Fluoride Absorption Research Articles

Irradiation of dental enamel with Q-switched lambda = 355-nm laser pulses: surface morphology, fluoride adsorption, and adhesion to composite resin.

Lasers can be used to modify the chemical composition of dental enamel to increase the bond strength to restorative materials and to render the mineral phase more resistant to acid dissolution. Previous studies have suggested a synergistic relationship between CO(2) laser irradiation and fluoride treatment on increased resistance to acid dissolution. In this study a near-UV laser operating with lambda = 355-nm laser pulses of 3-5 nanoseconds duration was used to modify the surface morphology of dental enamel to increase the bond strength to restorative materials and increase the uptake of topical fluoride to render the surface more resistant to acid dissolution. We hypothesize that the short UV laser pulses are primarily absorbed by protein and lipid localized between the enamel prisms resulting in removal of intact mineral effectively etching the surface without thermal modification of the mineral phase. Such modification is likely to increase the permeability of the enamel surface and the subsequent absorption of fluoride. In addition, there is an increase in surface roughness without the formation of a layer of loosely adherent, thermally modified enamel that increases the bond strength to composite restorative materials. The surfaces of blocks of bovine enamel, 5 x 5 mm(2), were uniformly irradiated by 355-nm laser pulses and subsequently bonded to composite. The shear bond test was used to assess the bond strength of non-irradiated blocks (negative control), acid etched blocks (positive control), and laser irradiated blocks. The resistance to acid dissolution was evaluated using controlled surface dissolution experiments on irradiated samples, irradiated samples exposed to topical fluoride, and non-irradiated control samples with and without fluoride. The laser surface treatments significantly increased the shear-bond strength of enamel to composite, to a level exceeding 20 MPa which was significantly more than the non-irradiated control samples and significantly less than the acid etch. Laser irradiation alone and topical fluoride application alone did not significantly increase the resistance to acid dissolution. The laser treatment followed by topical application of fluoride significantly increased the resistance to acid dissolution to a level of over 50% versus the control samples. We present a novel method for increasing bond strength to restorative materials and enhancing fluoride delivery to enamel surfaces and shed some light on the underlying mechanisms of caries inhibition via laser treatment and topical application of fluoride.

The absorption and excretion of fluoride and arsenic in humans

The absorption and excretion of fluoride and arsenic were measured in a group of healthy volunteers given drinking water with naturally high concentration of fluoride (F 2.3 mg/l) , or high concentration of arsenic (As 0.15 mg/l), or high concentrations of both fluoride and arsenic (F 2.25 mg/l, As 0.23 mg/l and F 4.05 mg/l, As 0.58 mg/l), respectively. The results indicated that, for arsenic, the absorption rate, the proportion of urinary excretion and the biological-half-life did not show statistically significant differences between drinking water containing high arsenic alone and drinking water containing different levels of high arsenic and fluoride. Excretion and retention of arsenic were positively correlated to the total arsenic intake. Similar results were observed for fluoride. This suggests that there are different metabolic processes for arsenic and fluoride in respect to absorption and excretion; and no joint action can be attributed by these two elements.

Combined effects of diets with reduced calcium and phosphate and increased fluoride intake on vertebral bone strength and histology in rats.

Ingested fluoride is incorporated into bone apatite and can affect the structural integrity of bone. Fluoride absorption in the gut and incorporation into bone is affected by the presence of other ions, including calcium. We hypothesized that a low calcium phosphate diet combined with high fluoride intake would have independent detrimental effects on vertebral bone strength. We measured the vertebral biomechanical properties and bone histology for rats given controlled diets with varied fluoride and calcium phosphate intakes for either 16 or 48 weeks. Diets were designed to produce mild calcium deficiency while keeping Ca:P ratio constant. Hence calcium deficiency was accompanied by a proportional phosphate deficiency. Calcium phosphate deficiency (25% of normal) significantly diminished vertebral strength only in younger rats. As the rats grew older, the effects of calcium phosphate deficiency were mitigated. Calcium phosphate deficiency reduced vertebral strength in young rats primarily by reducing the trabecular bone volume. The highest fluoride intake (50 mg/L) significantly diminished vertebral strength, but there was no effect of lower fluoride intakes on bone strength. In contrast to calcium phosphate deficiency, high fluoride intake had no effect on trabecular bone volume but instead increased the amount of unmineralized osteoid, particularly in older rats. This impairment of mineralization by fluoride appeared to be the primary cause of the diminished vertebral strength. The detrimental effects of fluoride on vertebral bone strength were not amplified by calcium phosphate deficiency.

