The turnover of carbohydrate carbon in a cultivated soil estimated by 13C natural abundances

Autor: Derrien, Delphine, Marol, Christine, Balabane, May, Balesdent, Jerome
Přispěvatelé: Centre National de la Recherche Scientifique (CNRS), Unité de recherche Science du Sol (USS), Institut National de la Recherche Agronomique (INRA), Département Environnement et Agronomie (DEPT EA)
Jazyk: angličtina
Rok vydání: 2006
Předmět:
Zdroj: European Journal of Soil Science
European Journal of Soil Science, Wiley, 2006, 57 (4), pp.547-557. ⟨10.1111/j.1365-2389.2006.00811.x⟩
ISSN: 1351-0754
1365-2389
DOI: 10.1111/j.1365-2389.2006.00811.x⟩
Popis: International audience; Understanding the chemical composition of soil organic matter (SOM) requires the determination of the dynamics of each class of compounds. We measured the dynamics of carbon in neutral carbohydrates by use of natural 13C labelling in an experimental wheat and maize sequence extending over 23 years. The isotopic composition of individual neutral monosaccharides was determined in hydrolysed particle-size fractions by gas chromatography/combustion/isotope ratio mass spectrometry (GC/C/IRMS) of trimethylsilyl (TMS) derivatives. The sensitivity in terms of 13C/12C ratios ranged between 1 and 2‰ depending on the monosaccharide. The age distribution of neutral sugar carbon was very similar to that of total soil carbon. Particulate organic matter (POM) was characterized by the predominance of glucose and xylose of vegetal origin. In POM > 200 µm, the mean age of sugar-C (5 years) was slightly less than that of total carbon (7 years). Xylose was younger than glucose. The fine fraction 0–50 µm contained mainly glucose, arabinose, galactose, xylose, fucose and mannose, which had predominantly microbial origins. The mean age of carbohydrate carbon in the fraction 0–50 µm was between 60 and 100 years and was similar to that of total organic carbon (OC). No difference in the age of carbon between the individual monosaccharides was found. The POM fraction 50–200 µm had an intermediate signature and turnover. Considering the typical lability of carbohydrates, the relatively great age of carbohydrate carbon may be explained by physical or chemical protection from degradation, as well as by recycling of soil organic matter carbon by soil microbes.
Databáze: OpenAIRE
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