Departments of 1 Medicine and 2 Molecular Physiology and Biophysics, Vanderbilt University School of Medicine, Nashville, Tennessee 37232-6303
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ABSTRACT |
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Nitric oxide, when released into the bloodstream, is quickly scavenged by Hb in erythrocytes or oxidized to nitrite. Nitrite can also enter erythrocytes and oxidize Hb. The goals of this work were to determine the mechanism of erythrocyte nitrite uptake and whether this uptake causes oxidant stress in these cells. Erythrocytes took up 0.8 mM nitrite with a half-time of 11 min. Nitrite uptake was sensitive to temperature and to the pH and ionic composition of the medium but was not inhibited by the specific anion-exchange inhibitor DIDS. About 25% of nitrite uptake occurred on the sodium-dependent phosphate transporter and the rest as diffusion of nitrous acid or other species across the plasma membrane. Methemoglobin formation increased in proportion to the intracellular nitrite concentration. Nitrite reacted with erythrocyte ascorbate, but ascorbate loading of cells decreased nitrite-induced methemoglobin formation only at high nitrite concentrations. In conclusion, nitrite rapidly enters erythrocytes and reacts with oxyhemoglobin but does not exert a strong oxidant stress on these cells.
nitric oxide; ascorbic acid; ascorbate free radical
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INTRODUCTION |
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NITRIC OXIDE (NO) is released in the vascular bed by endothelial cell NO synthase and by the inducible form of the enzyme present in activated inflammatory cells (25). Much of the NO released into the bloodstream should be scavenged by Hb in erythrocytes (16) or converted to nitrite in the presence of molecular oxygen (13, 29). Because of its stability, nitrite has been used extensively to confirm the previous existence of NO (4, 22). Nitrite will also be removed from the bloodstream by erythrocytes, although the rapidity with which this uptake occurs, as well as its mechanism, is controversial. Using nitrite-induced formation of methemoglobin as a measure of nitrite uptake, Zavodnik et al. (40) found that rates of methemoglobin formation were similar in erythrocytes and in erythrocyte hemolysates. This led them to conclude that the cell membrane poses little barrier to the entry of nitrite. In contrast, microspectrophotometric analysis of methemoglobin formation in single erythrocytes showed that nitrite enters the cells very slowly and not at all in the presence of glucose (36). In another study, the half-time for disappearance of 60 µM nitrite outside pig erythrocytes was reported to be ~12 min, which was considered slow relative to the circulation time (33).
In addition to wide variation in measurements of erythrocyte nitrite uptake, the mechanism by which nitrite enters erythrocytes is also unclear. In resealed erythrocyte ghosts, nitrite efflux was accelerated by other monovalent anions and inhibited by DIDS, which is a specific inhibitor of the anion-exchange (AE-1) protein in this cell (31). These findings implicate the latter protein in nitrite transport. However, the more recent studies of Zavodnik et al. (40) failed to show inhibition of nitrite-induced methemoglobin formation by DIDS when erythrocytes were incubated with nitrite. If nitrite does not enter erythrocytes by the AE-1 protein, then the means by which it is taken up remain to be established.
Once inside erythrocytes, nitrite reacts with oxyhemoglobin, which leads to the formation of nitrate and methemoglobin (10). The extent to which nitrite is reduced by the major low-molecular-weight antioxidants within erythrocytes is uncertain. Nitrite added to erythrocytes has been reported to oxidize GSH in rat erythrocytes (3). However, concern had been previously raised that GSH loss in such studies was due to its destruction after cell lysis (5). Ascorbic acid has long been known to reduce nitrite to NO (20, 27), and this has been proposed as a mechanism for extracellular NO regeneration in brain (26). However, ascorbate reduction of nitrite is rapid only at acid pH (9, 18, 27), and intracellular reaction of nitrite and ascorbate has not been demonstrated.
To address these issues, nitrite uptake and metabolism were studied in human erythrocytes. Erythrocytes removed nitrite from the medium in a dose-dependent manner that was very sensitive to temperature and pH, moderately sensitive to sodium and phosphate in the medium, and insensitive to DIDS. Together, these results favor diffusion of nitrite or nitrous acid (HNO2) across the erythrocyte membrane, with some uptake on the sodium-dependent phosphate transporter. Nitrite within erythrocytes reacted primarily with Hb but also depleted ascorbate when Hb was partly converted to methemoglobin. There was a slow but detectable reaction of ascorbate with nitrite that was associated with ascorbate depletion in intact cells. However, the high capacity for erythrocytes to scavenge nitrite is due largely to rapid uptake and reaction with Hb.
