J.
Mareš
*ab,
J.
Karjalainen‡
b,
P.
Håkansson‡
a,
S.
Michaeli§
d and
T.
Liimatainen§
bc
aNMR Research Unit, Faculty of Science, University of Oulu, P.O. Box 3000, FIN-90014, Finland. E-mail: jiri.mares@iki.fi
bResearch Unit of Health Sciences and Technology, Faculty of Medicine, University of Oulu, Finland
cDepartment of Radiology, Oulu University Hospital, Oulu, Finland
dCenter for MR Research, Radiology Department, University of Minnesota, Minneapolis MN55455, USA
First published on 1st August 2023
The chemical exchange of labile protons of the hydroxyl groups can be exploited in a variety of magnetic resonance experiments to gain information about the groups and their physicochemical environment. The exchangeable –OH protons provide important contributions to the T2 of water signals thus contributing to the T2-weighted contrast of MRI images. This exchange can be exploited more specifically and sensitively in chemical exchange saturation transfer (CEST) or longitudinal rotating frame relaxation (T1,ρ) experiments. Since glucose is omnipresent in living organisms, it may be seen as a rather universal probe. Even though the potential was first recognized many years ago, practical use has remained scarce due to numerous challenges. The major limitation is the rather low glucose concentration in most tissues. The other obstacles are related to multiple dependencies of the exchange parameters, such as temperature, pH, and concentration of various ions that are not known in sufficient detail for glucose. Thus, we embarked on evaluating the exchange parameters of a model that included every relevant chemical site for all –OH protons in both dominant enantiomers of glucose. We have (1) obtained conventional one-dimensional proton NMR spectra of glucose solutions in suitable temperature ranges, (2) we have iterated through several exchange models with various degrees of freedom determined by the number of distinguishable –OH proton sites and compared their performance, (3) we extrapolated the parameters of the best model of physiological temperature and (4) we demonstrated the use of the parameters in virtual experiments. As the main results, (1) we have obtained the temperature dependence of exchange parameters with reliable confidence intervals in three different pH values, with two of them reaching physiological temperature, and (2) we show how the parameters can be used in virtual experiments, helping to develop new applications for glucose as an NMR/MRI probe.
The role of glucose in assessing clinical conditions in MRI has been mostly limited to academic discussions. Its potential in creating MRI contrast through its exchange properties is used in CEST-based MRI.6,7 The so-called Gluco-CEST has been proposed for the study of glucose concentration or as a pH-sensitive biomarker.6,7 Measurements of glucose in tumours have also been the aim of many other studies.7–11
The sensitivity of the –OH exchange rate with respect to pH can be used in principle for the measurement of pH.12 There are also challenges in using the –OH groups of glucose. One challenge is associated with the low concentration of glucose in blood, and the concentration of glucose in other tissues is usually even lower. This can be elevated by various means, but to a rather limited extent. One option has been to introduce a glucose derivative with a reduced metabolic rate,13,14 accumulating larger concentrations in tissues, with a risk of toxicity. Similarly, derivatives of disaccharides, sucralose and maltitol, used as artificial sweeteners, have been used in brain tumour imaging in rat models.15,16
Another problem is related to the small chemical shift of glucose –OH groups with respect to water. This challenge is more apparent at low magnetic fields of clinical MRI instruments, where the glucose –OH resonances cannot be easily targeted in CEST experiments without obscuring the results by irradiating the water resonance as well. The challenges of glucose-CEST in 3T have been extensively investigated in recent studies.17,18 Both drawbacks of the glucose properties are being alleviated at higher magnetic fields. To be able to evaluate the potential of glucose as a biomarker for MRI in clinical studies, it is crucial to know its properties accurately. Only then can valid conclusions be drawn from simulations of CEST spectra under realistic conditions, including a slightly inhomogeneous magnetic field, temperature, pH, or diffusion. It is important to know the details of the chemical shift values of the –OH protons with respect to water protons, and their exchange rate as a function of temperature, pH, and possibly other factors, such as concentrations of ions acting as proton exchange catalysts.19 The proton chemical exchange rates have been previously determined with various validity ranges.17,18,20,21 In the case of glucose, there has been a great uncertainty about the exchange rates and chemical shifts of individual hydroxyl protons, as well as their dependence on pH. This is mostly due to the fact that the exchange is in the intermediate-to-fast regime, and therefore it is detectable only indirectly under physiological conditions, as the –OH peaks coalesce into a (broadened) water peak. To properly evaluate these measurements or assess the feasibility of new techniques, it would be invaluable to have a detailed model of exchange, accurately parameterized, with known dependencies on all the properties of the solution. The confidence intervals of the measured parameters are also of critical importance. Such a comprehensive set of parameters is not available in the literature. Here, we build a model including every possible chemical site for all relevant –OH protons in both dominant enantiomers of the glucose in solution.
