Abstract

Humus forms are a distinctive morphological indicator of soil organic matter decomposition. The spatial distribution of humus forms depends on environmental factors such as topography, climate and vegetation. In montane and subalpine forests, environmental influences show a high spatial heterogeneity, which is reflected by a high spatial variability of humus forms. This study aims at examining spatial patterns of humus forms and their dependence on the spatial scale in a high mountain forest environment (Val di Sole/Val di Rabbi, Trentino, Italian Alps). On the basis of the distributions of environmental covariates across the study area, we described humus forms at the local scale (six sampling sites), slope scale (60 sampling sites) and landscape scale (30 additional sampling sites). The local variability of humus forms was analyzed with regard to the ground cover type. At the slope and landscape scale, spatial patterns of humus forms were modeled applying random forests and ordinary kriging of the model residuals. The results indicate that the occurrence of the humus form classes Mull, Mullmoder, Moder, Amphi and Eroded Moder generally depends on the topographical position. Local-scale patterns are mostly related to micro-topography (local accumulation and erosion sites) and ground cover, whereas slope-scale patterns are mainly connected with slope exposure and elevation. Patterns at the landscape scale show a rather irregular distribution, as spatial models at this scale do not account for local to slope-scale variations of humus forms. Moreover, models at the slope scale perform distinctly better than at the landscape scale. In conclusion, the results of this study highlight that landscape-scale predictions of humus forms should be accompanied by local- and slope-scale studies in order to enhance the general understanding of humus form patterns.

Highlights

  • Humus forms are a distinctive morphological indicator of soil organic matter decomposition, since they integrate both the sequence of organic horizons (OL = litter, OF = fragmented residues, OH = humified residues) above the mineral soil and the soil structure in the mineral soil as a result of soil biological activities [1,2,3]

  • This study aims at examining spatial patterns of humus forms and their dependence on the spatial scale in a high mountain forest environment (Val di Sole/Val di Rabbi, Trentino, Italian Alps)

  • The results indicate that the occurrence of the humus form classes Mull, Mullmoder, Moder, Amphi and Eroded Moder generally depends on the topographical position

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Summary

Introduction

The spatial arrangement of humus forms corresponds to spatial patterns of soil ecological processes. From the local to the landscape scale, different factors and processes influence spatial soil ecological patterns [7,8]. Study areas in the high mountains were found to be characterized by a high small-scale variability of humus forms related to micro-topography and local ground cover differences [9,10,11]. Environmental factors such as climate, relief, parent material, vegetation, and land use shape landscape units with different humus systems [12,13,14,15]. In mountain environments with similar geological conditions, relief is the most decisive factor, as it controls mesoclimate, hydrological processes, erosion dynamics and vegetation zones [16,17,18]

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