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NTIS 바로가기지하수토양환경 = Journal of soil and groundwater environment, v.23 no.6, 2018년, pp.90 - 103
임가희 (국립환경과학원 환경기반연구부 토양지하수연구과) , 이홍길 (국립환경과학원 환경기반연구부 토양지하수연구과) , 김형섭 (국립환경과학원 환경기반연구부 토양지하수연구과) , 노회정 (국립환경과학원 환경기반연구부 토양지하수연구과) , 고형욱 (국립환경과학원 환경기반연구부 토양지하수연구과) , 김지인 (국립환경과학원 환경기반연구부 토양지하수연구과) , 조훈제 (국립환경과학원 환경기반연구부 토양지하수연구과) , 김현구 (국립환경과학원 환경기반연구부 토양지하수연구과)
Although fluoride is an essential trace element, ingestion of excessive amount of fluoride could have detrimental effect on human health. Generally, the bioavailability of fluoride in soils was low, but it could be harmful to the environment depending on the soil properties. Therefore, it is necessa...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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불소를 함유하고 있는 광물은 무엇이 있는가? | , 2005), 불소를 함유하고 있는 광물은 수백 개에 이르는 것으로 알려져 있다(Weinstein and Davison, 2004). 매우 희귀하지만griceite(LiF) 라는 광물은 불소를 73% 함유하고 있으며(Weinstein and Davison, 2004), 그 외에 불소를 함유하고 있는 주요 광물로는 fluorite(CaF2), fluoroapatite (Ca5(PO4)3F), cryolite(Na3AlF6), villiaumite(NaF), topaz (Al2(SiO4)F2) 등이 있다(Handa, 1975; Hem, 1985; Apambire et al., 1997; Cronin et al. | |
1,000 mg/kg 이상의 고농도를 보이는 불소 오염토양이 발생하는 원인은 무엇인가? | 토양에 존재하는 불소화합물의 농도는 20에서 수천 mg/ kg까지 다양하게 보고되고 있으며(Davison, 1983), 일반적으로 토양 중 불소는 20~500 mg/kg의 농도 분포를 보이는 것으로 알려져 있다(Kabata-Pendias and Pendias, 1984). 1,000 mg/kg 이상의 고농도를 보이는 불소 오염토양은 자연적으로 불소함량이 높은 모암으로부터 발생했거나 인위적인 불소 오염원의 투입으로 발생한다(Yadav et al., 2018). | |
과도한 불소가 인체에 미치는 영향은 무엇인가? | , 2011). 과도한 불소는 치아표면에 반점을 착색시키고, 인대를 석회화시키는 불소증(fluorosis)을 발생시킨다(Kowalski, 1999; Fawell et al., 2006; Death et al., 2015). 또한 지적 발달에 영향을 미치며(Sun et al., 2000), 호르몬 생산을 방해한다(Peckham et al., 2015). |
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