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EXPERIMENTAL PROCEDURES |
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Materials. Sigma/Aldrich Chemical (St. Louis, MO) supplied dehydroascorbic acid (DHA), tetrapentylammonium bromide, sulfanilic acid, DIDS, sodium nitrite, HEPES, and sodium ascorbate. New England Nuclear Life Science Products (Boston, MA) supplied H332PO4.
Preparation of erythrocytes and resealed erythrocyte ghosts. Blood was drawn from volunteers just before each experiment and was anticoagulated with heparin. Except where noted, erythrocytes were prepared by three centrifugation washes in 10 volumes of PBS. The latter consisted of 140 mM NaCl and 12.5 mM Na2HPO4 in deionized water, pH 7.4. The buffy coat of leukocytes was carefully removed from the surface of the erythrocyte pellet with each wash.
Measurement of methemoglobin.
Packed erythrocytes were hemolyzed by dilution with mixing in 10
volumes of deionized water. Methemoglobin in hemolysates was determined
according to Winterbourn (38) as the difference in
absorbance of diluted lysate between 577 and 630 nm, adjusted for the
respective extinction coefficients of oxyhemoglobin and methemoglobin.
In these crude hemolysates, there was a background of absorption at 630 nm due to cell membranes and cytosolic components. The level of this
background present in control cells was subtracted from each
determination of methemoglobin, and the results were expressed as the
percent increase in methemoglobin relative to total Hb
(oxyhemoglobin + methemoglobin).
Assay of intracellular ascorbate, GSH, GSSG, nitrite, and nitrate. The ascorbate content of erythrocytes was measured as previously described (23). This method uses filtration of diluted erythrocyte hemolysate through a Centricon YM-10 membrane (Millipore, Bedford, MA) to obtain a clear Hb-free filtrate that is suitable for direct assay of ascorbate by HPLC. The same method was used to prepare samples for measurement of the cellular contents of GSH (12) and GSSG (35). Concentrations of intracellular antioxidants, nitrite, and nitrate are expressed relative to the cytoplasmic space, which was taken as 70% of the packed cell volume (28).
Measurement of nitrite uptake. Erythrocytes at a 20% hematocrit were incubated at the indicated temperature in PBS that contained 5 mM D-glucose and 1.2 mM sodium nitrite, unless otherwise noted. At specified times, aliquots of mixed cells and buffer were removed, the cells were pelleted in a microfuge, and the nitrite concentration was determined in the supernatant. Intracellular nitrite was measured following ultrafiltration of hemolysates that had been hemolyzed by dilution in six volumes of water, as described above for assay of ascorbate and GSH. Nitrite was measured according to the method of Saville (30), with omission of ammonium sulfamate and mercuric chloride. The sensitivity of the assay was 0.5 µM with the use of nitrite standards. Nitrate was measured in the same samples as nitrite by the copper-cadmium method of Cortas and Wakid (8).
Ionic dependence of nitrite uptake. Erythrocytes at a 20% hematocrit were washed three times by centrifugation in five volumes of buffers of different ionic compositions before measurement of nitrite uptake, as described in Measurement of nitrite uptake. All buffers contained 5 mM D-glucose and were adjusted to pH 7.4 just before the incubations. These buffers were PBS, PBS in which sodium had been replaced by potassium of the same molarity, and PBS in which phosphate had been replaced by 12.5 mM HEPES.
Measurement of radioactive phosphate uptake. Erythrocytes at a 2.5% hematocrit were incubated at room temperature in 1 ml of HEPES buffer that contained 5 mM D-glucose, 25 µM DIDS, 1 µCi of H332PO4, and the indicated concentration of nitrite. After 20 min, the cells were pelleted in a microfuge, washed once in 1 ml of ice-cold HEPES buffer, and lysed with 0.2 ml of 25% m-phosphoric acid. The suspension was mixed and then microfuged, and an aliquot of the supernatant was placed in 4 ml of liquid scintillation fluid and counted in a Packard CA-2000 liquid scintillation counter on settings for 32P with quench correction. Radioactivity was corrected for the results of a time 0 sample and normalized to the total radioactivity added.
