| FLUORIDE |
International Society for Fluoride Research | Table of Contents 32(1) 1999 |
Note: please leave images on for viewing mathematical symbols. If you're using Netscape and notice ? marks or empty squares where characters should be, change your encoding to Central European ISO-8859-2 or Central European Windows 1250
Research Report
FLUORIDE UPTAKE CHARACTERISTICS OF FLY ASH
R Piekos and S Paslawska
Gdansk, Poland
SUMMARY: Retention of fluoride ion in dynamic experiments on columns packed with fly ash was studied at 20°C with a series of aqueous solutions containing 1, 5, 10, 20, 50, and 100 mg F-/L. The flow rate through a 450-g bed was
2 mL/hr. At the lowest F- concentration (1 mg/L), the F- level in the effluent initially increased and then gradually decreased down to 0 mg/L after 120 hours. With higher F- concentrations in the feed solutions, the F- concentration in the effluent steadily decreased reaching 0 mg/L after 120 - 168 hours. We conclude that coal fly ash is an effective sorbent for F- ions, especially at high concentrations in water.
Keywords: Coal burning, Fluoride removal, Fly ash, Water.
INTRODUCTION
Wastewaters from phosphate fertilizer plants may contain up to 2 per cent of fluoride.1 Increased levels of fluoride can also be present in effluents from the fluorine industry,1 glass etching,1 and in ground water around aluminum smelters.2,3 The problem of high fluoride concentration in groundwater resources has become an important health-related geo-environmental issue in some areas. Examples include the state of Rajasthan, India, where nearly 3 million people are reported to consume excess fluoride-containing water,4,5 and the upper regions of Ghana, where 23 per cent of wells have fluoride concentrations above the WHO recommended maximum guideline limit of 1.5 mg/L.6 In the Gdansk region, high fluoride levels (1.90 - 3.00 mg/L) were detected in Malbork drinking water supplies.7 Since excessive amounts of fluoride may cause adverse health effects to humans and animals, there is a need for defluoridation of industrial wastewaters. Classical procedures of defluoridation involve precipitation, adsorption, ion exchange, and membrane techniques.8 Of these, the most popular and cost-effective is precipitation of fluoride with lime. However, the resulting calcium fluoride, though sparingly soluble, still poses environmental concern and must be safely disposed of.
Fly ash is the major solid waste by-product from coal-fired power plants. It is produced as a fine residue carried off in the flue gases with relatively uniform particle size distribution in the 1 to 100 µm range. The main components of fly ash are silica, alumina, iron oxides, calcium oxide, and residual carbon. The fineness of the fly ash particles and the inherent large surface area (1 to 6 m2 g-1),9 together with the content of unburnt carbon, make it a good candidate for utilization as an inexpensive sorbent.
A literature survey revealed that fly ash has been used for removing heavy metals10-17 and radionuclides18 from aqueous solutions, for treatment of wastewaters to remove organic compounds19-22 and color,23 as a coal desulphurization agent,24 and - together with hydrated lime - for SO2 removal from flue gases.25
Dynamic experiments on leaching of trace elements from fly ash, carried out by Dybczynski and co-workers26 have shown that distilled water (1800 mL) leached out ca 23% of fluoride and simulated acid rain (H2SO4, pH 2.5, 1800 mL) ca 38% (both figures taken from a bar graph) of fluoride from 10 g of the material placed in a thin layer between two filter papers, during 6 hours.
There is also evidence27 that the capital and operating costs of wastewater treatment by fly ash to remove turbidity, fluoride, and to reduce COD, are lower than those by conventional lime precipitation.
