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Phosphorous
Organic Phosphorous
Components of soil organic matter and plant tissue
Phosphate sugars
Nucleic Acids (DNA/RNA)
ATP
Phospholipids
ATP
Importance
Essential Macronutrient
Limiting Resource
Present in Fertilizers, animal wastes, wastewater
Availability can be very limited
Fertility
10 -15% of applied fertilizer phosphorous used by plants
85 – 90% is bound to soil particles or forms insoluble solids
=>excess application
=>saturation of soil capacity
=> mobility in the environment
-Total soil phosphorous is low
-Most of the total is unavailable to plants
-Much of soil P forms insoluble solids
(limiting to availability)
P-impacted
Unimpacted
Soil Phosphorous
PO4
-3
Inorganic
H2PO4
- HPO4
-2
H3PO4
(Orthophosphate)
The form of available phosphorus is pH-dependent
Plant Availablity
H2PO4
- HPO4
-2
pH 3-6 pH 8-11
pH 6-8
Optimum pH = 6.5 for mineral soils
Most Available
Acidic Soils
Acid Soils (Low pH)
Aluminum and Iron availability increased at low pH
Al(OH)3
FeOOH
Solubility increased
Al3+ Fe3+
Al(OH)3 + 3H+ = Al3+ + 3H2O
example
Aluminum Precipitation at Low pH
H2PO4
-
(pH 3-6)
Al3+ + H2PO4
- + 2H20 = Al(OH)2H2PO4 + 2H+
(Insoluble)
Al(PO4) • H2O
Variscite
Al3+ + PO4
-3 = Al(PO4)
simplified
Form of available P at low pH:
H2PO4
- combines with free Al3+ and Fe3+
Basic Soils (High pH)
Calcium Binding in Basic Soils
CaCO3
CaCO3 + 2H2(PO4)- = Ca [H2(PO4)]2 + CO3
2-
CaHPO4
Ca5(PO4)3OH (Apatite mineral)
(higher calcium availability)
H2(PO4)- is the available form of P
Availability and pH
Low pH High pH
Aluminum and Iron
phosphates
Calcium Phosphates
Formation of insoluble solids
Reaction with Soil Minerals
Fixation on Iron and Aluminum
A dominant interaction between Phosphorus and
soils is strong interaction with Iron and Aluminum Oxides
Al
Al
OH
OH
OH
Fe
Fe
OH
OH
OH
Fixation: Aluminum/Iron oxides
Fe
Fe
OH
OH
OH
H2(PO4)-
+
Fe
FE
OH
OH
H2(PO4)-
OH-
+
Fe
Fe
OH
OH
OH
P OH
O-
OH
O-
+
Fe
Fe
OH
OH
P OH
O-
OH
O-
Coatings on Sands and Silicate Clays
Fe coating
Fe
Fe
OH
OH
H2(PO4)-
Organic Matter
Organic matter does not typically
bind strongly with phosphorus.
Organic matter covers fixation sites
Organic matter reacts with free Fe and Al
Organic matter competes for anion exch. sites
Organic Matter tends to increase P availability
-Plant Available
-Fe, Al bound
-Calcium bound
- Fixed on oxides
H2PO4
- HPO4
-2
Al(PO4) • H2O
Ca3(PO4)2
H2PO4
-
Inorganic Soil Phosphorous
Inorganic
(low)
Phosphorus is generally removed from solution by soil processes
These processes have a finite capacity to retain phosphorus
When the capacity is exceeded, phosphorus can become mobile.
South Florida and Phosphorus
Historic flow patterns in the
Kissimmee – Okeechobee – Everglades
system has been significantly altered,
beginning in the late 1800’s.
The design was to drain significant
areas for agriculture and development
and to prevent floodwaters from
communities to the south and east.
Historic Flow Patterns
Okeechobee and the Everglades
Development
"The first and most abiding
impression is the utter
worthlessness
to civilized man, in its
present condition, of the
entire region."