Ascorbate and nitrite loading of erythrocytes. To increase intracellular concentrations of ascorbate in erythrocytes, cells at a 10% hematocrit were incubated for 15 min at 37°C in PBS containing 5 mM D-glucose and 400 µM DHA. DHA is taken up by the cells on the glucose transporter and immediately reduced to ascorbate, which is then trapped in the cells (37). We previously showed that ascorbate leakage from erythrocytes loaded in this manner is negligible over a 30-min incubation at 37°C (24). Loading of cells with nitrite was carried out by incubating control or DHA-treated cells with the indicated concentration of nitrite for an additional 60 min at 37°C. In some experiments, extracellular nitrite and nitrate concentrations were measured at this point. To determine intracellular nitrite and nitrate concentrations after nitrite loading, cells were pelleted in a microfuge, washed three times by centrifugation in 10 volumes of ice-cold PBS, and taken for determination of nitrite, nitrate, or methemoglobin. Use of ice-cold buffer prevented the efflux of nitrite during the centrifugation washes.
Electron paramagnetic resonance spectroscopy for detection of the ascorbate free radical. Changes in the concentration of the ascorbate free radical (AFR) were measured by electron paramagnetic resonance (EPR) spectroscopy. EPR data were acquired on a Bruker EMX 8/27 spectrometer equipped with a BVT300 variable-temperature controller. Sample temperature was maintained at 37°C during data acquisition by blowing precooled nitrogen into the cavity through the front optical port. X-band EPR spectra were collected using a ER041XG-DHA microwave bridge and ER4103TM/9614 cavity. Sample incubations were carried out in a Wilmad WG 804 aqueous-flow flat cell. The magnetic field was fixed at a value that corresponded to the maximum signal intensity of the low field resonance line of the AFR. The conversion time of the spectrometer was chosen to result in a sweep time of 167 s (since each data set contained 2,048 points, the timing resolution was ~0.082 s/point). Other spectrometer settings were as follows: 0.5 G modulation amplitude, 100 kHz modulation frequency, and 10 mW microwave power. The flat cell was preloaded with buffer or a suspension of erythrocytes at the indicated hematocrit to permit tuning of the spectrometer, and the experiment was initiated by starting the time sweep to record a baseline signal. After ~10 s, buffer or erythrocyte suspension that had been mixed with nitrite was injected, and the change in AFR signal amplitude was followed with time. The concentration of the AFR was determined by calibration of the instrument using the signal of 10 µM Tempol.
Statistical analysis. Values are means ± SE from the indicated number of experiments. Differences between treatments were analyzed with the computer program SigmaStat 2.0 (Jandel Scientific, San Rafael, CA) using two-way ANOVA with post hoc testing by Tukey's test or paired Student's t-test as appropriate. P < 0.05 was considered significant.
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RESULTS |
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Nitrite uptake by erythrocytes.
As shown in Fig. 1A, nitrite
was stable under the incubation conditions used in these studies.
However, in the presence of 20% erythrocytes, the extracellular
nitrite concentration fell progressively during incubation at 37°C,
reaching ~15% of the initial value at 60 min. Fitting the latter
results with a monoexponential function and residual resulted in a
half-time of 11 min. The disappearance of nitrite from the medium
outside erythrocytes was mirrored in time by an increase in
methemoglobin within the cells (Fig. 1B). When nitrite had
fallen to low levels outside the cells, methemoglobin formation ceased.
Cells incubated without nitrite formed little methemoglobin (Fig.
1B). Together, these results show that the cell-induced
decrease in extracellular nitrite concentrations was due to its uptake
and subsequent reaction with Hb.
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Ionic dependence of nitrite uptake.
Nitrite uptake by erythrocytes was sensitive to the ionic composition
of the incubation medium. As shown in Fig.
3A, replacing sodium in PBS
with potassium significantly slowed the rate of nitrite entry into
erythrocytes compared with a control incubation in PBS. Substituting
HEPES for phosphate as the buffer anion enhanced nitrite uptake to a
small but significant extent over a 30-min incubation (Fig.
3B). The inhibition by phosphate was further evaluated by
measuring effects of increasing nitrite concentrations on
32Pi uptake. Uptake of
32Pi was linear with time under these
conditions (results not shown). Since phosphate is known to be largely
transported on the AE-1 protein (32), incubations also
contained 25 µM DIDS to block this component. As shown in Fig.
