Anuji
Abraham‡
a,
David C.
Apperley
a,
Stephen J.
Byard
b,
Andrew J.
Ilott§
a,
Andrew J.
Robbins¶
a,
Vadim
Zorin||
a,
Robin K.
Harris
a and
Paul
Hodgkinson
*a
aDepartment of Chemistry, University of Durham, Durham DH1 3LE, UK. E-mail: paul.hodgkinson@durham.ac.uk
bCovance Laboratories Limited, Willowburn Avenue, Alnwick NE66 2JH, UK
First published on 21st January 2016
A combination of solid-state NMR techniques, including 13C/1H correlation, 2H magic-angle spinning NMR and first principles calculation are employed to characterise the role of water in different hydration states of sildenafil citrate. The 13C spectrum is fully assigned for the first time and direct correlations made with respect to the crystal structure. 2H magic-angle spinning NMR is demonstrated to be a powerful tool for the study of dynamic and exchange processes in complex hydrate systems, allowing the behaviour at multiple solvate sites to be characterised without the need for expensive and selective labelling. Use of the 2H double-quantum frequency allows resolution of the different sites and, consequently, data fitting to determine rates of spin-diffusion between the different sites. The water is shown to be highly dynamic, undergoing C2 rotation, with chemical exchange between different water molecules and also with the host structure. The methods adopted are applicable to the investigation of an extensive range of hydration types found in pharmaceutical drug substances.
Sildenafil citrate (the active component of Viagra™) is a monobasic salt and, based on solution-state pKa properties, the citrate anion is expected to be deprotonated at C34. Its structure is shown in Scheme 1, together with the numbering scheme of the atoms used here. Only one polymorphic form has been reported. As discussed below, the crystal structure of this form takes up water reversibly, with no significant hysteresis or change of form on exposure to high humidity. Qualitative insights into the interaction of water with solid sildenafil citrate have previously been derived from 13C and 15N cross-polarisation magic-angle spinning (CPMAS) NMR.4 Here, variable-temperature 13C and 2H spectra, together with 13C/1H HETCOR experiments and first-principles computation, are used to develop a comprehensive picture of the interaction of water with the drug material, and to resolve discrepancies in spectral assignment with other solid-state NMR studies.5
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Scheme 1 Molecular schematic of sildenafil citrate, indicating the numbering of carbon and nitrogen atoms used in ref. 4 and this work. Note that both molecules are shown, as conventionally represented, in their neutral forms, while XRD and NMR are consistent with a transfer of H+ from the C34 carboxylic acid group to N26 in the solid state. |
13C CPMAS spectra were acquired as a function of temperature on a Varian Unity Inova spectrometer operating at 299.82 MHz for 1H (75.40 MHz for 13C), with a sample of hydrated sildenafil citrate packed into a 5 mm o.d. zirconia rotor. Holes in the end-cap of the rotors avoided any risk of pressure build-up on dehydration. CPMAS spectra (at 5 kHz MAS rate) were acquired with 204 repetitions, a recycle delay of 5 s and CP contact time of 1 ms, allowing at least 20 minutes at each temperature before acquisition to allow for thermal equilibration. The order of acquisition is indicated in Fig. 1. Note that temperatures are quoted as set and do not attempt to correct for sample heating due to MAS; these corrections are estimated to range from +5 °C for 5 kHz spinning in a 5 mm rotor to a maximum of +25 K for 10 kHz spinning in a 5 mm rotor.
13C/1H HETCOR experiments were carried out at ambient probe temperature on a Varian VNMRS spectrometer operating at 399.88 MHz for 1H (100.56 MHz for 13C), with samples packed into 4 mm o.d. zirconia rotors. The magic-angle spinning rate was 8 kHz. FSLG 1H decoupling was used in the indirect dimension at a power equivalent to 96.2 kHz, and the same power was applied for TPPM decoupling in the direct dimension. Lee-Goldburg cross-polarisation was used with both 0.1 and 1 ms contact times. 200 acquisitions were acquired with a 5 s recycle delay for each of 32 increments in t1, using a spectral width of 14.7 kHz. The 1H chemical shift axis was rescaled following a reference spectrum of glycine acquired under the same conditions (using 3.0 ppm and 8.4 ppm as the reference shifts of the CH3 and NH3+ signals respectively).
