Introduction

The first step to analyse a solution of interest is elucidation of both the molecular structure and the amount of each component involved. This basic information is crucial for understanding the physical, chemical and biological properties of the solution. The information is also required for engineering and industrial utilization of components. Among the many analytical methods available, NMR is one of the most powerful and widely used to obtain quantitative information on components in solution in a native state. For example, 2D 1H–13C heteronuclear single-quantum correlation (HSQC)1, in which peak overlap in 1D spectra is mitigated by the increased dimensionality, is widely used to analyse the various components and polymer compositions of solubilized woody biomass2,3,4,5. However, as the authors have been careful to point out, because of (primarily) the non-linearity resulting from HSQC-responses to the vastly different relaxation rates of components in the solution, or to end groups vs. internal units in a polymer, only relative integrals are reportable and not true quantitation. The current methods are therefore really only applicable to comparative analyses between samples. Attempts to improve the quantitation6,7 are unwieldy or do not address all of the issues. Here we describe a new quantitation method, TAF (tolerant of any factors) quantitation method, in which the calibrated volume integral of a 1H–13C correlation peak is proportional to the absolute amount.

Results

Skewing of the Quantitation with HSQC Caused by Size-dependent Decay of Magnetization

A low molecular weight (320 Da) lignin dimer that includes the most abundant inter-unit linkage in lignin and curdlan, a high molecular weight (81 kDa average) β-1,3-linked glucan (Supplementary Fig. S1), were dissolved together in DMSO so that the concentration of the lignin dimer was equal to that of the monomer unit of the curdlan on the basis of the area of each peak in the one-dimensional 1H spectrum. The HSQC spectrum of this sample was recorded with the Fig. 1a pulse sequence and is shown in Supplementary Fig. S1 with the assignments. The volume of the peak corresponding to each CH moiety was obtained and normalized so that the average of the volume for the peaks of the lignin dimer was 1 (Fig. 2a); the volume of each peak from the lignin dimer was almost the same. The volume of each peak from the curdlan was also almost the same, but much less than 1, the average being 0.671 (Table 1). This is due to the differences in magnetization losses through transverse relaxation during the INEPT and reverse INEPT periods of the HSQC pulse-program. The transverse relaxation rate of the curdlan is much faster than that of the lignin dimer due to the extreme molecular weight difference (81,000 vs. 320)8. Therefore, despite the monomer concentrations’ being equal, the loss of magnetization during the periods is much larger for the curdlan units than for the lignin dimer, resulting in a much smaller volume for each curdlan HSQC peak. In this situation, it is impossible to correctly determine the amount of each component in solution from the HSQC spectrum. Development of a method to achieve correct quantitation in such cases has long been sought.

Table 1 The averages of the volumes of individual HSQC peaks for a lignin dimer and a curdlan.
Figure 1
figure 1

Pulse sequences used.

(a) 1H–13C HSQC pulse sequence, (b) 1H–13C TROSY pulse sequence, (c) TROSY pulse sequence with coherence-selection, (d) TROSY sequence modified from (c) to diminish the contribution of Cz, (e) TROSY sequence modified from (c) to diminish the contribution of Hz, (f) HSQC pulse sequence with coherence-selection (HSQC’) and (g) TROSY sequence modified from (d) to insert a period for extra reduction of magnetization. Narrow and wide bars represent 90° and 180° pulses, respectively. Black and white bars represent rectangular and adiabatic pulses, respectively. I and R indicate pulses for inversion and refocusing. GN and GH are gradients for coherence selection. τ, τ1 and τ2 were set to 1.563, 1.204 and 1.208 ms, respectively. The repetition delay was set to 10 s. The phase of all pulses is x, unless indicated. Phase cycling and frequency discrimination of each pulse sequence are as follows. (a) Phase cycling is φ1 = y, -y; φ2 = 2(x), 2(−x); and receiver = 2(x, −x). Frequency discrimination is obtained by States-TPPI phase cycling of φ1. (b–e) Phase cycling for the first FID is ψ = −y or y; φ1 = y, -y, −x, x; φ2 = y; φ3 = x; and receiver = x, −x, −y, y. Phase cycling for the second FID is ψ = −y or y; φ1 = −y, y, −x, x; φ2 = −y; φ3 = -x; and receiver = x, −x, −y, y. For each t1 increment, φ1 and the receiver are inverted. The data are processed as described by Kay et al.12. (f) Phase cycling is φ1 = y, −y; φ2 = 2(x), 2(−x); and receiver = 2(x, −x). To obtain a complex interferogram, the gradient GN of a second FID is inverted. For each t1 increment, φ1 and the receiver are inverted. The data are processed as described by Kay et al.12. (g) Phase cycling and data processing are the same as (c), except for ψ and φ1. For the first FID, φ1 = −y, y, −x, x. For the second FID, φ1 = y, −y, −x, x.

