Micromorphological, wet-chemical and 13C NMR spectroscopic characterization of density fractionated forest soils

G. Beudert; I. Kögel-Knabner; W. Zech

doi:10.1016/0048-9697(89)90148-4

Micromorphological, wet-chemical and ¹³C NMR spectroscopic characterization of density fractionated forest soils

G. Beudert, I. Kögel-Knabner, W. Zech

Universität Bayreuth

Research output: Contribution to journal › Article › peer-review

15 Scopus citations

Abstract

Decomposition and humification were studied within two forest humus profiles (mor and moder) by means of density fractionation combined with subsequent micromorphological, wet-chemical, and CPMAS 13C NMR spectroscopic characterization of the fractions. The data show that the decomposition of plant polysaccharides leads to a relative accumulation of refractory structures within the plant residues of the mineral soils: non-phenolic aromatic structures for the mor and long-chain unsubstituted aliphatic structures for the moder. In both mineral soil horizons the organo-mineral complexes have high carbohydrate contents.

Original language	English
Pages (from-to)	401-408
Number of pages	8
Journal	Science of the Total Environment
Volume	81-82
Issue number	C
DOIs	https://doi.org/10.1016/0048-9697(89)90148-4
State	Published - Jun 1989
Externally published	Yes

Access to Document

10.1016/0048-9697(89)90148-4

Cite this

@article{148726521eef4a82aa181d59eebb4604,

title = "Micromorphological, wet-chemical and 13C NMR spectroscopic characterization of density fractionated forest soils",

abstract = "Decomposition and humification were studied within two forest humus profiles (mor and moder) by means of density fractionation combined with subsequent micromorphological, wet-chemical, and CPMAS 13C NMR spectroscopic characterization of the fractions. The data show that the decomposition of plant polysaccharides leads to a relative accumulation of refractory structures within the plant residues of the mineral soils: non-phenolic aromatic structures for the mor and long-chain unsubstituted aliphatic structures for the moder. In both mineral soil horizons the organo-mineral complexes have high carbohydrate contents.",

author = "G. Beudert and I. K{\"o}gel-Knabner and W. Zech",

note = "Funding Information: ACKNOWLEDGEMENTS We are indebted to Dr. P.G. Hatcher for obtaining the 13CNMR spectra and to the Deutsche Forschungsgemeinschaft (SFB 137) for financial support.",

year = "1989",

month = jun,

doi = "10.1016/0048-9697(89)90148-4",

language = "English",

volume = "81-82",

pages = "401--408",

journal = "Science of the Total Environment",

issn = "0048-9697",

publisher = "Elsevier B.V.",

number = "C",

}

TY - JOUR

T1 - Micromorphological, wet-chemical and 13C NMR spectroscopic characterization of density fractionated forest soils

AU - Beudert, G.

AU - Kögel-Knabner, I.

AU - Zech, W.

N1 - Funding Information: ACKNOWLEDGEMENTS We are indebted to Dr. P.G. Hatcher for obtaining the 13CNMR spectra and to the Deutsche Forschungsgemeinschaft (SFB 137) for financial support.

PY - 1989/6

Y1 - 1989/6

N2 - Decomposition and humification were studied within two forest humus profiles (mor and moder) by means of density fractionation combined with subsequent micromorphological, wet-chemical, and CPMAS 13C NMR spectroscopic characterization of the fractions. The data show that the decomposition of plant polysaccharides leads to a relative accumulation of refractory structures within the plant residues of the mineral soils: non-phenolic aromatic structures for the mor and long-chain unsubstituted aliphatic structures for the moder. In both mineral soil horizons the organo-mineral complexes have high carbohydrate contents.

AB - Decomposition and humification were studied within two forest humus profiles (mor and moder) by means of density fractionation combined with subsequent micromorphological, wet-chemical, and CPMAS 13C NMR spectroscopic characterization of the fractions. The data show that the decomposition of plant polysaccharides leads to a relative accumulation of refractory structures within the plant residues of the mineral soils: non-phenolic aromatic structures for the mor and long-chain unsubstituted aliphatic structures for the moder. In both mineral soil horizons the organo-mineral complexes have high carbohydrate contents.

UR - https://www.scopus.com/pages/publications/0024531166

U2 - 10.1016/0048-9697(89)90148-4

DO - 10.1016/0048-9697(89)90148-4

M3 - Article

AN - SCOPUS:0024531166

SN - 0048-9697

VL - 81-82

SP - 401

EP - 408

JO - Science of the Total Environment

JF - Science of the Total Environment

IS - C

ER -

Micromorphological, wet-chemical and ¹³C NMR spectroscopic characterization of density fractionated forest soils

Abstract

Access to Document

Other files and links

Fingerprint

Cite this