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Distinction of soil thermal regimes under various experimental vegetation covers

1993/11/01 by Allen C. Balisky, Philip J. Burton · 1 citation
Agricultural and Biological Sciences · Chemistry · Earth and Planetary Sciences · Engineering · #Atmospheric sciences #Biology #Botany #Chemistry #Ecology #Environmental science #Geology #Geology and Paleoclimatology Research #Microclimate #Pasture and Agricultural Systems #Rubus #Soil science #Tree Root and Stability Studies #Vegetation (pathology)

paper · pdf · doi:10.4141/cjss93-043

openalex publication_date 1993/11/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/06/26

Abstract

Five vegetation treatments were established in 1.2 m × 1.2 m plots in 1990: (1) bare mineral soil, (2) Epilobium angustifolium, (3) Rubus spectobilis, (4) Alnus rubra and (5) a mixture of all three species. Soil temperatures were measured at 10-cm depths in three replicates of each treatment during the early summer of 1991. Mean, maximum and minimum temperatures always exhibited the same rank order of treatments — bare > Epilobium > Rubus > mixture > Alnus — but the latter four treatments were not readily distinguishable. A data-adjustment procedure based on Fourier analysis was conducted and its utility discussed for use in the separation of treatment effects where observations exhibit a detectable diurnal cycle. Using this method, the soil thermal regime of the Epilobium treatment was demonstrated to be statistically distinct from that of the bare plots and from those of the other vegetation treatments. Key words: Fourier analysis, diurnal pattern, soil temperature, vegetation effects, microclimate

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