2H MAS spectra were recorded on a Varian InfinityPlus spectrometer using samples packed into 5 mm o.d. MAS rotors and at a Larmor frequency of 76.71 MHz, using a MAS rate of 8.5 kHz. 256 transients were acquired at each temperature using a recycle delay of 8 s. Most spectra were obtained via direct excitation using a 2H 90° pulse of 7.7 μs, referenced to external CDCl3 at 7.2 ppm, and using 1H TPPM decoupling. Where required, the magic angle was adjusted using either [d6]α-oxalic acid6 or [d1]-alanine to limit broadening due to magic-angle mis-set.
2H DQ/SQ EXSY spectra were acquired using the DQ/SQ correlation experiment of ref. 7, but extending the z-filter to provide the exchange period of an EXSY experiment, and using cross-polarisation for excitation. 32 transients were averaged for each of 32 t1 increments with Δt1 = 4/νrot = 400 μs, and 4 s recycle delay, using a MAS rate of 10 kHz. 1H decoupling was used by default in the acquisition dimension, although this was not observed to have a significant impact on spectral resolution. Spectra were generally acquired with “synchronised acquisition” so that spinning sidebands were folded on to centrebands in both dimensions to improve signal-to-noise ratio and quantification. A series of spectra was recorded with mixing times ranging from 1 ms to 2 s at two set temperatures, −50 and −30 °C. Note that the mixing time was actively synchronised with the rotor phase at all but the shortest mixing times.8,9 Processing of the 2D spectra involved modest Gaussian line-broadenings of 100 Hz and 50 Hz in the direct and indirect dimensions respectively prior to Fourier transformation. Further analysis was performed in Matlab,10 as described in the ESI.†
The DVS and TGA results show that the XRD studies are compatible, with the different reported levels of hydration reflecting differences in sample environment and differences in modelling of the disordered water. It is, therefore, a reasonable starting point for calculations to use the XRD structure with the water sites fully occupied and the same structure, but with the water atoms removed, as models for the fully hydrated and dehydrated materials respectively. The isostructural nature of the hydrated and dehydrated forms is confirmed by the calculation results below.
Warming the sample to higher temperatures than 40 °C leads to further changes in the same regions of the spectrum. In contrast, however, these changes are irreversible; the final spectrum obtained at ambient temperature is identical to that of “dry” sildenafil citrate obtained by storage at 0% RH.4 The spectrum of the dehydrated material is not significantly temperature dependent, with the exception of the C11/C12 propyl resonances (compare the final spectra obtained at 120 °C and 25 °C). This suggests that the dynamics of the propyl region depend on the occupancy of the water site. Similar observations have been made via13C T1 (spin–lattice) relaxation times in the hydrated and dehydrated forms of thiamine hydrochloride monohydrate.23
Fig. 2 shows the 2H magic-angle spinning spectra obtained as a function of temperature. The sample was held for an extended period at 55 °C to measure 2H T1 values, which are summarised in Table S1.† It is clear from spectra acquired before and afterwards that the bulk of the dehydration occurred during this period. The low temperature spectra show three regions of intensity (in addition to any free water signal). The very broad and quickly relaxing peak at 3.7 ppm is assigned to water in sildenafil citrate tunnels. This can be readily distinguished from adventitious water, which appears as a signal around 5–6 ppm, marked with an asterisk in the dashed spectrum of Fig. 2. In contrast to the other signals, this peak is not associated with a noticeable spinning sideband manifold, and so represents a small fraction of the total water signal. This usefully illustrates that adventitious and channel water can be clearly distinguished using 2H MAS NMR, in contrast to bulk techniques such as DVS and TGA. The broadness of the peak for channel water and its extremely short relaxation time are consistent with rapid flips of the water molecules about their C2 axis. The signal around 17 ppm is readily assigned to the C33 acid H site (O33H) on the basis of the CASTEP-predicted shifts. As discussed below in the context of the two-dimensional 2H experiments, and confirmed by the HETCOR experiments, the feature around 11 ppm contains the other exchangeable H signals: the remaining citric acid protons, O35H and O31H, and the protonated nitrogen sites N5H and N26H.