Figure 2
figure 2

Calibration of volumes of HSQC correlation peaks to correctly determine the amount of each component.

The volumes of each correlation peak of the 1H–13C HSQC spectrum recorded with either the Fig. 1a pulse sequence (a) or the Fig. 1f pulse sequence (d). The volume of the peak corresponding to each CH moiety was obtained. The volumes are normalized so that the average of the volumes for the peaks of the lignin dimer is 1. Calibrated volumes were calculated and plotted for HSQC/α2 (b), HSQC/β2 (c) and HSQC’/γ2 (e). Error bars represent standard deviations of four independent experimental data sets.

Analysis of the Skew with Product Operator Formalism and a Hint for Preventing the Skew

The loss of magnetization during the two INEPT periods can be traced using the product operator formalism9. At time a in the Fig. 1a pulse sequence, the operator is Hz and becomes 2HzCx at time b after the INEPT period (where H and C refer to proton and carbon magnetization). When the transverse relaxation during the INEPT period is taken into account, the virtual magnetization decreases to δ∙2HzCx at time b, where 0 < δ < 1. When t1 is assumed to be 0 for simplicity, the relevant operator at time c is −δ∙2HzCx and it becomes δ2Hx at time d after the reverse INEPT period, where reduction of magnetization due to the transverse relaxation during the reverse INEPT period is also taken into account. It should be noted that the transverse relaxation during the t1 period affects the width of the correlation peak but does not affect its volume. Therefore, the discussion under the assumption of t1 = 0 does not lose generality for examining the effect of transverse relaxation on the volume of the correlation peak.

The Fig. 1b pulse sequence is that of transverse relaxation optimized spectroscopy (TROSY)10,11. Tracing the magnetization for TROSY, Hz at time a becomes δ∙2HzCx at time b in the same way. δ∙2HzCx can be expressed as δ∙HαCx − δ∙HβCx. When t1 is 0, the relevant operators at time c are δ∙HαCx − δ∙HβCx and they become δ∙ε∙HyCβ + δ∙ε∙HyCα at time d, where ε is such that 0 < ε < 1, the reduction of magnetization due to the transverse relaxation during the ST2-PT (single transition to single transition polarization transfer) period between c and d being taken into account. It should be pointed out that only the second term of δ∙ε∙HyCβ + δ∙ε∙HyCα, i.e., δ∙ε∙HyCα, is detected with a coherence-selection method in an actual experiment, as explained below. In the case of TROSY, Cz at time a also contributes to the TROSY signal. It becomes −Cx at time b after the INEPT period. It should be noted that the magnetization does not decrease due to the transverse relaxation during the INEPT period, because the magnetization is always along either the z-axis or −z-axis. −Cx can be expressed as −HαCxHβCx. When t1 is 0, the relevant operators at time c are −HαCxHβCx and they become −ε∙HyCβ + ε∙HyCα at time d, where the reduction during the ST2-PT period is taken into account in the same way. Again, only the second term, ε∙HyCα, is detected in an actual experiment. In summary, Hz at time a becomes δ∙ε∙HyCα at time d, whereas Cz at time a becomes ε∙HyCα. Both contribute to the same TROSY signal. A remarkable point is that Hz decreases during both the INEPT and ST2-PT periods, whereas Cz reduces during just the ST2-PT period. This difference was utilized to develop the new quantification method, as follows.

The Method for the Correct Quantitation by NMR

Suppose the lower right component of four fine structures of a TROSY correlation peak is detected in an experiment. The intensities of steady-state Hz and Cz magnetizations are assumed to be u and v, respectively. When a phase of the 1H pulse labelled with ψ in the Fig. 1b pulse sequence is set to −y, henceforth this pulse sequence is designated as pulse b(-y), signals originating from Hz and Cz are both added at the TROSY peak. On the other hand, when this phase is set to y, henceforth this pulse sequence is designated as pulse b(y), the latter signal is added with a negative sign12. Thus, the volume of the TROSY peak for a b(-y) pulse sequence is proportional to δ∙ε∙u + ε∙v = ε∙(δ∙u + v), whereas that for a b(y) pulse sequence is proportional to δ∙ε∙u–ε∙v = ε∙(δ∙uv).

