Soil CO2 flux, also often referred as soil respiration is defined as the emission of CO2 generated in the soil as a result of microbial and root activities. Soil CO2 flux was measured and related to soil temperature and moisture in a 21 year old rubber plantation in central Kerala for a period of two years (June, 2010 to May, 2012). Measurements were made on an hourly basis for 272 days in the first year and 308 days in the second year. Soil respiration varied between the two years as well as between seasons in a given year due to variations in soil temperature and moisture. Total amount of CO2 emitted was more in 2010-11 (26.1 tonnes ha-1) than in 2011-12 (20.7 tonnes ha-1) which was apparently related to more rainfall and number of rainy days in 2010-11 than in 2011-12. Soil respiration was slightly more in the night than in the day indicating that the cooler temperature of the night favoured more soil respiration. Soil respiration was higher during monsoon and summer seasons than during post monsoon and winter seasons in both the years. During monsoon, post monsoon, winter and summer seasons, the soil CO2 fluxes were 2.21, 1.45, 1.47 and 2.19 μmol m-2 s-1, respectively in 2010-11. In 2011-12, the soil CO2 fluxes were 1.78, 1.15, 0.98 and 1.75 μmol m-2 s-1 during monsoon, post monsoon, winter and summer seasons, respectively. In general, warmer temperatures favoured more soil respiration when sufficient moisture was available in the soil. When soil moisture status remained continuously high for longer periods, soil CO2 fluxes were impaired. Sudden and intense rainfall during an otherwise relatively dry period led to voluminous eruption of CO2 from soil as observed during many instances in winter and summer seasons in both the years. This may be due to burst of entrapped CO2 in soil pores by rain water. Availability of moisture in soil was more critical than the soil temperature for soil respiration during summer whereas during wet periods, the soil temperature was more important. Rising temperature and changes in the amount and pattern of rainfall as a consequent effect of climate change may affect soil respiration rates which can have profound impact on global carbon cycle and also on soil organic matter, a key component that determines soil fertility.
Hevea brasiliensis, Climate change, Soil CO2 flux, Soil respiration, Soil moisture, Soil temperature