Abstract:SynopsisThe proton magnetic relaxation time, 2'1, has been measured at 29 MHz in 0.1M KH2P04 and 0.1M NaCl (both pH 6 ) aqueous solutions of human ferrihaemoglobin, the protein concentrations ranging from 0.5 to 5 mM per haem. The linear dependence on protein concentration of the enhancement in relaxation rates, A(l/Tl), due to the presence of the paramagnetic iron in haemoglobin was confirmed at 34°C and a t -10°C. In the middle temperature range there is a thermally activated process, whose energy of activat… Show more
“…The major result is that outer sphere relaxation accounts for a substantial part of the observed solvent proton relaxation rate. At low fields and 60C, it is about two-thirds of the total at all values of pH considered; at 350C it is less, consistent with a contribution from thermally activated exchange of a water molecule from the inner sphere (Pifat et al, 1973). Moreover, as mentioned, these are lower limits.…”
Section: Methemoglobinsupporting
confidence: 64%
“…These authors, as remarked above, ascribed all the relaxation to outer sphere effects. Pifat et al (1973), in an extensive investigation of the temperature dependence of proton relaxation in solutions of methemoglobin, also concluded ". .…”
It is now more than 20 years since Davidson and collaborators (1957, Biochim. Biophys, Acta. 26:370-373; J. Mol. Biol. 1:190-191) applied the theoretical ideas of Bloembergen et al. (1948. Phys. Rev. 73:679-712) on outer sphere magnetic relaxation of solvent protons to studies of solutions of methemoglobin. From then on, there has been debate regarding the relative contributions to paramagnetic solvent proton relaxation by inner sphere (ligand-exchange) effects and by outer sphere (diffusional) effects in methemoglobin solutions. Gupta and Mildvan (1975. J. Biol. Chem 250:146-253) extended the early measurements, attributed the relatively small paramagnetic effects to exchange with solvent of the water ligand of the heme-Fe3+ ion, and interpreted their data to indicate cooperativity and an alkaline Bohr effect in the presence of inositol hexaphosphate. They neglected the earlier discussions entirely, and made no reference to outer sphere effects. We have measured the relaxation rate of solvent protons as a function of magnetic field for solutions of methemoglobin, under a variety of conditions of pH and temperature, and have given careful consideration to the relatively large diamagnetic corrections that are necessary by making analogous measurements on oxyhemoglobin, carbonmonoxyhemoglobin, and cyano- and azide-methemoglobin. (The latter two, because of their short electronic relaxation times, behave as though diamagnetic). We show that the paramagnetic contribution to solvent relaxation can be dominated by outer sphere effects, a result implying that many conclusions, including those of Gupta and Mildvan, require reexamination. Finally, we present data for fluoro-methemoglobin, which relaxes solvent protons an order of magnitude better than does methemoglobin. Here one has a startling breakdown of the dogma that has been the basis for interpreting many ligand-replacement studies; in contrast to the prevailing view that replacement of a water ligand of a protein-bound paramagnetic ion by another ligand should decrease relaxation rates, replacement of H2O by F- increases the relaxation rate drastically. The data can all be reconciled, however, with what is anticipated from knowledge of ligand interactions in the heme region.
