Organic Carbon Analysis

Objective

  • To determine the organic carbon content of the <63m m fraction of the sediment

Equipment and Reagents

Temperature-controlled oven, preset to 60oC + 5

Balance capable of weighing to 0.0001g

Magnetic stirrer

2 x 1litre volumetric flasks

2 x 100ml burettes graduated to 0.1ml

4 x 10ml pipettes with suction bulb

2 x beakers 0.5litre capacity

1 x 25ml measuring cylinder

A desiccator containing anhydrous silica gel

Washbottle/spray filled with distilled water

Distilled water

The following reagents need to be of analytical reagent quality

Potassium dichromate N solution. Dissolve 49.035 g of potassium dichromate in distilled water to make 1 litre of solution.

Ferrous sulphate, approximately 0.5N solution. Dissolve approximately 140g of ferrous sulphate in 0.5N sulphuric acid to make 1 litre of solution (add 14ml of concentrated sulphuric acid to distilled water to make 1 litre of 0.5N sulphuric acid solution). NOTE this solution is unstable in air and should be kept tightly stoppered. It needs to be standardised against the dichromate solution each day it is used.

Sulphuric acid, concentrated, relative density of 1.84.

Orthophosphoric acid, 85%, relative density of 1.70 to 1.75.

Indicator solution. Dissolve 0.25g of diphenylaminesulphonate in 100ml of distilled water.

Methodology

  1. Standardisation of Ferrous sulphate. 10ml of the N potassium dichromate solution is run from a burette into a 0.5litre beaker. 20ml of concentrated sulphuric acid is then added very carefully using a 25ml measuring cylinder. Swirl and allow to cool for some minutes. Add 200ml of distilled water, followed by 10ml of orthophosporic acid and 2ml of indicator (using different 10ml pipettes). Set to stir on a magnetic stirrer. Ferrous sulphate is then added from a second burette in 0.5ml increments (or as a rapid drip), until the colour of the solution changes from blue to green. A further 0.5ml of potassium dichromate is then added, turning the colour back to blue. Ferrous sulphate is then added drop by drop, with the stirrer operating, until the single drop when the colour changes from blue to green. The total volume of ferrous sulphate used (x) then needs to be recorded, to the nearest 0.05ml.

  2. Prepare a batch of up to twelve samples for analysis.

  3. Grind the sample  in a mortar and pestle to remove all aggregations.

  4. Place approximately 5g of the powder into a pre-weighed (4dp) 30ml Pyrex beaker.

  5. Oven dry  (105oC) for half a day.  With a stainless steel spatula/spoon place about 1g of sediment into a pre-weighed 25ml beaker. Weigh to 0.0001g. Add all powder to a 0.5litre beaker. Repeat for all samples, placing each weighed powder into a new beaker.

  6. Removal of carbonates (method of Shaw). Add 25ml of sulphurous acid to each 25ml beaker (sufficient for 1g of carbonate, although checking is recommended). Swirl thoroughly and leave for 3 hours minimum. Then evaporate the beakers to dryness in the oven at 60oC. NOTE this acid is gives an extremely unpleasant vapour, use a a fume cupboard.

  7. Sample titrations. 10ml of the N potassium dichromate solution is run from a burette into the 0.5litre beaker. 20ml of concentrated sulphuric acid is then added very carefully using a 10ml pipette. Swirl thoroughly for about 1 minute then allow to cool on a wooden surface for 30 minutes. Add 200ml of distilled water, followed by 10ml of orthophosporic acid and 2ml of indicator (using different 10ml pipettes). Set to stir on a magnetic stirrer. Ferrous sulphate is then added from a second burette in 0.5ml increments increments (or as a rapid drip), until the colour of the solution changes from blue to green. A further 0.5ml of potassium dichromate is then added, turning the colour back to blue. Ferrous sulphate is then added drop by drop, with the stirrer operating, until the single drop when the colour changes from blue to green. The total volume of ferrous sulphate (y)used then needs to be recorded, to the nearest 0.05ml.

  8. IMPORTANT NOTE: The total volume of potassium dichromate used to oxidise the organic matter in the soil is determined by

  9. 10.5 x (1-y/x) ml

    The correct results are only given if between 5 and 8ml of potassium dichromate are used. Analyses should be repeated if a widely different volume has been used, adjusting the weight of sample used to give the correct volume of potassium chromate oxidised. If the sample is green after the addition of the orthophosphoric acid, too much carbon is present and the sample size needs to be decreased.

  10. Enter the standardisation values and the results from each titration the EXCEL file for calculating the organic carbon content of the samples. The assumption is implicit in the calculations that approximately 77% of the carbon in the organic matter is oxidised using this method.

This methodology is based on:

British Standard BS 1377

Walkely, AJ. Agric. Sci 1935:25,598 – 609

Shaw, K. J Soil Sci. 1959, 10, 316-326