Seasonal changes in soil temperature and snow-cover under different simulated winter conditions: Comparison with frost hardiness of Scots pine (Pinus sylvestris) roots

1999 ◽  
Vol 1 (4) ◽  
pp. 485-492 ◽  
Author(s):  
M.L Sutinen ◽  
T Holappa ◽  
A Ritari ◽  
K Kujala
1998 ◽  
Vol 28 (6) ◽  
pp. 946-950 ◽  
Author(s):  
Marja-Liisa Sutinen ◽  
Aulis Ritari ◽  
Teuvo Holappa ◽  
Kauko Kujala

The seasonal changes in soil temperature and in the frost hardiness of adult Scots pine (Pinus sylvestris L.) trees was studied between September 1991 and February 1993 in a pine forest located in Finnish Lapland. Air and soil (humus layer and 5 cm depth of mineral soil) temperatures were measured continuously every second hour. The frost hardiness of the roots in the humus layer and in the mineral soil (down to 10 cm) was measured by means of the electrolyte-leakage method. The temperature in the humus layer varied between 21.2°C and –3.2°C and in the mineral soil between 21.6°C and –2.4°C. The temperature in the humus layer was continuously slightly colder than in the mineral soil from late August until May. The frost hardiness of the pine roots was lowest (about –5°C) in May and during the first week of September. Frost hardiness stayed at its maximum of about –20°C during November and December and slightly decreased in January and February. During most of the sampling time, the frost hardiness of the roots in the humus layer was greater than in the mineral soil. There was a clear relationship between the soil temperature and the frost hardiness of roots.


1996 ◽  
Vol 26 (9) ◽  
pp. 1602-1609 ◽  
Author(s):  
Marja-Liisa Sutinen ◽  
Kari Mäkitalo ◽  
Raimo Sutinen

The survival of conifer roots under winter conditions is not well understood. The effect of long-lasting freezing at extremely low temperatures on the survival of the roots of Scots pine (Pinussylvestris L.) seedlings from a timberline seed source was studied. One-year-old containerized seedlings were kept for 4 months under winter conditions typical of the subarctic region. The freezing treatment was accelerated by preventing snow accumulation on half of the seedlings. The proportion of living root tissue and the amount of sugars (glucose, fructose, and sucrose) and starch in the needles and roots were measured at weekly intervals. The temperature within the growth medium without snow cover fell on a number of occasions to −30 °C. The lowest temperature recorded within the snow-covered growth medium was −20 °C. The sugar content increased faster and to a higher level in the seedlings without snow cover, but it did not affect root survival. The proportion of living root tissue without a cover of snow decreased by 80% by the end of December, and the roots were completely injured by the end of February. There was only a slight decrease in the proportion of living roots among seedlings covered by snow. The reduced root survival was not directly related to exposure to the lowest freezing temperatures; instead, it was manifested some weeks after exposure. This suggests that dehydration resulting from prolonged severe freezing caused root damage. The presence of a cover of snow reduces subzero temperature extremes and the severity of dehydration; together, these result in enhanced root survival.


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