The PDF file you selected should load here if your Web browser has a PDF reader plug-in installed (for example, a recent version of Adobe Acrobat Reader).

If you would like more information about how to print, save, and work with PDFs, Highwire Press provides a helpful Frequently Asked Questions about PDFs.

Alternatively, you can download the PDF file directly to your computer, from where it can be opened using a PDF reader. To download the PDF, click the Download link above.

Fullscreen Fullscreen Off


In this study, the soil CO2 efflux was measured by closed dynamic system method along with soil and meteorological parameters at 1600, 1700 and 1800 m elevations along different directional-aspects over a period of one year. The annual CO2 efflux rate (Fc) varied from 1.02 to 22.57 μmol m–2 sec–1, which was highest in the rainy season. The annual average Fc was maximum (8.67 μmol m–2 sec–1) at east facing slope followed by 7.58 and 7.32 μmol m–2 sec–1 at south facing slope and north facing slope respectively. Temperature (Ts), moisture (Sm) and evaporation of soil were found to be significant variables and selected to develop the regression model with R2 value of 0.85. The effect of soil moisture on Fc above 15°C Ts exhibited a better relationship with R2 value of 0.48 and temperature sensitivity (Q10) was found 3.25. This study reveals that the key controlling factors of CO2 efflux rate are soil moisture and soil temperature, which explains 66% variation in soil CO2 efflux.

Keywords

Seasonal Variation, Soil CO2 Efflux, Soil Moisture, Soil Temperature, Spatial Variation, West Himalayas.
User
Notifications
Font Size