Nitrite anions comprise the largest vascular storage pool of nitric oxide (NO), provided that physiological mechanisms exist to reduce nitrite to NO. We evaluated the vasodilator properties and mechanisms for bioactivation of nitrite in the human forearm. Nitrite infusions of 36 and 0.36 μmol/min into the forearm brachial artery resulted in supra- and near-physiologic intravascular nitrite concentrations, respectively, and increased forearm blood flow before and during exercise, with or without NO synthase inhibition. Nitrite infusions were associated with rapid formation of erythrocyte iron-nitrosylated hemoglobin and, to a lesser extent, S-nitroso-hemoglobin. NO-modified hemoglobin formation was inversely proportional to oxyhemoglobin saturation. Vasodilation of rat aortic rings and formation of both NO gas and NO-modified hemoglobin resulted from the nitrite reductase activity of deoxyhemoglobin and deoxygenated erythrocytes. This finding links tissue hypoxia, hemoglobin allostery and nitrite bioactivation. These results suggest that nitrite represents a major bioavailable pool of NO, and describe a new physiological function for hemoglobin as a nitrite reductase, potentially contributing to hypoxic vasodilation.
Nitrite is a vasodilator at high concentrations in vitro1,2,3,4,5,6. In vivo plasma levels of nitrite are in the range of 150-1,000 nM, and the concentration in aortic ring tissue is >10 μM (refs. 7,
Consistent with the bioconversion of intravascular nitrite to NO, we and others have observed arterial-to-venous gradients of nitrite across the human forearm at rest and during regional NO synthase inhibition, with increased consumption of nitrite occurring during exercise8,26. Other research groups have reported large arterial-to-venous gradients of nitrite also form across the human forearm during NO synthase inhibition25. Unlike the simpler case of oxygen extraction across a vascular bed, nitrite is both consumed—as evidenced by arterial-to-venous gradients during NO synthase inhibition and exercise—and produced in the vascular bed by endothelial NO synthase–derived reactions of NO with oxygen. Supporting the existence of an intravascular NO species capable of storage and distal delivery of NO bioactivity, multiple research groups have observed that red blood cells and plasma 'loaded' with NO, by exposure to NO solutions, NO gas or NO donors, can export an 'NO-like' bioactivity and induce vasodilation in vitro and in vivo11,27,28,29,30,31,32. We have previously evaluated the reaction products formed in human blood during inhalation of NO gas, and found significant increases in plasma nitrite and limited formation of plasma and erythrocyte S-nitroso-proteins, suggesting a role for nitrite in the transduction of NO bioactivity along the vasculature29. We therefore considered the possibility that nitrite, rather than S-nitrosothiols, is the largest intravascular storage pool for NO, and that nitrite bioactivation to NO could vasodilate regions with tissue oxygen debt in the human circulation.
Vasodilatory properties of nitrite in vivo
Eighteen healthy subjects (nine males and nine females, aged 21–50 years) were enrolled in a physiological study to determine whether nitrite is a vasodilator and to examine nitrite's in vivo chemistry. In part I of the protocol, the normal hemodynamic and metabolic responses to exercise and to inhibition of NO synthesis in the forearm were measured as controls for part II, in which these interventions were done during nitrite infusion (Fig. 1a,b; see Supplementary Note online for detailed description of control observations). Parts I and II were conducted in random order.
To determine whether nitrite has vasoactivity in humans, in part II of the protocol we infused sodium nitrite in bicarbonate-buffered saline (final concentration of 36 μmol/ml) into the brachial arteries of the 18 subjects, to achieve an estimated intravascular nitrite concentration of ∼200 μM (ref. 25). After infusion of sodium nitrite at 1 ml/min for 5 min, nitrite levels in the ipsilateral antecubital vein increased to 221.82 ± 57.59 μM (Fig. 2a). Forearm blood flow increased by 175% over resting values; venous hemoglobin oxygen saturation, pO2 and pH levels increased significantly (all P < 0.01) over preinfusion values, indicating increased perfusion of the forearm.
