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Title

Types and chemical composition of organic matter in reforested lignite-rich mine soils

AuthorsRumpel, C.; Knicker, Heike ; Kögel-Knabner, I.; Skjemstad, J. O.; Hüttl, R. F.
KeywordsMine soils
Lignite
Organic matter
CPMAS 13C and 15N NMR spectroscopy
Radiocarbon dating
Magnetic susceptibility
Issue DateOct-1998
PublisherElsevier
CitationGeoderma 86 (1–2): 123–142 (1998)
AbstractIn the post-mining landscapes of Lusatia, forest soils develop from extremely aeid, lignite-rich open cast mine spoils. The sites have been ameliorated with 8sb from lignite-fired power stations prior to afforestation. During stand development, incorporation of plant-derived organic matter leads to an intimate mixture with the substrate-derived lignite in the first centimetres of the soil CAí horizon). The objective of the study was to characterise and to compare the composition of organic matter of mine soils under forest which contain substantial amounts of lignite. Therefore, the forest floor and the mineral soil (Ai and Cv horizon) under a 20-year-old pine and a 36-year-old red oak site were analysed for elemental composition, magnetic susceptibility, chemical structure by cross-polarisation magic angle spinning (CPMAS) I3C and ISN nuclear magnetic resonance (NMR) spectroscopy and lignite content by radiocarbon dating. The 13e CPMAS NMR spectra of!he forest fioor and Ai horizon reveal signals at 56, 72, 105, 119, 130 and 150 ppm, indicating the presence of carbohydrates and lignin ariginating from plant material. Additionally, structures characteristic for lignite material (aromatic and aliphatic carbon) could be observed in the Oh and Ai horizons. Using radiocarbon dating, 25 to 83% of the total carbon in these horizons can be assigned to lignite. Lignite carban may also indicate carbonaceous particles derived from amelioration ash as well as from lignite-derived airborne contamination, which are possible carbon sources of the forest floor and the surface soil. 13C NMR and radiocarbon dating show that the subsoil Cv horizon. is dominated by carbon derived from lignite. From these results it is concluded that mine soils, rich in lignite contain up to four organic matter types, namely lignite inherent to the parent substrate, organic matter derived from decomposition of plant residues, carbonaceous particles in amelioration ash and carbonaceous particles from airborne lignite-derived contamination. 15N NMR spectroscopy revealed that most of the nitrogen of these soils is of recent biogenic origin.
Description20 pages, 4 figures, 6 tables, 49 references.
URIhttp://hdl.handle.net/10261/82279
ISSN0016-7061
E-ISSN1872-6259
Appears in Collections:(IRNAS) Artículos
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