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HJ 615-2011Soil. Determination of organic carbon. Potassium dichromate oxidation spectrophotometric method (English PDF)

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Issued by

Ministry of Ecology and Environment

Level / Type

National · Mandatory

Issue date

April 15, 2010

Implementation date

October 1, 2011

Scope

HJ 615-2011 (Soil. Determination of organic carbon. Potassium dichromate oxidation spectrophotometric method) is available as an English-translated PDF.

HJ 615-2011 — This standard specifies the potassium dichromate oxidation-spectrophotometry for the determination of organic carbon in soil. This standard applies to the determination of organic carbon in air-dried soil.

This standard does not apply to chloride ion (Cl-) content greater than 2.0 × 104 mg/kg Determination of salinized soil or salinized soil. When the sample amount is 0.5 g, the detection limit of the method is 0.06% (by dry weight), and the lower limit of determination is 0.24% (by dry weight).

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Document preview — HJ 615-2011

National Standard of the People's Republic of China

ICS
13.080
Classification
Z 18

Issued by: Ministry of Ecology and Environment

Contents

  • Foreword
  • 1 Scope of application
  • 2 Normative references
  • 3 Principle of the method
  • 4 Interference and elimination
  • 5 Reagents and materials
  • 6 Instruments and equipment
  • 7 Samples
  • 7.1 Sample collection and preservation
  • 7.2 Preparation of samples
  • 7.3 Determination of dry matter content
  • 8 Analysis steps
  • 8.1 Drawing of the calibration curve
  • 8.2 Determination
  • 8.3 Blank test
  • 9 Calculation and representation of results
  • 9.1 Calculation of results
  • 9.2 Results representation
  • 12 Precautions

Foreword

In order to implement the "Environmental Protection Law of the People's Republic of China", protect the environment, protect human health, and regulate the determination method of organic carbon in soil, Develop this standard.

This standard specifies the potassium dichromate oxidation-spectrophotometry for the determination of organic carbon in soil.

This standard is the first release.

This standard was formulated by the Science and Technology Standards Department of the Ministry of Environmental Protection.

This standard is mainly drafted by. Dalian Environmental Monitoring Center.

This standard is verified by. Tianjin Environmental Monitoring Center, Liaoning Environmental Monitoring Experimental Center, Shenyang Environmental Monitoring Center Station, Anshan Municipal Environmental Monitoring Center Station, Jinzhou Environmental Monitoring Center Station and Yingkou Environmental Monitoring Center Station.

This standard was approved by the Ministry of Environmental Protection on April 15, 2011.

This standard has been implemented since October 1, 2011.

This standard is explained by the Ministry of Environmental Protection.

Determination of soil organic carbon - Potassium dichromate oxidation - spectrophotometric method

1 Scope of application

This standard specifies the potassium dichromate oxidation-spectrophotometry for the determination of organic carbon in soil.

This standard applies to the determination of organic carbon in air-dried soil. This standard does not apply to chloride ion (Cl-) content greater than 2.0 × 104 mg/kg Determination of salinized soil or salinized soil.

When the sample amount is 0.5 g, the detection limit of the method is 0.06% (by dry weight), and the lower limit of determination is 0.24% (by dry weight).

2 Normative references

The contents of this standard refer to the following documents or their terms. For undated references, the valid version applies to this standard.

HJ 613 Determination of dry matter and moisture in soils - Gravimetric method HJ/T 166 Technical Specifications for Soil Environmental Monitoring

3 Principle of the method

Under heating, the organic carbon in the soil sample is oxidized by excess potassium dichromate-sulfuric acid solution, and hexavalent chromium (Cr6) in potassium dichromate it is reduced to trivalent chromium (Cr3), which is proportional to the content of organic carbon in the sample, and the absorbance is measured at 585 nm.

The content of chrome (Cr3) is used to calculate the organic carbon content.

4 Interference and elimination

4.1 The ferrous ion (Fe2) in the soil leads to a high determination of organic carbon. The soil sample can be spread into 2~ during sample preparation A thin layer of 3 cm thick, fully exposed in air, oxidizes ferrous ions (Fe2) to ferric ions (Fe3) to eliminate interference.

4.2 Chloride ion (Cl-) in the soil results in a high determination of soil organic carbon, which is eliminated by adding an appropriate amount of mercury sulfate.

5 Reagents and materials

Analytical purification reagents in accordance with national standards were used for analysis, unless otherwise stated. The experimental water is <=0.2 mS/m at 25 °C.

Deionized water or distilled water.

5.1 Sulfuric acid. rho(H2SO4) = 1.84 g/ml.

5.2 Mercury sulfate.

5.3 Potassium dichromate solution. c (K2Cr2O7) = 0.27 mol/L.

Weigh 80.00 g of potassium dichromate in an appropriate amount of water, dissolve it, transfer it to a 1 000 ml volumetric flask, dilute to volume with water, and shake well. Solution storage Store in a reagent bottle at 4 °C.

5.4 Standard glucose solution. rho(C6H12O6)=10.00 g/L.

Weigh 10.00 g of glucose in an appropriate amount of water, dissolve it, transfer it to a 1 000 ml volumetric flask, dilute to volume with water, and shake well. The solution is stored in in the reagent bottle, the validity period is one month.

6 Instruments and equipment

6.1 Spectrophotometer. 585 nm wavelength with a 10 mm cuvette.

6.2 Balance. Accuracy is 0.1 mg.

6.3 Constant temperature heater. The temperature control accuracy is 135 °C ± 2 °C. The constant temperature heater has a heating hole, and the hole depth should be higher than that in the glass tube with a plug the liquid level is about 10 mm, and the plug glass tube is exposed to the heating hole portion of about 150 mm.