4, increasing concentrations of nitrite
significantly inhibited 32Pi uptake in
DIDS-treated cells, although the effect was partial and observed only
at 2 mM nitrite. Phosphonoacetic acid, which inhibits the
Na-Pi cotransporter in renal brush-border membranes with an
inhibition constant of 1.3 mM (34), had no effect on erythrocyte nitrite uptake at
15 mM (results not shown). Nonetheless, the inhibition of 32Pi uptake by nitrite and
the inhibition of nitrite uptake by phosphate suggest that nitrite can
use the Na-Pi cotransporter present in erythrocytes, albeit
with a low affinity.
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Oxidant stress induced by nitrite.
The fate of nitrite incubated with erythrocytes was evaluated with the
experiments shown in Figs. 5 and
6. Erythrocytes were first
incubated with increasing concentrations of nitrite, washed by
centrifugation to remove remaining extracellular nitrite, and taken for
assay of intracellular nitrite and methemoglobin. To increase as much
as possible the intracellular concentrations of nitrite in this
experiment at a given initial extracellular nitrite concentration, the
hematocrit was 10%, rather than 20%, as used in the experiment shown
in Fig. 1. Nevertheless, intracellular nitrite concentrations did not
increase appreciably until the extracellular nitrite concentration
exceeded 200 µM (Fig. 5A). On the other hand, consistent
increases in methemoglobin content were observed after the cells were
incubated with 100 µM extracellular nitrite (Fig. 5B). The
sensitivity of methemoglobin formation to the intracellular nitrite
concentration becomes more apparent when methemoglobin formation is
expressed as a function of the measured intracellular nitrite
concentration for the control sample (Fig. 5C). In three of
the experiments shown in Fig. 5, intracellular nitrate was also
measured and was unchanged by increasing extracellular nitrite
concentrations (results not shown). At 1 mM added nitrite, almost
one-half of the Hb in these cells was converted to methemoglobin during
the 60-min incubation.
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DISCUSSION |
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Erythrocytes have long been thought to scavenge nitrite that is
generated from oxidation of NO in the bloodstream (10). For this reason, it is debatable whether any nitrite can be detected in
blood plasma. Published measurements of nitrite in serum or plasma
range from undetectable (2, 11) to 0.4 µM (17,
29) to as high as 8.8 µM (1). Scavenging of
nitrite by erythrocytes could also be important when the local nitrite
concentration in blood increases dramatically in response to NO release
from endothelial or inflammatory cells. We found that erythrocytes can
rapidly take up and metabolize nitrite at concentrations much greater than expected in vivo with little evidence of oxidant stress, aside
from methemoglobin formation. At extracellular nitrite concentrations expected in blood in vivo (i.e., 100 µM), there was little
intracellular nitrite accumulation (Fig. 5A) or
methemoglobin formation (Fig. 5B). The lag in methemoglobin
formation with increasing extracellular nitrite probably relates to the
function of methemoglobin reductase (39) to recycle
methemoglobin. When the capacity of this enzyme is exceeded, nitrite
accumulates within the cells and methemoglobin is formed (Fig.
5C).
At least part of the capacity for erythrocytes to scavenge nitrite relates to rapid uptake of extracellular nitrite. In our experiments, erythrocytes took up 500 µM nitrite with a half-time of 11 min (Fig. 1), in agreement with previous results from uptake studies using pig erythrocytes (33) and from studies in human erythrocytes in which nitrite uptake was inferred from the rate of methemoglobin formation (40). In the latter study, it was concluded that the erythrocyte membrane posed little barrier to nitrite entry, since rates of methemoglobin formation in hemolysates were similar to those in intact cells (40). Our result showing that intracellular AFR is generated in response to uptake of extracellular nitrite over a 2-min period (Fig. 7B) also suggests rapid transmembrane equilibration of nitrite followed by a slower, but irreversible, reaction with Hb that allows progressive uptake of nitrite from the medium. Thus the erythrocyte membrane does present a barrier to nitrite entry but probably does not limit the reaction of nitrite with Hb.
Nitrite appears to cross the erythrocyte membrane by more than one
mechanism. Simple transmembrane diffusion of NO2 is
probably minimal because of the negative charge of nitrite. Another
possibility suggested by Zhao et al. (41) is that nitrite solutions contain small amounts of gaseous nitrogen oxides, such as
nitric oxide (NO·), nitrogen dioxide (NO2·), dinitrogen
trioxide (N2O3), and dinitrogen tetroxide
(N2O4), which would readily diffuse across the
cell membrane. Diffusion of HNO2, which has a
pKa of 3.2 (19), is also plausible.