In this study, we started by measuring glucose solutions in standard phosphate buffered saline (1× PBS22) at three pH points and at temperature ranges suitable for resolving at least a subset of –OH proton sites for a given pH. We then tested several exchange models, including various numbers of distinct exchange sites and their interdependency. The parameters of the models together with error margins were estimated using Markov chain Monte Carlo simulation, which also allowed us to choose the most suitable exchange model. Taking the temperature dependence of the best-model parameters, we could extrapolate the exchange parameters to physiological temperature for a subrange of physiological pH values.
In this study, we investigate the dependence of the exchange parameters of the –OH protons of glucose on temperature and pH. In addition to pH, the chemical composition is kept constant, close to the physiological state, by using the standard 1× PBS buffer. We prepared samples of 1 M glucose in 1× PBS and adjusted the pH to three different values. To measure the exchange parameters, i.e., exchange rates and chemical shifts, of each –OH site, we measured the temperature series of standard proton NMR spectra. The temperature ranges were selected after the initial screening, such that the highest temperature still contains resolution, allowing us to visually distinguish at least subsets of –OH signals. It was assumed that the –OH region of the spectrum is determined by the chemical exchange. To obtain the exchange parameters, a suitable model was gradually selected. The model consisting of distinct chemical shift sites and exchange rates is used to simulate the spectrum, which in turn enables finding the exchange parameters during the fitting procedure. We have therefore decided to employ Markov chain Monte Carlo (MCMC)23 simulation to facilitate the fitting.
![]() | (1) |
|ρ(τ)〉 = P(τ)|ρ(0)〉, | (2) |
The simulation was defined by the list of chemical shifts, exchange rates, and fractional concentrations. An example defining the simulation of the spectrum of 1 M glucose at 269.5 K is given in Table S11 of the ESI,† assembled from Tables S1, S7 and S8 of the ESI.† Only water and the exchanging –OH protons of glucose were included in the simulations of the spectra. Only the chemical-shift term of the NMR spin Hamiltonian was considered. This means that the simulation consists of isolated spins in pools with exchange, equivalent to the Bloch–McConnell equations.26
The spectral line widths were assumed to be determined purely by the exchange broadening, and no additional relaxation mechanisms were considered. This can be justified by the observation that the line width of non-exchangeable protons of glucose is between ca. 15 Hz at the lowest temperature of 270 K and 7.5 Hz at 290 K. The –OH, similar to other glucose protons, do not have close-by protons acting as partners for dipolar relaxation, therefore it can be assumed that their intrinsic relaxation rate due to a combination of mechanisms such as dipole–dipole and CSA interactions would be similar, with upper ranges of 15 and 7.5 Hz for 270 and 295 K. These relaxation rates contribute to the line width, so ignoring them causes a slight overestimation of the exchange rate determined using our approach. This overestimation is gradually less important with increasing temperature, with an upper bound around 1% error at 295 K. The same simplification was used before, e.g. in ref. 27.
For the simulated spectra, the same parameters were used as for the experimental spectra, time-domain points, line-broadening exponential window function, and spectral width for processing. For fitting, the simulation is performed in every iteration to obtain the error as the sum of squares using the difference between the corresponding ∼3800 spectral points. To be able to directly compare the simulated and experimental spectra, the simulated spectrum was further modified by a second-order polynomial employed to simulate the baseline correction with parameters included in the fitting model. Then the section, exactly corresponding to the experimental one, is extracted and normalized. The integral of the section was left as an additional fitting parameter (with a narrow range of 0.8–1.2 multiple of the normalization constant) in the model, resulting in a total of 4 fitting parameters for the baseline.
With nine independent chemical shifts of glucose –OH groups and one for water, the Liouvillian matrix has dimensions of 40 × 40. Every spectrum, including setup, takes around 3–4 seconds to simulate.