“…The major result is that outer sphere relaxation accounts for a substantial part of the observed solvent proton relaxation rate. At low fields and 60C, it is about two-thirds of the total at all values of pH considered; at 350C it is less, consistent with a contribution from thermally activated exchange of a water molecule from the inner sphere (Pifat et al, 1973). Moreover, as mentioned, these are lower limits.…”
Section: Methemoglobinsupporting
confidence: 64%
“…These authors, as remarked above, ascribed all the relaxation to outer sphere effects. Pifat et al (1973), in an extensive investigation of the temperature dependence of proton relaxation in solutions of methemoglobin, also concluded ". .…”
It is now more than 20 years since Davidson and collaborators (1957, Biochim. Biophys, Acta. 26:370-373; J. Mol. Biol. 1:190-191) applied the theoretical ideas of Bloembergen et al. (1948. Phys. Rev. 73:679-712) on outer sphere magnetic relaxation of solvent protons to studies of solutions of methemoglobin. From then on, there has been debate regarding the relative contributions to paramagnetic solvent proton relaxation by inner sphere (ligand-exchange) effects and by outer sphere (diffusional) effects in methemoglobin solutions. Gupta and Mildvan (1975. J. Biol. Chem 250:146-253) extended the early measurements, attributed the relatively small paramagnetic effects to exchange with solvent of the water ligand of the heme-Fe3+ ion, and interpreted their data to indicate cooperativity and an alkaline Bohr effect in the presence of inositol hexaphosphate. They neglected the earlier discussions entirely, and made no reference to outer sphere effects. We have measured the relaxation rate of solvent protons as a function of magnetic field for solutions of methemoglobin, under a variety of conditions of pH and temperature, and have given careful consideration to the relatively large diamagnetic corrections that are necessary by making analogous measurements on oxyhemoglobin, carbonmonoxyhemoglobin, and cyano- and azide-methemoglobin. (The latter two, because of their short electronic relaxation times, behave as though diamagnetic). We show that the paramagnetic contribution to solvent relaxation can be dominated by outer sphere effects, a result implying that many conclusions, including those of Gupta and Mildvan, require reexamination. Finally, we present data for fluoro-methemoglobin, which relaxes solvent protons an order of magnitude better than does methemoglobin. Here one has a startling breakdown of the dogma that has been the basis for interpreting many ligand-replacement studies; in contrast to the prevailing view that replacement of a water ligand of a protein-bound paramagnetic ion by another ligand should decrease relaxation rates, replacement of H2O by F- increases the relaxation rate drastically. The data can all be reconciled, however, with what is anticipated from knowledge of ligand interactions in the heme region.
“…Although initial studies about the paramagnetic relaxation in methemoglobin attributed the relaxation enhancement to the “inner sphere” mechanism, i.e., only water ligated with heme relaxes fast, and then exchange with bulk water. However, an extensive investigation of proton relaxation dependence on temperature had shown that the exchange rate between ligated water and bulk water was not fast enough to induce the fast relaxation, and Koenig et al measured the relaxation dispersion curve at multiple magnetic fields and proved the “outer sphere” mechanism, i.e., the fluctuation of the dipolar coupling between water and paramagnetic protein due to water diffusion, dominated the paramagnetic relaxation. Therefore, Freed's diffusion model which described water molecules diffusing around the paramagnetic complex was used to fit the field dependence of the paramagnetic relaxivities of methemoglobin and deoxyhemoglobin in Figure .…”
Purpose
To propose and evaluate a model for the blood water T1 that takes into account the effects of hematocrit fraction, oxygenation fraction, erythrocyte hemoglobin concentration, methemoglobin fraction and plasma albumin concentration.
Methods
Whole blood and lysed blood T1 data were acquired at magnetic fields of 3T, 7T, 9.4T and 11.7T using inversion-recovery measurements and a home-built blood circulation system for maintaining physiological conditions. A quantitative model was derived based on multi-variable fitting of this data.
Results
Fitting of the model to the data allowed determination of the different parameters describing the blood water T1 such as those for the diamagnetic and paramagnetic effects of albumin and hemoglobin, and the contribution of methemoglobin. The model correctly predicts blood T1 at multiple fields, as verified by comparison with existing literature.
Conclusion
The model provides physical and physiological parameters describing the effects of hematocrit fraction, oxygenation, hemoglobin concentration, methemoglobin fraction and albumin concentration on blood water T1. It can be used to predict blood T1 at multiple fields.
“…Bovine haemoglobin was prepared as described previously. 6 The final dialyses were against 0.1 M phosphate buffer, pH 6, with the addition of Horse metmyoglobin from Koch and Light was used without further purification. The lyophilized powder was dissolved in the same buffer and centrifuged a t 14000 g for 20 min.…”
SynopsisThe longitudinal proton magnetic relaxation times TI were measured for ferri (met)-and carbonmonoxy-bovine haemoglobin and equine myoglobin in 0.1 M KH2P04 aqueous solutions near pH 6 a t 5°C and 35°C from 1.5-to 60-MHx Larmor frequencies. I t is concluded that the correlation time T C for the dipole-dipole interaction of electron and nuclear spins is in fact the electron (ferric) spin relaxation time 7 s being close to 1..5 X At 35°C the paramagnetic relaxation rates are not determined solely by the relaxation of protons exchanging from the haem pocket with bulk solvent. Hence, 7~ at 33°C cannot be calculated from the dispersion data obtained a t this temperature. The relevance of this for the determination of interspin distances T is discussed. sec for both metHb and methfb at 5°C.
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