In view of the advantages of fly ash as a low-cost sorbent, it seemed worth-while to study its efficiency in removing fluoride ion from high-fluoride waters.
|
F- conc. in incoming soln. – mg/L |
Aliquot of effluent taken for analysis - mL |
Sampling time hrs |
F- concentration in effluent - mg/L | ||
| First expt. | Second expt. | Mean | |||
| 0 |
4.0 |
24 48 72 |
1.0 0.8 0.5 |
0.8 0.6 0.5 |
0.9 0.7 0.5 |
| 1 |
1.0 |
24 48 72 96 |
1.8 0.8 0.5 0 |
2.0 1.5 0.9 0 |
1.9 1.2 0.7 0 |
| 5 |
1.0 |
24 48 72 96 120 |
3.8 1.8 1.5 0.5 0 |
3.9 1.9 1.5 0.3 0 |
3.8 1.8 1.5 0.4 0 |
| 10 |
1.0 |
24 48 72 96 120 144 |
7.5 5.3 3.6 1.9 0.5 0 |
6.8 5.2 3.9 2.5 0.9 0 |
7.1 5.2 3.7 2.2 0.7 0 |
| 20 |
0.1 |
24 72 120 168 |
12.5 5.5 2.5 0 |
13 7.0 3.5 0 |
12.6 6.2 3 0 |
| 50 |
0.1 |
24 72 120 168 |
17 12.5 5.5 0 |
18 13.5 4.2 0 |
17.5 13 4.8 0 |
| 100 |
0.1 |
24 72 120 168 |
25 15 4.8 0 |
22.5 17.5 5.8 0 |
24 16 5.3 0 |
DISCUSSION
Inspection of the results presented in the Table shows that the sorption of fluoride increases with increasing concentration of incoming solution. Pure water leaches fluoride from fly ash in which it is likely to occur in the form of fluorite and metal fluoride complexes. When a solution with low fluoride concentration (1 mg/L) is passed through the column, the fluoride level in the effluent is initially higher than in the incoming solution (1.9 mg/L average after 24 hrs) owing to concurrent leaching of the fluoride contained in fly ash. However, after 120 hrs the effluent becomes completely free of fluoride.
It is remarkable that the retention capacity of fly ash increases with increasing fluoride concentration in incoming solution. This finding is best illustrated by the decrease in F- levels of the solutions after 24 hrs. For the 5, 10, 20, 50 and 100 mg/L F- concentrations the respective drops in F- concentration are 24, 28, 36.5, 65 and 76 per cent. Complete retention of the fluoride by fly ash occurs after 120-144 hrs for the lower F-concentrations (1, 5, and 10 mg/L) and after 168 hrs for the higher F- concentrations.
The explanation for the high sorption capacity of fly ash with respect to the fluoride ion seems quite straightforward if one considers its high CaO content (7.2%) on the one hand, and a slow flow rate of the solution through the column (ca 40 mL/24 hrs) on the other. The hydration of the oxide is responsible for the high pH of the water slurry of fly ash (pH exceeding 10). The resulting calcium hydroxide reacts with the fluoride to afford a sparingly soluble calcium fluoride.
A simple calculation shows that in the total quantity of 450 g of fly ash packed in the column, there is 32.4 g (0.58 mole) of CaO, whereas 500 mL of the most concentrated F- solution (100 mg/L) contains only 0.0025 mole of F-.
Strong sorptive capacity of residual carbon is also likely to contribute to this process. Recent investigations into the morphology and bulk physicochemical properties of this fly ash component, carried out by Hurt and associates,29 led to the following conclusions (numbering by the present authors):
Especially supportive to our belief are conclusions (iii) and (v) above. Firstly, large pores of the carbon which are capable of accommodating oxygen molecules with the diameter of ca 300 pm, can also provide good access to much smaller fluoride ion with the diameter of 172 pm. Secondly, the surface area of the carbon (100 to 200 m2g-1) is much larger than that of bulk fly ash (1 to 6 m2g-1).9
We conclude that a double mechanism is likely to operate in the retention of fluoride by fly ash: chemical binding by calcium hydroxide and physical sorption by residual carbon particles.
This paper was presented and discussed at the XXIInd Conference of the International Society for Fluoride Research in Bellingham, Washington USA (24-27 August, 1998).
REFERENCES
| FLUORIDE 32 (1) 1999 pp 14-19 | International Society for Fluoride Research | |
| Home | Table of Contents | ISFR Board | Subscription Submissions | Announcements | Authors | Subject Index |