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ABSTRACT
The effects of CO2 from plant roots in facilitating the dissolution of CaCO3 and the reclamation of sodic soils was studied by comparing the HCO3- concentrations of leachates and the less of adsorbed Na from pots of cropped and uncropped soils receiving uniform leaching with salt-free water. It was found that the effect of CO2 on the replacement of adsorbed Na was measureable but small, and of less importance than the effect brought about by the hydrolysis of CaCO3 upon leaching. Data were obtained which indicate that alfalfa roots release more CO2 than Rhodesgrass roots, and that more of the CO2 is retained in the soil at high moisture levels than at low moisture levels.
1 Contribution from the U. S. Salinity Laboratory, Soil and Water Conservation Research Division, A.R.S., U.S.D.A., Riverside, California, in cooperation with the 17 Western States and the Territory of Hawaii.
2 Chemist and Soil Scientist, respectively.
Received for publication June 14, 1957. Accepted for publication August 6, 1957.
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