Briefly, in MCMC, similarly to other procedures for fitting parameters of a given model, there is a vector of experimental data Yexp, together with an error estimate such as YSEM, which defines our prior probability distribution. The parameters of a model are defined as residing within given boundaries. Initially, each parameter is placed in a random position within its boundary. The n parameters are then randomly varied to sample the n-dimensional space. To do that, a (pseudo)random number is generated on the unit interval and multiplied by a step size ki, corresponding to the ith parameter. The product is added to the ith parameter and the model is reevaluated, obtaining a vector of model data Ymodel. The change is accepted if the error E with respect to Yexp is smaller than with the unchanged parameters (ΔE < 0), as would be done in a standard minimization procedure. If ΔE > 0, the change is accepted if e−ΔE < urnd, where urnd is again a (pseudo)random number from the unit interval. In this way, the simulation samples the n-dimensional space. The sampling is the most efficient if the change is accepted with 50% probability. Therefore, during the initial stage of the MCMC, the step ki is adjusted to obtain roughly a 50% acceptance rate. This is repeated later before a production phase, preferably when the parameters sample the higher probability region. If the parameter leaves its boundaries, it is returned within them by taking its mirror with respect to the crossed boundary. The error E is related to a common sum of squares RSS, but scaled by YSEM and the inverse temperature of the MCMC simulation Tinv. . In the favourable case, the global minimum is found during the simulation, together with the posterior distribution in a Bayesian sense, which is further processed to obtain the confidence interval of a desired 1 − α, here 95%. The distribution of a given parameter is, in general, not symmetric around the optimal value of the parameter, and therefore also the confidence interval is not symmetric. In this study, we have symmetrized the confidence intervals to comply with common practice in reporting the uncertainty. This is largely justified by the fact that the distributions are not far from symmetric (see Fig. S8 in the ESI†).
In order to obtain sufficient statistics for reliable error ranges, the length of the production part of the simulation was twenty thousand steps. The number of spectra simulations was this number multiplied by the number of parameters of a given model. One measure to estimate if the simulation is long enough can be obtained by the step-correlation, which should be small on a scale of trajectory steps. Examples of such correlation functions are shown in Fig. S9 in the ESI.† Based on those, the simulation is long enough.
For the initial fitting of the low-temperature, lower pH spectrum, the ranges of fitted parameters are shown in Table S12 of the ESI.† Unless the assignment of the peak is obvious, such as for C1 or C6, the chemical shift ranges do not determine the assignment a priori. The ranges of exchange rates are always kept such that they safely accommodate the true value. This has been checked for all results. For the spectra measured at higher temperatures and higher pH, the chemical shift fitting ranges were narrowed to non-overlapping ranges to fix the assignment obtained for low-temperature spectra fittings. The fitting ranges of the exchange rates were very broad, not restricting the sampled values (see Table S13 of the ESI†).
In order to extend the exchange rates to higher temperatures, up to a physiological temperature of 310 K, we have performed one more fitting series, to obtain the temperature dependence of the exchange rates, governed by the Eyring equation. We have tabulated the exchange rates from 260 K to 310 K for two different pH values of 6.21 and 7.00. Partial parameterization has also been obtained for the third pH value of 7.38. Using the exchange parameters, we show examples of virtual NMR and MRI experiments and discuss further possible use.
For evaluation of the temperature dependence, we selected the restricted model described in Section 3.2, containing six separate exchange rates and nine chemical shifts. Extrapolation of exchange rates to higher temperatures for individual –OH sites can be obtained by fitting to the Eyring equation.34–36
![]() | (3) |
The fitting was done using the linearized form of eqn (3), which allowed us an error propagation into κ and ΔG‡ and subsequently into extrapolated temperature ranges. The analysis was performed using a Python library called uncertainties.37 The linear fit of the equation y ≐ ax + b is done by combining a and b into vector ab, and forming a “design matrix” xab. This results in a simple matrix equation y ≐ xab. For actual calculation, the x matrix contains a column of x values and a second column of ones. Then ab ≐ x−1,p·y, where −1,p indicates pseudoinversion of a non-square matrix. The only mathematical operations, pseudoinversion and matrix multiplication, are directly available from the uncertainties.unumpy package. Therefore, the vector y can be used with its confidence intervals during calculation of a and b. Exponential and logarithmic functions, needed for linearization of the Eyring equation, are also directly available in “uncertainties”. The confidence intervals in Tables S1–S6 in the ESI,† are therefore obtained by propagation of the reliable confidence intervals of the exchange rates obtained by the MCMC simulations. They do not contain additional uncertainty due to the imperfection of these points along the linearized Eyring equation dependency. The same holds for the κ and ΔG‡ confidence intervals in Table 2.
