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- W1977314006 abstract "The reaction of sodium fluoride solution with soils and soil minerals at constant pH has been assessed as a possible single-value characteristic in the classification of soils, particularly those containing significant amounts of poorly ordered inorganic material. A suitable method involves reaction of the soil or clay at 25°C with 0·85 M sodium fluoride at pH 6·8, the amount of OH− released after 25 min being taken as the single-value characteristic. There was a statistically significant correlation between the amount of OH− released and the amount of alumina extracted with cold 5 per cent sodium carbonate solution from both freely drained and poorly drained Scottish soils. The multiple correlation coefficients were improved for freely drained soils by including the dithionite-extracted ferric oxide and the silica soluble in 5 per cent sodium carbonate solution. The procedure is not suitable for surface soils, because of interference by organic matter, or for carbonate-containing soils unless carbonate is removed." @default.
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- W1977314006 date "1976-03-01" @default.
- W1977314006 modified "2023-09-27" @default.
- W1977314006 title "THE REACTION OF FLUORIDE WITH SOILS AND SOIL MINERALS" @default.
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- W1977314006 doi "https://doi.org/10.1111/j.1365-2389.1976.tb01975.x" @default.
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