Buckingham Smith
1835
First Survey
In 1850, the Swamplands Act Passed
Population: 87,445
Transferred 20 million aces to FL for drainage and reclamation
11 miles (17.7 km) of
canal south of Lake
Okeechobee towards
Miami.
1881
Hamilton Disston
50,000 acres drained
Okeechobee north to Kissimmee
and west to the Gulf of Mexico.
1904
“pestilence-ridden swamp”
Empire of the Everglades
Broward Elected
1905
Everglades Drainage
District
Authorized Canals, taxes
By 1920, 4 major canal systems linked Okeechobee to the Atlantic,
By 1920
Began in 1881
Melaleuca Tree 1906
Invasive ornamental
359,000 acres
displaces native vegetation
6-12 ft. growth per year
1928
1911
1914-1918
Florida East Coast Railway
Tamiami Trail
WWI
Flagler
1928 Belle Glade
Hurricane
135 mph winds
20-foot deep floodwaters
South of Okeechobee
3000 to 8000 dead
143 miles of levee
45 feet high and 150 feet wide
After the storm
Hoover Dike
19 water control structures
Hoover Dike (1932)
Everglades Agricultural Area (EAA)
Perimeter Levee (1954)
Water Conservation Areas
(management of flow)
Former extent of Kissimmee
Basin and floodplain
To Gulf
To Atlantic
Drainage
Historic Current
EAA
Phosphorus loading to S. Florida Ecosystem
Inputs North
and South of
Okeechobee
Dairy/Beef
Crop Production
Kissimmee Basin
Sugar, Rice, Veg.
700,000 ac
EAA
Crops: Everglades Agricultural Area
1940’s thousands of acres converted to agricultural production
1959 Cuban exiles established sugar plantations
1960s Sugar production increased 4-fold
Today, sugarcane production contributes
two-thirds of the economic production of
Everglades agriculture, and uses nearly
80% of the crop land in the EAA
Sugar and vegetable production
contributes phosphorus
to the ecosystem primarily through
fertilizers and to a lesser extent through
decomposition of plants.
EAA
382,000 acres
46% U.S.
Palm Beach, Glades, Hendry
Sugar
Celery 260 200 140 80 20 0 0 0 0
Endive 200 175 150 125 100 75 50 25 0
Escarole
200 175 150 125 100 75 50 25 0
Lettuce (Head) 200 175 150 125 100 75 50 25 0
Radish 100 40 0 0 0 0 0 0 0
Romaine 200 175 150 125 100 75 50 25 0
Sugar Cane 120 100 80 40 20 0 0 0
0
Phosphorus Fertilization (lbs/ac)
Low Soil P V. High Soil P
Phosphorus loading to S. Florida Ecosystem
Inputs North
and South of
Okeechobee
Dairy/Beef
Agriculture
Kissimmee Basin
Dairy and Beef Kissimmee drainage basin 12,000 km2
In 1521 Ponce de Leon
brought horses and cattle
to Florida, making it the
oldest cattle raising state
in the country.
No other part of our country
had cattle until the Pilgrims
brought cattle in the early 1600's
Florida's ranchers now raise
the third largest number of
cattle of any state east of the
Mississippi
(1947)
Phosphorus
Solid Manure:
5.5 g / kg total Phosphorus
One cow can excrete between 40
and 60 g of phosphorus per day
Subject to movement via runoff, stream
flow, soil water movement, and
groundwater movement
Cattle and Dairy
Okeechobee, Highlands, and Glades
Counties: 328,000 head (19% of total)
Okeechobee County is ranked number one for all cattle in the state
The Kissimmee river alone
contributes about 20% of the
phosphorus flowing into
Lake Okeechobee
The Lower Kissimmee River Basin is among
largest sources of external phosphorus loading to
Lake Okeechobee
Kissimmee – Okeechobee - Everglades
Okeechobee, in turn, is a source
of phosphorus to the Everglades
Surface Water Improvement Management Act: SWIM
SWIM Plan priority basins
Mandates phosphorus load level of 397 tons/yr
Clean Water act: 154.3 tons per year
deadline of January 1, 2015
Lake
(1987)
Target level of 40 ppb
in Lake Okeechobee
The Dairy Rule (1987)
creating lagoons to capture and contain dairy waste
Dairy Buy-Out Program
to facilitate removal of animals from dairies not able to comply
Works of the District Rule
permits are required for all discharges into waterways
Implement Best Management Practices (BMPs)
buffer areas around places animals congregate, eliminating
phosphorus fertilization near tributaries, reducing phosphorus
imports in animal feeds, reducing animal density
Some Strategies
19 of 45 Dairies Remain
SWIM target: 397 tons
Phosphorus Loads to Okeechobee
Above
Target
2007: 146 ton reduction of P entering Okeechobee
Above
SWIM
target
(tons)
Phosphorus concentrations in the Lake remain at about 117 ppb
The target level is 40 ppb.
