By Suresh Patel
In the environment fluorides occur both naturally (rock weathering, volcanic emissions) as well as due to human activities (phosphate rock mining, steel industry, drinking water fluoridation). In natural waters, concentration of fluoride is low, ranging up to 5 ppm; however certain wastewaters from steel or mining plants have increased fluoride content of up to 80 ppm.
In order to comply with environmental regulations, as well as to reduce costs, steel and mining process waters are often recycled in reverse osmosis plants operating at high recovery (70-80%). In these conditions brine waters that have highly concentrated fluoride and calcium content exceed the supersaturation of calcium fluoride and form a precipitate due to low calcium fluoride solubility in water (16 ppm at 20°C).
This article examines laboratory studies that were carried out to investigate additives that can control calcium fluoride precipitation in waters with high calcium fluoride saturation indices of up to 300.
Analysis of Waters Containing High Fluoride Content
Typical water that is found in steel industry plants contains fluoride levels of up to 80 mg/l. The studies focused on wastewaters from two steel mill plants in Asia. The waters are recycled in reverse osmosis plants at recoveries of around 70-80%.
Analysis on these two waters was carried out and calcium fluoride saturation indices were calculated using the following equation: