氟化物污染评价及其与土壤化学性质的关系

P. A, E. M, B. N
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摘要

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