Seasonal changes in soil temperature and in the frost hardiness of Scots pine (Pinus sylvestris) roots under subarctic conditions

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.

2020 ◽  
Vol 19 (3) ◽  
pp. 59-71
Author(s):  
Joanna Siwek ◽  

Aim of the study: The aim of the study was to investigate the effect of hurricane-driven deforestation and reforestation on diurnal changes in soil temperatures in the Tatra Mountains (Poland). Material and methods: Soil temperature was measured at 0.20 m of depth in the mineral soil horizons on both north-facing and south-facing slopes in the deforested subcatchment and in the control woodland subcatchment. Soil temperature measurements were collected every 10 minutes in 2015–2020. The cross-correlation analysis was applied in order to determine the magnitude of the delay of soil temperature to air temperature changes at four studied sites during a day. Results and conclusions: The effect of deforestation on diurnal changes in soil temperature manifested itself mainly via a larger range of diurnal soil temperatures during warmer part of the year. In the summer months the diurnal soil temperature range for deforested slopes was 1 to 3℃ higher than that for wooded slopes. Diurnal soil temperature ranges were found to strongly decline with reforestation. Deforested slopes were characterized by a more rapid soil temperature reaction to changes in air temperature over the course of the day. Cross-correlation revealed that soil temperature changes on a deforested, south-facing slope occurred 4 to 5 hours later relative to changes in air temperature, while the delay for a wooded slope facing the same direction was usually 7 to 8 hours. Soil temperatures in the summer, both during the day and at nighttime, were higher on deforested slopes than wooded slopes. This indicates that deforestation may significantly intensify soil warming caused by global climate warming.


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