Abstract:Almost half of the total rural area of Guizhou Province and many regions within the 11 adjacent provinces in southwestern China have a long history (at least 70 years) of endemic fluorosis, including dental fluorosis and osteofluorosis along with its associated deformities and disabilities. Over decades of research, this specific type of endemic fluorosis has been defined as coal-burning fluorosis, which is distinct from drinking-water fluorosis. It is generally acknowledged that indoor burning and combustion … Show more
“…Fluorosis in general, has been identified in various countries (Sinha et al 2000). Almost half of the rural areas of Guizhou province and many regions within the 11 adjacent provinces in southwestern China have a long history (at least 70 years) of endemic fluorosis, including dental fluorosis and osteofluorosis along with its associated deformities and disabilities (Liang et al 2011). Unless effectively controlled, industrial F -emissions, especially from phosphate fertilizer plants and plants producing aluminum, iron, glass, and ceramics, are significant environmental hazard to the biocenosis of water ecosystems (Maria et al 2001).…”
Studies were conducted on the bioconcentration of fluoride (F(-)) in five submerged plants species. Ceratophyllum demersum, Hydrilla verticillata, Potamogeton malaianus, Myriophyllum verticillatum and Elodea nuttallii were all able to remove F(-) from water to some degree of efficiencies. At 5-20 mg F(-)/L culture solution, C. demersum had the best F(-)-removal performance, E. nuttallii had the poorest F(-)-removal performance among these plants. The relative growth rate (RGR) of the five species varied in different concentrations of F(-), of which C. demersum had the highest RGR. Its RGR decreased by 26.3 %, 63.2 % and 73.7 % from controls at 5, 10 and 20 mg F/L, respectively.
“…Fluorosis in general, has been identified in various countries (Sinha et al 2000). Almost half of the rural areas of Guizhou province and many regions within the 11 adjacent provinces in southwestern China have a long history (at least 70 years) of endemic fluorosis, including dental fluorosis and osteofluorosis along with its associated deformities and disabilities (Liang et al 2011). Unless effectively controlled, industrial F -emissions, especially from phosphate fertilizer plants and plants producing aluminum, iron, glass, and ceramics, are significant environmental hazard to the biocenosis of water ecosystems (Maria et al 2001).…”
Studies were conducted on the bioconcentration of fluoride (F(-)) in five submerged plants species. Ceratophyllum demersum, Hydrilla verticillata, Potamogeton malaianus, Myriophyllum verticillatum and Elodea nuttallii were all able to remove F(-) from water to some degree of efficiencies. At 5-20 mg F(-)/L culture solution, C. demersum had the best F(-)-removal performance, E. nuttallii had the poorest F(-)-removal performance among these plants. The relative growth rate (RGR) of the five species varied in different concentrations of F(-), of which C. demersum had the highest RGR. Its RGR decreased by 26.3 %, 63.2 % and 73.7 % from controls at 5, 10 and 20 mg F/L, respectively.
“…Consequently, developmental defects of the tooth are referred to as coal-burning dental fluorosis [ 4 ]. Extensive investigations have revealed that the fluoride levels of coal used in most places are generally lower than the national average [ 5 , 6 ]. Except for a few regions with high fluoride content in coal, this pathway is not the only contributor to the prevalence of dental defects in China [ 7 ].…”
“…Using time-of-flight secondary ion mass spectrometry (TOF-SIMS) combined with on-site coal combustion tests, Liang et al [27] verified that naturally outcropping coal, commonly used by locals, was rich in sulfuric acid. This led to the proposition of a new perspective: during usage of coal-fired systems, sulfuric acid facilitates the release of fluorine in the form of hydrogen fluoride (HF), which then pollutes the environment.…”
It is common practice to use clay for coal-burning in fluorosis areas on the border of Yunnan, Guizhou, where coal-bearing strata is widely outcropped, and clay for coal-burning is usually considered to be collected from efflorescent clay in coal-bearing strata by some scholars. However, the relevant chemical properties of the clay, the mechanism that causes the fluorosis are not clear and the chemical forms of fluorine species present during transfer from the clay to the human body remain unclear. In this study, approximately 71 samples of efflorescent clay of coal-bearing strata were collected from seven counties in this area, and the results showed that those samples had a high-fluorine content with an average of 751 μg•g -1 (237-1,764 μg•g −1 , n = 71). The clays were rich in acid with an average pH of 5.81 (2.39-8.25, n = 71) and the acidic clays accounted for 52% of the total clay samples. The sulfate (SO 4
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