The simplest model with separate chemical shifts of α and β allowed only at –OH of C1 fails to recover one important and some minor features of the spectra, as can be seen in Fig. 5. Contrary to our original assumption, it turned out that the splitting of the –OH sites due to α- and β-anomers is not limited only to the anomeric –OH, but also influences the chemical shift of other –OH protons so significantly that this can be clearly resolved. Looking at the molecular structure of these anomers (Fig. 1), this is hardly surprising. In the case of the α-glucose, the anomeric –OH oxygen can be in the van der Waals distance from the –OH protons of carbon-2.
Inspection of the spectrum in Fig. 5 shows that there are other minor features within the –OH groups on the glucose ring that may also be caused by chemical shift differences of the other –OH protons at carbons 3 or 4, or both. Therefore, instead of allowing only one more –OH proton to assume different chemical shifts for α- and β-anomers, we considered also cases in which distinct chemical shifts and exchange rates of the three or four –OH protons were allowed (see the schematics in Fig. 2). The only –OH site that was not considered was that at carbon-6, for which there is no evidence of splitting from our measurements. However, this may be reconsidered in future studies where higher resolutions could be achieved. The comparison is shown in Fig. 6.
In all of these models, the exchange rates of well separated signals, the C1,α, C1,β and the C6 give the same results within ∼10 Hz, whereas the exchange rates for the overlapping signals are not conclusive. This also results in poor fits of the temperature dependence to the temperature series (data not shown). This series of models, created mechanistically by adding more sites with both distinct chemical shifts and exchange rates, is therefore failing in the important goal of being sufficiently robust due to unrealistic degrees of freedom. For example, “split 2” has five glucose OH sites, of which two are split due to α and β enantiomers, as illustrated in Fig. 2. Besides OH at C1,α, C1,β, one more site is split like (1.0;δi;kex,i) → ([0.36,0.64];[δi,α,δi,β];[kex,i,α,kex,i,β]), where the first field 1.0 → [0.36,0.64] represents the fractional concentration of the sites. Similarly to the distinct chemical shift δ, the exchange rate kex at positions 2, 3 and 4 may differ for different enantiomers due to the long-range effect of the conformation at C1. But, as discussed in Section 4.5, the spectra do not contain enough information to resolve these, and as we see in the following section, it is better to assume that the kex,i for all but the C1 sites are the same for both enantiomers.
The best fits for every distinct exchange rate can be visually inspected in Fig. 7 and 8. Fig. S6 and S7 in the ESI,† show details around the measured temperatures. One can notice the steep temperature dependence of the hemiacetalic –OH at C1 for both α and β anomers. These are possibly the most important signals, as their large chemical shift with respect to water makes them the easiest target for CEST or off-resonance T1,ρ experiments. Due to the largest chemical shift difference, they also have the largest impact on the T2 of the water signal. For convenience, we report tabulated values together with 95% confidence intervals in the ESI,† in the range between 260 K to 310 K with 0.25 K step. These are expected to be sufficient for most applications. As an example, we show separately parameters at the human physiological temperature of 310 K in Table 1.
