The soil temperature at depths of 20, 50 and 100 cm has been higher in the summertime in the cultivated fen soil at Leteensuo than in cultivated Sphagnum peat soil, while the latter again had higher temperatures than Sphagnum bog in its natural state. There is a remarkable difference in soil temperature between two bogs of different geographical location, namely, Leteensuo and Pelsonsuo. At Leteensuo, which lies in the southern part of Finland, the soil begins to warm up at a much earlier date than at Pelsonsuo and the soil temperature is higher. The effective soil temperature (referred to +5°C) at 20 cm depth is nearly twice as high as at Pelsonsuo; at a greater depth it is even three times as high
Two main types of permafrost are found in northern Finland. The most widely known occurence is in mi...
Microbial processes in soil are moisture, nutrient and temperature dependent and, consequently, accu...
Reports Canadian Defence Research Board's study, 1950-54. Experiments on rates of freeze and thaw of...
The soil temperature at depths of 20, 50 and 100 cm has been higher in the summertime in the cultiva...
Soil temperature strongly influences physical, chemical, and biological activities in soil. However,...
Dataloggers: T: i-Button DS1921G, Maxim Integrated Products. Cumulative soil temperature sums were c...
Soil temperature regime substantially influences soil classification in Soil Taxonomy particularly i...
In this study air and ground temperature measurements taken over a 3-year period in a virgin peat bo...
The mean annual soil temperature, evaluated for the depths 5, 10, 20, 50 and 100 cm is negative and ...
vokKirjasto Aj-kKivennäismaan ja turvemaan lämpöoloista Pelsonsuolla vuosina 1955-195
Climate change has caused an increase of the soil temperature of the top 100 cm of 1.5 C on average ...
Hydrology controls the physical, chemical and biological processes in peatlands and hence could be t...
Seasonally frozen depth of peat soils in Western Siberia at six oligotrophic forested bogs (ryams) w...
This paper compares winter soil temperatures at five high arctic sites (Ny Alesund, West Spitsbergen...
Peat plateaus and palsas are characteristic morphologies of sporadic permafrost, and the transition ...
Two main types of permafrost are found in northern Finland. The most widely known occurence is in mi...
Microbial processes in soil are moisture, nutrient and temperature dependent and, consequently, accu...
Reports Canadian Defence Research Board's study, 1950-54. Experiments on rates of freeze and thaw of...
The soil temperature at depths of 20, 50 and 100 cm has been higher in the summertime in the cultiva...
Soil temperature strongly influences physical, chemical, and biological activities in soil. However,...
Dataloggers: T: i-Button DS1921G, Maxim Integrated Products. Cumulative soil temperature sums were c...
Soil temperature regime substantially influences soil classification in Soil Taxonomy particularly i...
In this study air and ground temperature measurements taken over a 3-year period in a virgin peat bo...
The mean annual soil temperature, evaluated for the depths 5, 10, 20, 50 and 100 cm is negative and ...
vokKirjasto Aj-kKivennäismaan ja turvemaan lämpöoloista Pelsonsuolla vuosina 1955-195
Climate change has caused an increase of the soil temperature of the top 100 cm of 1.5 C on average ...
Hydrology controls the physical, chemical and biological processes in peatlands and hence could be t...
Seasonally frozen depth of peat soils in Western Siberia at six oligotrophic forested bogs (ryams) w...
This paper compares winter soil temperatures at five high arctic sites (Ny Alesund, West Spitsbergen...
Peat plateaus and palsas are characteristic morphologies of sporadic permafrost, and the transition ...
Two main types of permafrost are found in northern Finland. The most widely known occurence is in mi...
Microbial processes in soil are moisture, nutrient and temperature dependent and, consequently, accu...
Reports Canadian Defence Research Board's study, 1950-54. Experiments on rates of freeze and thaw of...