Absorption of Hydrogen Fluoride by Ash Foam Glass

An active absorption of hydrogen fluoride vapors by high-porous foam glasses produced by thermal activation of coal ashes is observed. The mechanisms of the processes involved are investigated by the magnetic resonance method and X-ray powder diffraction analysis. It is shown that incorporation of fluorine into the glass matrix is accompanied by its progressive destruction with the formation of microcrystalline and X-ray amorphous phases of individual chemical compounds.

Absorption of Fluoride and Aluminum, and Transferrin Binding of Aluminum in Rats

Absorption of Fluoride and Aluminum, and Transferrin Binding of Aluminum in Rats

Effects of caffeine on fluoride, calcium and phosphorus metabolism and calcified tissues in the rat

This 6-week study was designed to determine the effects of graded doses of caffeine intake (3, 25 or 100 mg/kg per day) on the metabolic balance and tissue concentrations of fluoride, calcium and phosphorus in Sprague–Dawley rats. Caffeine intake did not affect the absorption, urinary excretion or balance of fluoride, the plasma, bone or enamel concentrations of fluoride, nor the occurrence of incisor enamel fluorosis. Neither did it affect the metabolism of calcium or phosphorus except that the urinary excretion of calcium was increased. This effect, however, was not sufficient to influence significantly calcium balance. The ash content of the femur epiphysis and bone mineral content of the tibia were significantly reduced only in the group exposed to the highest dose of caffeine. These effects on bone were not significantly related to the balance of calcium or phosphorus. It was concluded that caffeine, even at an extremely high level of intake, has no detectable effect on the balance or tissue concentrations of fluoride, calcium or phosphorus in the rat.

Reduction of the bioavailability of fluoride from Antarctic krill by calcium

The bioavailability of fluoride from krill exoskeleton and the effect of additional calcium on the bioavailability of fluoride from krill paste were evaluated using young rats. Fluoride from the exoskeleton showed a high apparent absorption of 80%. Approximately 3.6% of this fluoride was deposited in the femur, and 44% in the rest of the carcass. The presence of 1.5% and 2.5% calcium (CaCO3) in the diet -1.0 and 2.0% above the minimum recommended content respectively- significantly reduced the bioavailability of fluoride from krill paste. The apparent absorption of fluoride from the paste was reduced by 33.8 and 45.8%, deposition in the femur by 48.1 and 58%, and retention in the rest of the carcass by 44.4 and 55.6%, respectively. The need for further studies using lower amounts of fluoride and calcium and other chemical forms of calcium is indicated.

PH-dependent fluoride transport in intestinal brush border membrane vesicles

Fluoride (F) absorption from the rat stomach and urinary bladder, hamster cheek pouch, and the renal tubules of several species are pH gradient-dependent. These observations led to the hypothesis that F crosses these epithelia in the form of the undissociated acid, HF. Several recent reports, however, have provided evidence that F absorption from the rat small intestine is insensitive to the lumenal pH. We report here our evidence that F uptake by rabbit intestinal brush border membrane vesicles (BBMV) occurred rapidly and with an overshoot only in the presence of an inward-directed proton gradient. In the absence of a proton gradient or in the presence of an outward-directed gradient, F uptake was slow and without an overshoot. In the presence of an inward-directed proton gradient, F uptake was partially inhibited by DIDS and DEP but not by diBAC. PCMBS inhibited F uptake by up to 83% in a dose-response manner. DiBAC appeared to reduce intravesicular pH slightly but the other reagents had no effect. When the uptake buffer contained chloride or nitrate, F uptake was partially inhibited compared to the mannitol or gluconate controls. It was concluded that F transport across the rabbit intestinal BBMV occurs via a carrier-mediated process which may involve cotransport of F with H + or exchange of F with OH −. The inhibitory effects of DIDS, DEP and PCMBS may occur by affecting this carrier-mediated transport.

Fluoride pharmacokinetics and changes in lumbar spine and hip bone mineral density.

