2013
DOI: 10.2478/v10285-012-0064-6
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Effects of Dwarf Pine Stands on Slope Deformation Processes, as a Basis for their Management in the Hrubý Jeseník Mountains

Abstract: This paper studies non-indigenous dwarf pine stands in the Hrubý Jeseník Mountains, from the perspective of their spatial and genetic relations to slope phenomena of deformation character. The paper contains a typology of regional slope deformations, data on their spatial distribution and specific properties, including risk estimates of their origination or further development in case of potential future dwarf pine stand clearings, as well as a three-stage categorization of dwarf pine stands based on this tend… Show more

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Cited by 6 publications
(5 citation statements)
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“…The main disturbance factors in the study area are probably gelifluction (Křížek et al, 2019) and activity of red deer (Šenfeldr et al, 2012). The highest seedling densities, on the KP plots (see Table 1), were due to their having soil substrate susceptible to gelifluction along with the highest red deer abundance (Křížek et al, 2019; Roštínský, Šenfeldr, & Maděra, 2013), both causing frequent disturbance. As the seedling density is modulated by site‐specific disturbance intensities, the site as random effect was found to have a noticeable effect on the presence or absence of seedlings.…”
Section: Discussionmentioning
confidence: 99%
“…The main disturbance factors in the study area are probably gelifluction (Křížek et al, 2019) and activity of red deer (Šenfeldr et al, 2012). The highest seedling densities, on the KP plots (see Table 1), were due to their having soil substrate susceptible to gelifluction along with the highest red deer abundance (Křížek et al, 2019; Roštínský, Šenfeldr, & Maděra, 2013), both causing frequent disturbance. As the seedling density is modulated by site‐specific disturbance intensities, the site as random effect was found to have a noticeable effect on the presence or absence of seedlings.…”
Section: Discussionmentioning
confidence: 99%
“…In the region of Hruby Jesenik, changes in alpine timber line were estimated in details in many papers (e.g. Šenfeldr & Maděra, 2011;Šenfeldr et al, 2014;Roštínský et al 2013), but this issue is out of aim of this study.…”
Section: Discussionmentioning
confidence: 99%
“…Flows of the second type commence as shallow slides of the regolith cover, usually very thin (c. 1 m thick), within forested slopes of considerable steepness (>25°). They have been recorded in the Karkonosze, Jizerské hory, Śnieżnik Massif and, particularly, Hruby Jeseník range (Hrádek, 1984;Pilous, 2011;Parzóch et al, 2012;Roštínský et al, 2013). Some transform into flows and move along a narrow track (in respect to length), whereas others continue sliding down to the valley floor across a wider zone up to 30 m such as the debris slide in the Śnieżnik Massif in 2011 (Parzóch et al, 2012).…”
Section: Debris Slides and Flowsmentioning
confidence: 99%