Here we define α for each peak as

Then, it was deduced that α is equal to δ∙u/v. Here, u/v is a constant, so it is concluded that α is proportional to δ. In the case of HSQC, magnetization decreases by a factor of δ2 due to transverse relaxation during the INEPT and reverse INEPT periods, as discussed above. Therefore, when the volume of each HSQC peak is divided by α2 of each peak, the effect of reduction due to transverse relaxation is cancelled out. Thus, it is expected that the volume of each peak can be quantitatively compared without skew caused by variation in the transverse relaxation rate. Figure 2b clearly indicates that this idea works well in practice. The calculated volumes for curdlan increased and are all close to 1, the average being 0.989 (Table 1). This is exactly what we expect for a mixture in which the concentrations of the lignin dimer and the monomer unit of curdlan are the same.

For a TROSY experiment, only the second term of either δ∙ε∙HyCβ + δ∙ε∙HyCα originating from Hz or −ε∙HyCβ + ε∙HyCα originating from Cz is detected, as mentioned above. In order to reduce the number of phase cycling steps, a coherence-selection method11,12 is applied to the Fig. 1c pulse sequence by introducing τ1 - 13C 180° pulse – τ1 and τ2 - 1H 180° pulse – τ2 units coupled with a gradient after the t1 period and prior to the t2 period, respectively. Then, α was calculated for each peak with its volume in the TROSY spectrum obtained via the Fig. 1c pulse sequence, as follows.

Here, the meaning of c(−y) and c(y) is the same that of b(−y) and b(y). Reduction of magnetization due to transverse relaxation occurs during the times of the two units described above. However, this does not affect α, because the effect is cancelled out due to division in the calculation of α. In fact, Fig. 2b was obtained from the α derived with the Fig. 1c pulse sequence. Thus, a TROSY pulse sequence that incorporates the coherence-selection method can be successfully used to obtain α for the correct quantitation.

Suppose a case in which there are wide distributions of the transverse relaxation rates for a signal of a component in a polymer containing many same components. The magnetization losses during the INEPT and reverse INEPT periods differ depending on the transverse relaxation rate. Concerning a certain signal, our method determines the sum of the magnetization losses caused by various transverse relaxation rates. This information can be used to correct the skew of quantitation for a certain signal in the same way. Thus, our method is valid even if there are wide distributions of the transverse relaxation rates for a signal.

Alternative Method for the Correct Quantitation

In the method described in the previous section, the intensities of signals originating from Cz might be slightly distorted during the INEPT period by the longitudinal relaxation after the first 13C 180° pulse. In the case of the current sample, the distortion is negligible, less than 1%. But in other cases, the distortion might be problematic. For those cases, we have also developed an alternative method for quantitation utilizing TROSY. For the Fig. 1d pulse sequence, a 13C 90° pulse and a gradient are added at the beginning of the Fig. 1c pulse sequence to purge steady-state Cz magnetization. Thus, for the Fig. 1d pulse sequence, only Hz is present at time a to contribute to the volume of the TROSY peak. For the Fig. 1e pulse sequence, the INEPT unit of the Fig. 1c pulse sequence is replaced by a 13C 90° pulse. Thus, for the Fig. 1e pulse sequence, only Cz is present at time a to contribute to the volume of the TROSY peak. As discussed above, Hz at time a becomes −δ∙ε∙HyCα after the ST2-PT period of the TROSY pulse, while Cz at time a becomes ε∙HyCα. Thus, the volume of the TROSY peak for the Fig. 1d pulse sequence is proportional to δ∙ε∙u, whereas that for the Fig. 1e pulse sequence is proportional to ε∙v. Here, the reduction of magnetization during the [τ1 - 13C 180° pulse - τ1] and [τ2 - 1H 180° pulse - τ2] units coupled with a gradient is ignored, because this effect is cancelled out due to division in the following equation to calculate β, as explained above. We define β for each peak as

β is equal to δ∙u/v. Again, u/v is a constant, so it is concluded that β is proportional to δ. When the volume of each HSQC peak that is affected by the factor δ2 is divided by β2 of each peak, the effect of reduction due to transverse relaxation is cancelled out and thus the volume of each peak can be quantitatively compared without skew caused by variation in the transverse relaxation rate. Figure 2c clearly indicates that this alternative idea also works well. The volumes for curdlan are again all close to 1, the average being 1.025 (Table 1).