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Fig. 7 Fits of the temperature series for the sample of pH = 6.21. The exchange rates obtained by MCMC fit for each site are shown at calibrated temperatures. See further details in the ESI,† Fig. S5. |
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Fig. 8 Fits of the temperature series for the sample of pH = 7.00. The exchange rates obtained by MCMC fit for each site are shown at calibrated temperatures. See further details in the ESI,† Fig. S6. |
k ex/Hz (pH = 7.00) | δ ppm (pH = 7.00)a | k ex/Hz (pH = 6.21) | δ/ppm (pH = 6.21)b | Atom |
---|---|---|---|---|
Comprehensive listings of exchange rates over a broad temperature range are tabulated in the ESI.a The chemical shifts correspond to measurement at 277 K.b The chemical shifts correspond to measurement at 295 K. | ||||
1699 ± 8 | 0.77576 ± 0.00018 | 1569 ± 10 | 0.763 ± 0.003 | C6 |
1613 ± 24 | 1.2361 ± 0.0016 | 957 ± 24 | 1.230 ± 0.013 | C3/4α |
1613 ± 24 | 1.3004 ± 0.0011 | 957 ± 24 | 1.347 ± 0.004 | C3/4β |
2620 ± 40 | 1.2200 ± 0.0005 | 1154 ± 20 | 1.208 ± 0.008 | C3/4α |
2620 ± 40 | 1.4371 ± 0.0009 | 1154 ± 20 | 1.415 ± 0.002 | C3/4β |
1832 ± 22 | 1.0599 ± 0.0004 | 1042 ± 8 | 1.055 ± 0.003 | C2,α |
1832 ± 22 | 1.2255 ± 0.0034 | 1042 ± 8 | 1.252 ± 0.008 | C2,β |
6830 ± 90 | 2.0726 ± 0.0007 | 1736 ± 8 | 2.116 ± 0.001 | C1,α |
9950 ± 100 | 2.8231 ± 0.0011 | 2635 ± 13 | 2.835 ± 0.001 | C1,β |
Recording the spectra in the condensed range does not imply any principal problem as far as the dependence is concerned, eqn (3), used for extrapolation captures the physics correctly (see also Section 4.3). In practice, extrapolation to the temperature region distant from the measured points brings a large demand on the accuracy of these points. The accuracy of these measured points is expressed in a 95% confidence interval obtained from the fitting. Besides that, there is an unknown inaccuracy of the temperature setting in the measurement, even after careful temperature calibration. For the sample of pH = 7.00, we have not seen alarming signs in the data.
The parameters of the Eyring equation are presented with errors from the linearized fit in Table 2 and in Table S14 of the ESI,† with more decimal places. Confidence intervals are briefly discussed in Section 4.4.
pH | 6.21 | ΔG‡ [J mol−1] |
---|---|---|
Site/parameter | κ | |
C6 | (1.37 ± 0.08) × 10−6 | (2.227 ± 0.013) × 104 |
C3/4 | (1.54 ± 0.34) × 10−6 | (2.38 ± 0.05) × 104 |
C3/4 | (2.5 ± 0.4) × 10−5 | (3.054 ± 0.035) × 104 |
C2 | (8.2 ± 0.6) × 10−6 | (2.793 ± 0.017) × 104 |
C1,α | 0.0162 ± 0.0007 | (4.617 ± 0.010) × 104 |
C1,β | 0.00126 ± 0.00006 | (3.852 ± 0.011) × 104 |
pH | 7.00 | ΔG‡ |
---|---|---|
Site/parameter | κ | |
C6 | (1.43 ± 0.05) × 10−5 | (2.810 ± 0.008) × 104 |
C3/4 | (6.0 ± 0.7) × 10−5 | (3.192 ± 0.025) × 104 |
C3/4 | 0.00228 ± 0.00027 | (4.006 ± 0.027) × 104 |
C2 | 0.000231 ± 0.000021 | (3.508 ± 0.021) × 104 |
C1,α | 0.247 ± 0.024 | (4.966 ± 0.022) × 104 |
C1,β | 0.071 ± 0.005 | (4.549 ± 0.017) × 104 |
pH | 7.38 | ΔG‡ |
---|---|---|
Site/parameter | κ | |
C6 | 0.042 ± 0.005 | (4.551 ± 0.028) × 104 |
C3/4 | (1.1 ± 0.6) × 103 | (6.83 ± 0.13) × 104 |
C3/4 | 0.00080 ± 0.00023 | (3.68 ± 0.07) × 104 |
C2 | (2.1 ± 0.8) × 103 | (7.00 ± 0.09) × 104 |
C1,α | (5.7 ± 2.1) × 102 | (6.54 ± 0.08) × 104 |
C1,β | 2.9 ± 0.9 | (5.23 ± 0.07) × 104 |
The temperature dependence of the chemical shift with respect to the water line was not closely investigated. The chemical shifts are therefore reported (see the ESI,† Tables S7–S10) only at the measured temperature points. This should not be too limiting, since the temperature dependence is quite modest, considering its consequences on NMR/MRI experiments.