As the temperature is raised, the resolved citrate signal clearly broadens and coalesces with the water signal, which becomes too broad to be observed. Only a single signal peak at 10 ppm is seen at 10 °C, although is it difficult to judge whether a subset of, or all, the 2H sites are in exchange. The rate of exchange must be on a frequency of kHz, corresponding to collapsing a 15 ppm shift range at 76.8 MHz NMR frequency. As the temperature rises, and the sample dehydrates, the spectrum becomes less symmetric and a peak around 16 ppm appears. This corresponds to the O33H citrate signal, no longer broadened by exchange, consistent with the CASTEP calculations that show a shift of −0.5 ppm between “wet” and “dry” structures for this site. As also observed in the 13C experiments, no significant changes are observed on lowering the temperature back to the starting point, which is consistent with a lack of H-exchange/water dynamics in the dehydrated material.
As detailed in the ESI,† quadrupolar parameters were obtained for the resolved sites by fitting the 2H spectra from “wet” and dehydrated samples at −58 °C. The most informative parameters are those for the peak assigned to sequestered water. The CQ of 97 kHz and asymmetry parameter of 1 are characteristic for water molecules undergoing a rapid C2 flip, but not other significant re-orientational dynamics.26
2H DQ/SQ EXSY experiments were used to try to provide more quantitative insight into the exchange processes. Fig. 3 shows an example DQ/SQ 2H EXSY spectrum obtained at −50 °C on a “wet” sample, using cross-polarisation for excitation. As expected, using the double-quantum frequency in the indirect dimension dramatically improves resolution since this is unaffected (to first order) by the quadrupolar coupling and so is less sensitive to magic-angle mis-set and motional broadening.7 The broad peak at 10–12 ppm is clearly resolved into a smaller peak about 11.5 ppm and a large peak about 10 ppm. The HETCOR-derived and computed hydrogen shifts of N5H, N26H, O31H and O35H are too overlapped to confidently assign the peaks. The peak at 11.5 ppm is tentatively ascribed to the other citrate carboxylic acid proton, O35H, on the basis of its similar intensity to the O33H peak and its calculated proton chemical shift. The use of cross-polarisation allowed short recycle delays, but resulted in spectra without an observable signal from D2O. Use of direct-excitation, rather than cross-polarisation, to observe EXSY spectra containing a water signal was unsuccessful, however; it was difficult to excite a water double-quantum signal in the DQ/SQ experiment, and at short mixing times (e.g. 7.1 ms) strongly distorted 2D spectra were obtained in the simple SQ/SQ version of the experiment. This presumably relates to the rapid C2 flips of the water, violating the EXSY requirement that the NMR frequency is stable during the t1 and t2 measurement periods. At long mixing times (e.g. 71.4 ms), undistorted spectra were observed, but without a water resonance, as the troublesome water signal has been lost through relaxation (a T1 of 37 ms was measured at −35 °C).
Exploiting the additional site resolution provided by the DQ/SQ experiment, the build-up of the EXSY cross-peaks was used to estimate rates of magnetisation exchange between the sites, following the methodology described in the ESI.† As illustrated in Fig. 4, very satisfactory fits were obtained. The rates of exchange were found, however, to be identical within experimental uncertainty for the two measurement temperatures, as summarised in Table S4.† This implies that magnetisation transfer in these experiments was dominated by 2H spin-diffusion rather than chemical exchange. It has previously been observed that magic-angle spinning tends to enhance rates of magnetisation exchange via dipolar couplings between 2H sites.40 As noted in the discussion of the data in Table S4,† measurement of 2H spin-diffusion rates might provide useful information on spatial proximity, in the same way that 1H spin-diffusion has been used to provide constraints for structure solution.27,28 In this case, however, the overall structure is known and so the spin-diffusion results provide little additional insight.
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Fig. 4 Intensities of cross-peaks in 2H DQ/SQ EXSY spectrum and corresponding fits obtained on hydrated sildenafil citrate at −50 °C. Columns correspond to frequencies in the direct (single-quantum) dimension, and rows to indirect dimension (double-quantum) frequencies. Error bars indicate one-standard deviation uncertainties on the intensity values. The corresponding figure for data acquired at −30 °C can be found as Fig. S3 of the ESI.† |
Experimental 13C shifts were obtained from the spectra of dehydrated and hydrated samples at ambient probe temperature and −80 °C respectively (results tabulated in the ESI†). In cases where resonances overlapped (e.g. C25 and C27), the same experimental shift was assumed for the different sites. The detailed assignment of the experimental chemical shifts is discussed below in the context of the HETCOR experiments.