Debate about the use of fluoride for the treatment of vertebral osteoporosis has centered not only on whether fluoride treatment decreases vertebral fractures, but also the interindividual vertebral bone mineral density (BMD) response, the potential for nonvertebral fractures, as well as side effects and tolerability. These effects may be dose dependent and, in this study, we examine the pharmacokinetics of sodium monofluorophosphate (MFP) in osteoporotic patients and relate this to changes in BMD. Plasma fluoride absorption curves were measured from 0 to 6 h after ingestion of MFP at baseline and during long-term dosing in 21 patients with vertebral osteoporosis (T scores < or = 2). BMD was measured at baseline and at 12 months at the lumbar spine (LS), femoral neck (FN), trochanter, and Ward's triangle. We found that fluoride elimination was inversely related to creatinine clearance. LS BMD increased from a median of 0.77 g/cm2 (range 0.69 to 0.99) at baseline to 0.88 g/cm2 (0.75 to 1.13) (p < 0.001) after 12 months. This equates to a median increase of 12% (range -1.2 to 37). Median femoral neck BMD decreased from 0.75 g/cm2 (0.62 to 0.94) at baseline to 0.69 g/cm2 (0.62 to 0.92) (p = 0.13) after 12 months. This equates to a decrease of -2% (-19 to 10). BMD at the other hip sites also decreased slightly. Changes in LS and FN BMD were not significantly related (r = 0.28, p = 0.29). The various pharmacokinetic parameters measured were not related to changes in LS BMD; however, there was an inverse relationship between trough fluoride concentration during long-term dosing and change in FN BMD. Further studies are required to see if this relationship can be used to monitor osteoporotic patients treated with fluoride and prevent significant decreases in FN BMD and possibly fractures at this site.

A Physiologically Based Pharmacokinetic Model for Fluoride Uptake by Bone

A sex-specific, physiologically based pharmacokinetic (pbpk) model has been developed to describe the absorption, distribution, and elimination of fluorides in rats and humans. Growth curves generated by plotting mean body weights (kg) against age (weeks or years) are included in the simulation model to allow the integration of chronic fluoride exposure from birth to old age. The model incorporates age and body weight dependence of the physiological processes that control the uptake of fluoride by bone and the elimination of fluoride by the kidneys. Six compartments make up the model. These are lung, liver, kidney, bone, and slowly and rapidly perfused compartments. The model also includes two bone subcompartments: a small, flow-limited, rapidly exchangeable surface bone compartment and a bulk virtually nonexchangeable inner bone compartment. The inner bone compartment contains nearly all of the whole body content of fluoride, which, in the longer time frame, may be mobilized through the process of bone modeling and remodeling. The model has been validated by comparing the model predictions with experimental data gathered in rats and humans after drinking water and dietary ingestion of fluoride. This physiological model description of absorption, distribution, and elimination of fluoride from the body permits the analysis of the combined effect of ingesting and inhaling fluorides on the target organ, bone. Estimates of fluoride concentrations in bone are calculated and related to chronic fluoride toxicity. The model is thus useful for predicting some of the long-term metabolic features and tissue concentrations of fluoride that may be of value in understanding positive or negative effects of fluoride on human health. In addition, the pbpk model provides a basis for across-species extrapolation of the effective fluoride dose at the target tissue, bone, in the assessment of risk from different exposure conditions.

The use of fluoride absorption and secretion to demonstrate gastrointestinal physiology

The use of fluoride absorption and secretion to demonstrate gastrointestinal physiology

Absorption and Retention of Dietary and Supplemental Fluoride by Infants

There is a widespread belief that an adequate intake of fluoride during the pre-eruptive stage of enamel formation (i.e., from the diet in frequent small doses throughout the day) will be protective against caries in later life. To obtain data on bio-availability and retention of fluoride in one age group (infants), we studied 3 treatment regimens: In Regimen A, small amounts of fluoride were obtained from the diet in frequent doses throughout the day; in Regimen B, a fluoride supplement (0.25 mg) was given once each day with a feeding; Regimen C was similar to regimen B except that the fluoride supplement was given 1 h before a feeding. For the 3 regimens, the respective mean absorptions of fluoride were 90.1, 88.9, and 96.0% of intake, and the respective retentions were 12.5, 47.1, and 52.3% of intake. Neither the difference in absorption nor the difference in retention between regimens B and C was statistically significant. By subtracting the background urinary excretion of fluoride (i.e., excretion of fluoride while diet was the sole source of fluoride) from the excretion after administration of the fluoride supplement, we calculated that 68.1% of the supplement was retained in Regimen B and 73.0% of the supplement in Regimen C. The difference was not significant.

