“…For example, increasing soil moisture with proximity to the trunk has been attributed to increased stemflow (Gersper and Holowaychuk, 1970), suppressed evaporation due to canopy shadowing and insulation by leaf litter (Birkeland, 1984), and the influence of greater organic matter content on soil structure under the canopy (Brady, 1984). Variations in soil pH may relate to the influence of the canopy on leaching processes (Birkeland, 1984), primarily through spatial patterns in the acidity of litter underneath the canopy (Zinke, 1962), or through stemflow processes (Gersper and Holowaychuk, 1970). Similarly, subcanopy patterns in soil nitrogen (Harradine, 1954) have been ascribed to litter characteristics (Zinke, 1962;Callaway and Nadkarni, 1991) or facilitation by the tree canopy of subcanopy species which contribute organic matter (Garcia-Moya and McKell, 1970).…”