1985
DOI: 10.1016/0143-148x(85)90004-7
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The mobility of soluble fluoride in soils

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Cited by 181 publications
(108 citation statements)
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“…But it should be noted that P affects the availability of F only in case of very high amounts of P in soil. Therefore, in our experiments a statistically significant increase of soluble F was detected in the both soil depths in accordance with the rates of the applied fertilizer, which presumably were induced by the decrease of soil pH (r=-0.92 p < 0.01) (Pickering, 1985;Barrow & Ellis, 1986;Loganathan et al, 2006). The significant increase of the amount of soluble F in the subsurface soil might be due to its leaching from the upper soil layer.…”
Section: )supporting
confidence: 75%
“…But it should be noted that P affects the availability of F only in case of very high amounts of P in soil. Therefore, in our experiments a statistically significant increase of soluble F was detected in the both soil depths in accordance with the rates of the applied fertilizer, which presumably were induced by the decrease of soil pH (r=-0.92 p < 0.01) (Pickering, 1985;Barrow & Ellis, 1986;Loganathan et al, 2006). The significant increase of the amount of soluble F in the subsurface soil might be due to its leaching from the upper soil layer.…”
Section: )supporting
confidence: 75%
“…Fluoride can be released in the environment from phosphate fertilizers, which include fluorine as an impurity (Pickering, 1985;Skjelkvale, 1994). Phosphate fertilizers commonly contain from 1.3 to 3.0% fluorine (McLaughlin et al, 1996), much higher than those analyzed here.…”
Section: Pollutant Sourcesmentioning
confidence: 99%
“…5f). Air pollutants from coal combustion and phosphate fertilizers are common sources of F -in the environment (Pickering, 1985). The fertilizers contained soluble F -ranging from 60 to 255 mg/kg with an average value of 175 mg/kg, while, coal samples contained total F -ranging 5.12 to 20.1 mg/kg with an average value of 10.2 mg/ kg (Table 5).…”
mentioning
confidence: 99%
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“…Estimated to be 13 th most abundant element in the earth's crust [1,2], fluoride is widely dispersed in nature, and the amount of fluoride presented naturally in groundwater is highly dependent upon the individual geological environment from which the water is obtained [3,4]. Fluoride occurs in a combined form in rocks and soils in a wide variety of minerals such as fluorspar (fluorite) (CaF 2 ), cryolite (Na 3 AlF 6 ), apatite (Ca 5 (PO 4 ) 3 F), topaz (Al 2 SiO 4 (F,OH) 2 ), amphiboles and micas [5].…”
Section: Introductionmentioning
confidence: 99%