1991
DOI: 10.1016/0269-7491(91)90024-q
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Reversibility of stemflow-induced soil acidification in Swedish beech forest

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Cited by 18 publications
(14 citation statements)
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“…In view of the particularly large solute fluxes from mature babassu palms and considering that these palms occupy only 0.03% of the study area, the forest floor around babassu stems is likely a microsite with soil properties distinct from the bulk soil. Studies from a wide range of forest types provide evidence that sites that receive considerable amounts of stemflow tend to show a relatively low pH and high element turnover rates (Chang and Matzner, 2000a;Falkengren-Grerup and Björk, 1991). There is evidence from Rondônia forests that combination of higher soil moisture and high NO À 3 availability could create hotspots for denitrification and N 2 O emission (Garcia-Montiel et al, 2003).…”
Section: Stemflow and Its Relevance For Persistent Chemical Hotspotsmentioning
confidence: 99%
See 1 more Smart Citation
“…In view of the particularly large solute fluxes from mature babassu palms and considering that these palms occupy only 0.03% of the study area, the forest floor around babassu stems is likely a microsite with soil properties distinct from the bulk soil. Studies from a wide range of forest types provide evidence that sites that receive considerable amounts of stemflow tend to show a relatively low pH and high element turnover rates (Chang and Matzner, 2000a;Falkengren-Grerup and Björk, 1991). There is evidence from Rondônia forests that combination of higher soil moisture and high NO À 3 availability could create hotspots for denitrification and N 2 O emission (Garcia-Montiel et al, 2003).…”
Section: Stemflow and Its Relevance For Persistent Chemical Hotspotsmentioning
confidence: 99%
“…Throughfall solute deposition patterns, for instance, show a temporal stability at scales of weeks to several months (Raat et al, 2002;Staelens et al, 2006;Zimmermann et al, 2008Zimmermann et al, , 2007. Stemflow-induced microsites, in contrast, persist for decades or even longer depending on the lifespan of the tree (Chang and Matzner, 2000a;Falkengren-Grerup and Björk, 1991). Because babassu palms have an average lifespan of 150-180 years (Pinheiro, 2004) the stemflow-induced microhabitat around these palms exists for more than a century.…”
Section: Stemflow and Its Relevance For Persistent Chemical Hotspotsmentioning
confidence: 99%
“…Although stemflow-induced soil acidification has been widely reported for F. sylvatica (e.g. Falkengren-Grerup, 1989;Falkengren-Grerup and Bjork, 1991;Chang and Matzner, 2000), no known studies have documented stemflow-induced soil acidification for species having excurrent forms (e.g. Pinus), gentler branch inclination angles, and lower stemflow production values.…”
Section: Introductionmentioning
confidence: 98%
“…Stemflow, i.e. water running down along branches and stem, has been often considered to explain acidification of the stemflow area under beech [17,18,19,15,8,16], more especially in polluted countries [49,48,24,21,43]. Changes in litter quantity and quality under the canopy of trees have been also evoked, more especially the role of bark deposition [50,26,19].…”
Section: Introductionmentioning
confidence: 99%