Abstract

The aims of this study were to determine the degree of lignin degradation and to investigate changes in the chemical composition of the organic matter in the forest floor in an N fertilized Norway spruce forest soil. Needle litter and mor humus were collected from the field experiment at Skogaby in southern Sweden (56degrees33'N; 13degrees13'E). The spruce stand had been fertilized for I I years with 100 kg N ha(-1) yr(-1) as (NH4)(2)SO4. The degree of lignin degradation was determined with alkaline CuO oxidation followed by HPLC analysis. The chemical composition of the organic matter was characterized by CPMAS C-13 NMR. Tannin was specifically analyzed using dipolar dephasing CPMAS C-13 NMR and the N distribution was studied by CPMAS N-15 NMR. The C-to-N ratios in the fertilized Oi and Oe layers were significantly lower than in the unfertilized layers (24 compared to 34 and 23 compared to 27, respectively). Neither the sum of the CuO oxidation products (Vanillyls + Syringyls + Cinnamyls expressed as VSC) nor the acid-to-aldehyde ratio ((Ac/Al)(V)) showed any significant treatment effects. The content of aromatic C (including phenolic C) was significantly lower in the unfertilized than in the fertilized Oi layer (18 versus 21 %). In the unfertilized soil, VSC was positively correlated (r = +0.63, p < 0.05) with the C-to-N ratio, whereas the phenolic C content was negatively correlated (r = -0.61, p < 0.05). The tannin index showed a tendency of increasing from Oi to Oe layers in both treatments. Most of the organic N was found as amide-N, whereas no heterocyclic N was detected. We have not been able to show any major C structural changes due to N fertilization. We suggest that the significantly higher content of aromatic and phenolic C in the fertilized Oi layer is due to an initial stimulation of the microbial community. (C) 2004 Elsevier Ltd. All rights reserved

Published in

Soil Biology and Biochemistry
2004, volume: 36, number: 4, pages: 609-618
Publisher: PERGAMON-ELSEVIER SCIENCE LTD

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