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Seasonal and spatial variation of extractable trace metal fractions in topsoils under mixed forest
Author(s) -
Wenzel Walter W.,
Alge Guntram,
Blum Winfried E. H.,
Brandstetter Anton,
Pollak Michael A.,
Riedler Christian,
Schulte Andreas
Publication year - 1996
Publication title -
zeitschrift für pflanzenernährung und bodenkunde
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 0044-3263
DOI - 10.1002/jpln.1996.3581590404
Subject(s) - spatial variability , cambisol , seasonality , sampling (signal processing) , coefficient of variation , soil science , soil water , environmental science , trace metal , chemistry , environmental chemistry , metal , mathematics , statistics , organic chemistry , filter (signal processing) , computer science , computer vision
Metal extractability from soils may be affected by analytical errors, sample preparation, inaccurate sampling as well as by natural variation in space and time. During one year, we sampled the Ah horizons of a forested Luvi‐Calcaric Cambisol from 43 subplots in a visually homogeneous area of 0.5 ha six times to determine the spatial and seasonal variation of pH, OC, and Fe, Mn, Cr, Cu, Ni, Pb and Zn extractable by 0.1 M BaCl 2 and 0.05 M Na 2 ETDA. As indicated by a two‐way ANOVA, the spatial and seasonal variations of all parameters were significant at p < 0.01. The metal‐specific ranges of seasonal variation varied between 21% and 90% of the minima for Na 2 EDTA, and 15% and 71% for 0.1 M BaCl 2 . The error due to within‐subplot variability and inaccurate sampling, tested by sampling twice in April 1992, was small compared to the natural seasonal and spatial variation. The relative differences between the means of the two samplings tended to increase with the coefficients of spatial variation, suggesting an increasing contribution of within‐subplot variability to the sampling error. The study shows that both spatial and seasonal variation of extractable metal fractions may bias the analysis of mobile metal fractions in a rarely predictable way.