2007: 146 ton reduction of P entering Okeechobee
Internal Loading
Decomposition of submerged aquatic vegetation
releasing phosphorus back into the water column
Dissolution of compounds in sediments which
bind and store phosphorus.
Two Sources
Phosphorus and Iron
Phosphorus has a strong affinity for iron
FePO4
Solid Precipitate
Readily incorporates into bottom sediments
Internal Loading
Internal Loading
Dissolved phosphorus combines with oxidized iron (Fe3+) to create
an insoluble compound that becomes buried in lake sediments.
If oxygen contents are reduced (anoxic bottom sediments) the
Fe3+ converts to Fe2+ which solubilizes the compound returning P to water.
P released by sediments is taken up by photosynthetic
algae faster than it can be returned to the sediments
Fe3+ + PO4
3- = Fe(PO4)
solid
(PO4)
Fe
to water
2+
Fe3+ high oxygen Fe2+ low oxygen
3-
Simplified:
RECOMMENDATION – Control Internal Phosphorus Loading.
Phosphorus-rich mud sediments need to be removed from the lake
to the maximum extent that is practical, in order to reduce internal
phosphorus loading. Unless this internal loading is substantially
reduced, it may take as long as 100 years for the lake to respond to
watershed phosphorus control programs.
Lake Okeechobee Action Plan
Developed by the Lake Okeechobee Issue Team
December 6, 1999
Lost Lands
Hoover Dike (1932)
Everglades Agricultural Area (EAA)
Perimeter Levee (1954)
Water Conservation Areas
(management of flow)
Former extent of Kissimmee
Basin and floodplain
To Gulf
To Atlantic
Historic Current
EAA
Sugar, Rice, Veg.
700,000 ac
EAA
Crops: Everglades Agricultural Area
Florida to Buy Out Sugar Land for Everglades
Restoration
WTVJ NBC 6
June 25, 2008: WEST PALM BEACH, Florida -- The largest U.S.
producer of cane sugar, U.S. Sugar Corp., would close up shop in a
$1.75 billion deal to sell its 292 square miles of land to Florida for
Everglades restoration, the company president and Florida Governor
Charlie Crist said Tuesday.
The deal, announced at a news conference at the Arthur R. Marshall
Loxahatchee National Wildlife Refuge, allows the state to buy U.S.
Sugar's holdings in the Everglades south of Lake Okeechobee, the
heart of the wetland ecosystem.
186,000 acres
Organic soils possessing
high natural fertility
Historically flooded
Under flooded conditions, oxygen levels tend to be low
The diffusion of oxygen through water is about
1000 times slower than diffusion through air
Water restricts the movement of oxygen
Flooded Marsh
Organisms?
Aquatic Plants Die
Heterotrophic microorganisms decompose tissues
Aerobic heterotrophic organisms use oxygen
Oxygen becomes depleted in water; it cannot
diffuse fast enough to support aerobic heterotrophs
Anaerobic heterotrophs become dominant
Anaerobic Heterotrophic Organisms
Can use energy stored in complex carbon
compounds in the absence of free oxygen
The energy is obtained by exchanging
electrons with elements other than oxygen.
