2016
DOI: 10.1007/s11368-016-1409-2
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Effect of tea plantation age on the distribution of fluoride and its fractions within soil aggregates in the hilly region of Western Sichuan, China

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Cited by 16 publications
(9 citation statements)
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“…However, as also observed in the present study, previous works that examined the fractional distribution of fluoride in soil identified the Res‐F as a predominant fraction 17,46,47 normally existing in mineral form and hardly bioavailable 47 . As regards to the WS‐F, that together with the Ex‐F is considered to form the labile and available soil fluoride pool, 48 values measured in the study area were from 2.7 to 5.5 times higher compared to those found by Dagnaw et al 44 . being also always significantly higher than the threshold of 16.4 mg kg −1 of available fluoride in soil established by EPA, FAO, and WHO as cited by Lakshmi et al ., 23 Limón‐Pacheco et al 40 .…”
Section: Discussionsupporting
confidence: 78%
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“…However, as also observed in the present study, previous works that examined the fractional distribution of fluoride in soil identified the Res‐F as a predominant fraction 17,46,47 normally existing in mineral form and hardly bioavailable 47 . As regards to the WS‐F, that together with the Ex‐F is considered to form the labile and available soil fluoride pool, 48 values measured in the study area were from 2.7 to 5.5 times higher compared to those found by Dagnaw et al 44 . being also always significantly higher than the threshold of 16.4 mg kg −1 of available fluoride in soil established by EPA, FAO, and WHO as cited by Lakshmi et al ., 23 Limón‐Pacheco et al 40 .…”
Section: Discussionsupporting
confidence: 78%
“…identified the Res-F as a predominant fraction 17,46,47 normally existing in mineral form and hardly bioavailable. 47 As regards to the WS-F, that together with the Ex-F is considered to form the labile and available soil fluoride pool, 48 values measured in the study area were from 2.7 to 5.5 times higher compared to those found by Dagnaw et al 44 being also always significantly higher than the threshold of 16.4 mg kg −1 of available fluoride in soil established by EPA, FAO, and WHO as cited by Lakshmi et al, 23 Limón-Pacheco et al 40 and Paul et al 41 Soil WS-F is highly related to the soil type: factors such as pH, clay minerals, organic matter and concentration of P and Ca are the main drivers of fluoride solubility in soil. Furthermore, in sodic soils, fluoride adsorption has been found to decrease with increasing exchangeable sodium percentage (ESP) level or pH.…”
Section: Discussionmentioning
confidence: 99%
“…Many factors influence the concentration of elements including F in tea plants and its product including cultivar type and growth conditions (soil pH; the F and aluminium contents and their forms in soils; rainfall, altitude, air, and soil pollution from industrial sources and urban activities), horticultural practices (the application of chemical and organic fertilizers, use of pesticides and soil conditioners, the F content of water used for irrigation, mechanical or hand plucking, and age of leaves), the period of withering, and the mechanical processes used in the treatment and packaging of tea [36, 132150]. …”
Section: Discussionmentioning
confidence: 99%
“…Considering that higher F content has been found in BT infused in teabags than loose orthodox BT [6, 134, 150], it would appear that the introduction of the black CTC teabags to international tea markets post-1970 and the change in origin of imported tea significantly altered population exposure to F. This is evident in the differences in F levels reported in our study with those reported for BT products in NZ during the 1940s [68]. In NZ, population exposure was further exacerbated by the rapid expansion of water fluoridation in the 1960s.…”
Section: Discussionmentioning
confidence: 99%
“…In soils, chemical sequential extraction has been employed to separate total fluoride (T‐F) presumably into water extractable fluoride (F (H2O) ), magnesium chloride (MgCl 2 ) extractable fluoride (F (MgCl2) ), fluoride bound to Mn/Fe hydroxides (F (oxides) ), fluoride bound to organic matter (F (OM) ), and residual fluoride (F (Res) ) (Fig. 2), 21–23 external fluoride can be transformed into other forms in soil solutions 24 . Another evaluation of soil fluoride is extracted independently by water (F (H2O) ) or calcium chloride (CaCl 2 ) solution (F (CaCl2) ) 22 .…”
Section: Fluoride In Soil and Bioavailability To Tea Plantsmentioning
confidence: 99%