22: Biogeochemistry - Soil N and P Flashcards
Nitrogen (N) cycle
Nitrogen is the most limiting nutrient for plant growth
Is disrupted at the global level by industrial fixation of atmospheric N, leading to environmental pollution
This cycle is also ‘leaky’—it exchanges with other compartments - environmental pollution
Chemical forms of N
Takes 9 different forms in soil, transformations catalyzed by enzymes (these 9 different forms have different oxidation states)
Major processes in the N cycle
Biological N fixation
Mineralization/immobilization
Nitrification
Denitrification
Biological N fixation
Conversion of nitrogen gas in air to plant available N
Soil prokaryotes use nitrogenase to break the triple bond in N2
Mineralization/immobilization
Mineralization (ammonification) - organic N converted to mineral form (NH4+); common among microbes (organoheterotrophs)
Immobilization (assimilation) - mineral N taken up by microbes, converted to organic forms; common among all microbes
- Can limit plant growth and productivity depending on the C:N ratio of the organic matter
- Leads to competition between plants and microorganisms for soil inorganic N
Nitrification
The oxidation of ammonia into nitrate. Proceeds in 3 steps carried out by microorganisms
Conditions leading to nitrification
Oxidation (needs good soil aeration)
High ammonium availability
Warm, moist, but well-aerated soils
Nitrate leaching
NO3- is ‘washed out’ of the root zone and slowly moves out of the soil
Can lead to eutrophication of water courses
Denitrification
Reduction of nitrate back to nitrogen gasses
Performed by microorganisms
What soil conditions lead to higher denitrification rates?
High soil NO3- concentrations
Water saturation
High soil organic matter contents
Terrestrial phosphorus (P) cycle
P is one of the 3 primary plant macronutrients - regulates photosynthesis and plant primary productivity
Also a nutrient for microbes and soil biota, C:P ratios regulate mineralization
Can cause eutrophication of water systems when leached out of the soil
Sorption of phosphates
Phosphate is adsorbed into positively charged colloids in the soil (like aluminum and iron oxides, organic matter, clays with pH-dependent charges)
Precipitation of phosphate
Tend to react with cations to form secondary soil minerals: calcium, iron, and aluminum phosphates. Precipitation reactions depend largely on soil pH. There is only a very narrow range of soil pH where phosphates are soluble.
Precipitation is a chemical process that removes phosphate from water to form solid precipitates