Open Access Article
Dmitrii Aleshin*a,
Korin Butbula,
Itai Hahamya,
Daniel Abergelb and
Lucio Frydman
*a
aDepartment of Chemical and Biological Physics, Weizmann Institute of Science, Rehovot 7610001, Israel. E-mail: dmitrii.aleshin@weizmann.ac.il; lucio.frydman@weizmann.ac.il
bChimie Physique et Chimie du Vivant – UMR 8228, Département de chimie, Ecole normale supérieure, PSL University, Sorbonne Université, CNRS, 75005 Paris, France
First published on 15th May 2026
The exceptionally high spin polarizations that result from dissolution dynamic nuclear polarization (d-DNP), can lead to unusual liquid-state nuclear magnetic resonance (NMR) spectral features. This study analyzes such features, when performing d-DNP of hyperpolarized water to dissolve and sensitize the NMR spectra of co-dissolved molecules. Most evident among the collective spin effects that arise in such “HyperW” experiments is the very strong radiation damping (RD) affecting the water resonance. In addition, the presence of such strongly magnetized water signal alters both the amplitude and the phase of resonances emerging from the solutes co-dissolved in the hyperpolarized H2O, for as long as these remain within the RD-broadened line width of water's resonance. These phase- and amplitude RD effects are superimposed on cross-relaxation and chemical exchange effects, which will also affect the phases and amplitudes of all peaks. Demonstrations and derivations of these effects, as well as a discussion of their consequences in HyperW experiments on solute-oriented measurements, are presented.
Despite this potential, HyperW experiments are not without challenges. A most evident feature associated to these experiments, are the large linewidths that can characterize the hyperpolarized water 1H NMR resonance: when subject to small tip angle excitations, these can span several kHz regardless of shimming. This reflects the severe radiation damping (RD) arising in these experiments; i.e., the collective interaction between water's large 1H magnetization, and the NMR detection circuit. In these RD-dominated acquisitions, the water's free induction decay (FID) will generate a current in the detection coil, whose emitted radiofrequency (RF) field will act back on the spins.38–47 This will drive hyperpolarized water's nuclear magnetization back towards the longitudinal z axis, as if it were an on-resonance pulse. Such RD effects have long been a feature of conventional NMR, particularly in 2D 1H–15N correlation experiments where high water concentrations are common;48 however, under d-DNP conditions, the dramatically increased H2O polarization will amplify conventional RD effects by orders-of-magnitude. These strong RD fields will evidently affect the water's spin dynamics; as here discussed and exemplified, such strong water RD fields will also influence the 1H NMR signals of co-dissolved solutes, leading to frequency shifts and to offset-dependent phase distortions. In addition to these RD effects, the HyperW experiment will also significantly affect the overall intensities of the co-dissolved solute signals; part of this will result, as previously reported,18,24,29,30 in large enhancements of labile solute protons that readily exchange with the hyperpolarized solvent. In addition, also non-labile protons can have their intensities changed by intermolecular cross-relaxation effects. These polarization transfer phenomena will interplay with the RD effects, leading to a non-trivial calculation of the actual signal enhancements. These and other features related to the solute's NMR in HyperW experiments are further described below – first with experimental examples, and thereafter with theoretical derivations accompanied by numerical simulations that explain these.
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2 H2O/glycerol mixture containing 10 mM 4-aminoTEMPO, to microwave irradiation for 1 h at 1.6 K. The procedure was carried out in a 3.35 T Oxford Instruments HyperSense® polarizer, using 120 mW of microwave power positioned at 94.10 GHz. The hyperpolarized pellets were dissolved with 4 mL of superheated D2O buffer, adjusted to pH 7 for the pyridine/propanol tests (aka. sample I) and to pH 3 for alanine-oriented experiments (sample II). The hyperpolarizer → NMR magnet transfer was aided by a stream of Helium gas pressurized to 10 bar, which transferred the hyperpolarized water into 5 mm NMR tubes within 8 s. Inside this 11.7 T NMR magnet, tubes with either 10 µL of 1
:
1 vol. pyridine/propanol mixture (sample I) or 150 µL of a 1 M alanine solution in D2O (pH 3, sample II) were already waiting, inside a pre-shimmed triple-resonance Prodigy® Bruker probe. The probe was maintained at room temperature (25 °C) yet the transfer lines between the Hypersense and NMR magnets were kept at ≈45 °C, to lengthen the water 1H T1 times to ≥8 s. The final volume of the solution after the hyperpolarized water injection was controlled by an Arduino-based controller,49 and set to reach a final total value of ≈470 µL. Repeated experiments indicated a net d-DNP enhancement of ca. 1200× for the water 1Hs, vs. their thermal 11.7 T counterparts.