At pH 7.4, the HNO2 concentration of a 1 mM solution of
NO2
would be ~60 nM (41). Since the
HNO2 concentration would increase logarithmically with a
decrease in pH, this could account in part for our observation that a
decrease in pH of the medium increases nitrite uptake (Fig. 2). The
effect of pH on nitrite transport could also be due to a pH-dependent
change in function of a transport protein.
In the erythrocyte the most likely protein-dependent route for entry of a monoanion such as nitrite is the AE-1 protein. However, our results measuring nitrite uptake as the disappearance of nitrite from the incubation medium showed no inhibition by DIDS. This finding confirmed that of Zadvodnik et al. (40), who used methemoglobin formation to reflect nitrite uptake. Under the conditions employed in the present studies, DIDS should completely block transport on AE-1 (32). It was previously shown in pancreatic acinar cells that DIDS-sensitive bicarbonate transporters were the major route of entry of nitrite (41), but this does not appear to be the case for human erythrocytes. Previous measurements of nitrite efflux in erythrocyte ghosts indicated that DIDS was inhibitory (31). Whereas AE-1 is not involved in nitrite influx, it could still be involved in nitrite efflux (31).
At least part of the uptake of nitrite by erythrocytes in our experiments occurred on the Na-Pi cotransport system that has been described in these cells (32). The initial rate of nitrite uptake was inhibited by ~25% by removal of sodium from the incubation medium and by inclusion of phosphate (Fig. 3). There was also a corresponding inhibition by nitrite of DIDS-insensitive 32Pi uptake by erythrocytes (Fig. 4), which coincides with at least partial uptake on this transporter. Shoemaker et al. (32) found 75% of phosphate uptake by erythrocytes to occur on the AE-1 protein and 20% on the Na-Pi cotransport system. In contrast to the present results, phosphate uptake on the latter protein decreases with a decrease in medium pH (32). It is possible that the opposite effect observed in the present studies was due to enhanced diffusion of HNO2 with decreasing medium pH and that this obscured a decrease in nitrite transport on the Na-Pi cotransport system. The erythrocyte Na-Pi cotransporter appears to differ from the well-characterized renal brush-border membrane protein in its sensitivity to inhibitors. Neither arsenate (32) nor phosphonoacetic acid (present studies) inhibited phosphate transport in erythrocytes, whereas both are known inhibitors of the renal brush-border membrane Na-Pi cotransporter (34). Nonetheless, on the basis of the extent of inhibition of nitrite uptake by the addition of phosphate and removal of sodium (Fig. 3), nitrite uptake on the erythrocyte Na-Pi cotransport system could account for as much as 25% of nitrite uptake at pH 7.4. The remainder appears to be due to diffusion of HNO2 and gaseous species across the membrane.
Once taken up by erythrocytes, nitrite reacted largely with Hb, resulting in methemoglobin formation (Figs. 1 and 5). Little nitrite or nitrate accumulated in the cells, even at very high extracellular nitrite concentrations relative to those expected in plasma. In addition to increased amounts of methemoglobin within the cells, raising the nitrite concentration in the medium also increased nitrate outside the cells (Fig. 6). This indicates oxidation of nitrite in conjunction with methemoglobin formation. The failure to account for all the nitrite added to the cells as nitrite or nitrate is unexplained but could be due to reactions of nitrite with cell proteins, including Hb, which would form nitrosohemoglobin (7).
The ability of ascorbate to reduce nitrite to NO is well established, and this has prompted speculation that recycling of nitrite to NO by ascorbate in the brain could be of physiological importance (26). However, the ascorbate-nitrite reaction is typically measured at low pH, where it is rapid (18, 27). Low pH facilitates the formation of species such as H2NO2+ and N2O3, which will nitrosate the ascorbate anion, with subsequent release of NO (27). We found that ascorbate did react directly with nitrite at pH 7.4, albeit slowly, on the basis of the generation of the AFR (Fig. 7A). It has long been known that DHA is generated in this reaction, and it was predicted that the AFR would be an intermediate (9). Our EPR findings of a pH-dependent increase in the AFR after mixing nitrite and ascorbate confirm this prediction. Subsequent reaction of the AFR with nitrite or with another molecule of the AFR serves to generate DHA. It is also likely, but less certain, that the ability of nitrite to generate the AFR in intact cells (Fig. 7B) is due to direct reaction of nitrite and ascorbate. The latter effect could be due in part to reaction of ascorbate with other oxidants generated from nitrite within the cells. Scavenging of these products by ascorbate would tend to inhibit subsequent methemoglobin formation (see below).
