OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING,

Slides:

Advertisements

Similar presentations

Nitrogen Cycle Ch.2.2.

Advertisements

Nitrogen Fixation: Nitrogen fixation is one process by which molecular nitrogen is reduced to form ammonia. Ammonification: The chemical transformation.

What is the Nitrogen cycle The nitrogen cycle is the biogeochemical cycle that describes the transformations of nitrogen and nitrogen- containing compounds.

Printable Nitrogen Cycle Interactive Nitrogen Cycle

Soil Biogeochemical Cycles Carbon, Nitrogen, Phosphorus.

Nitrogen Cycle The nitrogen cycle is the movement of nitrogen through different environmental segments.

Learning outcomes Describe the cycle of carbon through the ecosystem Describe how humans have affected the carbon cycle.

Nitrogen Cycle Sources Lightning Inorganic fertilizers Nitrogen Fixation Animal Residues Crop residues Organic fertilizers.

Lecture 8 NITROGEN GES175, Science of Soils. Slide 8.2.

Nitrogen Cycle Topic 1016 D Matt Jakubik. Facts Earth’s Atmosphere is almost 80 % nitrogen (N2) Earth’s Atmosphere is almost 80 % nitrogen (N2) Most nitrogen.

Nutrient Circulation Waste is in the form of dead organisms: animals/ plants/ leaves faeces urine All can contain nutrients and/or energy If the nutrients.

NITROGEN FIXATION 3 methods. 1.LIGHTENING a. high temps cause nitrogen & oxygen to for nitrogen monoxide b. this is oxidized by oxygen to form nitrogen.

The Nitrogen Cycle.

Core Training Feb 9th In-Service

Role of Bacteria in Nitrogen Cycle

Sensor Based Technology for Predicting Soil Organic Carbon (Organic Matter) Kent Martin.

(commercial fertilizers)

Role of microorganisms in the cycling of elements

NITROGEN CYCLE Explains how NITROGEN moves through an ecosystem.

Soil Biogeochemical Cycles Carbon, Nitrogen, Phosphorus.

Nitrogen Cycle. Nitrogen Most abundant element in the atmosphere 78% of the air we breathe is N ₂.

Nitrogen Cycle.

NITROGEN CYCLE. Nitrogen Cycle  All organisms use nitrogen in DNA and Proteins  Most abundant form element in atmosphere  Forms of Nitrogen:  NH 4.

NITROGEN CYCLE. What does this have to do with me?

Soil Biogeochemical Cycles Carbon, Nitrogen, Phosphorus.

Nutrient Cycles. Learning Objectives Understand the role of organic breakdown in nutrient cycles Be able to draw a diagram of the carbon cycle Understand.

Nitrogen cycle Chien-Ming Li MD, Ph.D.. Nitrogen cycle 1.Nitrogen fixation 2.Ammonification 3.Nitrification 4.Assimilation 5.denitrification.

Learning objectives Success criteria Decomposition and the nitrogen cycle Describe the role of decomposers in the decomposition of organic material Describe.

1. What is Nitrogen?  N makes up about 78% of our atmosphere.  N in the atmosphere it is mostly in the form of ______, which is a compound that plants.

Nitrogen Cycle Describe the role of decomposers in the decomposition of organic material. Describe how microorganisms recycle nitrogen within ecosystems.

THE NITROGEN CYCLE.

Soil Biogeochemical Cycles

Nitrogen Cycle.

Cycles of the Earth & Biogeochemical Cycles Nitrogen Cycle

What is nitrogen?. What is nitrogen? Nitrogen is in the Nonmetals Group Periodic Table.

The Nitrogen Cycle Chapter 16.3.

Nutrient Recycling – The Nitrogen Cycle

Nutrient Cycling Chapter 7.

Submitted by, SREEJITH P S4 EEE ROLL NO:- 54

Nutrient Cycles aka Biogeochemical Cycles

NITROGEN CYCLE.

