Determination of soil organic matter (By wet method)
Organic matter
Remains of plants (roots, leaves and
shoots) and dead animals and decay of animal products can build organic
residues 9in soil.
Soil organic matter can have determined by
soil organic kits and wet chromate method (Walkley, 1947). Soil organic matter
gives you rough values. Soil cannot be used at present time. In humid regions
the organic carbon is an indicator of % organic matter in soil. In humid region
the organic carbon is high and at the same time in dry areas organic carbon iv
low as compared to the humid region.
If organic carbon is greater or equal than
50% then it is muck soil and if the organic carbon is greater or equal than 20%
then the soil is peat soil. In Pakistan the organic carbon is less than 1%.
Principle
This method involves or relies upon
oxidation of potassium dichromate by organic compound and remaining reduced
from K2Cr2O7 can further undergo oxidation reduction by ferrous sulphate
titration.
Apparatus
Dispenser, pipette, burette, magnet
stirrer, Teflon, capped stirrer.
Reagents
1.
1 N of
K2Cr2O7
2.
0.5 M
FeSO4 + 5 ml concentrated sulfuric acid
3.
Concentrated
H2SO4 (98% pure specific gravity of 1.84 w/w)
4.
Phosphoric
acid (H3PO4)
5.
Diphenyl-amine
indicator (1g of diphenylamine in100 ml of concentrated H2SO4). Don’t make
indicator in water.
Procedure
·
1g air dry
soil in 500ml beaker.
·
10ml
K2Cr2O7 in it by pipette.
·
Add 20ml
concentrated H2SO4 with the help of dispenser and then add 10ml H3PO4 by
dispenser.
·
Wait for
at least 10 minute.
·
Now add
200 ml DI water.
·
Add 10-15
drops od diphenyl indicator.
·
Now
titrate the solution with 0.5 M feslous sulphate until you don’t get green
colour.
·
Always use
two blanks samples for measurements of soil organic matter.
·
Further
these blanks samples must undergo the same procedure expect the addition of
soil.
Calculation
M= 10/ volume of blank
sample
%
oxidizable carbon (w/w) =V (blank sample) -- V (sample)
% Total
oxidized soil organic matter = 1.74 xoxidizable organic matter
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