Assessment of Fluoride Contamination and its Relationship with Chemical Properties of Soil

P. A, E. M, B. N
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Abstract

The present study deals with surveying and analyzing the Fluoride concentration in the Reddiyarchatram block of Dindigul district of Tamil Nadu and establishing a correlation coefficient with the other soil chemical properties. The result indicated that water soluble fluoride content forms a negative correlation with soil pH, signifying that soil pH plays a prominent role in the solubility of fluoride. Water-soluble fluoride content has a positive relationship with soil available nitrogen, potassium and sodium indicating that presence of F in the soil increase their availability and vice versa. Soil phosphorus forms a significant positive correlation with fluoride. It says that increase in P content increases soil F. Also, a soil organic carbon and calcium presence affects the water soluble fluoride content as they form a significant negative correlation. Water-soluble fluoride forms a negative relationship with soil electrical conductivity, total dissolved solids, available potassium and sodium, suggesting these factors play a major role in F availability in soils. Results concluded from the present study show soils with low pH, low organic matter content, high phosphorus, and low calcium plays a prominent role in F solubility from the fluoride-bearing minerals which directly increase the concentration of the water soluble fluoride in the upper layers of the soil.
氟化物污染评价及其与土壤化学性质的关系
本研究对泰米尔纳德邦Dindigul地区Reddiyarchatram地块的氟化物浓度进行了调查和分析,并建立了与其他土壤化学性质的相关系数。结果表明,水溶性氟含量与土壤pH呈负相关,说明土壤pH对氟的溶解度起着突出的作用。水溶性氟含量与土壤速效氮、钾、钠呈正相关关系,表明土壤中F的存在增加了土壤速效氮、钾、钠的有效性,反之亦然。土壤磷与氟呈显著正相关。研究表明,磷含量的增加会增加土壤氟含量。此外,土壤有机碳和钙的存在会影响水溶性氟化物含量,因为它们形成了显著的负相关关系。水溶性氟与土壤电导率、总溶解固体、速效钾和速效钠呈负相关,表明这些因素在土壤氟有效性中起主要作用。研究结果表明,低pH、低有机质、高磷、低钙的土壤对含氟矿物对氟的溶解度起突出作用,直接增加了土壤上层水溶性氟的浓度。
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