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1.IntroductionThe use of Lambert-Beer’s law to model the optical behavior of hemoglobin solutions and solve for oxygen saturation requires knowledge of the optical density per unit path length per unit concentration at two wavelengths.1, 2 An important assumption required by these models is that the change in optical density with changing oxyhemoglobin saturation is the weighted average of the optical density of pure oxyhemoglobin and deoxyhemoglobin. 1, 2, 3, 4 These models also assume that the optical density is unaffected by physiological changes in carbon dioxide concentration, pH, or other compounds known to change the configuration of the hemoglobin structure such as 2,3 bisphosphoglycerate.5, 6 Recent work showing that the pH of hemoglobin and blood can be measured using near-IR wavelengths to interrogate the specimen independent of oxyhemoglobin saturation7, 8 and published extinction coefficients for oxyhemoglobin and deoxyhemoglobin that vary significantly (by as much as 20%) make the use of these parameters without calibration controls problematic.3 Steinke and Shepherd developed and empirically verified a model equation for red blood scattering and absorption losses from forward transmitted collimated light with the form:9, 10 where is the transmitted light striking a narrow angle detector, is the total cross-sectional loss, is the absorption cross section, is the scattering cross section, and is the path length through a plane of blood. Converting Eq. 1 into optical density space gives:where is the optical density due to the absorption and scattering of light ; is the optical density of a hemoglobin solution having the same oxyhemoglobin saturation, hemoglobin concentration, and path length as the blood sample; and is the apparent optical density due to scattering.9 Note that Eqs. 1, 2 use the same path length for the scattering loss and the absorption loss . In addition, many subsequent investigators attempting to measure the oxyhemoglobin saturation of blood using this equation have modeled scattering loss as a constant with changing wavelength when data is obtained in a narrow range. Combined, these two assumptions facilitate three or more wavelength approaches to the oximetry of blood in vivo. 3, 11, 12, 13, 14, 15 However, when in vivo oximetry has been attempted using these approaches, the combination of scattering with the above assumptions related to the behavior of hemoglobin is associated with significant difficulty making calibrated measurements. 3, 4, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21Our group has recently described a new method for measuring oxygen saturation in hemoglobin solutions that is insensitive to path length, pH, or concentration changes.22 The wavelength band required for this analysis is narrow, leading to the hope that this simple method for measuring blood oxyhemoglobin saturation might also be insensitive to scattering effects facilitating in vivo measurements. In the following, we report the results of our work designed to measure the impact of red blood cell scattering on forward transmission from 450 to . In addition, we evaluate how this scattering loss influences the blue-green spectral shift seen with changing oxyhemoglobin saturation. 2.MethodsWe obtained blood from two healthy volunteers according to an Institutional Review Board approved protocol. The blood was anticoagulated using citrate dextrose solution A with the pH of the anticoagulant adjusted using dilute hydrochloric acid or dilute sodium hydroxide as needed so that the blood pH after anticoagulation was 6.6, 7.1, or 7.4. The donated blood was stored on ice while aliquots of the blood were centrifuged at for , followed by aspiration of the plasma from the packed red blood cell mass. Because blood samples anticoagulated and stored undergo red blood cell lysis over time, we evaluated the plasma from each centrifuged sample for hemoglobin content using the spectrophotometer. If lysis occurred, the sample was rejected, a new sample was obtained from a donor, and the blood preparation procedure repeated. These blood samples were placed in a blood oxygenation system of our own design, described in detail elsewhere,23 and either plasma or packed cells obtained by centrifugation of an aliquot of the same blood sample was used to set the desired blood hemoglobin concentration. Each sample was set to the desired blood oxyhemoglobin saturation using a gas mixture that was warmed and humidified at . The gas mixtures included a fixed concentration of carbon dioxide (partial pressure of ) and various mixtures of oxygen and nitrogen.23 The blood samples were then pumped at a rate of through either a Starna or Starna flow cell in a Cary 100 Spectrophotometer. The Cary Spectrophotometer was standardized using a saline solution in the respective 100- or cuvette to set 100% transmission and then blocking the beam to set 0% transmission. The spectra of the blood samples were measured at 2-nm increments with a 2-nm bandwidth. The spectrum was measured for each sample with a pH of 6.6, 7.1, or 7.4, a path length of 100 or , and hemoglobin concentrations from 6.6 to (hematocrit from 19 to 48%). We measured the spectra of cell free hemoglobin solutions with the same hemoglobin concentration ([Hb]), path length, pH and oxyhemoglobin saturation as the blood . Hemoglobin samples were prepared from fresh packed human red blood cells in the following manner. Anticoagulated blood was centrifuged at for , and the buffy coat removed along with the plasma by aspiration. Either distilled water was added or 0.02% saponin was added to the packed red blood cells followed by centrifugation and filtration to remove the red blood cell membranes leaving concentrated hemoglobin solutions.2 The hemoglobin solutions were each set to the desired concentration using saline and the oxyhemoglobin saturation was set using the same oxygenation system that we used for the blood samples described above and elsewhere.23 Each time a sample of blood was pumped through the cuvette in the spectrophotometer or a hemoglobin sample was placed in a cuvette, an aliquot was evaluated using a Nova Biomedical pHOX Co-Oximeter that measured the oxyhemoglobin saturation (package material reports an accuracy to less than saturation), the concentration of carboxyhemoglobin, and the concentration of methemoglobin. The blood and hemoglobin solutions were prepared from the same source and the concentrations of hemoglobin species in the samples were comparable. Neither donor was a smoker and the sum of the carboxyhemoglobin and methemoglobin was less than 4% of the total hemoglobin present in each sample. 