The systemic nitrite concentration was 16 μM, as measured in the contralateral arm, and was associated with a systemic decrease in mean blood pressure of ∼7 mm Hg (P < 0.01). Consistent with immediate NO generation from nitrite during arterial-to-venous transit, iron-nitrosylated hemoglobin in the ipsilateral antecubital vein increased from 55.7 ± 11.4 to 693.4 ± 216.9 nM during nitrite infusion. During forearm exercise (with continued nitrite infusion), blood flow increased further. Metabolic stress was present, as evidenced by reduced forearm venous hemoglobin oxygen saturation, pO2 and pH levels compared with baseline values. Venous nitrite levels declined, indicating that increased blood flow to the forearm was diluting the concentration of infused nitrite. Despite decreasing forearm nitrite concentration during exercise, iron-nitrosylated hemoglobin levels increased, indicating an augmented rate of NO generation from nitrite during exercise stress (Fig. 2a).
After cessation of nitrite infusion and substitution of saline as the intra-arterial infusate for 30 min, repeat baseline measurements showed persistent elevations in systemic levels of nitrite, iron-nitrosylated hemoglobin and methemoglobin (Fig. 2b) compared with values obtained almost 1 h previously, before the infusion of nitrite. A persistent vasodilator effect was also apparent, as forearm blood flow was significantly higher (4.79 ± 0.37 versus 3.94 ± 0.38 ml per min per 100 ml tissue; P = 0.003) and systemic blood pressure was significantly lower (82.1 ± 3.7 versus 89.2 ± 3.5 mm Hg; P = 0.002) than initial preinfusion values. We then reinfused the brachial artery with sodium nitrite (36 μmol/ml) and NG-monomethyl-L-arginine (L-NMMA; 8 μmol/min) again to inhibit regional synthesis of NO. We observed vasodilator effects of nitrite on resting and exercise forearm blood flow similar to those observed during nitrite infusion without L-NMMA (Fig. 2b). This is in contrast to the vasoconstrictor effect of NO synthase inhibition with L-NMMA observed in part I of the protocol (Fig. 1b).
Vasodilatory properties of nitrite at physiological concentrations
As a test of the physiological relevance of vascular nitrite as a vasodilator, the concentrations of the nitrite infusions were decreased by 2 logs to 400 nmol/ml. An infusion of 400 nmol/ml nitrite at 1 ml/min for 5 min significantly increased forearm blood flow in all ten subjects from 3.49 ± 0.24 to 4.51 ± 0.33 ml per min per 100 ml tissue (Fig. 3a; P = 0.0006). Blood flow significantly increased at rest and during NO synthase inhibition, with or without exercise (Fig. 3b; P < 0.05 under all conditions). Mean venous nitrite levels increased from 176 ± 17 nM to 2,564 ± 462 nM after a 5-min infusion, and exercise venous nitrite levels decreased to 909 ± 113 nM (secondary to the diluting effects of increased blood flow during exercise; Fig. 3c). Again, the vasodilator effects of nitrite were paralleled by an observed formation of both iron-nitrosylated hemoglobin and S-nitroso-hemoglobin across the forearm circulation (Fig. 3d). These data suggest that basal levels of nitrite, from 150–1,000 nM in plasma to 10,000 nM in vascular tissue7,8,9, are likely to contribute to resting vascular tone and hypoxic vasodilation.
The vasodilatory property of nitrite during basal blood flow conditions, when tissue pO2 and pH are not exceedingly low, was unexpected. These results suggest that the previously hypothesized mechanisms for nitrite reduction, nitrite disproportionation and xanthine oxidoreductase activity, all of which require extremely low pO2 and pH values not typically encountered in normal physiology, must be complemented in vivo by additional factors that catalyze nitrite reduction. We now report that deoxyhemoglobin effectively reduces nitrite to NO, a mechanism described by Doyle et al. in 1981 (ref. 33), within one half-circulatory time from artery to vein. This mechanism provides graded production of NO along the physiological oxygen gradient, tightly regulated by hemoglobin oxygen desaturation.
