Q Fluoride is the most electronegative of all chemical elements.
Q It is 17% in the order of frequency of occurrence of the elements.
Q The average crustal abundance is 300 mg/kg.
Q Mostly granite and granitic gneiss terrain.
O Apatite (Ca10(PO4)6F2)one of the major fluoride minerals.
Q Fluoride as complex hydroxy-silicates and hydroxyalumino-silicates, in
which the hydroxyl ions (OH) may be largely replaced by fluoride, as
observed in amphiboles and minerals of the mica family (biotite and
muscovite).
O Fluoride in the ground/surface water derives from the weathering and
subsequent leaching of fluoride-bearing minerals in rocks and soils like
Q Fluoride is one such ion that causes health problems in people living in
more than 25 nations around the world. Fluoride concentration of at least
0.6 mg/l is required for human consumption as it will help to have stronger
teeth and bones.
Q Consumption of water with fluoride concentration above 1.5 mg/l results
in acute to chronic dental fluorosis where the tooth become coloured from
yellow to brown. Skeletal fluorosis which causes weakness and bending of
the bones also results due to long term consumption of water containing
high fluoride.
k
Q Several rocks have fluoride bearing minerals like apatite, fluorite, biotite
and hornblende. The weathering of these rocks and infiltration of rainfall
through it increases fluoride concentration in groundwater.
Q WHO drinking water 1-1.5 mg/l.
Q Fluoride does not exhibit any colour, taste or smell
en re: i n
Fluoride Hydrogeochemistry
Q The high HCO, bearing water has alkaline nature, which favours
the higher mobility of F- ions in the groundwater. Solubility of
fluoride in soils is highly variable and has the tendency to be
higher at pH > 6. Higher F- concentration observed to have higher
pH values.
Q Fluoride rich groundwater in many parts of the world are often of
Na-HCO, type with low Ca?* concentrations and neutral to alkaline
pH values. Several studies have demonstrated positive correlations
between F- and both HCO, and Na* in high F- groundwater as well
as an inverse relationship between F and Ca ” concentrations in
Fluoride (mg/l) fects on human body
Below 0.5 Dental Caries
0.5 to 1.0 Protection against dental
caries. Takes care of bone
and teeth
1.5 to 3.0 Dental fluorosis
3 to 10 Skeletal fluorosis (adverse
changes in bone structure)
10 or more Crippling skeletal fluorosis
and severe osteoclerosis
IS
Fluorosis
Excess fluoride in the
body
(above 1.5 — 2 ppm)
Skeletal Fluorosis Dental Fluorosis
19 states in India have groundwater that is rich in
fluoride
+ In village Tilsipani of Mandia district in Madhya
Pradesh, 74.4 per cent of children and adolescents below
age 20 have dental motting. and 51.2 por cent are afflicted
with genu vakgum (knock knees).
® Groundwater surveys in Unnao district of ur conducted
Defluoridation process
Q Numerous exsitu methods are available for defluoridation of water
either at household or community level.
O Activated charcoal and activated alumina are the widely used
adsorbents. Brick, bone char, fly ash, red mud, rice husk, kaolinite,
bentonite, ceramic etc. are some of the other absorbents capable of
effectively removing fluoride from groundwater.
Q The effective removal of fluoride by these absorbents depends on
the initial concentration of fluoride, pH, contact time, type of
absorbent and its size. Nalgonda technique which is a well known
technique uses alum, lime and bleaching powder followed by rapid
mixing, flocculation, sedimentation and filtration.