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GES175, Science of Soils Lecture 8 NITROGEN Slide 8.2 Slide 8.3 Slide 8.4 Oxidation States of Soil N N Form Name Oxidation state organic-N -3 NH4+ ammonium N2 dinitrogen gas NO2- nitrite +3 NO3- nitrate +5 -3 0 (oxidation) (reduction) Nitrogen Redox Processes Oxidation: loss of eReduction: gain of e-3 +5 NH4+ NO38 e- transfer Slide 8.6 N-cycle plant & animal residues 5 5 NO3- 4 N2 organic-N 2 3 1 NO2- 3 NH4+ Mineralization vs. Immobilization Fate of N if added to soil??? Low C:N (high N content) Alfalfa, peas, grass Slide 8.8 High C:N (low N) straw, bark, sawdust Slide 8.9 Ammonia Volatilization - gaseous loss of N Ammonia Volatilization Urea: CO(NH2)2 NH3 +CO2 + H2O urea soil enzymes & H2O - Most volatilization when: coarse or sandy-textured soils low clay and low organic matter (which adsorb NH4+) dry alkaline surface Nitrification NH4+ NO2- NO3ammonium nitrite nitrate - oxidation of N * Autotrophic bacteria • obtain energy from N oxidation • Nitrosomonas NH4+ NO2- + energy • Nitrobacter NO2- NO3- + energy Nitrification (cont’d) * Rapid in well-aerated, warm, moist soils • aerobic organisms (O2 is required) • little NO2- accumulation * Acid-forming process NH4+ +3/2O2 NO2- + 2H+ + H2O Nitrogen (nitrate?) Leaching Eutrification Denitrification Denitrification Gaseous loss of N upon N reduction NO3- + e+ e+ e+ e NO2- NO N2O N2 nitric oxide nitrous oxide Denitrification (cont’d) * Microorganisms responsible: • facultative anaerobes - prefer O2 but will use N for a terminal e- acceptor • mostly heterotrophic - use organic-C for energy source (reductions require energy) Denitrification (cont’d) * Denitrification enhanced by: • low O2 (flooding) • high O.M. (energy source) • high NO3- Denitrification (cont’d) * Metabolic reduction is not denitrification (no N gas formation) organisms NO3- NO3- NH4+ organic-N - N is reduced for use in protein formation Nitrogen Fixation N2 (organisms) NH4+ * Symbiotic relation between bacteria and plants: - legumes + - rhizobium Nitrogen Fixation Bacteria: Rhizobium genus (species specific) R. meliloti - alfalfa R. trifolii - clover R. phaseoli - beans - bacteria require plant to function - inoculation of seed (coat seed with proper bacteria) Process: nodule Rhizobium (b) Process: organic-N N2 Rhizobium organic-C C from plant photosynthesis N from fixation of N2 symbiosis Quantity of N Fixed Alfalfa and clover provide 100 - 250 kg N/ha/yr (mature stand, good fertility & pH) Beans and peas less fixation but high protein food with minimum N input added N fertilizer lowered N fixation Symbiotic Nodules - Nonlegumes * Organisms l actinomycetes - Frankia * Plants l Alders and other trees Symbiotic - without nodules * Azolla/Anabaena complex blue-green algae (N-fixer) in leaves floating fern in rice paddies * Rhizosphere organisms use root exudates (C) l large areas l Nonsymbiotic N-fixation: Free-living Organisms * Bacteria and blue-green algae l aerobic and anaerobic l small amounts: 5 - 50 kg/ha/yr l inhibited by available soil N