Intravascular formation of NO and S-nitrosothiol
Before and during nitrite infusions, blood was drawn from the brachial artery and antecubital vein, and the whole blood was immediately (at the bedside to minimize processing time) lysed 1:10 in an NO-hemoglobin 'stabilization solution'. The iron-nitrosylated hemoglobin and S-nitroso-hemoglobin content was determined by tri-iodide-based reductive chemiluminescence and electron paramagnetic resonance (EPR) spectroscopy (described in Methods). As previously reported30 and recently confirmed9, the baseline levels of S-nitroso-hemoglobin and iron-nitrosyl-hemoglobin were at the limits of detection (<50 nM or 0.0005% NO per heme), with no artery-to-vein gradient. After nitrite infusion as in part II of the protocol, venous levels of iron-nitrosylated hemoglobin and S-nitroso- hemoglobin rose substantially (Fig. 4a–c). This formation of iron-nitrosylated hemoglobin across the forearm circulation was confirmed by EPR spectroscopy (Fig. 4b). The formation of both NO-hemoglobin adducts occurred across the vascular bed, with a half-circulatory time of less than 10 s. The rate of NO formation was measured as iron-nitrosylated and S-nitroso-hemoglobin content and quantified by subtraction of the arterial from the venous levels with the difference being multiplied by blood flow. The NO formation rate increased greatly during exercise, despite a significant decrease in the venous concentration of nitrite secondary to the dilution of regional nitrite concentration by increased blood flow (Fig. 4d; P = 0.006 for iron-nitrosylated hemoglobin and P = 0.02 for S-nitroso-hemoglobin, by repeated-measures ANOVA).
The amounts of iron-nitrosylated and S-nitroso-hemoglobin formed in vivo in this study are notable. With a transit time of less than 10 s through the forearm circulation during exercise, infused nitrite (200 μM regional concentration) produced ∼750 nM iron-nitrosylated hemoglobin and 200 nM S-nitroso-hemoglobin (Fig. 4b,c). The formation of both NO-hemoglobin adducts was inversely correlated with hemoglobin-oxygen saturation, which fell during exercise stress, as measured from the antecubital vein by co-oximetry (r = −0.7 and P < 0.0001 for iron-nitrosylated hemoglobin; r = −0.45 and P = 0.04 for S-nitroso-hemoglobin; Fig. 4e). Addition of 200 μM nitrite to whole blood at different oxygen tensions (0–100%) recapitulated the in vivo data, with increasing concentrations of iron-nitrosylated hemoglobin being formed at lower oxygen tensions (r = −0.968 and P < 0.0001 for iron-nitrosylated hemoglobin; r = −0.45 and P = 0.07 for S-nitroso-hemoglobin; data not shown). This strongly suggests that iron-nitrosylated hemoglobin and S-nitroso-hemoglobin formation was dependent on the reaction of nitrite with deoxyhemoglobin.
These data are consistent with the previous characterization of the reaction of nitrite with deoxyhemoglobin to form NO and iron- nitrosylated hemoglobin33. Nitrite is first reduced to form NO and methemoglobin, with a rate constant of 2.9 M−1s−1 (measured at 25 °C, pH 7.0)33. This reaction is pseudo-first order, governed by the vast amounts (20 mM) of intraerythrocytic hemoglobin, and limited by the rate of nitrite uptake by the erythrocyte membrane. NO then either binds to deoxyhemoglobin to form iron-nitrosylated hemoglobin, escapes the erythrocyte (discussed below) or reacts with other higher oxides (such as NO2, to form N2O3 and S-nitroso-hemoglobin; discussed later). These reactions are represented by the following equations:
NO2− (nitrite) + HbFe2+ (deoxyhemoglobin) + H+ → HbFe3+ (methemoglobin) + NO + OH−
NO + HbFe2+ (deoxyhemoglobin) → HbFe2+NO (iron-nitrosylated hemoglobin)
We confirmed that the reaction of deoxyhemoglobin and nitrite is second-order in nitrite and hemoglobin by conducting kinetic measurements, first with a molar excess of nitrite to hemoglobin, and then with an excess of hemoglobin to nitrite. We found the same bimolecular rate constant, 0.47 ± 0.07 M−1s−1, for both conditions at 25 °C and pH 7.4. This rate constant is similar to that found by Doyle et al. at this pH (1 M−1s−1)33.