6.4 Plug glass tube. With 100 ml mark line, the diameter is 35~45 mm.

Note. The outer wall of the glass tube with the plug must be able to adhere to the inner wall of the heating hole of the thermostat heater, otherwise the digestion is not guaranteed.

6.5 Centrifuge. 0 to 3 000 r/min with a 100 ml centrifuge tube.

6.6 Soil screen. 2 mm (10 mesh), 0.25 mm (60 mesh), stainless steel.

6.7 Common instruments and equipment used in general laboratories.

7 Samples

7.1 Sample collection and preservation

The collection and storage of soil samples refer to the relevant regulations of HJ/T 166.

7.2 Preparation of samples

Place the soil sample in a clean white enamel tray and spread it into a thin layer 2 to 3 cm thick. First remove the residues such as plants, insects, stones, etc.

Crush the clods with rafts, dry naturally, and turn them several times a day when they are dry. Mix the air-dried soil thoroughly, use the quartering method, take two parts, one part Retained, one part was passed through a 2 mm soil sieve for dry matter determination. Remove 10-20 g of the sample from the 2 mm sieve and further finely grind it.

It was placed in a brown stoppered glass via a 60 mesh (0.25 mm) soil sieve for testing.

7.3 Determination of dry matter content

Accurately weigh the appropriate amount of air-dried soil, and determine the dry matter content according to HJ 613.

8 Analysis steps

8.1 Drawing of the calibration curve

8.1.1 Separate 0.00, 0.50, 1.00, 2.00, 4.00 and 6.00 ml glucose standard solution (5.4) in 100 ml with a solution in the glass tube, the corresponding organic carbon masses were 0.00, 2.00, 4.00, 8.00, 16.0, and 24.0 mg, respectively.

8.1.2 Add 0.1 g of mercury sulfate (5.2) and 5.00 ml of potassium dichromate solution (5.3), and shake well. Slowly add 7.5 ml of sulfuric acid (5.1), Shake gently.

8.1.3 Turn on the thermostat heater and set the temperature to 135 °C. When the temperature rises to near 100 ° C, the above-mentioned plug-dissolved glass tube is opened.

Into the heating hole of the thermostat heater, start timing when the instrument temperature shows 135 °C, and heat for 30 min. Then turn off the thermostat heater switch, Remove the glass tube with a plug digestion tube and cool to room temperature. Slowly add about 50 ml of water to each of the stoppered glass tubes and continue to cool to room temperature.

Make up to 100 ml of the line with water and shake it.

8.1.4 Measure the absorbance at a wavelength of 585 nm using a 10 mm cuvette with water as a reference.

8.1.5 Correct the absorbance at zero concentration to the ordinate and the corresponding organic carbon mass (mg) as the abscissa to draw a calibration curve.

8.2 Determination

Accurately weigh the appropriate amount of sample (7.2), carefully added to the 100 ml stoppered glass tube to avoid staining. Add the reagent according to 8.1.2, Digest, cool, and make up according to 8.1.3. After the constant volume, the test solution was allowed to stand for 1 h, and about 80 ml of the supernatant was taken to the centrifuge tube at 2 000 r/min.

Centrifuge for 10 min, then stand still until clarified; or stand still in the stoppered glass tube until clarified. Finally take the supernatant according to 8.1.4 the amount of absorbance. The relationship between soil organic carbon content and sample volume is shown in Table 1.

Table 1 Relationship between soil organic carbon content and sample size

Soil organic carbon content /% 0.00 ~ 4.00 4.00 ~ 8.00 8.00 ~ 16.0 Sample size/g 0.400 0 ~ 0.500 0 0.200 0 ~ 0.250 0 0.100 0 ~ 0.125 0

Note 1. When the sample organic carbon content exceeds 16.0%, increase the amount of potassium dichromate solution and redraw the calibration curve.

Note 2. Under normal circumstances, it takes about 8 hours for the test solution to stand for clarification after centrifugation or to stand still for clarification for about 8 hours.

8.3 Blank test

No sample is added to the glass tube with plug digestion, and the measurement is carried out according to the procedures of 8.1.2, 8.1.3 and 8.1.4.

9 Calculation and representation of results

9.1 Calculation of results

The organic carbon content in the soil (by dry weight, mass fraction, %) is calculated according to formula (1) and formula (2).

Wm m= × (1)

( ) 100

AA aw

Where. - the mass of dry matter in the sample, g; 1m M--sample sample amount, g;

Dmw -- dry matter content (mass fraction) of soil, %;

Ocomega - the content of organic carbon in soil samples (by dry weight, mass fraction), %;

A--the absorbance of the sample digestion solution;

0A - the absorbance of the blank test;

A--the intercept of the calibration curve;

b--The slope of the calibration curve.

9.2 Results representation

When the measurement result is 1.00%, the relative deviation of the two measurement results is <=10.0%.

11.3 When testing each batch of samples, a certified reference material shall be analyzed and its measured value shall be within the guaranteed value range.

11.4 The correlation coefficient of the calibration curve should be greater than or equal to 0.999.

12 Precautions

12.1 In order to ensure the uniformity of the heating temperature of the constant temperature heater, when the sample is digested, 15 ml is placed in the heating hole without the sample.

The sulfuric acid (5.1) has a plug-dissolving glass tube to avoid the heating of the thermostat heater.

12.2 Sulfuric acid has strong chemical corrosiveness. Wear protective equipment as required to avoid contact with skin and clothing. Sample elimination the solution should be operated in a fume hood. The waste liquid after the test should be disposed of properly.

......
This preview omits tables, figures, formulas and parts of the technical clauses. The complete document — 7 pages — is available in the English PDF.

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