Nitrogen (nitrate)
Sulfur (sulfate)
Iron (Fe3+)
C6H12O6 + 3NO3
- + 3H2O = 6HCO3
- + 3NH4
+
1796 kJ
C6H12O6 + 3SO4
2- + 3H+ = 6HCO3
- + 3HS-
453 kJ
C6H12O6 + 6O2 → 6CO2 + 6H2O 2880 kJ
Anaerobic respiration is less efficient
and produces less energy.
Therefore, anaerobic decomposition is
much slower than aerobic decomposition.
Flooded Soils
additions
Losses (CO2)
Accumulation of organic
matter at the soil surface
Organic matter is added to the
soil faster than it can be
decomposed by microorganisms
Organic matter
limestone
anaerobic decomposition
of organic matter is
much slower than aerobic
decomposition.
Buildup of Organic soils
Organic matter decomposes slowly
when submerged in water.
(anaerobic decomposition)
Soils throughout the glades historically have
been submerged. (anaerobic conditions)
Led to vast amounts of organic matter
accumulation, sometimes >10 ft. thick.
Organic matter continues
to accumulate as long as
flooded conditions persist.
EAA
Drainage exposes soils
to oxygen and decomposition
by aerobic heterotrophic
organisms which can more
efficiently decompose
organic matter
Drainage
additions
Losses (CO2)
Aerobic decomposition
(much more efficient)
Conversion from anaerobic to
Drainage
Losses of organic matter
by decomposition exceed
new additions – soils disappear
C6H12O6 + 6O2 → 6CO2 + 6H2O
Subsidence of Organic soils
up to 10 feet
1912 to 2000
Public Funding Issues Revisited in State’s Buyout of U.S. Sugar
South Florida Business Journal - by Paul Brinkmann
a bill in the Florida Senate that would require voter approval
of any certificates of appreciation (bonds) issued by water districts.
Comprehensive Everglades Restoration Plan
restoration, preservation, and protection of the South Florida ecosystem
provide for water supply and flood protection
recover and sustain those essential hydrological and biological
characteristics that defined the original pre-drainage Everglades
Restoration of More Natural Flow Regimes
interconnected and interrelated wetlands
reestablishment of native plant communities
Low levels of nutrients
Next: Phosphorus and South Florida

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Lecture 19 Phosphorous.ppt

  • 2. Organic Phosphorous Components of soil organic matter and plant tissue Phosphate sugars Nucleic Acids (DNA/RNA) ATP Phospholipids ATP
  • 3. Importance Essential Macronutrient Limiting Resource Present in Fertilizers, animal wastes, wastewater Availability can be very limited
  • 4. Fertility 10 -15% of applied fertilizer phosphorous used by plants 85 – 90% is bound to soil particles or forms insoluble solids =>excess application =>saturation of soil capacity => mobility in the environment -Total soil phosphorous is low -Most of the total is unavailable to plants -Much of soil P forms insoluble solids (limiting to availability)
  • 7. Plant Availablity H2PO4 - HPO4 -2 pH 3-6 pH 8-11 pH 6-8 Optimum pH = 6.5 for mineral soils Most Available
  • 9. Acid Soils (Low pH) Aluminum and Iron availability increased at low pH Al(OH)3 FeOOH Solubility increased Al3+ Fe3+ Al(OH)3 + 3H+ = Al3+ + 3H2O example
  • 10. Aluminum Precipitation at Low pH H2PO4 - (pH 3-6) Al3+ + H2PO4 - + 2H20 = Al(OH)2H2PO4 + 2H+ (Insoluble) Al(PO4) • H2O Variscite Al3+ + PO4 -3 = Al(PO4) simplified Form of available P at low pH: H2PO4 - combines with free Al3+ and Fe3+
  • 12. Calcium Binding in Basic Soils CaCO3 CaCO3 + 2H2(PO4)- = Ca [H2(PO4)]2 + CO3 2- CaHPO4 Ca5(PO4)3OH (Apatite mineral) (higher calcium availability) H2(PO4)- is the available form of P
  • 13. Availability and pH Low pH High pH Aluminum and Iron phosphates Calcium Phosphates Formation of insoluble solids