To explore the effects of red blood cell membrane nitrite uptake rate on the formation of intraerythrocytic iron-nitrosylated hemoglobin, we examined the kinetics of the reaction of 200 μM nitrite with deoxygenated whole blood at 37 °C. Iron-nitrosylated hemoglobin formed at an observed rate constant (k) of 0.0035 ± 0.006 s−1 (Fig. 4f,g). Assuming a concentration of 20 mM for the concentration of hemoglobin in the red blood cell, this corresponds to a bimolecular rate of 0.18 ± 0.03 M−1s−1, which is substantially lower than the rate expected by measurements made by Doyle et al., and indicates that the in vivo rate is limited by erythrocyte nitrite uptake. Using this rate and a 10-s artery-to-vein transit time (with the equation (0.28)(200 μM) (1 − e−kt)), we would expect 1.9 μM of iron-nitrosylated hemoglobin formation in vivo. This result would be similar in magnitude to the observed formation of ∼750 nM iron-nitrosylated hemoglobin across the arterial-to-venous gradient (Fig. 4).
We also observed the formation of significant amounts of S-nitroso-hemoglobin in vivo during nitrite infusion. It was recently proposed that nitrite reacts with deoxyhemoglobin to make iron-nitrosylated hemoglobin, and that the subsequent 'transfer' of the NO to the cysteine 93 of the β-chain of hemoglobin to form S-nitroso-hemoglobin is mediated by reoxygenation and the quaternary T-to-R structural transition state of hemoglobin34. However, a direct transfer of NO from the heme to the thiol would require NO oxidation to NO+, and such 'cycling' has not been reproduced by other research groups35. It has recently been suggested that nitrite catalyzes the reductive nitrosylation of methemoglobin by NO, a process that generates the intermediate nitrosating species dinitrogen trioxide (N2O3)36. Additional reactions of nitrite with hemoglobin produce reactive oxygen metabolites (such as superoxide and hydrogen peroxide37,38,39). Such reactions of NO radicals with oxygen radicals will provide competitive pathways for S-nitrosothiol formation in the presence of high-affinity NO sinks such as hemoglobin and deserve further study.
Nitrite reductase activity of deoxyhemoglobin
To determine whether free NO radicals can be formed from the reaction of nitrite and deoxyhemoglobin, we reacted 100 and 200 μM nitrite with deoxygenated erythrocytes (5-ml volume containing a total of 660 and 1,000 μM in heme) in a light-protected, helium-purged reaction vessel in line with a chemiluminescent NO analyzer. The injection of nitrite into a solution of deoxygenated erythrocytes resulted in the liberation of NO into the gas phase (Fig. 5a,b). There was no release from nitrite in a buffer control under the same conditions, and significantly (P < 0.05) less NO was released upon addition of nitrite to oxygenated erythrocytes (100% oxygen). The observed rate (area under the curve of increased steady-state NO generation after nitrite injection, calculated over 120 s) of NO production in the 5-ml reaction volume was consistent with an NO production rate of 47 pM/s (corresponding to an estimated rate of 300–500 pM/s in whole blood). Although NO formation rates in this experimental system cannot be extrapolated to rates of NO formation in vivo, the experiments illustrate two important concepts. First, a fraction of the free NO can escape autocapture by the remaining heme groups; this is likely to be possible only because nitrite is only converted to NO by reacting with deoxyhemoglobin, and because its 'leaving-group' is the met(ferric)heme protein that will limit scavenging and inactivation of NO33. Second, the rate of NO production is increased under anaerobic conditions, which indicates a nitrite-deoxyhemoglobin reaction.
We next evaluated whether the vasodilator properties of nitrite could be reproduced in an aortic ring bioassay system, and whether this vasodilation is potentiated by deoxygenated erythrocytes. Rat aortic rings were suspended in custom-made vessel baths that were sealed and fitted with an oxygen electrode, allowing simultaneous measurement of vessel tension and pO2. Figure 5c shows representative tracings of vessel tension and pO2, measured during deoxygenation of rat aortic rings exposed to red blood cells (0.3% hematocrit, 300 μM heme) and nitrite (2 μM). To determine the relationship between oxygen tension, vessel tone and the impact of erythrocytes and nitrite, vessel tension was plotted as a function of pO2 (Fig. 5d). Control vessels spontaneously relaxed after reaching a pO2 of ∼10 mM Hg (Fig. 5e). Addition of 2 μM nitrite did not affect this process. Addition of rat erythrocytes alone increased the oxygen tension at which dilation was initiated (Fig. 5e), and addition of nitrite and erythrocytes together significantly (P < 0.004) left-shifted the vessel tension- pO2 threshold curve (Fig. 5c,d) such that vasodilation was observed at oxygen tensions <40 mm Hg (P < 0.004). Lower concentrations of nitrite (500 nM) that fall within the physiological range also significantly promoted vasodilation in the presence of red blood cells, compared with red blood cells or nitrite alone (Fig. 5d) (P < 0.05).