It is worth noting that different –OH groups have different pH dependences. For example, at 270 K (see Tables S1, S3 and S5 in the ESI†), the primary –OH group at C6 has a slower exchange rate at pH = 7.00 than at pH = 6.21 and at pH = 7.38 the exchange rate is again slightly higher. The secondary –OH groups at C2 to C4 exchange slower at lower pH. The hemiacetal –OH group at C1 is at the other edge of dependence, with the exchange rate increasing steeply upon pH increase. The difference in pH dependencies gives in principle the possibility to clarify more than one variable (such as glucose concentration and pH) at a time.
Knowing the chemical exchange parameters of glucose under the given chemical conditions, we can e.g. straightforwardly evaluate its contribution to the water T2 or T1,ρ. This further depends only on glucose concentration, and (a known) external magnetic field. This gives the possibility to measure the glucose concentration, which may be important in some cases. In other cases, it may be easy to measure the glucose concentration by different means, whereas the subject of interest may become pH or phosphate concentration. Even simultaneous measurement of two unknowns may be possible in principle. For assessing this possibility, reliably parameterized dependencies presented in this study may be crucial.
Glu–OH → Glu–O− + H+ |
H–OH → H–O− + H+ |
A more rigorous option would be to build a global model including the temperature dependence through the parameters of the Eyring equation. In this approach, the posterior distribution of the parameters would be directly obtained. Such a model would therefore contain two parameters determining the exchange rate in any temperature, only doubling the number of fitted variables as compared to fitting of a single temperature at a time, so 12 instead of 6 variables. At the same time, there is no similarly simple model for chemical shift values. If keeping the chemical shift values as fitted variables, this would multiply the number of variables by the number of temperatures, so 54 instead of 9. On the other hand, the chemical shift changes are very small especially for those other than the anomeric site at C1, therefore a linear correction can be considered, with two parameters for each chemical shift. The baseline correction can also be kept independent, resulting in 24 instead of 4 parameters, or, it may be justified to change the parameters into constants. Depending on the choice, the resulting model would contain 30, 66 or 90 parameters, requiring many more steps in order to sample the posterior distributions sufficiently. We did not attempt to follow this option in the current study, though it may be a straightforward extension of this study in the future.
In this section, we exceptionally measure samples with lower concentrations of glucose, to estimate the possible bias in the exchange rate values due to the high concentration used throughout this study. We measured 1 M, 0.2 M and 0.04 M glucose in PBS buffer in pH = 6.21, at 280 K and 290 K.¶ We used again only the conventional 1H spectra at 11.7 T spectrometer, this time with 2048 and 8192 scans for 0.2 M and 0.04 M samples, respectively. Using the same MCMC procedure to obtain the exchange rates, we were able to process well only the 0.2 M spectra, furthermore restricted only to the C1 resonances. The glucose OH region together with the fitted spectra are plotted in Fig. S10 in the ESI.† The 0.04 M spectra would require a different model for the baseline correction due to the ca. 2750 times stronger water signal nearby. Consequently, at 290 K, the fit quality for 0.04 M is poor compared to the other spectra. At 280 K the situation is more favourable, so we still include the results. The concentration dependence of the exchange rates is shown in Table 3.
Temperature, concentration | C1,α | C1,β |
---|---|---|
280 K, 1.0 M | 230.2 | 474.9 |
280 K, 0.2 M | 200.7 | 430.6 |
280 K, 0.04 M | 195.1 | 416.7 |
290 K, 1.0 M | 504.6 | 921.2 |
290 K, 0.2 M | 356.4 | 650.4 |
The results show that the concentration dependence is itself also temperature dependent. For 280 K, the ratio kex,1M/kex,0.2M is 230.2/200.7 = 1.14 and 474.9/430.6 = 1.10 for the α and β enantiomers of protons at C1, respectively. At 290 K, the ratios are already 1.42 for both α and β enantiomers. This has important consequences for our results, which are, in principle, correct only for the high concentration of glucose. Furthermore, we could not extract information on the concentration dependence of other exchangeable sites. On the other hand, both diluted and concentrated glucose in a pure phosphate buffer are far from the real composition of different physiological fluids. In any case, our results cover a limited subspace of conditions influencing the exchange rates. Interestingly, we see a surprising agreement between our results and the published results in Section 4.7.
