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Domination of hillslope denudation by tree uprooting in an old-growth forest

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00027073%3A_____%2F17%3AN0000018" target="_blank" >RIV/00027073:_____/17:N0000018 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/17:00096015

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0169555X16305001" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0169555X16305001</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.geomorph.2016.10.006" target="_blank" >10.1016/j.geomorph.2016.10.006</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Domination of hillslope denudation by tree uprooting in an old-growth forest

  • Original language description

    Razula forest preserve in the Carpathian Mountains of the Czech Republic is an unmanaged forest that has not been logged or otherwise anthropically disturbed for at least 83 years, preceded by only infrequent selective logging. Weexamined this 25 ha area to determine the dominant geomorphological processes on the hillslope. Tree uprooting displaces about 2.9 m3 of soil and regolith per year, representing about 1.5 uprooted trees ha−1 yr−1, based on forest inventory records dating back to 1972, and contemporary measurements of displaced soil and pit-mound topography resulting from uprooting. Pits and mounds occupy N14% of the ground surface. Despite typical slope gradients of 0.05 mm−1, and up to 0.41, little evidence of mass wasting (e.g., slump or flow scars or deposits, colluvial deposits)was noted in the field, except in association with pit-mound pairs. Small avalanche and ravel features are common on the upslope side of uproot pits. Surface runoff features were rare and poorly connected, but do include stemwash erosion associated with stemflow. No rills or channels were found above the valley bottom area, and only small, localized areas of erosion and forest litter debris indicating overland flow.Where these features occurred, they either disappeared a short distance downslope (indicating infiltration), or indicate flow into tree throw pits. Surface erosion is also inhibited by surface armoring of coarse rock fragments associated with uprooting, as well as by the nearly complete vegetation and litter cover. These results show that the combination of direct and indirect impacts of tree uprooting can dominate slope processes in old-growth, unmanaged forests. The greater observed expression of different hillslope processes in adjacent managed forests (where tree uprooting dynamics are blocked by management activities) suggests that human interventions can change the slope process regime in forest ecosystems.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

    <a href="/en/project/GA16-15319S" target="_blank" >GA16-15319S: Ecosystem engineering and soil complexity in old-growth temperate forests</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2017

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Geomorphology

  • ISSN

    0169-555X

  • e-ISSN

    1872-695X

  • Volume of the periodical

    276

  • Issue of the periodical within the volume

    1 January 2017

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    10

  • Pages from-to

    27-36

  • UT code for WoS article

    000388777800004

  • EID of the result in the Scopus database