1/40
Soils exam 3 review
Name | Mastery | Learn | Test | Matching | Spaced |
|---|
No study sessions yet.
Nitrogen role
major part of amino acids, the building block of proteins and enzymes. Also important for chlorophyll.
Nitrogen deficiency signs
stunted, thin stems, chlorosis of entire leaf including veins with oldest leaves showing first. Mobile from old to new.
Nitrogen oversupply signs in plants
Enlarged but weak cells, lodging, delayed maturity, disease and pest susceptibility.
Nitrogen forms taken up
Dissolved Nitrate and ammonium
Nitrogen distribution (pools)
Most in atmosphere or crustal rock
Nitrogen distribution (fluxes)
Atmospheric nitrogen is held in triple bonds, must be fixed to be usable. Leaching transfers from land to water. Is returned back to the atmosphere via denitrification by microbes.
Nitrogen immobilization
the soil becomes devoid of nitrogen when microorganisms require more N than the soil can provide. They scavenge nitrate and ammonium.
Nitrogen mineralization
Most soil nitrogen is in large unobtainable organic molecules so it must be converted to inroganic forms like nitrate and ammonium.
Ammonia volatilization
Alkaline soils (pH > 7) promote the conversion of ammonium to ammonia gas, increasing volatilization.
nitrification
Nitrosomonas first oxidize ammonium to nitrite. Then nitrobacteria convert the nitrite to nitrate, increasing acidity.
ammonification
decomposers convert organic nitrogen from dead organisms or waste into ammonium
denitrification
nitrate converted to gaseous forms (N2). The final step of the N cycle.
N fixation
N2 to NH3 via the niotrogenase enzyme.
Phosphorous deficiency signs
stunted, thin stems, dark leaves, older leaves show fir4st
phosphorous role
essential to ATP, DNA, RNA, enhances flowering, fruiting, maturation, and photosynthesis
potassium role
an activator for cellular enzymes, adjusts osmotic balance, opens stomatesp
potassium deficiency signs
leaf tip chlorosis or tearing edges first in older leaves.
The 4 available forms of potassium
in primary minerals
non exchangeable in secondary minerals
exchangeable on colloid surfaces
soluble in water
The 3 forms of phosphorous
organic (labile or protected)
calcium bound (inorganic)
Fe/Al bound (inorganic)
the types of organic phosphourous
Di and monoester, phospholipids derived from cell membranes
Under what type of C/N ratio is phosphorous immobilization likely
high C/N ratio
Calcium role
component of cell walls (stiffness), cell elongation and division, membrane permeability, enzyme
calcium deficiency signs
stuck leaves, stunted meristem, blossom end rot, poor roots
the 3 forms of calcium
minerals
organic complexes
exchange sites
magnesium role
central component of chlorophyll molecule, synthesis of oils and proteins, enzyme activation for metabolism
magnesium deficiency signs
chlorosis everywhere but veins, first appearing in older leaves
serpentine soils
little calcium, weathering from mafic soils
silicon is
the second most abundant element in crust
silicon role
rigidity, stimulates growth, alleviates other deficiencies/toxicity
phytolith
microscopic silica in cell walls that provides support and repels herbivores or fungal disease
hemicellulose vs cellulose
cellulose is a strong rigid chain like polymer while hemicellulose is weaker and branch like.
types of labile organic matter
living biomass, detritus, partially degraded tissue, free biomolecules
types of protected organic matter
protected tissue/cell walls , protected biomass, char
priming effect
increased decomposition of relatively stabile protected humus occurs due to enhanced biological activity.
how does C/N ratio impact rate of decomposition
low ratio speeds up decomposition while a high one causes immobilization.
immobilization
nutrients become locked up by microbial ise when they are converted from inorganic to organic
influence of climate on soil carbon
decomposition increases with warmer temps, precip erodes it away
most abundant, available form of P
carbon bound inorganic
ways plants access P
longer roots/hairs
exude compounds that release P from Fe/Al
acidify the rhizosphere to speed dissolution of Ca-P
exude enzymes that cleave P from organic compounds
exude growth stimulators to attract rhizobacteria
attract micorhizal fungi
Sulfur role
mimics that of N (protein synthesis)
sulfur deficiency signs
chlorosis of young leaves first, stunted growth