In order to approach the physiological concentration of glucose, we would need to follow also the concentration dependence of the exchange rate as well as its temperature dependence. Only then could we extrapolate to physiological temperature and concentration. In order to extend the study into this dimension, a combination of our approach of conventional 1H spectra with CEST spectra and CPMG/T1,ρ relaxation measurements would probably be required to cover the different regimes reliably.
The concentration dependence has also been observed in ref. 27 during a study of proton exchange at hydrated formaldehyde and its pH dependence in 0.01 M phosphate buffer. The authors reported 34 ± 18% faster exchange rate for 0.6 M as compared to 0.3 M solution. In Table 4 we also compare the exchange rates of formaldehyde in different pH and 1.1 °C with exchange rates at anomeric proton, which has similar chemical properties. We see closer similarity in the rates for pH 7.0 and 7.38, while for pH = 6.21, the differences are much larger.
pH | 6.21 | 7.0 | 7.38 |
---|---|---|---|
C1,α | 148.7 | 490.1 | 1130 |
C1,β | 332.2 | 882.5 | 1772 |
Formaldehyde (ref. 27) | 608 | 826 | 1242 |
The self-catalysis has been proposed for explanation of the concentration dependence of the exchange rate in the case of formaldehyde. The same would be consistent with our observations. In this respect, the first possibility is that the catalyst is the glucose molecule in Fig. 2, with all the OH groups in a neutral form. In order to become a catalyst, these OH groups would have to act as a stronger catalyst than the water OH groups.
The other option would be that the glucose becomes a catalyst only when it is itself in a process of proton exchange, and therefore ionized. In the short lifetime of the ionized form, in higher concentrations, there would be a higher chance to meet other molecules and catalyse their proton exchange.
The observation that the concentration dependence is itself strongly temperature dependent can be used to decide about the mechanism after detailed evaluation of competing dependencies, such as the molecular diffusion competing with the lifetime of the ionized form.
In both of these cases, the self catalysis reminds us also about the possible intramolecular proton exchange included in our models “with cross”, discussed in Section 4.5, since the nearby OH group at the same molecule can act as a catalyst for the other as if there was a local increase in concentration. In polysaccharides, the intramolecular proton exchange could scale up further. The current data do not contain enough evidence to make such predictions, as we were able to evaluate the concentration dependence of the exchange rate only for the chemically exceptional C1 protons, not present in common polysaccharides.
Notes | Assignment | ||||||
---|---|---|---|---|---|---|---|
C6 | C3/4 | C3/4 | C2 | C1,α | C1,β | ||
a Values of the chemical shifts δ and fractional concentrations are for α and β enantiomer, respectively, where applicable. The fractional concentration, cfrac should be understood so that one distinct proton site has a value of 1.0. This is consistent with the cited literature. b The values at pH = 7.38 should not be considered reliable for 310 K. c Model 1 has many features of our model, so keeping in mind the 0.2 difference in pH, it can be compared with our model at pH = 7.00, the largest difference is for sites C2,3,4, where we note ca. 3–5 times faster exchange rate compared to our model. d Model 2 does not assign the resonances correctly, and also overlooks the α,β enantiomeric ratio. This is especially important for the resonances at 2.0 and 2.9 ppm, as these are well resolved, most significant in terms of the possibility to irradiate them separately for example in the CEST experiment. They are also the most effective in causing R2 type of relaxation. It is therefore important to use the correct fractional concentrations that are ca. 0.36 and 0.64, and not 1.0 and 1.0. The exchange rates are not directly comparable, for which one reason is the five-times less concentrated phosphate buffer solution. e Model 3, similarly to Model 2, disregards the α,β enantiomeric ratio, which is important for the resonance at C1, here at 2.2 and 2.8 ppm. Besides the pH difference, the buffer composition is the same as in our study, therefore the exchange rates are also comparable. | |||||||
This worka | δ ppm | 0.763 ± 0.003 | 1.230 ± 0.013, 1.347 ± 0.004 | 1.208 ± 0.008, 1.415 ± 0.002 | 1.055 ± 0.003, 1.252 ± 0.008 | 2.116 ± 0.001 | 2.835 ± 0.001 |
c frac | 1.0 | 0.36, 0.64 | 0.36, 0.64 | 0.36, 0.64 | 0.36 | 0.64 | |
pH = 6.21 | 1569 ± 10 | 957 ± 24 | 1154 ± 20 | 1042 ± 8 | 1736 ± 8 | 2635 ± 13 | |
pH = 7.00 | 1699 ± 8 | 1613 ± 24 | 2620 ± 40 | 1832 ± 22 | 6830 ± 90 | 9950 ± 100 | |
pH = 7.38 | 5760 ± 100 | 21![]() |
3270 ± 120 | 22![]() |
34![]() |
28![]() |
We see perhaps surprising agreement for exchange rates at the anomeric sites, when comparing our results at pH = 7.00 and the results of Model 1 and Model 3 at pH = 7.2. There seems to be a nearly identical effect of high glucose concentration and increased pH value by 0.2 units in diluted samples of glucose in PBS.
