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Essential Plant Nutrients
16 Elements are Essential for Plants
O, C, H,
N, K, P, Ca, Mg, S,
Cl, Fe, B, Mn, Zn, Cu, Mo,
Si, Na
Macronutrients
Micronutrients
Species dependent
Oxidation States of Soil NOxidation States of Soil N
N Form Name Oxidation stateorganic-N -3
NH4+ ammonium -3
N2 dinitrogen gas 0
NO2- nitrite +3
NO3- nitrate +5
Fertilizer: N (first of three digit rating)
Nitrogen Nitrogen RedoxRedox ProcessesProcesses
Oxidation: loss of e-
Reduction: gain of e-
-3 +5NH4
+ NO3-
8 e- transfer
NN--cyclecycleplant & animal residues
organic-N
NH4+NO2
-
NO3-
N2
11
22
33
33
4455
(mineralization)
(nitrification)
(nitrification)
(denitrification)
(fixation)
(immobilization)
Polysaccharides (cellulose…)Organic Acids
Amino acids, Peptides, ProteinsLipids
NucleotidesPeptidesLignin
CelluloseProteinsLignin
Humus
CO2
NH3
NH3
C:N
> 25:1
C:N
10:1
Organic Matter Mineralization
4-12Bacteria
9-16Alfalfa
20-80Grass
130-400Wood
60-70Pine Needle
45-70Maple Leaf
C:NMaterial
Carbon to Nitrogen Ratios
Ammonia VolatilizationAmmonia VolatilizationUrea:
CO(NH2)2 → NH3 +CO2 + H2Ourea soil enzymes& H2O
- Most volatilization when:coarse or sandy-textured soils
low clay and low organic matter (which adsorb NH4
+)
dry alkaline surface
NitrificationNitrificationNH4
+ → NO2- → NO3
-
ammonium nitrite nitrate- oxidation of N
* Autotrophic bacteria• obtain energy from N oxidation• Nitrosomonas
NH4+ → NO2
- + energy
• NitrobacterNO2
- → NO3- + energy
NitrificationNitrification (cont’d)(cont’d)
* Rapid in well-aerated,warm, moist soils
• aerobic organisms(O2 is required)
• little NO2- accumulation
* Acid-forming processNH4
+ +3/2O2→ NO2- + 2H+ + H2O
N In
put (
met
ric to
ns x
106 )
N Input Sources to Mississippi River
Soil Mineralization
Fertilizer
DenitrificationDenitrification
Gaseous loss of N upon N reduction
+ e- + e- + e- + e-
NO3- → NO2
- → NO → N2O → N2
nitric nitrousoxide oxide
DenitrificationDenitrification (cont’d)(cont’d)* Microorganisms:
• facultative anaerobes- prefer O2 but will use NO3
-
for a terminal e- acceptor• heterotrophic
- use organic-C for energy source
* Denitrification enhanced by:• low O2 (flooding)• high O.M. (energy source)• high NO3
-
DenitrificationDenitrification (cont’d)(cont’d)* Metabolic reduction: Denitrification?
(no N gas formation)
NO3-
organisms
NO3- → NH4+ → organic-N
- N is reduced for use in protein formation
Biological Nitrogen FixationBiological Nitrogen Fixation
N2 (organisms)→ NH4+
* Symbiotic relation between * Symbiotic relation between bacteria and plants:bacteria and plants:
-- legumeslegumes++
-- rhizobiumrhizobium
Bacteria: Rhizobium genus (species specific)
R. meliloti - alfalfaR. trifolii - cloverR. phaseoli - beans
- bacteria require plant to function as N-fixers
Nitrogen FixationNitrogen Fixation
(b) Process:(b) Process:
C from plant photosynthesis
N from fixation of N2⇒⇒ symbiosissymbiosis
RhizobiumRhizobium
organicorganic--CC
NN22organicorganic--NN
Quantity of N FixedQuantity of N FixedAlfalfa and clover
≈ 100 - 250 kg N/ha/yr(mature stand, good fertility & pH)
Beans and peasless fixation but high protein food
with minimum N input
added N fertilizerlowered N fixation
Symbiotic Nodules Symbiotic Nodules -- NonlegumesNonlegumes* Actinomycetes - Frankia +
Alders and other trees
Symbiotic Symbiotic -- without noduleswithout nodules* Azolla/Anabaena complex
blue-green algae (N-fixer) in leaves offloating ferns
NonsymbioticNonsymbiotic NN--fixation:fixation:FreeFree--living Organismsliving Organisms
* Bacteria (Azotobacter, Azospirillum) and blue-green algae (Anabaena)
aerobic and anaerobic
small amounts: 5 - 50 kg/ha/yr
inhibited by available soil N