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40 Cards in this Set

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fates of mineralized nutrients

leaching


immobilization


adsorption

3 of them

compenents of OM

living biomass


•dead roots and unrecognizable material


•humus

organic carbon vs organic matter

OM = 50% OC

humification

humus becomes co2 + h2o + plant nutrients through oxidation decomposition and mineralization

becomes 3 things through 3 processes

fates of OM

•mineralization


•oxidation


•decompisition

3

how carbon is used respired/incorporated

2/3 of g respired


1/3 of g incorporated in tissues

C:N ratios

>25:1:


•immobilization of soil microorganisms


•more competition for N means mobile microorganisms uptake all N and plants suffer N deficiency


•decay is slowed


<25:1:


•no immobilization

remediate excess C with more N

components of OM

•lignins


•polyphenols


•fats and waxes


•cellulose


•hemicellulose


•crude/simple proteins


•starches and sugars

slow decomp to fast decomp

factors that increase OM and how?

more precipitation


●more plant growth


•lower temperatures


●slower decompisition


•less tillage


●less oxidation


•less drainage


●less o2 =less decomp


•high clay/silt %

5

losses of OM

erosion


•tillage


•fire


•increased Nitrogen


•plant removal


•over grazing

Importance of N % dry weight

part of amino & nucleic acids


in charge of chlorophyll


root growth


growth & overall productivity


2.5-4% dry weight


1-6% in legumes

plant available forms of N

NH4+


•ammonium


NO3-


•nitrate

effects of N deficiency

•chlerosis


yellowing of leaves in older leaves bc N is mobile


•necrotic spots


brown dead parts of leaves

effects N toxicity

ammonium toxicity


light brown scorching


•nitrate toxicity


tan colored toxicity

N fixation

lightening


•N fixing bacteria

fates of N

immobilization and mineralization

volatilization of N

high pH


•low OM%


•low clay%


•higher temps


•sandy soils

5

nitrification increases with..

good aeration


•warm soils


•dry soils


•after rain


•after spring thaw


•after tillage

ph and H+ concentration

10^-pH = h+ concentration



-log (h+ concentration) = pH

precipitation effects on pH

makes soils more acidic because it adds H+

N in Humboldt

mineralization of OM into ammonium


•august annuals dead perennials dormant=low demand for N means increase of leaching


•spring soil still too cold for mineralization but plants grow


•late spring


active mineralization


•summer


bc lack of moisture mineralization and plant growth slowed

phosphorus uses in plants

needed for atp


part of DNA RNA


phospholipid bilayer


0.2-0.4% plant matter


mobile in plants immobile in soils

what % of plants

phosphorus deficiencies

stunted growth


weak stems


poor flowering


delayed maturity


older leaves first

fates of phosphorus

adsorption and desolation


•immobilization and mineralization


•plant root uptake (enhanced by myccorhizae)

problems with phosphorus

susceptible to leaching


•most compounds unavailable to plants


•low concentration in upper layer


•10-15% used


•only available between 6-7 pH

p fixation

made unavailable to plants


least->most


2:1, 1:1, fe or al oxide

which clays fix the most

available forms of Phophorus

H2PO4


pH: 4-5.5


•HPO4


pH:>7

chelation

creation of shell around iron and aluminum

Potassium plant uses

over 80 different enzymes require K

potassium (K) deficiency

begins on tips as chlerosis then becomes necrosis as guard cells suffer

K+ cycle

minerals weather to be obtained by plants


most K ->least K


biotite feldspar muscovite

slowly available K

1-10% of K


•secondary minerals


•fixed in 2:1

readily available K+

0.1-0.2%


90% exchangeable

grass tetony

too much K in plant matter causes animals that eat it to get Mg deficiency

excess K

serpentine soils

high Mg means less K+ intake

calcareous soils

high in K means less Mg uptake

nutrient management required when:

imbalance of minerals


•removed


•leakage


•simplification


•high productivity needed

goals of nutrient management

production of high quality plants


maintain/enhance soil quality


protect the environment

liebigs law of minimum

must attend to the least abundant element before seeing a change

Argillic horizon

Ultisols

what soil tax?