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Erosion Effects on Carbon Dioxide Concentration and Carbon Flux from an Ohio Alfisol

R.M. Bajracharyaa, R. Lala and J.M. Kimbleb

a School of Natural Resour., The Ohio State Univ., 2021 Coffey Rd., Columbus, OH 43210 USA
b USDA–NRCS Natl. Soil Survey Center, Federal Bldg. Rm. 152, 100 Centennial Mall North, Lincoln, NE 68508 USA



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Fig. 1 Mean soil air CO2 concentrations for four erosion phases during different seasons of the year (summer: Jun.–Aug.; autumn: Sep.–Nov.; winter: Dec.–Feb.; spring: Mar.–May). Bars indicate standard deviation about the mean. Fisher's LSD values are same for comparison of erosion phase (small letters) and season (capital letters) means

 


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Fig. 2 Variation of soil CO2 concentrations, mean diurnal CO2–C flux from the soil surface, soil temperature and soil moisture, averaged across all erosion phases during the study period from May 1996 to June 1997

 


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Fig. 3 First-order (bottom) and second-order (top) regression fit relationships for soil temperature vs. CO2 concentration across all erosion phases

 





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