1929
DOI: 10.1021/ie50240a029
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Ratio of Fluorine to Phosphoric Acid in Phosphate Rock

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Cited by 15 publications
(16 citation statements)
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“…The percentages of fluorine were nearly constant in the mechanical fractions from a particular sample, rn tile case Of the pebble phosphated the fluorine content of the original 8 samples was approximately constant and did not vary with the phospllorus pentoxide content, which is in agreement with results previously obtained on this type of phosphate( 7 ) . 'In all the samples analyzed during this investigation, the The loss was particularly great in the rock phosphates, the silica concentrated to a marked extent Inzoluble in 1 decrease in the percentages of silica as the particle , Sb: 0, ; Fl,,or?ne-P O, ratio a After drying at 105' C.…”
supporting
confidence: 89%
“…The percentages of fluorine were nearly constant in the mechanical fractions from a particular sample, rn tile case Of the pebble phosphated the fluorine content of the original 8 samples was approximately constant and did not vary with the phospllorus pentoxide content, which is in agreement with results previously obtained on this type of phosphate( 7 ) . 'In all the samples analyzed during this investigation, the The loss was particularly great in the rock phosphates, the silica concentrated to a marked extent Inzoluble in 1 decrease in the percentages of silica as the particle , Sb: 0, ; Fl,,or?ne-P O, ratio a After drying at 105' C.…”
supporting
confidence: 89%
“…56, Tennessee brown-rock phosphate, was used in the majority of the experiments with different fusion mixtures. Previous analyses (11) of this material by the volatilization method, together with analyses during the present investigation, indicate that it contains between 3.45 and 3.55 per cent fluorine. For the purpose of the present paper a fluorine value of 3.45 per cent is used.…”
Section: Methodssupporting
confidence: 71%
“…The fluorine content is variable within a considerable range but is always much less than the theoretical for fluoro-apatite (22,63,97,98,105,106,110,113,114,117,199,216). The minerals in fossil bone usually contain increased amounts of fluorine (42,165,175,176,177), which appear to enter the lattice by isomorphous replacement of COs and H2O (74) or OH (114).…”
Section: B Minor Constituentsmentioning
confidence: 99%