Effects of plasma fluoride and dietary calcium concentrations on GI absorption and secretion of fluoride in the rat.

This 30-day balance study with weanling rats was designed to determine the effects of plasma fluoride and dietary calcium concentration and their interaction on the absorption, balance, and tissue concentrations of fluoride. The three major groups differed according to the total exposure and plasma concentrations of fluoride. One group received fluoride only in the diet and the other two received additional fluoride by continuous infusion from miniosmotic pumps implanted S.C. Each group was divided into two subgroups with dietary calcium concentrations of 0.4% or 1.4%. Fluoride intake with the diet did not differ among the groups. Fecal fluoride excretion was directly related to plasma fluoride concentration. The absorption and balance of dietary fluoride were inversely related to plasma fluoride concentration. These effects were greatest in the groups fed the 1.4% calcium diet. The interactions of plasma fluoride and dietary calcium on these variables were highly significant (P < 0.0001). The balance of dietary fluoride was negative in the four groups that received additional fluoride by infusion. In the two groups that received fluoride only in the diet, the plasma and bone fluoride concentrations were 41% and 59% lower, respectively, in the 1.4% dietary calcium group. The findings indicate that net fluoride secretion into the GI tract can occur when plasma fluoride concentrations and calcium intake are elevated. They suggest that elevated plasma fluoride levels and calcium intake are factors that may diminish the effect of oral fluoride treatment in osteoporotic patients.

Two‐color multiphoton decomposition of 1‐bromo 2‐fluoroethane

AbstractMultiphoton decomposition of 1‐bromo 2‐fluoroethane (CH2BrCH2F, BFE) with a two‐color CO2 infrared laser is reported as a function of number of laser pulses. For single color irradiation at a wavelength chosen to excite BFE, the decomposition product, vinyl fluoride, which accumulates during the many‐pulse MPD experiment, is found to deactivate BFE decomposition. When a second laser, tuned to a vinyl fluoride absorption is introduced, coincident with the first, the vinyl fluoride is found to activate further BFE decomposition. These results are accounted for in terms of a pressure‐dependent model. Changes in model parameters, upon addition of the second laser, are shown to be consistent with interpretations in terms of collision‐dependent reaction schemes. © 1994 John Wiley &amp; Sons, Inc.

Influence of gastric acidity on fluoride absorption in rats.

The rate of F absorption from the stomach is pH-dependent, with greater absorption at low pH. Since the rate of absorption is also strongly influenced by the rapidity of gastric emptying, we have compared the relative importance of gastric acidity and gastric emptying in overall F absorption. Male rats (350 g, n = 85) were pre-treated with cimetidine (to inhibit gastric acid secretion) or pentagastrin (to stimulate gastric acid secretion) or were untreated controls, and given 50 micrograms F by stomach intubation. The pH of the F-containing solution was varied in the cimetidine-pre-treated group (pH 1.5, 5.5, 8.5), and was 5.5 for the control and pentagastrin-pre-treated groups. Gastric emptying was measured by addition of 14C polyethylene glycol to the F solution as an unabsorbed marker of fluid movement. F absorption was measured after 10, 20, and 40 min. The rate of gastric emptying was unaffected by pre-treatment or pH of the intubating solution. Initially, F absorption was greatest at low pH. After 40 min, absorption was comparable in all groups, averaging approximately 70% of the initial dose. The extent of absorption from the stomach was inversely related to pH, but increased absorption from the small intestine compensated for the low gastric absorption at high pH.

The RV Variability of Yellow Giants

AbstractThe hydrogen fluoride (HF) absorption cell technique has been used at the Canada-France-Hawaii Telescope for over a decade to monitor the radial velocity variability of nearby, solar-type stars in a search for substellar companions. As a complement to this program, we have also been monitoring a select group of G and K subgiants, giants and supergiants, which have all proved variable. We present here a brief summary of our analysis.

