2001
DOI: 10.1139/cjfr-31-6-1084
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Frost heaving in a boreal soil in relation to soil scarification and snow cover

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Cited by 7 publications
(7 citation statements)
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“…Thus, while the control and the short-term snow removal treatment had similar amounts of root length in the beginning of the season, this diverged over the course of the growing season. This reduction in root growth and in standing fine root biomass could be the result of direct cellular root damage as it has been shown in mature trees (Cleavitt et al 2008), or indirect root damage through frost movement of the soil as it can occur in boreal systems (Bergsten et al 2001). It could also be a result of the injury of the understorey vegetation and the strongly reduced plant cover and consequently less photosynthetically fixed carbon available for root growth, altered biomass allocation in the plants or a combination of all of the above.…”
Section: P L a N T R E S P O N S E S T O A Nmentioning
confidence: 96%
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“…Thus, while the control and the short-term snow removal treatment had similar amounts of root length in the beginning of the season, this diverged over the course of the growing season. This reduction in root growth and in standing fine root biomass could be the result of direct cellular root damage as it has been shown in mature trees (Cleavitt et al 2008), or indirect root damage through frost movement of the soil as it can occur in boreal systems (Bergsten et al 2001). It could also be a result of the injury of the understorey vegetation and the strongly reduced plant cover and consequently less photosynthetically fixed carbon available for root growth, altered biomass allocation in the plants or a combination of all of the above.…”
Section: P L a N T R E S P O N S E S T O A Nmentioning
confidence: 96%
“…), or indirect root damage through frost movement of the soil as it can occur in boreal systems (Bergsten et al . ). It could also be a result of the injury of the understorey vegetation and the strongly reduced plant cover and consequently less photosynthetically fixed carbon available for root growth, altered biomass allocation in the plants or a combination of all of the above.…”
Section: Plant Responses To An Absent Snow Covermentioning
confidence: 97%
“…However, negative effects on nutrient availability, soil bulk density, water relations, and soil biology are likely to accompany this treatment (Page-Dumroese et al 1989;McMinn and Hedin 1990;Bock and Van Rees 2002;Simard et al 2003). Scarification also increases the occurrence of frost-heaving among planted seedlings, especially on sites with fine soil texture, where seedlings are growing under conditions of below-freezing air temperatures, high soil moisture content, poor soil drainage, and limited vegetation or thin snow cover (Bergsten et al 2001;von der Gönna 1992).…”
Section: Introductionmentioning
confidence: 99%
“…Seedlings planted on mounds are also less subject to the shading, moisture and nutrient competition, and snowpress associated with competing vegetation (Spittlehouse and Stathers 1990;Letchford et al 1996;Haeussler 1989). In addition, since inverted humus mounds reduce capillary water rise, frost heaving of seedlings may be reduced (Bergsten et al 2001).…”
Section: Introductionmentioning
confidence: 99%
“…Deeper snow increases the chances of a sub‐nivean space forming by providing a higher temperature gradient between the ground and the ambient air (Marchand 1982, Sanecki et al 2006). Deep snow reduces the probability of ground icing, due to rain or early melting, especially if the snow cover forms quickly in the early winter (Bergsten et al 2001, Rixen et al 2004). Deep snow can also restrict access to small mammals by predators such as foxes (Angerbjörn et al 1999, Gilg et al 2006), although this may be less applicable to mustelids which can hunt lemmings under the snow (Reid and Krebs 1996).…”
mentioning
confidence: 99%