1H NMR spectra were acquired from ca. 5 s prior to the hyperpolarized water arrival into the NMR tube, till ca. two minutes after its arrival. Acquisitions used a 500 MHz Bruker Neo console, and small-angle (3°) tip pulses calibrated and tuned on appropriate volumes of a H2O/D2O (10/90) sample; such sample was also used for a pre-dissolution shimming. Data were collected as pseudo-2D datasets with 200 free induction decays (FIDs), an acquisition time of 0.2 s per FID, a 0.4 s inter-FID delay, a spectral width of 30.12 kHz, and a spectrometer dead time of 10 µs. To avoid sweep-field correction artifacts, deuterium lock and sweep systems were deactivated during the dissolution process.
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1 vol. pyridine/propanol in 460 µL hyperpolarized water. Panel (a) presents selected full-spectral-width small-tip-angle 1H NMR spectra, illustrating the dramatic changes in linewidth that the water resonance experiences as a function of post-dissolution time. Most noticeable is this central peak's large symmetric line width, that gradually narrows in unison with a shift in the peak's maximum. Such broad line shapes are unrelated to B0 inhomogeneities (which when present were usually due to the appearance of small bubbles leading to asymmetric peaks as expected from a z2-like distortion along the main axis); instead, the exponential decay that both the width and the center of mass of the water line exhibit (Fig. 1b), are hallmarks of a RD-dominated behavior. Furthermore, the similar decay constants that are observed for these two decays and for the decay of water's overall hyperpolarization, supports a common origin for all these effects. Notice that immediately after dissolution, the water resonance exhibits a maximal shift of 400 Hz. Such large frequency excursion cannot be attributed to demagnetization fields (DFs), which for the cylinder in question should be around 35 Hz under typical HyperW conditions (see SI, Section S1). Furthermore, a DF would shift all resonances in the spectrum by a similar amount, whereas solute signals shift only by ∼40 Hz over the course of the post-dissolution. Neither can these shifts be explained by the 15 °C bulk temperature changes undergone with the water upon being ported from the polarizer to the NMR probe: when measured in “dummy” unpolarized water dissolutions, such shifts would not exceed a few tens of Hz. On the other hand, water's 400 Hz exponentially decaying shift is fully consistent with a frequency-pushing arising from RD, as further discussed in the next section.
While also showing a marked post-dissolution time dependence, the solute resonances highlighted in Fig. 1c from propanol and pyridine, resonating respectively at 0.75, 1.4, 3.4 and at 7.31, 7.73 and 8.37 ppm values, behave quite differently from the water peak (≈4.8 ppm). In the initial post-dissolution traces these solutes are virtually invisible. Within the first 5 s or so their 1H NMR signature grows, but their peaks appear out-of-phase vs the water; in fact, they show opposite phases depending on whether they resonate at higher or lower offsets vis-à-vis the water. As RD decreases sufficiently for the water peak to stop overlapping with the solutes (≈10–20 s post-dissolution) peaks still show-up magnified, but now they have evolved into a common phase; a phase that is 180° shifted from that of the water. Finally, once the water 1Hs have reached thermal equilibrium (post-dissolution times >40 s) the solutes show conventional, positively-phased, J-split absorptive line shapes (Fig. 1c, bottom).
We ascribe the unusual solute phase behavior to the effect of water's RD field acting on these protons; as further described below this will – if large enough – impart phase peak shifts depending linearly on a site's (signed) offset relative to the water resonance. Consequently, solute resonances with opposite offsets relative to the water signal will accrue phases of opposite sign for as long as RD can act on their evolution – i.e., for as long as the water line overlaps with the solute resonances. Added on top of these RD effects is an intermolecular cross-relaxation that, for the case of small molecules like the ones being here considered, will lead to a negative nuclear Overhauser enhancement (NOE) between the hyperpolarized water protons and the non-labile propanol/pyridine protons – regardless of RD effects.2,4 This NOE naturally ceases once the water spins have reached thermal equilibrium, and therefore solutes and water return to a fully positive NMR trace.