To test whether the effect of red blood cells on nitrite-dependent vasodilation could be mediated by deoxyhemoglobin, vessel dilation experiments were conducted at a pO2 of 15 mm Hg, with cell-free hemoglobin, in the absence or presence of inositol hexaphosphate (IHP; Fig. 5f). IHP was used to modulate the oxygenation state of hemoglobin in this system. In the absence of IHP, hemoglobin remained saturated with oxygen at a pO2 of 15 mm Hg (p50 = 9 mm Hg oxygen; p50 is the pO2 at which hemoglobin is 50% saturated with oxygen), but was deoxygenated in the presence of IHP (p50 = 45 mm Hg oxygen). At a pO2 of 15 mm Hg and using a Hill coefficient of n = 2.8, the oxygen saturation would be 81% for hemoglobin with p50 = 9 mm Hg, and 4% for hemoglobin with p50 = 45 mm Hg. With a heme concentration of 25 μM, ∼82% of oxyheme is tetrameric. Addition of nitrite alone stimulated vasodilation, with a half-maximal effective concentration of 100–200 μM. IHP alone slightly inhibited this effect, whereas hemoglobin alone right-shifted the dose-dependence of nitrite, indicating an oxyhemoglobin-dependent oxidation of nitrite to nitrate. However, in the presence of IHP and hemoglobin at a pO2 of 15 mm Hg, nitrite-dependent vasodilation was potentiated by three orders of magnitude (half-maximal effective concentration of 100–200 nM). These results support a physiological model for nitrite reduction to NO by reaction with erythrocyte deoxyhemoglobin.
We show that nitrite-induced vasodilation in humans is associated with reduction of nitrite to NO by deoxyhemoglobin. Systemic levels of 16 μM resulted in systemic vasodilation and decreased blood pressure, and regional forearm levels of only 1–2 μM significantly increased blood flow at rest and with exercise-induced stress. In addition, conversion of nitrite to NO and S-nitrosothiol was mediated by reaction with deoxyhemoglobin, providing a mechanism for hypoxia-regulated catalytic NO production by erythrocytes or endothelial or tissue heme proteins. A nitrite-hemoglobin chemistry would support a role for the red blood cells in oxygen-dependent NO homeostasis, a concept first advanced by Stamler et al. but ascribed to S-nitroso-hemoglobin40,41. It would also provide a mechanism for the observation that red blood cells and plasma 'loaded' with NO, by exposure to high concentrations in solution or to NO gas or donors (invariably in equilibrium with high concentrations of nitrite), can export NO and induce vasodilation in vitro and in vivo11,27,28,29,30,31,32. We realize that the high concentrations of hemoglobin in red blood cells, coupled with the near-diffusion-limited reaction rates (∼107 M−1s−1) of NO with hemoglobin, seem to prohibit NO from being exported from the red blood cell. However, our data (Fig. 5) argue to the contrary. Perhaps the unique characteristics of the erythrocyte membrane, with its submembrane proteins and methemoglobin-rich microenvironment42, and the relatively lipophilic nature of NO, allow compartmentalized NO production at the red blood cell membrane. This, coupled with the small amounts of NO necessary for vasodilation, could account for the export of NO despite these kinetic constraints. Further study will be required to determine whether this reaction occurs primarily in the erythrocyte, as data in Figure 5 suggest, with subsequent export of NO or of S-nitrosothiol, or whether this is a primary reaction of nitrite with endothelial or smooth muscle heme proteins, such as myoglobin, soluble guanylyl cyclase, cytochrome P450 or mitochondrial cytochromes.
