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024 7 _ |2 DOI
|a 10.1111/j.1365-2389.2011.01401.x
024 7 _ |2 WOS
|a WOS:000297206100007
037 _ _ |a PreJuSER-17682
041 _ _ |a ENG
082 _ _ |a 630
084 _ _ |2 WoS
|a Soil Science
100 1 _ |0 P:(DE-HGF)0
|a Stumpe, B.
|b 0
245 _ _ |a Sample preparation and selection for qualitative and quantitative analyses with mid-infrared reflectance spectroscopy
260 _ _ |a Oxford [u.a.]
|b Wiley-Blackwell
|c 2011
300 _ _ |a 849 - 862
336 7 _ |0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
|a Journal Article
336 7 _ |2 DataCite
|a Output Types/Journal article
336 7 _ |0 0
|2 EndNote
|a Journal Article
336 7 _ |2 BibTeX
|a ARTICLE
336 7 _ |2 ORCID
|a JOURNAL_ARTICLE
336 7 _ |2 DRIVER
|a article
440 _ 0 |0 1973
|a European Journal of Soil Science
|v 62
|x 1351-0754
|y 6
500 _ _ |3 POF3_Assignment on 2016-02-29
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Mid-infrared spectroscopy (MIRS) is a well-established analytical tool for qualitative and quantitative analysis of soil samples. However, effects of soil sample grinding procedures on the prediction accuracy of MIR models and on qualitative spectral information have not been well investigated and, in consequence, not standardized up to now. Further, the effects of soil sample selection on the accuracy of MIR prediction models has not been quantified yet. This study investigated these effects by using 180 well-characterized soil samples that were ground for different times (0, 2 or 4 minutes) and then used for MIR measurements. To study the impact of sample preparation, soil spectra were subjected to principal component analyses (PCA), multiple regression and partial least square (PLS) analysis. The results indicate that the prediction accuracy of MIR models for soil organic carbon (SOC) and pH and the qualitative spectral information were better overall for lightly ground (2 minutes) soil samples compared with intensively (4 minutes) or unground soil samples. Whereas the grinding procedure did not show any effect on spectra of clay minerals, spectral information for quartz and for SOC was modified. Even though it is difficult to recommend a global standardized soil sample grinding procedure for MIR measurements because of different mill types available within laboratories, we highly recommend using an internally standardized grinding procedure. Moreover, we show that neither land use nor soil sampling depth influences the prediction of the SOC content. However, sand and clay content substantially affect the score vectors used by the PLS algorithm to predict the SOC content. Thus, we recommend using soil samples similar in texture for more precise SOC calibration models for MIR spectroscopy.
536 _ _ |0 G:(DE-Juel1)FUEK407
|2 G:(DE-HGF)
|a Terrestrische Umwelt
|c P24
|x 0
588 _ _ |a Dataset connected to Web of Science, Pubmed
700 1 _ |0 P:(DE-Juel1)VDB17057
|a Weihermüller, L.
|b 1
|u FZJ
700 1 _ |0 P:(DE-HGF)0
|a Marschner, B.
|b 2
773 _ _ |0 PERI:(DE-600)2020243-X
|a 10.1111/j.1365-2389.2011.01401.x
|g Vol. 62, p. 849 - 862
|p 849 - 862
|q 62<849 - 862
|t European journal of soil science
|v 62
|x 1351-0754
|y 2011
856 7 _ |u http://dx.doi.org/10.1111/j.1365-2389.2011.01401.x
909 C O |o oai:juser.fz-juelich.de:17682
|p VDB
|p VDB:Earth_Environment
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|b Erde und Umwelt
|k P24
|l Terrestrische Umwelt
|v Terrestrische Umwelt
|x 0
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|1 G:(DE-HGF)POF3-250
|2 G:(DE-HGF)POF3-200
|a DE-HGF
|b Marine, Küsten- und Polare Systeme
|l Terrestrische Umwelt
|v Addenda
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914 1 _ |y 2011
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |0 I:(DE-Juel1)IBG-3-20101118
|g IBG
|k IBG-3
|l Agrosphäre
|x 0
970 _ _ |a VDB:(DE-Juel1)132238
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IBG-3-20101118
980 _ _ |a UNRESTRICTED


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