Studies of Thermal Transformations of Humic and Fulvic Acids in Soils I. Infrared Spectroscopy and Temperature-Programmed Pyrolysis Mass Spectrometry
- 1 July 1997
- journal article
- research article
- Published by Taylor & Francis in Chemistry and Ecology
- Vol. 13 (4) , 237-248
- https://doi.org/10.1080/02757549708035530
Abstract
Temperature-programmed pyrolysis mass spectrometry and Fourier-transform infrared spectroscopy have been used to monitor structural changes of humic and fulvic acids isolated from soils in China, in the temperature range of 25-550°C. in this work, we found that decarboxylation is obvious as the main reaction with dehydration reaction from 150°C to 400°C, the anhydride can be identified from FT-IR spectra at temperature range from 200°C to 400°C; there are evident changes of the aromatic nucleus of humic and fulvic acids above 400°C, even remaining up to 550°C. Besides, some changes of adsorption water can be distinguished before 200°C, and the mass signal of sulphur dioxide was detected.Keywords
This publication has 5 references indexed in Scilit:
- The role of fulvic acid in the supergene migration of gold in tropical rain forest soilsGeochimica et Cosmochimica Acta, 1993
- Interactions of gold (III) chloride and elemental gold with peat-derived humic substancesChemical Geology, 1992
- Infrared Emission Spectroscopy of Some Sulfate MineralsApplied Spectroscopy, 1992
- Differential thermal analysis, thermogravimetry and in-source pyrolysis-mass spectrometry studies on the formation of soil organic matterThermochimica Acta, 1992
- Studies of thermal transformations of fulvic acids using Fourier transform-infrared emission spectroscopyJournal of Analytical and Applied Pyrolysis, 1992