Three factors uniquely position nitrite, rather than S-nitrosothiol, as the major vascular storage pool of NO. First, nitrite is present in substantial concentrations in plasma, erythrocytes and tissues7. Second, nitrite is relatively stable because it is not readily reduced by intracellular reductants (as are S-nitrosothiols30), and its reaction rate with heme proteins is 10,000 times less than that of authentic NO. Third, nitrite is only converted to NO by reacting with deoxyhemoglobin (or presumably deoxymyoglobin, deoxycytoglobin, deoxyneuroglobin or other oxygen-binding heme proteins), and its leaving-group is the met(ferric)heme protein that limits scavenging and inactivation of NO33. The nitrite pool therefore provides the ideal substrate for NO generation along the physiological oxygen gradient, potentially providing a new mechanism for hypoxic vasodilation. Therapeutic application of nitrite should result in selective vasodilation to hypoxemic tissue, and could be used to treat diseases associated with ischemic tissue, neonatal pulmonary hypertension and hemolytic conditions such as sickle-cell disease, where free hemoglobin released during hemolysis scavenges NO and disrupts NO-dependent vascular function43. Nitrite would not only inhibit the ability of free hemoglobin (by oxidizing it to methemoglobin) to scavenge NO, but would actually generate NO in tissue beds with low oxygen tension.
Protocol for human subjects.
The protocol was approved by the Institutional Review Board of the National Heart, Lung and Blood Institute, and informed consent was obtained from all volunteer subjects. Nine men and nine women, with an average age of 33 years (range 21–50 years), participated in the study. An additional ten subjects returned 3–6 months later for a second series of experiments with low-dose nitrite infusion. Detailed inclusion and exclusion criteria are described in Supplementary Methods online.
Forearm blood flow measurements.
Forearm blood flow measurements were made by strain-gauge venous-occlusion plethysmography, as previously described44. A series of measurements, termed parts I and II (detailed in Results, Figs. 1 and 2 and Supplementary Methods online), were conducted in randomized order to minimize the effect of time on forearm blood flow response during nitrite infusion. Part I of the protocol was designed as a control for part II, and is described in Figure 1 and Supplementary Methods online.
Nitrite (NaNO2; Mr = 69; 36 μmol/ml in 0.9% saline) was infused at 1 ml/min. Sodium nitrite for use in humans was obtained from Hope Pharmaceuticals (300 mg in 10 ml water), and 286 mg was diluted in 100 ml of 0.9% saline by the Pharmaceutical Development Service to a final concentration of 36 μmol/ml. For the final nine subjects studied, 0.01−0.03 μM sodium bicarbonate was added to the normal saline, so as to titrate the pH to 7.0–7.4. The nitrite solution was light-protected, and nitrite levels and free NO gas in solution were measured by reductive chemiluminescence after all experiments30. NO was present at a concentration of 50.5 ± 40.5 nM in nitrite solutions, and was unaffected by bicarbonate buffering. There was no correlation between NO levels in nitrite solutions and blood flow effects of nitrite (r = −0.23; P = 0.55). The total dose of sodium nitrite infused in our study participants was 1.08 mmol, or 75 mg (36 μmol/min × 15 min × 2 infusions), which is approximately one-third of the dose used in humans for emergency treatment of cyanide poisoning. In additional studies in ten subjects, the same stages of parts I and II of the protocol were followed with infusion of low-dose nitrite (0.36 μmol/ml NaNO2 in 0.9% saline, infused at 1 ml/min).
Measurement of red blood cell S-nitroso-hemoglobin and iron-nitrosylated hemoglobin.
S-nitroso-hemoglobin and iron-nitrosylated hemoglobin were assayed as previously described30,45. The assay was conducted on whole blood to prevent ex vivo chemistry from occurring during sample processing. The detailed protocol is described in Supplementary Methods online.
EPR spectroscopy of whole blood.
EPR spectroscopy was carried out at 137 K with a Bruker 4111 VT controller and ER-200 D ESR spectrometer set at 9.43 GHz, 10 mW, 5 G modulation, 0.1 s time constant and 100 s scans over 600 G. Each curve represents the average of ten 100-s scans. Arterial blood spectra were subtracted from venous blood spectra, indicating an increase in iron-nitrosylated hemoglobin from artery to vein.
