Colorimetric method to estimate the soil organic matter in karst areas

Proxy method to estimate SOC

Abstract

The increase in soil organic carbon (SOC) content contributes the mitigation of the effects of global climate change, thus it is important to know its levels. However, the SOC analysis can eventually be expensive and time consuming, as well as generating toxic waste. The measurement of soil color may be an indirect method more effective to estimate the SOC than traditional techniques. The principal aim of the study was to use color parameters through the CIE Lab system and some color indices, such as saturation and redness indices, to estimate the COS in a karst area of the municipality of Chetumal in the Yucatan Peninsula, Mexico. The percentage of COS was measured in 50 soil samples by conventional methods while the soil color was analyzed with the CIE Lab system. Both variables were correlated with the redness index. Based on color, the samples were separated into five groups, ranging from pinkish white to brownish gray. Multiple regression equations (SOC vs soil color parameters) were performed for each group and a medians comparison analysis was applied. The correlation adjustment between the redness index and COS is R²> 0.86. The values of the multiple regression equations were R²> 0.8. We conclude that the soil redness index, now named organic carbon index, can be used as a relatively quick approach to estimate the percentage of SOC in karst areas.