کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4573778 1629491 2013 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Soil surface CO2 efflux measurements in Norway spruce forests: Comparison between four different sites across Europe — from boreal to alpine forest
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
Soil surface CO2 efflux measurements in Norway spruce forests: Comparison between four different sites across Europe — from boreal to alpine forest
چکیده انگلیسی

Extensive measurements of soil surface (including vegetation cover) CO2 efflux were carried out on 80 positions at four different forest sites (Sweden, Germany, Czech Republic and Italy) using a closed dynamic chamber technique. The period of measurement was 4–5 consecutive days per site. Two approaches were used to analyze the measured data, the Q10 parameter and the Arrhenius relationship. Basic environmental factors such as soil temperature and moisture were measured. All the four investigated sites showed a positive dependence of the soil surface CO2 efflux on soil temperature. The four datasets generally resulted in good agreement (up to 93%) between the approaches and residual analysis showed no significant difference between approaches (less than 8%). The Q10 ranged between 2.0 and 2.3 among the sites. The highest spatial variation of the soil surface CO2 efflux at 10 °C (expressed by the coefficient of variation CV) ranged from 30 to 65% between sites.


► Measurements of soil surface CO2 efflux were carried out at four different forests.
► Two approaches were used to analyze the data, Q10 and Arrhenius relationship.
► The four datasets resulted in good agreement (up to 93%) between the approaches.
► All sites showed a positive dependence of soil CO2 efflux on soil temperature.
► The spatial variation of the soil surface CO2 efflux ranged 30–65% between sites.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Geoderma - Volume 192, January 2013, Pages 295–303
نویسندگان
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