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A comparison of measured and theoretical soil acidity diffusion coefficients over a wide range of pH
Author(s) -
NYE P. H.,
AMELOKO A.
Publication year - 1986
Publication title -
journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 0022-4588
DOI - 10.1111/j.1365-2389.1986.tb00019.x
Subject(s) - diffusion , range (aeronautics) , base (topology) , analytical chemistry (journal) , soil ph , chemistry , mineralogy , thermodynamics , materials science , mathematics , soil water , environmental chemistry , soil science , environmental science , physics , composite material , mathematical analysis
SUMMARY The soil acidity diffusion coefficients have been measured at two P co2 levels with values in the range 2–70 × 10 −9 cm 2 s −1 . The coefficient passed through an ill‐defined minimum in the pH range 5–6.5. Theoretical values, calculated on the basis that the only significant acid‐base carriers in the soil were the H 3 O + ‐H 2 O and H 2 CO 3 ‐HCO − 3 pairs, agreed well with the experimental values over the whole pH range at P co2 = 0.005 atm. Agreement was not so good however at a CO 2 pressure of 0.0003 atm., especially in the neutralalkaline pH range. This was thought to be due to difficulties in maintaining this level of CO 2 throughout the soil samples.
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