  • 14. Reaction with Soil Minerals
  • 15. Fixation on Iron and Aluminum A dominant interaction between Phosphorus and soils is strong interaction with Iron and Aluminum Oxides Al Al OH OH OH Fe Fe OH OH OH
  • 18. Coatings on Sands and Silicate Clays Fe coating Fe Fe OH OH H2(PO4)-
  • 19. Organic Matter Organic matter does not typically bind strongly with phosphorus. Organic matter covers fixation sites Organic matter reacts with free Fe and Al Organic matter competes for anion exch. sites Organic Matter tends to increase P availability
  • 20. -Plant Available -Fe, Al bound -Calcium bound - Fixed on oxides H2PO4 - HPO4 -2 Al(PO4) • H2O Ca3(PO4)2 H2PO4 - Inorganic Soil Phosphorous Inorganic (low) Phosphorus is generally removed from solution by soil processes These processes have a finite capacity to retain phosphorus When the capacity is exceeded, phosphorus can become mobile.
  • 21. South Florida and Phosphorus
  • 22. Historic flow patterns in the Kissimmee – Okeechobee – Everglades system has been significantly altered, beginning in the late 1800’s. The design was to drain significant areas for agriculture and development and to prevent floodwaters from communities to the south and east. Historic Flow Patterns Okeechobee and the Everglades
  • 24. "The first and most abiding impression is the utter worthlessness to civilized man, in its present condition, of the entire region." Buckingham Smith 1835 First Survey In 1850, the Swamplands Act Passed Population: 87,445 Transferred 20 million aces to FL for drainage and reclamation
  • 25. 11 miles (17.7 km) of canal south of Lake Okeechobee towards Miami. 1881 Hamilton Disston 50,000 acres drained Okeechobee north to Kissimmee and west to the Gulf of Mexico.
  • 26. 1904 “pestilence-ridden swamp” Empire of the Everglades Broward Elected
  • 27. 1905 Everglades Drainage District Authorized Canals, taxes By 1920, 4 major canal systems linked Okeechobee to the Atlantic,
  • 29. Melaleuca Tree 1906 Invasive ornamental 359,000 acres displaces native vegetation 6-12 ft. growth per year
  • 30. 1928 1911 1914-1918 Florida East Coast Railway Tamiami Trail WWI Flagler
  • 31. 1928 Belle Glade Hurricane 135 mph winds 20-foot deep floodwaters South of Okeechobee 3000 to 8000 dead
  • 32. 143 miles of levee 45 feet high and 150 feet wide After the storm Hoover Dike 19 water control structures
  • 33. Hoover Dike (1932) Everglades Agricultural Area (EAA) Perimeter Levee (1954) Water Conservation Areas (management of flow) Former extent of Kissimmee Basin and floodplain To Gulf To Atlantic Drainage
  • 35. Phosphorus loading to S. Florida Ecosystem Inputs North and South of Okeechobee Dairy/Beef Crop Production Kissimmee Basin
  • 36. Sugar, Rice, Veg. 700,000 ac EAA Crops: Everglades Agricultural Area
  • 37. 1940’s thousands of acres converted to agricultural production 1959 Cuban exiles established sugar plantations 1960s Sugar production increased 4-fold Today, sugarcane production contributes two-thirds of the economic production of Everglades agriculture, and uses nearly 80% of the crop land in the EAA Sugar and vegetable production contributes phosphorus to the ecosystem primarily through fertilizers and to a lesser extent through decomposition of plants. EAA 382,000 acres 46% U.S. Palm Beach, Glades, Hendry Sugar
  • 38. Celery 260 200 140 80 20 0 0 0 0 Endive 200 175 150 125 100 75 50 25 0 Escarole 200 175 150 125 100 75 50 25 0 Lettuce (Head) 200 175 150 125 100 75 50 25 0 Radish 100 40 0 0 0 0 0 0 0 Romaine 200 175 150 125 100 75 50 25 0 Sugar Cane 120 100 80 40 20 0 0 0 0 Phosphorus Fertilization (lbs/ac) Low Soil P V. High Soil P