pH 7.3 | 295.15 K (measurement) | 310.15 K (extrapol.) | |
---|---|---|---|
a Simulated by our program to verify the equality of the approaches. | |||
Ref. 45 | 3.0 T | 0.021 | 0.012 |
7.0 T | 0.060 | 0.053 | |
11.7 T | 0.077 | 0.102 | |
pH 6.21 | 3.0 T | 0.021 | 0.024 |
7.0 T | 0.030 | 0.047 | |
11.7 T | 0.032 | 0.056 | |
pH 7.00 | 3.0 T | 0.024 | 0.017 |
7.0 T | 0.048 | 0.055 | |
11.7 T | 0.058 | 0.089 | |
pH 7.38 | 3.0 T | 0.013 | 0.0055 |
7.0 T | 0.048 | 0.025 | |
11.7 T | 0.091 | 0.056 |
We can see that the relaxivity obtained experimentally by Yadav et al. at 22 °C for different magnetic fields is comparable to our results. For the physiological temperature, none of our conditions reach the predicted relaxivity of 0.102 s−1 mM−1. This high relaxivity at 37 °C, predicted by their two-site exchange model is near its maximum in its temperature dependence for 11.7 T. A more realistic model, such as in the current study, where there are more sites with different offsets and exchange rates, would generally predict a wider, and therefore lower, maximum of the relaxivity. We have simulated relaxivity as a function of temperature using our results in Fig. 10.
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Fig. 10 Simulated relaxivity at 11.7 T using our exchange models of glucose and compared to a one (and one) site model, nearly identical to that of ref. 45. |
The results are compared with the relaxivity at 11.7 T obtained by a two-site model, where the offset is at 1.44 ppm and the temperature dependence of kex is close to that reported by Yadav et al. The expected effect of a wider maximum of exchange rates for a model with more sites is not too significant in this case.
As can be seen in Fig. 11, with a half-echo time of 1.5 ms and longer, one obtains a spectrum with a rich phase pattern. It is clear that such spectra can be used to verify or refine the exchange rates.
Simulation of the CEST spectrum would be equally straightforward, and the results may be compared with many CEST-based studies. In the CPMG simulation, used in section 4.8, instead of simulating the FID, detecting only the whole magnetization on the quadrature detector is facilitated by ‖J†−·ρ‖, where J− is the Liouville state defined by the lowering operator and ρ is the density matrix. This would also be the case for imaging. We can promptly obtain the exchange contribution to T2.
We show a simple example of how the parameters can be used in virtual experiments, helping to develop new applications for glucose as an NMR/MRI probe. Knowing the chemical exchange parameters of glucose in the given chemical conditions, we can for example straightforwardly evaluate its contribution to the water T2 or T1,ρ. The exchange parameters give opportunities to determine either glucose concentration or pH, when the other parameter is known, or in favourable cases, also both simultaneously.
For future studies, it would be valuable to determine the pH dependence of exchange parameters using more pH points. The next additional dimension of the model, can be obtained by adding the dependence on phosphate ion concentration. This would result in a rather complete model of the exchange properties of glucose hydroxyls under any physiological conditions.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d3cp01973j |
‡ Authors J. K. and P. H. contributed equally. |
§ Authors S. M. and T. L. contributed equally. |
¶ (The temperatures are obtaned from the instrument reading, without calibration, therefore the rates slightly differ from those reported in Tables S1, S2 in ESI.†) |
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