SEASONAL-CHANGES IN SOIL-TEMPERATURE AND IN THE FROST HARDINESS OF SCOTS PINE (PINUS-SYLVESTRIS) ROOTS UNDER SUB-ARCTIC CONDITIONS

Citation
Ml. Sutinen et al., SEASONAL-CHANGES IN SOIL-TEMPERATURE AND IN THE FROST HARDINESS OF SCOTS PINE (PINUS-SYLVESTRIS) ROOTS UNDER SUB-ARCTIC CONDITIONS, Canadian journal of forest research (Print), 28(6), 1998, pp. 946-950
Citations number
25
Categorie Soggetti
Forestry
ISSN journal
00455067
Volume
28
Issue
6
Year of publication
1998
Pages
946 - 950
Database
ISI
SICI code
0045-5067(1998)28:6<946:SISAIT>2.0.ZU;2-N
Abstract
The seasonal changes in soil temperature and in the frost hardiness of adult Scots pine (Pinus sylvestris L.) trees was studied between Sept ember 1991 and February 1993 in a pine forest located in Finnish Lapla nd. Air and soil (humus layer and 5 cm depth of mineral soil) temperat ures were measured continuously every second hour. The frost hardiness of the roots in the humus layer and in the mineral soil (down to 10 c m) was measured by means of the electrolyte-leakage method. The temper ature in the humus layer varied between 21.2 degrees C and -3.2 degree s C and in the mineral soil between 21.6 degrees C and -2.4 degrees C. The temperature in the humus layer was continuously slightly colder t han in the mineral soil from late August until May. The frost hardines s of the pine roots was lowest (about -5 degrees C) in May and during the first week of September. Frost hardiness stayed at its maximum of about -20 degrees C during November and December and slightly decrease d 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 min eral soil. There was a clear relationship between the soil temperature and the frost hardiness of roots.