Fig. 2 presents another representative dissolution, this time for an alanine sample dissolved on hyperpolarized water. For all practical purposes, the water in these small-tip-angle experiments behaves identically as in the HyperW counterpart of Fig. 1. However, the labile amino protons in this case are enhanced much more than the non-labile methyl protons due to exchange-driven interchange with the hyperpolarized water protons, leading to a positive magnetization for the –NH3+ and to a negative NOE for the CH3. Still, since the phase-distortions imposed by water's RD effect are as in sample I, the ensuing phase distortion ends up having the same phase sign for both solute 1H signals: the enhancements of the CH3 and –NH3 magnetizations have now different signs, but so do their relative offsets vis-à-vis the water. Complicating somewhat the clear observation of this effect, is the fact that the amine protons are substantially broadened by their exchange with the water, as well as by relaxation of the second kind with the 14N. This extra broadening makes the NH3 peak nearly invisible once protons have returned to thermal equilibrium.
![]() | ||
| Fig. 2 Idem as in Fig. 1, but for 1H HyperW NMR experiments performed using alanine as the solute (sample II). | ||
In view of all this, we ascribe the main broadenings and shifts observed on the water peaks in these experiments, to RD effects. As mentioned, RD originates from feedback between the currents induced by the nuclear magnetization and the RF fields that these generate within the NMR probe detection circuit.38–47 In the lab-frame, these FID-induced magnetic fields can be expressed as:38
![]() | (1) |
Here µ0 is permeability of free space; η is the coil filling factor; Q is the quality factor of the receiving LC-circuit;
is a parameter defining the miss-tuning of the receiving circuit, with ω and ωLC being the spins Larmor and the probe's LC-circuit resonance frequencies, respectively; ψ = arctan (ΔLC) is a phase that the RD-induced field develops because of this miss-tuning; and the linearly polarized receiving coil is supposed to be aligned along the
x-axis (perpendicular to B0). The RD field in eqn (1)38 will act back on the spins, with a torque given by an angular rate constant RRD = λRDMz, where Mz is the magnitude of the z-magnetization at the time of excitation, and
. When this feedback field is included, the resulting rotating-frame Bloch equations become:52
![]() | (2) |
For a perfectly tuned probe ψ = 0;†
RD will then remain orthogonal to the transverse magnetization M⊥, acting like a soft RF pulse which nutates the magnetization back to the z-axis (Fig. 3a). As this reduces the transverse magnetization,39 RD is usually associated to a rapid FID transverse decay whose angular rate given by
– even if, unlike T2, this “rate” will not lead to a constant exponential function as its effects depend on the excitation and on the instantaneous tilt angle.53 This notwithstanding RRD gives an idea of the strength of RD effects; for typical probe filling factors η (0.0744)and cryoprobe quality Q factors (600–70044,45), the expected value under the HyperW conditions and small-pulse excitation described above should be
![]() | (3) |
RD can thus broaden the water signal into the 10 ppm range observed in Fig. 1 and 2, clearly dominating over DF effects.
The phase shift ψ in the equations above will be different from zero if the probe is slightly detuned; i.e., if there is a difference between the water Larmor and the maximal induced current impedance frequencies. This will move
RD away from orthogonality vis-à-vis
⊥ = Mx + iMy, leading to so-called “cavity pushing” effects45,54 which manifest as M-dependent frequency shifts of the signal. Indeed, in a Bloch-sphere rotating frame picture, RD-induced rotations will then occur around
RD fields that are no longer orthogonal to
⊥, producing an additional, time-dependent effective rotation around the z-axis (Fig. 3). Notice that owing to the metastable nature of d-DNP experiments, these “pushing” effects will not be constant throughout the HyperW post-dissolution series, but rather diminish with the decaying magnetization.
