1996
DOI: 10.1016/0016-7061(96)00026-2
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Soil chemical properties of a toposequence under primary rain forest in the Itacoatiara vicinity (Amazonas, Brazil)

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Cited by 30 publications
(15 citation statements)
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“…1b). Overall, cation concentrations in our study area ranged from 0.08 to 24.1 cmol(+) kg )1 , comparable with the overall range documented for Brazilian and Peruvian Amazonia (< 0.1-39 cmol(+) kg )1 ; Sanchez & Buol, 1974;Botschek et al, 1996).…”
Section: Floristic and Edaphic Patterns At The Pebas-nauta Boundarysupporting
confidence: 86%
“…1b). Overall, cation concentrations in our study area ranged from 0.08 to 24.1 cmol(+) kg )1 , comparable with the overall range documented for Brazilian and Peruvian Amazonia (< 0.1-39 cmol(+) kg )1 ; Sanchez & Buol, 1974;Botschek et al, 1996).…”
Section: Floristic and Edaphic Patterns At The Pebas-nauta Boundarysupporting
confidence: 86%
“…The spatial distribution of soil resources may result from disturbance history or differences in slope characteristics, since gaps tend be more abundant on steep slopes (Poorter et al 1994). In addition, species associated to slopes might be responding to a gradient of soil characteristics such as water availability (Becker et al 1988), nutrients (Botschek et al 1996;Gonzalez and Zak 1996), or soil texture (Chauvel et al 1987).…”
Section: Presence-absence Of Treesmentioning
confidence: 99%
“…High sand content and low clay and silt content could be a reason for low C and N accumulation in the 3-year-old stand (Table 2). Botschek et al (1996) noted that low clay content and lack of aggregation (i.e. absence of soil organic matter protection and stabilization) in coarse-textured soil are major factors limiting soil C storage capacity, despite higher C input from litterfall in the stand.…”
Section: Soil Propertiesmentioning
confidence: 99%