In all cases, excellent correlations are obtained between calculated and experimental 13C chemical shifts, cf. Fig. S4.† As typically observed, the slope of the fitted linear gradient is not exactly 1. Such deviations in slope may be due to the effects of nuclear delocalisation29 and/or systematic errors in the DFT methodology30 and cannot be readily calculated. We have taken the usual pragmatic approach of rescaling the calculated shifts to match the slope and mean of the experimental shifts.31 This has been done independently for each computed result prior to calculating the root-mean-square deviation between experimental and calculated shifts. As summarised in Table 1, there is little difference in the overall RMSD between experimental and calculated shifts for the different geometry-optimised shifts. Note that the citrate shifts are not particularly well-fitted by H-only optimisation, and the RMSD for these signals is significantly reduced when the position of the citrate atoms is allowed to “relax”. The anisotropic displacement parameters for several of the non-hydrogen citrate atoms are significantly elongated, suggesting the presence of (dynamic) disorder which may slightly distort the average citrate geometry in the starting crystal structure. Similar behaviour was observed for disordered acetic acid molecules in the diacetic acid solvate of diterbutaline sulfate.32
Geometry optimisation | “Wet” | “Dry” | ||
---|---|---|---|---|
All | Citrate | All | Citrate | |
H-only | 1.6 | 2.9 | 1.6 | 2.8 |
H + citrate | 2.0 | 0.8 | ||
All atoms | 1.8 | 1.4 |
Fig. 5 compares the differences in 13C shift between the hydrated and dehydrated sildenafil citrate resonances observed both experimentally and in computation. Experimental shifts were obtained from dehydrated and hydrated samples at ambient probe temperature and −80 °C respectively, while calculated shift differences are based on the (rescaled) shifts of the two H-only optimised structures. The sign of the changes is generally well predicted, although the calculations tend to overestimate their magnitude, which is likely to reflect the partial occupancy of the water sites in the hydrated sample. The possible effects of fractional water occupancy on 13C chemical shifts have previously been noted for the hemihydrate of a guanosine derivative.33 The agreement for sites that show significant temperature dependence and are likely to be affected by dynamics, e.g. C11 and C21, is noticeably poorer. This is expected given that the calculations are based on a single 0 K optimised structure. The agreement is far better than would be expected if the “errors” between calculated and experimental shifts were uncorrelated; the dotted lines in Fig. 5 are placed at ×1.6 ppm, where 1.6 ppm corresponds to the typical RMSD observed in Table 1. These results indicate that first-principles calculations can be used to understand relatively subtle differences for sites in otherwise equivalent environments. Significantly poorer correlations between wet vs. dry chemical shifts are obtained if either of the more fully optimised structures was used, i.e. the effect of the presence of water on the chemical shifts is better predicted when the non-H atoms are fixed in consistent positions.
Also shown in Fig. 6 are the corresponding computed chemical shifts based on the H-only geometry-optimised structures, with circles marking cross-peaks expected on the basis of distances between each carbon site and the nearest hydrogens, obtained using the crystal-viewing software gdis.36 Larger circles mark distances below 1.5 Å, corresponding to directly bonded CH pairs. In all cases, corresponding cross-peaks (marked in bold italics) were observed in the short-contact-time HETCOR experiment. A few longer-range contacts, corresponding to distances less than 2.0 Å, were also observed at these short mixing times. These cross-peaks were helpful in a number of cases. For example, the pair of lines at 130 and 131 ppm can be assigned to C15 and C17 using the predicted chemical shifts of the attached H sites, which differ by ∼2 ppm. This assignment disagrees with the ordering predicted from the computed 13C shifts alone, but is within the approximately 1.6 ppm “margin of uncertainty” suggested by the overall RMSD between computed and observed 13C shifts. In other areas, such as C30 and C32, the 13C and 1H shifts are both too strongly overlapped to allow the assignment to be improved.