This alternative method is more rigorous than the one in the previous section. However, the signals originating from Cz and Hz are discarded in pulses of Fig. 1de, respectively. Therefore, the alternative method needs more experimental time than the one in the previous section by the factor of √2. So, it is recommended to use one of two methods depending on the situation.

A variant of the method to correctly determine the amount

In order to achieve better water suppression, a Fig. 1f pulse sequence (HSQC’) is occasionally used to obtain an HSQC spectrum. A τ1 - 13C 180° pulse - τ1 unit coupled with a gradient is inserted after the t1 period of a Fig. 1a pulse sequence. When the Fig. 1f pulse sequence is used, the volume of each peak of a curdlan is much smaller than 1 (Fig. 2d), the average being 0.538 (Table 1). The average volume of curdlan peaks for a Fig. 1f pulse sequence is even smaller than that for a Fig. 1a pulse sequence. This is because loss of magnetization through transverse relaxation during the inserted period is also greater for a curdlan than for a lignin dimer. As measures to this situation, a unit of τ1/4 - 1H 180° pulse - τ1/4 - 13C 180° pulse - τ1/4 - 1H 180° pulse - τ1/4 is inserted prior to the t1 period of a Fig. 1d pulse sequence to make a Fig. 1g pulse sequence. The total duration of the inserted unit is τ1. Loss of magnetization through transverse relaxation occurs during this unit for τ1. Here, we define γ for each peak as

Then, the volume of each HSQC peak obtained with a Fig. 1f pulse sequence (HSQC’) is divided by γ 2 of each peak (Fig. 2e). In the case of a Fig. 1f pulse sequence, extra loss of magnetization occurs for a period of 2τ1. The volume for pulse g includes the effect of magnetization loss during the τ1 period. When the exponential-dependency of loss of magnetization on the period of relaxation is taken into account, it is regarded that a square of the volume for pulse g includes the effect of magnetization loss during the 2τ1 period. Therefore, division by γ 2 can compensate for the extra loss of magnetization during the 2τ1 period. Figure 2e clearly indicates that this method works well. All the volumes for a curdlan recovered, the average being 1.000 (Table 1). Thus, even when the Fig. 1f pulse sequence is used, correct quantitation can be achieved.

Discussion

In our methods, the steady state 13C magnetization is utilized. Its longitudinal relaxation time is generally longer than that of 1H magnetization. Therefore, longer recycling delay time is required to ensure the recovery of the 13C magnetization, which results in the increase of experimental time to some extent. In a case of the present sample, the 13C longitudinal relaxation time was longer for a curdlan than a lignin model dimer and the required recycling delay time was ca. 3.5 s which is five times as long as the 13C longitudinal relaxation time of a curdlan. The use of relaxation enhancing agents would be useful to reduce the experimental time, if necessary.

When intermolecular hydrogen bonds are formed, the apparent molecular size and rotational correlation time increase, which results in a fast transverse relaxation rate. Therefore, the presence of intermolecular hydrogen bonds also skews quantitation. Intermolecular hydrogen bonding is well known for cellulose and hemicelluloses, which are two of the three major components of woody biomass13. HSQC does not allow correct quantitation for these cases. However, the methods described here produce quantitative measures that are not affected by variations in the transverse relaxation rate. Therefore, this method is also valid for a system involving intermolecular hydrogen bonding, as is the case for woody biomass materials.

Quantitation with an HSQC spectrum is skewed not only by variation in the transverse relaxation rate among components of a mixture but also by variation in a one-bond C–H coupling constant, 1JCH. In order to maximize the efficiency of magnetization transfer during the INEPT and reverse INEPT periods, τ of the Fig. 1a pulse sequence is set to 1/(4∙1JCH). The 1JCH values differ significantly between aliphatic and aromatic C–H bonds for components involved in woody biomass, the natural 1JCH range being 115–220 Hz7. Therefore, when a certain τ value is set for HSQC, the efficiency of magnetization transfer differs for each component. This affects the volume of each HSQC correlation peak, which results in skewing of the quantitation. Again, however, the loss of magnetization during the INEPT and reverse INEPT periods due to mismatching between τ and 1/(4∙1JCH) for each component is automatically corrected with our method, when either HSQC/α2 or HSQC/β2 is calculated.

