Quantification of carbon derived from lignite in soils using mid-infrared spectroscopy and partial least squares

被引:59
作者
Rumpel, C [1 ]
Janik, LJ
Skjemstad, JO
Kögel-Knabner, I
机构
[1] Tech Univ Munich, Lehrstuhl Bodenkunde, D-85350 Freiburg, Germany
[2] CSIRO Land & Water, Glen Osmond, SA 5064, Australia
[3] Brandenburg Tech Univ, Dept Soil Protect & Recultivat, D-03013 Cotthus, Germany
关键词
lignite; organic matter; DRIFT spectroscopy; C-14; activity; partial least squares;
D O I
10.1016/S0146-6380(01)00029-8
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The total organic carbon (TOC) of many recultivated mine soils is composed of a fraction that is lignite-derived as well as a fraction that is derived From recent plant litter. In these soils, precise quantification of the lignite contribution to the TOC content can only be achieved with expensive and time consuming methods. In the present study, we tested diffuse reflectance infrared Fourier transform (DRIFT) spectroscopy in combination with multivariate data analysis partial least squares (PLS)I as a rapid and inexpensive means of quantifying the lignite contribution to the TOC content of soil samples. The conceptual approach included analysis of samples with different lignite content (bulk soil and particle size fractions) by DRIFT-spectroscopy and C-14 activity measurements. Afterwards, with both data sets a calibration curve was established by PLS and the lignite content predicted from the DRIFT spectra. A good fit was obtained between this approach and the radiocarbon analysis. Loading factors showed that this prediction was based on structural differences between the two organic matter types. We conclude that DRIFT spectroscopy can be used in combination with multivariate data analysis for the differentiation of carbon derived from lignite and carbon derived from recent organic matter in soils. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:831 / 839
页数:9
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