test, change your management practices.
It will help your bottom line as well as the
soil.” – Ray Weil – Univ of Maryland
Simple clod test: Healthy soil, at
left, holds together in water, while
poor soil falls apart.
Use of Soil Quality
 1) Match use and management
of land to soil capability,
because improper use of a soil
can damage it and the
ecosystem.
 2) Establish a baseline
understanding about soil
quality so that we can
recognize changes as they
develop.
 3) Use baselines to determine
if soil quality is deteriorating,
stable, or improving.
 Thus soil quality becomes a
good indicator of the health of
an ecosystem.
NatureWatch
Soil Quality
 Soil quality is the capacity of soils
within landscapes to sustain biological
productivity, maintain environmental
quality, and promote plant and animal
health.
 Protecting soil quality like protecting
air quality and water quality should
be fundamental goal of our Nation’s
Environmental Policy
http://www.directs
eed.org/soil_qualit
y.htm
http://www.nrsl.umd.edu/research/NRSLResearchAreaInfo.cfm?ID=14
Poor Good
SOIL HEALTH
 Soil Health is the change
in Soil Quality over time
due to human use and
management or to natural
events.
 Descriptive terms for Soil
Health
 Organic Matter - high
 Crop appearance =
green, healthy,lush
 erosion – Soil will not
erode
 earthworms – numerous
 infiltration – fast, no
ponding
 Compaction - minimal
Cornell researcher George Abawi describes soil health
strategies at an Onion Council field day in Wayne County,
N.Y.Photo by Carol R. MacNeil.
In Vernon and surrounding counties are the largest
concentration of organic farmers in Wisconsin.
Is this a good Idea? DYAD
 The Grimm Brother's fairy tale, Rumpelstiltskin spins straw
into gold.
 Thanks to advances in biotechnology, researchers can now
transform straw, and other plant wastes, into "green" gold -
cellulosic ethanol.
 While chemically identical to ethanol produced from corn or
soybeans, cellulose ethanol exhibits a net energy content
three times higher than corn ethanol and emits a low net
level of greenhouse gases.
 Recent technological developments are not only improving
yields but also driving down production cost, bringing us
nearer to the day when cellulosic ethanol could replace
expensive, imported "black gold" with a sustainable,
domestically produced biofuel.
 IS THIS A GOOD THING TO DO?
http://www.harvestcleanenergy.org/enews/enews_0505/enews_050
5_Cellulosic_Ethanol.htm

What is the health of this soil?
Soil organic matter A  presentation by Mr.Allah Dad Khan

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Soil organic matter A presentation by Mr.Allah Dad Khan

