Biogeochemistry in Akçakent Fluoride Deposits, Kırşehir, Turkey

Yıl 2024, Cilt: 7 Sayı: 2, 91 - 106, 31.12.2024

Mehmet Hazar Baba , Güllü Kırat , Özlem Balbaloğlu

https://doi.org/10.56728/dustad.1520978

Öz

Fluoride (F) is the anion of hydrofluoric acid, a pungent acid in the halogen group, which evaporates at 194 0C. Fluoride (F-) in the human body is absorbed from food and drink. The fluoride content of surface water is important for mineral exploration and human health. The reason for the low fluoride content in foods is water. Tomato plants and soil samples taken from the fluoride deposits of Akçakent (Kırşehir) and its surroundings are the main material of the study. The formation of fluorite deposits is associated with magmatic events. These deposits are found in the form of gangue minerals on the ceilings of the plutons. In rock-forming minerals (amphibole, mica, clay, apatite, and other water-containing minerals) F- only replaces OH-. F occurs in volcanic gases as HF. However, rocks in volcanic gas vents can be extremely altered. Hydrothermal solutions become acidic due to the absorption of fluoride. However, when they react with calcium and limestone, the pH value increases and basic fluorides are formed. Fluoride, CaF2, is a transparent and translucent, purple, green, brown, yellow, red, blue and colorless mineral.

Anahtar Kelimeler

fluoride, tomato, health, hydrothermal

Destekleyen Kurum

This study was produced from a master's thesis and was supported by Yozgat Bozok University Research Projects Unit (BAP) with the code 6601a-FBE/20-399.

Proje Numarası

6601a-FBE/20-399

Teşekkür

This study was produced from a master's thesis and was supported by Yozgat Bozok University Research Projects Unit (BAP) with the code 6601a-FBE/20-399. We thank you.

Akçakent Florit Yataklarının Biyojeokimyası, Kırşehir

Öz

Flor (F), halojenler grubunda yer alan, keskin kokulu bir asit olan hidroflorik asitin 194 oC'de buharlaşan anyonudur. İnsan vücudundaki florür (F-) yiyecek ve içecekler tarafından alınır. Yüzey sularının florür içeriği maden aramaları ve insan sağlığı açısından önemlidir. Gıdalardaki düşük florür içeriğinin nedeni sudur. Akçakent (Kırşehir) florit yatakları ve çevresinden alınan domates bitkileri ve toprak örnekleri çalışmanın ana materyalini oluşturmaktadır. Florit yataklarının oluşumu magmatik olaylarla ilişkilidir. Bu yataklar plütonların tavanlarında gang mineralleri şeklinde bulunur. Kaya oluşturan minerallerde (amfibol, mika, kil, apatit ve diğer su içeren mineraller) F-, yalnızca OH-'in yerini alır. Volkanik gazlarda büyük miktarda florür HF formunda bulunur. Ancak volkanik gaz çıkışlarındaki kayalar aşırı miktarda alterasyona maruz kalabilir. Hidrotermal çözeltiler florür içemesiyle asidik hale gelir. Ancak kalsiyum ve kireçtaşı ile reaksiyona girdiklerinde pH değeri yükselir ve bazik floritler oluşur. Florit mor, yarı saydam, şeffaf, mavi, yeşil, sarı, kahverengi, kırmızı ve renksiz bir mineraldir.

Anahtar Kelimeler

flor, domates, sağlık, hidrotermal

Etik Beyan

This study was produced from a master's thesis and was supported by Yozgat Bozok University Research Projects Unit (BAP) with the code 6601a-FBE/20-399.

Destekleyen Kurum

This study was produced from a master's thesis and was supported by Yozgat Bozok University Research Projects Unit (BAP) with the code 6601a-FBE/20-399.

Proje Numarası

6601a-FBE/20-399

Kaynakça

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