Tóth T. and B. Szabó. 2003. Method for the quick determination of soil organic matter in the field (Hung.). Agrokémia és Talajtan. 52:409-508. With the use of 60 representative samples, a laboratory comparison was made of field methods suitable for the determination of soil organic C content. The methods were evaluated by comparing them with the standard Tyurin method. The colour of the soil samples, especially the value read from the Munsell Colour Chart, exhibited a close correlation (R=0,73**) with the logarithm of the soil humus content. This indicates that it would be worth carrying out more detailed studies on the correlations between organic C content and soil colour. The field Walkley-Black method differs from the laboratory technique only in the quantity of reagents applied, so the organic matter is oxidized using potassium bichromate in concentrated sulphuric acid. When the sulphuric acid is added, the solution heats up considerably, so it must be cooled before being poured into test-tubes for a comparison of the colour of the solutions. As this method is dangerous it is not really suitable for field use. Both the absorbance measured using the field method (R=0,73**) and the order of the samples on the basis of absorbance (R=0,87**) exhibited a close correlation with the humus content determined using the Tyurin method. There was a correlation coefficient of 0,78** between the logarithm of the humus content and the basic EDTA transmittance. It was observed during the investigations that certain soil components (CaCO3, iron and aluminium oxides) modified the colour of the solution, thus interfering with organic matter estimation. The newly elaborated method involves treating the soil with acidic potassium permanganate solution, followed by the measurement of the carbon dioxide concentration formed over a period of three minutes, using a portable instrument with an infrared detector. The inorganic carbonate content of the soil is measured separately with the addition of sulphuric acid only. The correlation coefficient between the CO2 content recorded with the potassium permanganate method and the Tyurin humus content was 0,76**, while it was 0,81** for soil samples having less than 20% carbonate. Further improvement of the new method will be based on modifying the amount of sulphuric acid and water in such a manner that the concentration of acid during the determination of carbonates and organic matter should be the same. The present recovery rates of 12,5% for carbonate and 0,7% for organic carbon must also be improved in order to decrease the very different effects of the two carbon sources during the determination in the case of sample inhomogeneity. The reliability of the methods was tested by analyzing 12 samples in 4 replications using the coefficient of variation (CV). The smallest CV was obtained for methods based on the order of soil organic carbon values, followed by the Walkley-Black, Tyurrin, basic EDTA and potassium permanganate methods. The final comparison of the methods screened in the laboratory will be carried out in the field.