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INTRODUCTION
• IT IS A BIOGEOCHEMICAL CYCLE THAT DESCRIBES THE
MOVEMENT OF PHOSPHOROUS IS EXCHANGED AMONG THE
BIOSPHERE, LITHOSPHERE,AND HYDROSPHERE OF EARTH.
• UNLIKE MANY OTHER BIOGEOCHEMICAL CYCLE THE
ATMOSPHERE DOES NOT PLAY A SIGNIFICANT ROLE IN THE
MOVEMENT OF PHOSPHOROUS
• PHOSPHOROUS IS AN IMPORTANT CONSTITUENT OF
PROTOPLASM AND REQUIRED FOR METABOLISM OF ALL
LIVING ORGANISM.
• CARBON : NITROGEN : PHOSPHOROUS – 98 : 8.3 : 1
CARRINGTON SALT LOAM SOIL.
SOURCES
• ROCK DEPOSITS (SEDIMENTS)
• AGRICULTURE CROPS CONTAIN 0.05-0.5%
• ORGANIC FORMS- IN FORM OF PHYTIN, PHOSPHOLIPIDS,
NUCLEIC ACID, PHOSPHORYLATED SUGAR, COENZYMES,
ACID
• ADENOSINE TRIPHOSPHATE(ATP)
• SOIL IS RICH IN ORGANIC PHOSPHOROUS
STEPS OF PHOSPHOROUS CYCLE
• WEATHERING OF ROCKS – THE PHOSPHATE SALTS ARE
BROKEN DOWN FROM ROCK FROM THEIR THEY WASHED
AWAY INTO THE GROUND WHERE THEY MIX IN THE SOIL.
• ABSORPTION BY PLANTS- PHOSPHATE SALT FROM SOIL
ARE ABSORBED BY PLANTS . PLUS ADDED FERTILIZERS
ARE SOURCE OF PHOSPHOROUS.
• ABSORPTION BY ANIMALS – ANIMALS ABSORB IT FROM
PLANTS.
• RETURNING TO THE ENVIRONMENT THROUGH
DECOMPOSITION- AFTER THE DEATH OF PLANTS AND
ANIMALS BY THE PROCESS OF DECOMPOSITION IT GET
MIXES INTO THE SOIL AGAIN. WHICH ENDS UP INTO
SEDIMENTS AGAIN.
PROCESS INVOLVED
ALTERATION OF SOLUBILITY OF INORGANIC COMPOUNDS
OF PHOSPHOROUS
MINERALISATION OF ORGANIC PHOSPHATE COMPOUNDS
WITH THE RELEASE OF INORGANIC PHOSPHATE
IMMOBILISATION OF PHOSPHOROUS – CONVERSION OF
INORGANIC PHOSPHOROUS INTO ORGANIC FORM
ASSIMILATION- UTILISATION OF PHOSPHOROUS BY
MICROBIAL CELL TO MAKE CELL COMPONENTS
OXIDATION/REDUCTION REACTION OF INORGANIC
PHOSPHOROUS (PI) - EXIST IN TWO FORMS – (-3 FORM OF
PHOSPHINE AND +5 FORM OF ORTHOSPHOSPHATE)
ORGANIC PHOSPHATE COMPOUNDS(PHYTIN, PHOSPHOLIPIDS,
NUCLEIC ACID) ARE MINERALIZED TO ORTHOPHOSPHATE BY A
WIDE RANGE OF MICROORGANISMS THAT INCLUDE BACTERIA
(Bacillus subtilis, Arthrobacter), ACTINOMYCETES
(Streptomyces) AND FUNGI (Aspergillus, Penicillium)
CLEAVAGE OF PHOPHOROUS FROM ORGANIC MATTER IS DONE
BY PHOSPHATASE
MYCORRHIZAL FUNGI EXTRACT PHOSPHOROUS FROM SOIL
PHOSPHATE ALSO RETURN TO SOIL AND WATER THROUGH
DECAY EXCRETA AND DEAD BODIES OF ORGANISM
MINERALISATION
IMPORTANCE OF PHOSPHOROUS CYCLE
• VERY IMPORTANT FOR ALL ORGANISM
• COMPONENTS OF CELL MEMBRANE, NUCLEIC ACID,
• AS ATP PARTICIPATES IN RESPIRATION.
• IN ANIMALS- PART OF BONES AND TEETH
PHOSPHOROUS CYCLE by Pranzly.pptx

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PHOSPHOROUS CYCLE by Pranzly.pptx

  • 1.