  • 39. Phosphorus loading to S. Florida Ecosystem Inputs North and South of Okeechobee Dairy/Beef Agriculture Kissimmee Basin
  • 40. Dairy and Beef Kissimmee drainage basin 12,000 km2 In 1521 Ponce de Leon brought horses and cattle to Florida, making it the oldest cattle raising state in the country. No other part of our country had cattle until the Pilgrims brought cattle in the early 1600's Florida's ranchers now raise the third largest number of cattle of any state east of the Mississippi (1947)
  • 41. Phosphorus Solid Manure: 5.5 g / kg total Phosphorus One cow can excrete between 40 and 60 g of phosphorus per day Subject to movement via runoff, stream flow, soil water movement, and groundwater movement
  • 42. Cattle and Dairy Okeechobee, Highlands, and Glades Counties: 328,000 head (19% of total) Okeechobee County is ranked number one for all cattle in the state
  • 43. The Kissimmee river alone contributes about 20% of the phosphorus flowing into Lake Okeechobee The Lower Kissimmee River Basin is among largest sources of external phosphorus loading to Lake Okeechobee Kissimmee – Okeechobee - Everglades Okeechobee, in turn, is a source of phosphorus to the Everglades
  • 44. Surface Water Improvement Management Act: SWIM SWIM Plan priority basins Mandates phosphorus load level of 397 tons/yr Clean Water act: 154.3 tons per year deadline of January 1, 2015 Lake (1987) Target level of 40 ppb in Lake Okeechobee
  • 45. The Dairy Rule (1987) creating lagoons to capture and contain dairy waste Dairy Buy-Out Program to facilitate removal of animals from dairies not able to comply Works of the District Rule permits are required for all discharges into waterways Implement Best Management Practices (BMPs) buffer areas around places animals congregate, eliminating phosphorus fertilization near tributaries, reducing phosphorus imports in animal feeds, reducing animal density Some Strategies 19 of 45 Dairies Remain
  • 46. SWIM target: 397 tons Phosphorus Loads to Okeechobee Above Target 2007: 146 ton reduction of P entering Okeechobee Above SWIM target (tons)
  • 47. Phosphorus concentrations in the Lake remain at about 117 ppb The target level is 40 ppb. 2007: 146 ton reduction of P entering Okeechobee
  • 48. Internal Loading Decomposition of submerged aquatic vegetation releasing phosphorus back into the water column Dissolution of compounds in sediments which bind and store phosphorus. Two Sources
  • 49. Phosphorus and Iron Phosphorus has a strong affinity for iron FePO4 Solid Precipitate Readily incorporates into bottom sediments Internal Loading
  • 50. Internal Loading Dissolved phosphorus combines with oxidized iron (Fe3+) to create an insoluble compound that becomes buried in lake sediments. If oxygen contents are reduced (anoxic bottom sediments) the Fe3+ converts to Fe2+ which solubilizes the compound returning P to water. P released by sediments is taken up by photosynthetic algae faster than it can be returned to the sediments Fe3+ + PO4 3- = Fe(PO4) solid (PO4) Fe to water 2+ Fe3+ high oxygen Fe2+ low oxygen 3- Simplified:
  • 51. RECOMMENDATION – Control Internal Phosphorus Loading. Phosphorus-rich mud sediments need to be removed from the lake to the maximum extent that is practical, in order to reduce internal phosphorus loading. Unless this internal loading is substantially reduced, it may take as long as 100 years for the lake to respond to watershed phosphorus control programs. Lake Okeechobee Action Plan Developed by the Lake Okeechobee Issue Team December 6, 1999
  • 53. Hoover Dike (1932) Everglades Agricultural Area (EAA) Perimeter Levee (1954) Water Conservation Areas (management of flow) Former extent of Kissimmee Basin and floodplain To Gulf To Atlantic