  • 1.
  • 2. Soil Organic Matter A Lecture By Mr .Allah Dad Khan
  • 3. Soil Organic Matter=SOM Is this a healthy soil? Is this a healthy field?
  • 4. SOM  Soil Organic matter encompasses all organic components of a soil:  Fresh residues  Decomposing organic matter  Stable organic matter  Living organisms
  • 5. Soil Organic Matter  Soil organic matter =  all living organisms (microorganisms, earthworms, etc),  fresh residues (old plant roots, crop residues, recently added manures),  well-decomposed residues (humus).  The SOM content of agricultural topsoil is usually in the range of 1 to 6%.  This amount is the result of all additions and losses of SOM that have occurred over the years.  Non-cultivated soils will have SOM ranges between 3-10% Citizen Science – Kansas State
  • 6. Fresh Residues  Up to 15% of organic matter is fresh residue (usually <10)  Comprised mainly of litter fall  Many of the different types of plant litter can be recognized.
  • 7. Decomposing Organic Matter  Plant material is transformed from one organic compound to another mainly by organisms in the soil  Organisms create by-products, wastes, and cell tissue  Compounds released as waste by one organisms can often be used as food by another
  • 8. Soil Organic Matter =SOM  SOM is labile* -it can decline rapidly if the soil environment changes and renewable -it can be replenished by inputs of organic material to the soil.  * Labile = Constantly or readily undergoing chemical, physical, or biological change or breakdown; unstable.
  • 9. Adequate levels of SOM can be maintained with: 1. proper fertilization, 2. crop rotations, and tillage practices 3. Returning crop residues to the soil.
  • 10. Factors Controlling SOM  1) Kind of parent materials (texture primarily), climate, slope, and management practices that exist. (Sandy = Low & Clay = High)  2) Climate: PMs that have not lost their nutrients from excessive rainfall (leaching), and areas where temperature and water are adequate will have high SOM.  3) Management practices that affect crop biomass (yield and straw) production (water, fertilizer, variety), residue maintenance (equipment, harvest), and litter (wind) will also affect SOM content.  4) As dry matter production increases, SOM increases.  5) However, only that which remains after harvest along with root biomass will influence long-term SOM content. Established in 1876 the Morrow Plots are the oldest agronomic experiment fields in the United States. They include the longest-term continuous corn plot in the world. Located near the center of the University of Illinois' Urbana campus. manure, lime and phosphorus (MLP) Morrow Plots – Why the difference in SOM?
  • 11. How is SOM Measured? SOM is usually measured in the laboratory as organic carbon, Soil organic matter is estimated to contain 50% organic carbon (varies from 40 to 70%) with the rest of the SOM comprising of other elements (eg, 5% N, 0.5% P and 0.5% S). A conversion to SOM from a given organic carbon analysis requires that the organic carbon content be multiplied by a factor of 2.00(1.00/0.50). Thus, 2% SOM is about 1 % organic carbon. Testing for Soil Organic Carbon UF/IFAS Extension Soil Testing Laboratory
  • 12. Active Fraction  10 to 30% of the soil organic matter (active fraction) is responsible for maintaining soil microorganisms.  The active fraction of organic matter is most susceptible to soil management practices. (Inactive = humus) ACTIVE
  • 13. Adding Fresh OM  In a soil which at first has no readily decomposable materials, adding fresh tissue under favorable conditions:  1) immediately starts rapid multiplication of bacteria, fungi, and actinomycetes,  2) which are soon actively decomposing the fresh tissue. ADDED
  • 14. Fresh SOM  as most readily available energy sources are used up, microorganisms again become relatively inactive,  leaving behind a dark mixture usually referred to as humus – a stable organic compound
  • 15. Stable Organic Matter -Humus  Thus, soil organic compounds become stabilized and resistant to further changes by microorganisms  Stabilized organic matter acts like a sponge and can absorb six times its weight in water
  • 16. HUMUS  Newly-formed humus=  a) combination of resistant materials from the original plant tissue,  b) compounds synthesized as part of the microorganisms' tissue which remain as the organisms die. (Fulvic and Humic Acid)  humus is mostly resistant to further microbial attack- N and P are protected from ready solubility Leaf Humus
  • 17. Function of Humus  holds water and nutrients;  sticks together & helps establish and maintain a strong crumb structure & thus reduce soil erosion  provides some nutrients (N & P) as it is slowly decayed by microbial activity,  Buffers effects of pesticides  humus decomposes at the rate of 2.5% per year  Creates good soil “ Tilth”  Coates the sand, silt, clay particles making them dark and the darker the color, the greater the amount of soil humus present. Humus = High Medium
  • 18. SOM Maintains soil “Tilth”  aiding infiltration of air and water  promoting water retention  reducing erosion BMI
  • 19. SOM = SOIL HEALTH  Measuring SOM is one step in assessing overall soil quality or soil health -  measuring various key attributes of soil organic matter quantity and quality will give an indication of the health of the soil.  Or Look at the state of the soil organisms in the soil.  Or look at how well the soil “Holds Together”. “If your soil clods can't pass the water test, change your management practices. It will help your bottom line as well as the soil.” – Ray Weil – Univ of Maryland Simple clod test: Healthy soil, at left, holds together in water, while poor soil falls apart.
  • 20. Use of Soil Quality  1) Match use and management of land to soil capability, because improper use of a soil can damage it and the ecosystem.  2) Establish a baseline understanding about soil quality so that we can recognize changes as they develop.  3) Use baselines to determine if soil quality is deteriorating, stable, or improving.  Thus soil quality becomes a good indicator of the health of an ecosystem. NatureWatch
  • 21. Soil Quality  Soil quality is the capacity of soils within landscapes to sustain biological productivity, maintain environmental quality, and promote plant and animal health.  Protecting soil quality like protecting air quality and water quality should be fundamental goal of our Nation’s Environmental Policy http://www.directs eed.org/soil_qualit y.htm http://www.nrsl.umd.edu/research/NRSLResearchAreaInfo.cfm?ID=14 Poor Good
  • 22. SOIL HEALTH  Soil Health is the change in Soil Quality over time due to human use and management or to natural events.  Descriptive terms for Soil Health  Organic Matter - high  Crop appearance = green, healthy,lush  erosion – Soil will not erode  earthworms – numerous  infiltration – fast, no ponding  Compaction - minimal Cornell researcher George Abawi describes soil health strategies at an Onion Council field day in Wayne County, N.Y.Photo by Carol R. MacNeil. In Vernon and surrounding counties are the largest concentration of organic farmers in Wisconsin.
  • 23. Is this a good Idea? DYAD  The Grimm Brother's fairy tale, Rumpelstiltskin spins straw into gold.  Thanks to advances in biotechnology, researchers can now transform straw, and other plant wastes, into "green" gold - cellulosic ethanol.  While chemically identical to ethanol produced from corn or soybeans, cellulose ethanol exhibits a net energy content three times higher than corn ethanol and emits a low net level of greenhouse gases.  Recent technological developments are not only improving yields but also driving down production cost, bringing us nearer to the day when cellulosic ethanol could replace expensive, imported "black gold" with a sustainable, domestically produced biofuel.  IS THIS A GOOD THING TO DO? http://www.harvestcleanenergy.org/enews/enews_0505/enews_050 5_Cellulosic_Ethanol.htm 
  • 24. What is the health of this soil?