  • 2. INTRODUCTION • IT IS A BIOGEOCHEMICAL CYCLE THAT DESCRIBES THE MOVEMENT OF PHOSPHOROUS IS EXCHANGED AMONG THE BIOSPHERE, LITHOSPHERE,AND HYDROSPHERE OF EARTH. • UNLIKE MANY OTHER BIOGEOCHEMICAL CYCLE THE ATMOSPHERE DOES NOT PLAY A SIGNIFICANT ROLE IN THE MOVEMENT OF PHOSPHOROUS • PHOSPHOROUS IS AN IMPORTANT CONSTITUENT OF PROTOPLASM AND REQUIRED FOR METABOLISM OF ALL LIVING ORGANISM. • CARBON : NITROGEN : PHOSPHOROUS – 98 : 8.3 : 1 CARRINGTON SALT LOAM SOIL.
  • 3. SOURCES • ROCK DEPOSITS (SEDIMENTS) • AGRICULTURE CROPS CONTAIN 0.05-0.5% • ORGANIC FORMS- IN FORM OF PHYTIN, PHOSPHOLIPIDS, NUCLEIC ACID, PHOSPHORYLATED SUGAR, COENZYMES, ACID • ADENOSINE TRIPHOSPHATE(ATP) • SOIL IS RICH IN ORGANIC PHOSPHOROUS
  • 4.
  • 5.
  • 6. STEPS OF PHOSPHOROUS CYCLE • WEATHERING OF ROCKS – THE PHOSPHATE SALTS ARE BROKEN DOWN FROM ROCK FROM THEIR THEY WASHED AWAY INTO THE GROUND WHERE THEY MIX IN THE SOIL. • ABSORPTION BY PLANTS- PHOSPHATE SALT FROM SOIL ARE ABSORBED BY PLANTS . PLUS ADDED FERTILIZERS ARE SOURCE OF PHOSPHOROUS. • ABSORPTION BY ANIMALS – ANIMALS ABSORB IT FROM PLANTS. • RETURNING TO THE ENVIRONMENT THROUGH DECOMPOSITION- AFTER THE DEATH OF PLANTS AND ANIMALS BY THE PROCESS OF DECOMPOSITION IT GET MIXES INTO THE SOIL AGAIN. WHICH ENDS UP INTO SEDIMENTS AGAIN.
  • 7. PROCESS INVOLVED ALTERATION OF SOLUBILITY OF INORGANIC COMPOUNDS OF PHOSPHOROUS MINERALISATION OF ORGANIC PHOSPHATE COMPOUNDS WITH THE RELEASE OF INORGANIC PHOSPHATE IMMOBILISATION OF PHOSPHOROUS – CONVERSION OF INORGANIC PHOSPHOROUS INTO ORGANIC FORM ASSIMILATION- UTILISATION OF PHOSPHOROUS BY MICROBIAL CELL TO MAKE CELL COMPONENTS OXIDATION/REDUCTION REACTION OF INORGANIC PHOSPHOROUS (PI) - EXIST IN TWO FORMS – (-3 FORM OF PHOSPHINE AND +5 FORM OF ORTHOSPHOSPHATE)
  • 8. ORGANIC PHOSPHATE COMPOUNDS(PHYTIN, PHOSPHOLIPIDS, NUCLEIC ACID) ARE MINERALIZED TO ORTHOPHOSPHATE BY A WIDE RANGE OF MICROORGANISMS THAT INCLUDE BACTERIA (Bacillus subtilis, Arthrobacter), ACTINOMYCETES (Streptomyces) AND FUNGI (Aspergillus, Penicillium) CLEAVAGE OF PHOPHOROUS FROM ORGANIC MATTER IS DONE BY PHOSPHATASE MYCORRHIZAL FUNGI EXTRACT PHOSPHOROUS FROM SOIL PHOSPHATE ALSO RETURN TO SOIL AND WATER THROUGH DECAY EXCRETA AND DEAD BODIES OF ORGANISM MINERALISATION
  • 9. IMPORTANCE OF PHOSPHOROUS CYCLE • VERY IMPORTANT FOR ALL ORGANISM • COMPONENTS OF CELL MEMBRANE, NUCLEIC ACID, • AS ATP PARTICIPATES IN RESPIRATION. • IN ANIMALS- PART OF BONES AND TEETH