The HF Precise Radial Velocity Programme at DAO

AbstractA programme to measure precise radial velocities of late-type stars is being carried out at the 1.22-m telescope of the Dominion Astrophysical Observatory (DAO). Wavelength-calibration fiducials are imposed directly on the stellar spectra by passing the starlight through a controlled hydrogen fluoride (HF) absorption cell placed in front of the coude spectrograph. Presently, the primary targets of the programme are bright G, K, and M giants. Preliminary results confirm the low-amplitude, radial-velocity (RV) variability of the yellow giants discovered at the Canada-Prance-Hawaii telescope using the HF technique. These yellow giants and additional bright candidates are now being continually monitored at DAO. Preliminary results also indicate that the “yellow giant” variability extends to the early-M giants. In addition to the RV variations, the data also yield information on the simultaneous variability of the Ca II λ8662 line, Teff, as well as the R - I index of the stars.

Effect of delayed gastric emptying on fluoride absorption in the rat

The rate and site of fluoride (F) absorption were compared in fasted 350 g male rats given 50 micrograms F (as NaF) in either water or a 7.5% pectin solution. Absorption was measured at intervals up to 2 h following gastric intubation. Gastric emptying was measured by inclusion of 14C-PEG in the F solution. The extent of gastric F absorption was derived from rates of gastric emptying (14C-PEG loss) and F loss. Pectin markedly slowed gastric emptying, but by 2 h, more than 90% of the solution had passed into the small intestine in both groups, and F absorption exceeded 90% in both groups. The rate of F absorption was initially much slower in the pectin group than in the group given F in water, and plasma F concentration increased more slowly and reached a lower maximum value. Absorption from the stomach was greater in the pectin group, but still accounted for only approx 25% of total gastrointestinal absorption. The reduced rate of F absorption and slower rise in plasma F concentration accompanying delayed gastric emptying indicate that passage of F into the small intestine is the major factor in rapid F absorption.

Fluoride bioavailability from immediate-release sodium fluoride with calcium carbonate compared with slow-release sodium fluoride with calcium citrate

The circadian variation in serum fluoride was compared between treatment with immediate-release sodium fluoride (IR-NaF) (30 mg) and calcium carbonate (500 mg calcium) and slow-release sodium fluoride (SR-NaF) (25 mg) and calcium citrate (400 mg calcium) in seven patients with postmenopausal osteoporosis maintained on long-term fluoride treatment. During 12 h following a dose of SR-NaF, serum fluoride levels could be largely kept within the therapeutic window (believed to be 95–190 ng/ml or 5–10 μmol/l). In contrast, IR-NaF produced a wide circadian fluctuation with peak-to-trough change of about 200 ng/ml. Compared to SR-NaF, IR-NaF caused a significantly higher peak fluoride concentration in serum (322 vs. 158 ng/ml), and greater area under the curve (2269 vs. 1321 ng · h/ml) and urinary fluoride (6.72 vs. 3.80 mg/12 h). Thus, fluoride absorption from IR-NaF was twice as high as that from SR-NaF.

Fluoride, calcium and phosphorus metabolism in the rat: Comparison of ‘natural ingredient’ with semipurified diets

Three groups of weanling female rats were fed different, commercially available, ‘natural ingredient’ diets containing 12, 28 or 45 parts/10 6 F, mainly as bone meal, for six weeks. Two other groups were fed a low-fluoride (0.76 parts/10 6) semipurified diet. They received fluoride doses, either in the drinking water or by daily intraperitoneal injection, which were approximately equal to the average dose of the other three groups. Rats on the ‘natural ingredient’ diets ingested more food and water and excreted more faeces arid urine, effects which were attributed to the higher amounts of dietary fibre, Na, K and Cl. Thus, at any given concentration of fluoride in the food or water, the level of fluoride ingestion and the ensuing effects would be influenced by the type of diet used. The values for fractional fluoride absorption (45–49%) and retention (38–47%) were similar among the groups given ‘natural ingredient’ diets. In the groups given semipurified diet, the corresponding values were about twice as high with the exception that fractional absorption was negative (−41%) in the injected group, which indicated net intestinal secretion of fluoride. Fluoride balances and tissue concentrations were highest in the groups fed the semipurified diet, even though the level of intake was not always higher. The fractional values for calcium and phosphorus absorption (41–51%) and retention (33–43%) were also similar among the groups given ‘natural ingredient’ diets. The corresponding values were about twice as high in the groups fed the semipurified diet. In terms of supporting maximum bone calcification, phosphorus absorption was marginal in two of the groups on the ‘natural ingredient’ diets. Because of their variable fluoride concentrations and ill-defined compositions, the use of ‘natural ingredient’ diets in research should be avoided.