The additional cross-peaks appearing at longer mixing time help to resolve most of the remaining ambiguities. Smaller circles in Fig. 6 mark potential cross-peaks corresponding to distances up to 2.5 Å. For example, long-range correlations to O33H and O35H hydrogen sites allow C33 vs. C35 to be assigned. The assignments are confirmed by the changes in the shifts of these peaks with hydration state. A small number of cross-peaks seem to correspond to even longer distances (up to 2.8 Å), but this may be associated with spin-diffusion of magnetisation between H sites and should be interpreted cautiously. For example, the apparent cross-peak between C31 and O33H is more likely to be a “relay” transfer than a direct correlation. Taken together, however, the computed 13C shifts, short-contact cross-peaks identifying H peaks, longer range correlations, and the peak movements between wet and dry samples allow all the resolved 13C peaks to be assigned with some confidence. The “evidence” used to assign each 13C peak is summarised in Table S5.† Overall, the availability of powerful computational tools, together with experimental HETCOR results, has allowed the sildenafil citrate assignment to be considerably refined compared to earlier work.4,5 First-principles calculations and HETCOR experiments have recently been used in a similar fashion to resolve conflicting spectral assignments for the API naproxen,37 and aid structure solution from PXRD data for an indomethacin/nicotinamide co-crystal.38 Note that Wawer et al.5 have different assignments for the solution-state NMR resonances in the 135–155 ppm region compared to ref. 4, inverting the assignments for the pairs C4/C6 and C1/C8 in the numbering used here. The current solid-state study also reverses the order of C4/C6 compared to our previous work, but not for C1/C8. The difference in shift between C4 and C6 (<4 ppm) is sufficiently small, however, to be ascribed to differences in shift between solid and solution states.
The most direct insight into hydration was provided by 2H MAS NMR, which allows multiple exchangeable sites to be studied simultaneously, without the need for bespoke isotopic labelling. The water molecules are found to be undergoing C2 flips and exchanging between water sites (information obtained from the 13C spectrum), even at the lowest temperatures studied (−58 °C). This is in good agreement with the XRD crystal structure, in which the water hydrogen atoms were located, but in which water sites were partially occupied. In addition, exchange of hydrogen between water and other exchangeable hydrogen sites, most evidently on the citrate ion, was observed as the temperature was raised. This is consistent with the easy deuteration of exchangeable sites from storing sildenafil citrate in a D2O-saturated atmosphere. The sensitivity of the 2H NMR signal to dynamics complicated, however, the use of magnetisation transfer experiments to measure the rate of this hydrogen exchange. It was, nevertheless, possible to derive rates of 2H spin-diffusion from double-quantum/single-quantum EXSY experiments, which may be useful in cases where the 2H MAS spectrum is sufficiently resolved.
Aided by computation, solid-state NMR has provided a detailed picture of the interaction of water molecules with the host sildenafil citrate structure in this non-stoichiometric hydrate. Although molecular dynamics simulations have allowed relatively slow molecular processes, on the order of microseconds, to be linked to NMR observations,41 reproducing the behaviour observed here in simulation will be extremely challenging, due to the size of the system (696 atoms in the unit cell) and the electronic re-arrangement involved in hydrogen exchange.
This work was supported under EPRSC grant number EP/D057159, and benefitted from discussions within the context of the EPSRC-funded collaborative computational project for NMR crystallography (CCPNC). Raw data and supporting electronic files associated with this publication can be accessed through data DOI: 10.15128/rf55z7713, as summarised in Table S6 of the ESI.†
Footnotes |
† Electronic supplementary information (ESI) available: Experimental details of XRD, TGA and DVS studies; details of 2H NMR studies; detailed information on peak assignment; contents of raw data bundle. CCDC 1062242. For ESI and crystallographic data in CIF or other electronic format see DOI: 10.1039/c5ce02234g. |
‡ Current address: Drug Product Science & Technology, Bristol-Myers Squibb, 1 Squibb Drive, New Brunswick, New Jersey 08903, USA. |
§ Current address: Department of Chemistry, New York University, 100 Washington Square East, New York, New York 10003, USA. |
¶ Current address: Solid-Form Solutions, 1 The Fleming Building, Edinburgh Technopole, EH26 0BE, UK. |
|| Current address: ExxonMobil Chemical Europe Inc., Hermeslaan 2, 1831 Machelen, Belgium. |
This journal is © The Royal Society of Chemistry 2016 |