Is thermal oxidation at different temperatures suitable to isolate soil organic carbon fractions with different turnover?-Reference-Cited by-同舟云学术

Is thermal oxidation at different temperatures suitable to isolate soil organic carbon fractions with different turnover?

Published:2010-02 Issue:1 Volume:173 Page:61-66
ISSN:1436-8730
Container-title:Journal of Plant Nutrition and Soil Science
language:en
Short-container-title:Z. Pflanzenernähr. Bodenk.

Author:

Helfrich Mirjam¹,Flessa Heiner²,Dreves Alexander³,Ludwig Bernard¹

Affiliation:

1. Department of Environmental Chemistry, University of Kassel, Nordbahnhofstraße 1a, 37213 Witzenhausen, Germany

2. Soil Science of Temperate and Boreal Ecosystems, University of Göttingen, Büsgenweg 2, 37077 Göttingen, Germany

3. Leibniz‐Laboratory for Radiometric Dating and Isotope Research, University of Kiel, Max‐Eyth‐Straße 11–13, 24118 Kiel, Germany

Funder

Deutsche Forschungsgemeinschaft

Publisher

Wiley

Subject

Plant Science,Soil Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.200700280

Reference42 articles.

1. Rearrangement of carbon and nitrogen forms in peat after progressive thermal oxidation as determined by solid-state 13C- and 15N-NMR spectroscopy

2. Thermogravimetry as a Method for Distinguishing Various Degrees of Mineralisation in Macromorphologically‐defined Humus horizons

3. Balesdent J. Mariotti A.(1996): Measurement of soil organic matter turnover using13C natural abundance in Boutton T. W. Yamasaki S. (eds.): Mass Spectrometry of Soils. Marcel Dekker New York pp. 83–111.

4. Natural 13C abundance as a tracer for studies of soil organic matter dynamics

5. Effets des ultrasons sur la distribution granulométrique des matières organiques des sols.;Balesdent J.;Science du Sol,1991

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