Finally, homonuclear 1H–1H couplings cause modulation during the INEPT and reverse INEPT periods, which results in the reduction of the volume of an HSQC correlation peak7. Our method can correct this reduction as well. The Q-HSQC method was successfully developed to correct the skewing of quantitation due to variation in 1JCH. Q-HSQC, however, cannot correct the skew caused by either homonuclear 1H–1H couplings or the variation in molecular size. In contrast, any loss of magnetization during the INEPT and reverse INEPT periods is corrected with our method, irrespective of its cause, to achieve correct quantitation. In this context, it should be added that the skew caused by the imperfection of each NMR pulse used in the INEPT and reverse INEPT periods is also corrected with our method.

The HSQC0 method was successfully developed for the correct quantitation14. Extrapolation using a series of HSQC spectra acquired with incremented repetition times (the time between the end of the first 1H excitation pulse to the beginning of data acquisition) is carried out in this method. This method utilizes long pulse sequences and thus suffers the loss of the signal intensity due to transverse relaxation. Therefore, it is difficult to apply this method to high molecular weight samples. Our method, the TAF quantitation method, utilizes the steady state 13C magnetization, as mentioned above. The polarization of 13C magnetization is smaller than that of 1H magnetization, ca. 1/4, which results in the low sensitivity of the signal originating from the steady state 13C magnetization. Although the use of the small polarization of 13C is an unpreferable point, it should be noticed that the unpreferable factor of 1/4 remains the same, without getting worse, even for high molecular weight samples. In addition, it should also be pointed out that the steady state 13C magnetization is free from the loss of the intensity due to transverse relaxation during the INEPT period of TROSY. Therefore, it is supposed that the TAF quantitation method is superior to the HSQC0 method for the application to high molecular weight samples.

In summary, the method described here, the TAF quantitation method, is tolerant of any factors that could skew quantitation: major variation in molecular size, intermolecular hydrogen bonding, variation in the 1JCH value, presence of homonuclear 1H–1H couplings and imperfections in NMR pulses. Moreover, the TAF method is applicable to high molecular weight samples. The developed TAF quantitation method is robust and generally applicable in a variety of different situations to assure correct quantitation, including in biomass plant cell wall NMR studies.

Methods

Sample Preparation

A lignin model dimer, guaiacylglycerol-β-guaiacyl ether, which models the most abundant linkage in lignin (Supplementary Fig. S1), was purchased from TCI, Japan (Tokyo). A curdlan, a high molecular weight linear polymer consisting of β-1,3-linked glucose residues (Supplementary Fig. S1), was purchased from Wako Pure Chemicals Industries Ltd (Osaka, Japan). The lignin dimer and curdlan were dissolved together in DMSO-d6. Initially, the concentrations of the lignin dimer and a curdlan were ca. 100 mM and 25 mg/ml, respectively. A one-dimensional 1H NMR spectrum was recorded. Then, on the basis of the area of each peak in the spectrum, the concentrations were further adjusted so that the concentration of the lignin dimer and that of a monomer unit of the curdlan were equal.

NMR Spectroscopy and Manipulation of Data

NMR spectra were recorded using Bruker DRX600 and AVANCEIII700 spectrometers, each equipped with a cryoprobe. HSQC and TROSY spectra were recorded using pulse sequences a-g shown in Fig. 1 at 298 K. The spectrum obtained with each pulse sequence was recorded four times. The volume of the peak corresponding to each CH moiety was obtained and its average and standard deviation were calculated for four independent experiments for each pulse sequence. The volumes or calibrated volumes were normalized so that the average of the volume for the peaks of the lignin dimer is 1. Data were processed and analysed with NMRPipe/NMRDraw15 and Sparky16. Pulse programs and parameters are available on request.

Additional Information

How to cite this article: Okamura, H. et al. Accurate and molecular-size-tolerant NMR quantitation of diverse components in solution. Sci. Rep. 6, 21742; doi: 10.1038/srep21742 (2016).