  • 55. Sugar, Rice, Veg. 700,000 ac EAA Crops: Everglades Agricultural Area
  • 56. Florida to Buy Out Sugar Land for Everglades Restoration WTVJ NBC 6 June 25, 2008: WEST PALM BEACH, Florida -- The largest U.S. producer of cane sugar, U.S. Sugar Corp., would close up shop in a $1.75 billion deal to sell its 292 square miles of land to Florida for Everglades restoration, the company president and Florida Governor Charlie Crist said Tuesday. The deal, announced at a news conference at the Arthur R. Marshall Loxahatchee National Wildlife Refuge, allows the state to buy U.S. Sugar's holdings in the Everglades south of Lake Okeechobee, the heart of the wetland ecosystem. 186,000 acres
  • 57. Organic soils possessing high natural fertility Historically flooded
  • 58. Under flooded conditions, oxygen levels tend to be low The diffusion of oxygen through water is about 1000 times slower than diffusion through air Water restricts the movement of oxygen Flooded Marsh Organisms?
  • 59. Aquatic Plants Die Heterotrophic microorganisms decompose tissues Aerobic heterotrophic organisms use oxygen Oxygen becomes depleted in water; it cannot diffuse fast enough to support aerobic heterotrophs Anaerobic heterotrophs become dominant
  • 60. Anaerobic Heterotrophic Organisms Can use energy stored in complex carbon compounds in the absence of free oxygen The energy is obtained by exchanging electrons with elements other than oxygen. Nitrogen (nitrate) Sulfur (sulfate) Iron (Fe3+)
  • 61. C6H12O6 + 3NO3 - + 3H2O = 6HCO3 - + 3NH4 + 1796 kJ C6H12O6 + 3SO4 2- + 3H+ = 6HCO3 - + 3HS- 453 kJ C6H12O6 + 6O2 → 6CO2 + 6H2O 2880 kJ Anaerobic respiration is less efficient and produces less energy. Therefore, anaerobic decomposition is much slower than aerobic decomposition.
  • 62. Flooded Soils additions Losses (CO2) Accumulation of organic matter at the soil surface Organic matter is added to the soil faster than it can be decomposed by microorganisms Organic matter limestone anaerobic decomposition of organic matter is much slower than aerobic decomposition.
  • 63. Buildup of Organic soils Organic matter decomposes slowly when submerged in water. (anaerobic decomposition) Soils throughout the glades historically have been submerged. (anaerobic conditions) Led to vast amounts of organic matter accumulation, sometimes >10 ft. thick. Organic matter continues to accumulate as long as flooded conditions persist.
  • 64. EAA Drainage exposes soils to oxygen and decomposition by aerobic heterotrophic organisms which can more efficiently decompose organic matter Drainage
  • 65. additions Losses (CO2) Aerobic decomposition (much more efficient) Conversion from anaerobic to Drainage Losses of organic matter by decomposition exceed new additions – soils disappear C6H12O6 + 6O2 → 6CO2 + 6H2O
  • 66. Subsidence of Organic soils up to 10 feet
  • 68. Public Funding Issues Revisited in State’s Buyout of U.S. Sugar South Florida Business Journal - by Paul Brinkmann a bill in the Florida Senate that would require voter approval of any certificates of appreciation (bonds) issued by water districts.
  • 69. Comprehensive Everglades Restoration Plan restoration, preservation, and protection of the South Florida ecosystem provide for water supply and flood protection recover and sustain those essential hydrological and biological characteristics that defined the original pre-drainage Everglades Restoration of More Natural Flow Regimes interconnected and interrelated wetlands reestablishment of native plant communities Low levels of nutrients
  • 70. Next: Phosphorus and South Florida