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Application of Continuous Wavelet Transform in Examining Soil Spatial Variation: A Review

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Abstract

An adequate understanding of soil spatial variation as a function of space and scale is necessary in ecological modeling, environmental prediction, precision agriculture, soil quality assessment and natural resources management. Soil spatial variation can be partitioned into frequencies (scale) and positions (location) by the wavelet transform. This review focuses mainly on different applications of the continuous wavelet transform (CWT) for the identification of the scale and location dependence of soil attributes. We discussed both wavelet spectra and wavelet coherence in our analysis of soil spatial variation. Global wavelet spectra, being the sum of wavelet spectra over all spatial locations at a scale, can be used to examine the dominant scale of variation. Furthermore, some variations at a particular scale persist over all locations (termed global features), whereas others are present at only a few locations (localized features). Wavelet spectra can be used to identify both localized and global features. The combination of localized and global features provides a complete picture of the scale-location information of different processes in the field and may provide better guidance in designing efficient management practices. Wavelet coherency partitions the total correlation between two variables into correlations at different scales and locations, while also revealing the scale- and location-specific relationship between those two variables. This relationship may be helpful in developing predictive links between one property and another.

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  1. Department of Soil Science, University of Saskatchewan, Saskatoon, Saskatchewan, S7N 5A8, Canada

    Asim Biswas & Bing Cheng Si

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  1. Asim Biswas
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  2. Bing Cheng Si
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Correspondence to Bing Cheng Si.

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Biswas, A., Si, B.C. Application of Continuous Wavelet Transform in Examining Soil Spatial Variation: A Review. Math Geosci 43, 379–396 (2011). https://doi.org/10.1007/s11004-011-9318-9

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  • DOI: https://doi.org/10.1007/s11004-011-9318-9

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