Kinetics of reaction of nitrite with deoxygenated erythrocytes. Venous blood was deoxygenated under a vacuum of <0.5 torr and cycled under 100% argon or medical gas (95% N2, 5% CO2), to give a minimum of 75% deoxygenation of total hemoglobin (average deoxygenation was 81 ± 4%; pH 7.4). Deoxygenated PBS was added as needed to bring the total hemoglobin concentration to 10 mM. The maximum hemolysis measured was 2% of heme. EPR spectroscopy of free hemoglobin in the lysate and packed red blood cell fractions after reaction with nitrite confirmed that the measured iron-nitrosylated hemoglobin signals were from the hemoglobin in the red blood cells. After equilibrating to 37 °C in a water bath, baseline EPR samples were extracted to deoxygenated tubes and immediately frozen in liquid nitrogen. Deoxygenated 0.03 M potassium nitrite stock solution was added to a final sample concentration of 200 μM nitrite and mixed by inversion, with subsequent EPR samples taken and frozen at 0, 1, 2, 3, 5, 10, 15 and 30 min. The concentration of iron-nitrosylated hemoglobin was determined by comparing the double integral of the measured spectrum to that of a standard.
Chemiluminescent detection of NO gas released from deoxyhemoglobin and deoxygenated erythrocytes after nitrite addition.
To determine whether free NO radicals can be formed by the reaction of nitrite and deoxyhemoglobin, we mixed 100 and 200 μM nitrite with 5 ml of 660 and 1,000 μM deoxygenated erythrocytes, respectively, in a light-protected reaction vessel purged with helium or oxygen in line with a chemiluminescent NO analyzer (Seivers). After allowing equilibration for 5 min, nitrite was injected and the rate of NO production was measured. Nitrite was injected into PBS as a control, and into 100 μM hemoglobin to control for hemolysis in the 660 and 1,000 μM deoxygenated erythrocyte solutions. At the end of all experiments, the visible absorption spectra of the supernatant and erythrocyte reaction mixtures were analyzed, and hemoglobin composition was deconvoluted using a least-squares algorithm. There was <100 μM hemolysis in the system, no hemoglobin denaturation and significant formation of iron-nitrosylated hemoglobin.
Aortic ring bioassay experiments.
Isometric tension was measured as described previously using rat thoracic aorta treated with indomethacin (5 μM) and precontracted with phenylephrine (100 nM) and L-NG- nitroarginine (100 μM)46. To investigate the effect of oxygen tension on vasodilation responses stimulated by nitrite and/or red blood cells, a vessel bath was custom designed (Radnoti) so that it could be sealed and accommodate an oxygen electrode to allow simultaneous monitoring of pO2 and vessel tone. Vessels were equilibrated in Krebs buffer at 37 °C at 609 mm Hg oxygen (achieved by perfusion of 95% O2 and 5% CO2). Oxygen tension was calibrated as previously described46. After reaching a stable tone, various treatments described in Results were added, and perfusion with 95% N2, 5% CO2 and helium were initiated (inclusion of helium was necessary to reduce oxygen tension to 0 mm Hg). Because the rates of deoxygenation varied in different vessel chambers, measurements were made only under conditions that allowed vessel tension and oxygen concentration to be determined simultaneously, in the same bath. The oxygen tension at which relaxation starrted was defined as the intersection between tangents drawn along the line formed at maximum tension as a function of oxygen concentration (i.e., when little change in tension occurs at high oxygen tension) and after relaxation responses were initiated. For experiments using cell-free hemoglobin, vessel baths were perfused with 95% N2 and 5% CO2, which decreased oxygen tension to 15 mm Hg. Nitrite-dependent vasodilation was then assessed by addition of incremental concentrations of nitrite in the presence and absence of hemoglobin (25 μM) and IHP (100 μm).
An a priori sample size calculation determined that 18 subjects would be necessary to detect a 25% improvement in forearm blood flow during nitrite infusion, when forearm NO synthesis had been inhibited by l-NMMA, compared with normal saline infusion control values (alpha = 0.05, power = 0.80). Two-sided P values, repeated-measures ANOVA and Pearson correlations were used as indicated. Measurements shown represent mean ± s.e.m.
Note: Supplementary information is available on the Nature Medicine website.
This work was supported by Clinical Center and National Heart, Lung and Blood Institute intramural funds (R.O.C. and M.T.G.), National Institutes of Health grant HL58091 (D.B.K.-S.), RO1HL70146 (R.P.P.) and Medical Scientist Training Program T32GM08361. We thank V. Annavajjhala for helpful laboratory assistance.
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Clinical Autonomic Research (2018)