THE NITROGEN CYCLE Lecture-1 Ecological Management

Nitrogen, Carbon, Phosphorus and Water Cycles

Soil Biogeochemical Cycles

Nitrogen Fixation.

Norman Borlaug Mother Teresa 1914 –

Why is NITROGEN Important?? Proteins and Amino Acids

Environmental Microbiology

Printable Nitrogen Cycle Interactive Nitrogen Cycle

The Nitrogen Cycle Nitrogen gas (N2)

co2 co2 co2 co2 O2 co2 co2 co2 Oceans co2 Fossil fuels

OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING,

OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING,

IV. Wastewater Treatment Topic IV. 3

Volcanoes (6.5%) 6 lbs/ac/yr in rainfall SO42- H2S Additions of Sulfur

OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING,

OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING,

OSU Corn Algorithm.

OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING,

Nitrogen cycle.

GES175, Science of Soils Lecture 8 NITROGEN.

Why is NITROGEN Important?? Proteins and Amino Acids

MOVEMENT BETWEEN PLANTS ANIMALS BACTERIA ATMOSPHERE SOIL

Why is NITROGEN Important?? Proteins and Amino Acids

Nitrogen Cycle review.

Printable Nitrogen Cycle Interactive Nitrogen Cycle

OXIDATION STATES ORGANIC MATTER PLANT AND ANIMAL RESIDUES AMINIZATION

Presentation transcript:

OXIDATION STATES ATMOSPHERE N2O NO N2 INDUSTRIAL FIXATION LIGHTNING, Haber Bosch ATMOSPHERE GLOBAL WARMING 15-40 kg/ha pH Rainfall TEMP N2O NO N2 INDUSTRIAL FIXATION LIGHTNING, RAINFALL N2 FIXATION PLANT AND ANIMAL RESIDUES HABER BOSCH 3H2 + N2 2NH3 (1200°C, 500 atm) OC Lignin SYMBIOTIC NON-SYMBIOTIC MESQUITE RHIZOBIUM ALFALFA SOYBEAN BLUE-GREEN ALGAE AZOTOBACTER CLOSTRIDIUM MATERIALS WITH N CONTENT > 1.5% (COW MANURE) MATERIALS WITH N CONTENT < 1.5% (WHEAT STRAW) 10-80 kg/ha FERTILIZATION PLANT LOSS AMINO ACIDS MICROBIAL DECOMPOSITION 0-50 kg/ha NH3 IMMOBILIZATION AMMONIA VOLATILIZATION AMINIZATION ORGANIC MATTER HETEROTROPHIC R-NH2 + ENERGY + CO2 BACTERIA (pH>6.0) FUNGI (pH<6.0) R-NH2 + H2O pH>7.0 NH2OH AMMONIFICATION FIXED ON EXCHANGE SITES IMMOBILIZATION R-OH + ENERGY + 2NH3 MICROBIAL/PLANT SINK Pseudomonas, Bacillus, Thiobacillus Denitrificans, and T. thioparus N2O2- 2NH4+ + 2OH- MINERALIZATION + NITRIFICATION +O2 NO2- Nitrosomonas DENITRIFICATION NO3- POOL NITRIFICATION OXIDATION STATES 2NO2- + H2O + 4H+ DENITRIFICATION LEACHING LEACHING VOLATILIZATION NITRIFICATION Nitrobacter + O2 NH3 AMMONIA -3 NH4+ AMMONIUM -3 N2 DIATOMIC N 0 N2O NITROUS OXIDE 1 NO NITRIC OXIDE 2 NO2- NITRITE 3 NO3- NITRATE 5 Joanne LaRuffa Wade Thomason Shannon Taylor Heather Lees Department of Plant and Soil Sciences Oklahoma State University ADDITIONS TEMP 50°F LEACHING LEACHING LOSSES LEACHING OXIDATION REACTIONS pH 7.0 REDUCTION REACTIONS 0-40 kg/ha