We found that increasing the ascorbate content of cells decreased the amount of methemoglobin formed when nitrite was added to the medium (Fig. 5B). However, this decrease was evident only at high loading concentrations of nitrite (>400 µM), when >20% of cellular Hb had been oxidized to methemoglobin. There are two plausible explanations for the effect of ascorbate to decrease nitrite-dependent methemoglobin formation. The first relates to direct reaction of ascorbate with nitrite or with its breakdown products. The ascorbate-induced decrease in methemoglobin formation was associated with a corresponding decrease in intracellular nitrite concentrations (Fig. 5A). This, along with the observations that ascorbate reacts with nitrite or its metabolites in buffer at pH 7.4 (Fig. 7A), that it generates the AFR within cells (Fig. 7B), and that it decreases ascorbate concentrations in intact cells (Fig. 8A), suggests that the ascorbate effect on methemoglobin formation is due to removal of nitrite within the cell. NO generated in the reaction of ascorbate and nitrite should react with any remaining oxyhemoglobin. Our finding of a decrease in methemoglobin formation in intact cells loaded with ascorbate could indicate that NO is not the major product of the reaction of ascorbate with nitrite or with its breakdown products. More likely, it could indicate reactions of NO other than those leading to methemoglobin formation. For example, NO generated in this reaction might serve to S-nitrosylate Hb, and S-nitrosohemoglobin could then form a reserve of NO that could be released under the proper conditions (14).
The second explanation for why ascorbate decreased nitrite-induced methemoglobin formation has to do with interference by ascorbate with the reaction between nitrite and oxyhemoglobin. Reaction of nitrite with oxyhemoglobin is thought to occur via a two-step process: a slow initial phase followed by a more rapid autocatalytic phase (10). In solutions of Hb, ascorbate has been shown to inhibit the autocatalytic phase of Hb oxidation by nitrite (6, 10, 15). It appears that reaction of ascorbate with superoxide, hydrogen peroxide, or peroxynitrite generated during this phase accounts for the inhibition (10). This effect could therefore account for at least part of the ability of ascorbate to decrease methemoglobin formation that we observed. However, in the intact cell, methemoglobin reductase recycles the Fe3+ in methemoglobin to Fe2+, which then can again bind oxygen to form oxyhemoglobin (21). These considerations also suggest that use of methemoglobin formation in intact erythrocytes to measure nitrite or NO generation outside the cells is at best only qualitative, since it depends on cellular uptake and methemoglobin reduction. Clearly, the cell system is quite complex. Our failure to find significant effects of ascorbate on methemoglobin formation at any but very high nitrite concentrations argues that the physiological relevance of the effect is small. Furthermore, since the cellular contents of GSH and GSSG were minimally affected by high concentrations of extracellular nitrite (Fig. 8, B and C), the oxidant stress induced by external nitrite was not sufficiently severe to overwhelm this cellular defense mechanism.
In conclusion, erythrocytes take up nitrite by at least two different mechanisms: one involving diffusion of HNO2 and one involving the Na-Pi cotransporter. When the capacity for oxyhemoglobin to consume nitrite within cells is decreased, high levels of intracellular ascorbate can partially prevent Hb oxidation due to nitrite or is oxidative products. This effect is due to direct reaction of ascorbate with nitrite or its breakdown products and/or to inhibition of Hb oxidation by ascorbate. Ascorbate reacts with intracellular nitrite at physiological pH. However, this reaction is slow relative to the ability of erythrocytes to scavenge nitrite. Notwithstanding methemoglobin formation, which is reversible, nitrite concentrations expected in vivo exert little oxidant stress in erythrocytes.
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ACKNOWLEDGEMENTS |
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This work was supported by National Institute of Diabetes and Digestive and Kidney Diseases Grant DK-50435.
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FOOTNOTES |
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Address for reprint requests and other correspondence: J. M. May, 715 Medical Research Bldg. II, Vanderbilt University School of Medicine, Nashville, TN 37232-6303 (E-mail: james.may{at}mcmail.vanderbilt.edu).
The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked "advertisement" in accordance with 18 U.S.C. Section 1734 solely to indicate this fact.
Received 9 June 2000; accepted in final form 7 August 2000.
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