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《Journal of Glaciology and Geocryology》 2005-05
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Influence of Environmental Factors on Soil CO_(2) Efflux and Its Spatial and Temporal Variations in Sub-alpine Scrub Forest of Qilian Mountains

CHANG Zong-qiang,\ FENG Qi,\ WU Yu-xia,\ SU Yong-hong (Laboratoryof Watershed Hydrology and Ecology of Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China)  
In the Qilian Mountains,sub-alpine scrub forestis the main vegetationtype and coversabout 42.58% of the total land area.Understanding of the sub-alpine scrub forestefflux of CO_(2)from the soil surface is a key component of the carbon balance of its ecosystem.Quantifying this flux and understanding the factors,which control the variation of temperature and soil moisture,are fundamental to understand the behavior of the ecosystem as a whole and to predict the consequences of climate change.Soil surface CO_(2)effluxes were measured on early April to late October 2004 witha LiCor 6400 gas exchange analyzer with soil respiration chamber attachment(LiCor Inc.,Lincoln,NE,USA).The analyzer is a closed infrared gas onethat measures soil respiration.FivePVC collars(0.008 m~(2)) areinstalled randomly a 5m 5m area,and the soil respirationwas measured continuously3 daysper month.Collars were imbedded approximately 2 cm into the soil and left in place throughout the measurement period.It wasnot measure until 1 week after installation to minimize the effects of disturbance from collar installation.And removed live vegetation inside the chamber collars at least 24 hr before measurements to minimize the influence of soil disturbance and root injury on the measurement.To evaluate the statistical models for estimating soil CO_(2)efflux,soil temperature and soil water content were measured.Soil temperature was measured at 15 cm by a probe attached to the IRGA chamber,and then a temperature profile was measured.Soil water content was measured by using time domain reflectometry(TDR;Tektronix cable tester) at each plot during the soil chamber measurements.During the growing season,the diurnal variation of meadow soil respiration in the mountain watershed of the Heihe River basin was low at night,with the lowest at 2:00~6:00,and started to rise rapidly during 7:00~8:30,and then descended during 16:00~18:30.The maximum soil CO_(2)efflux appeared during 11:00~16:00.The maximum of average soil CO_(2)efflux occurredin July and August,followed by May and September,and then by April and October.And it was basically consistent in April and October.The diurnal average of meadow soil CO_(2)efflux was between(0.79±0.60)μmol\5m~(-2)\5s~(-1)and(2.49±0.97)μmol\5m~(-2)\5s~(-1).Temperature,soil moisture and vegetation had great effects on the spatial variation of soil respiration in the area.
【Fund】: 中国科学院“百人计划”项目(2003401);; 国家自然科学基金项目(30271071)资助
【CateGory Index】: S714;
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