3.ResultsThe spectra of a blood sample with an oxyhemoglobin saturation of 98%, , path length of , and a pH of 6.6, the spectra of a hemoglobin solution with the same parameters and the difference spectrum are shown in Fig. 1 . The similarity between the spectrum of the blood and hemoglobin is obvious. The difference spectrum is nearly linear with wavelength having the form in the blue green region from . We note, however, that there remains a small negative hemoglobin signature in the difference spectra shown in Fig. 1. This negative hemoglobin signature was present in all or our difference spectra independent of saturation, blood hemoglobin concentration, path length, or pH. Recent work on scattering and the relative absorption of red blood cell (RBC) packaged hemoglobin versus cell free hemoglobin solutions indicates that the effective path length through blood is less than the equivalent path length through hemoglobin.16 Other work done modeling the components of the scattering and absorption cross sections reported a similar spectrum for the scattering component in this region.24, 25 Taken together, these results suggest that the assumption by Stienke and others that the value of in Eq. 1 is the same for the scattering cross section as it is for the absorption cross section may be inaccurate.16 Another possible explanation for this negative hemoglobin signature is that the changing refractive index with wavelength due to the contribution of the imaginary component causes a small but measurable change in the scattering properties of the red blood cells. Nevertheless, for our purposes, we wish to separate the contribution of hemoglobin absorption from scattering as much as possible. Based on the red blood cell packaging study16 and our findings, we analyzed the data shown in Fig. 1 in the following manner. We used the empirical spectrum of hemoglobin in Fig. 1 along with Lambert-Beer’s law to calculate the expected spectra with decreasing path length for this sample. We then calculated the difference spectra for these various hemoglobin path lengths and the blood spectrum from Fig. 1. Our goal was to minimize the residual hemoglobin signal in these difference spectra. We found that the hemoglobin signature was minimized for this sample pair by using a hemoglobin path length of 92 rather than . Figure 2 shows the resulting highly linear difference spectrum along with the parabolic blood and hemoglobin spectra in the region used for the blue-green minimum shift oximetry technique.22 Based on this result, we redefined Eq. 2 as follows: where is the ratio of the effective path length through hemoglobin to the cuvette path length for the blood sample. Substituting the linear relationship between this simplified scattering loss and wavelength into Eq. 3, we writeUsing eight paired hemoglobin and blood samples, we measured the optical densities at three wavelengths (476, 488, and ) with oxyhemoglobin saturations of 0.967, 0.88, 0.806, 0.722, 0.654, 0.591, 0.259, and 0.067. We then used Eq. 4 and the spectra of each sample pair to solve uniquely for , , and . The data were quite consistent with values for , , and (all errors shown are the standard deviation from the mean).Figure 3 shows the spectra of samples of blood with the same path length, pH level, and different oxyhemoglobin saturations in the region from 476 to . Note that the minimum of each spectrum marked with an arrow correlates with the oxygen saturation. Figure 4 shows the blood oxyhemoglobin saturation and the spectral minima of all 32 blood samples that we studied with a pH of 6.6, 7.1, or 7.4, a path length of 100 or , and blood hemoglobin concentrations from 6.6 to . These minima were measured using the parabolic fit technique described earlier22 without any compensation for path length or blood hemoglobin concentration. These spectral minima correlated strongly with the oxygen saturation measured using the cooximeter and the standard deviation of the residuals using the cooximeter measurements as the true values was 3.9% saturation. When compared to the previously reported oxyhemoglobin blue green shift using the same analysis techniques,22 the slope of the minimum versus oxyhemoglobin saturation plot is the same but the wavelength intercepts are changed. We analyzed our data empirically using the fit equation for the blue-green minimum shift method on hemoglobin solutions and the best fit to the scattering from the preceding. Substituting these two empirical equations, one reported previously and the other from the data already presented into Eq. 2 gives the following model description of the optical density of blood in the 476 to 516-nm region: This equation is another parabola with a new minimum given by setting the differential equal to zero and solving for or . Thus, the expected change in the minimum when compared to hemoglobin is a shift of the quantity . Since the slope of the scattering line in Fig. 2 as well as in the data sets above were negative , the shift in this transmission model with scattering is to the right (positive). In the group of blood samples analyzed here (hematocrits from 19-48%) shown in Fig. 3, the total shift to the right when compared to the hemoglobin signature published earlier22 was .4.ConclusionsThe scattering of whole blood from 460 to in this transmission system is linear and decreases with increasing wavelength. The blue-green minimum spectral shift with changing oxygen saturation seen in hemoglobin solutions is preserved in scattering whole blood at physiologic concentrations when spectra are measured in transmission, but the minima are shifted to the right by scattering. 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