The aforementioned RD-based arguments explain, via the hyperpolarization-dependent post-dissolution RRD values, most of the exponentially decaying water line widths and shifts summarized in Fig. 1b and 2b. However, obtaining a more perfect fit between these expectations and the results presented in Fig. 1 and 2, required invoking additional factors. These included the aforementioned, magnetization-dependent demagnetizing field and time-dependent water-cooling effects, which were accounted as described in more detail in the SI Section S1. Also in need of accounting was the fact that, given the strong RD effects arising in HyperW experiments, the loss of the initial part of the FID as imposed by the spectrometer's dead time, strongly influenced the apparent signal enhancement – and therefore the quantitation of the water signal as a function of time. Indeed, given a characteristic decay time (RRD)−1 ≈ 60 µs, a spectrometer dead time of ≈10 µs meant that ≈20% of the signal was effectively lost by the time of the data acquisition. These losses accounted for the non-exponential behavior that had been previously noted for integral-derived estimations of the post-dissolution HyperW enhancements;18,42,55 the data in Fig. 1 and 2 also show similar non-exponential apparent decays for the water hyperpolarization. Fig. 4 shows the increased initial water enhancements, arising when extrapolating back the best-fits of the hyperpolarization decay emerging from longer (≥10 s) post-dissolution times. These increased enhancements reflect the fact that the initial post-dissolution scans are subject to larger RD-induced polarization decay rates RRD, and hence so are their signal losses during the spectrometer's dead time. As the hyperpolarization decays and RD effects become smaller so do dead-time related losses, until eventually becoming negligible. To ensure quantitative accuracy, the influence of the spectrometer dead time therefore had to be explicitly accounted for.
![]() | ||
| Fig. 4 Experimental and back-extrapolated enhancements observed for water in Fig. 1 and 2, as a function of post-dissolution time. Blue circles account for a 10 µs dead-time correction of the water enhancements, as derived from the water line-shape simulations in Fig. 5. | ||
With all these provisions, numerical simulations based on eqn (2) could reproduce the experimental water line shape well (Fig. 5). The fitting parameters that these Bloch model required for recapitulating the examples in Fig. 1 and 2 included DNP enhancements of 1170 and 680, and ψ values of 10.2° and 11.5°, respectively. Achieving the close agreement between expectations and experiments shown in Fig. 5, also called for an unexpected, ≈2% variation of |λRD| over the initial (≈ 6 s) post-dissolution periods. This variation was modeled as‡
![]() | (4) |
![]() | ||
Fig. 5 Experimental and simulated water data corresponding to the dissolutions shown in Fig. 1 (left) and Fig. 2 (right). Experimental and simulated plots are shown as heatmap (top) and spectra (bottom). In the latter, simulated spectra (lines) are superimposed on experimental data (circles, shown sparsely every 90 points), and are displayed for post-dissolution times starting at 0.6 s, and with 2.4 s interval. | ||
![]() | (5a) |
![]() | (5b) |
, and superscripts w, s denote the water and solute spins, respectively.
Given that the solute magnetization is much smaller than that of water, Msz/Mwz ≪ 1, eqn (5) will contain very rapidly and more slowly decaying terms. For instance −δ·Mw+ and
will induce an initial fast decay, but their influence on the precessing Ms+ solute FID which originate the peaks in Fig. 1 and 2 can, to zero order be neglected. In fact, to 0th order, only the dominant RD term acting on the water magnetization and the usual precession of Ms+ matter. To such order, eqn (5) can be solved to retrieve these two transverse magnetizations as
| Mw+(t) = Mw+(0)e−δ·t | (6a) |
| Ms+(t) = Ms+(0)eiΔωt | (6b) |
To first order, however, the solute signal also experiences the effect of the RD-active magnetization via the
term: this represents a perturbation caused by water's RD on the solute. Conversely, assuming all experiments were done with small-tip-angle but broadband pulses, the ensuing
relation means that Mw+(0)Msz ≈ Ms+(0)Mwz; i.e., that also the
term may provide a contribution to the detected Ms+ to the same order. To derive such potential higher-order effects we look for general solutions of a first-order-revised version of eqn (5b):
![]() | (7) |
This can be solved using a Green-function expansion
![]() | (8a) |
![]() | (8b) |
![]() | (8c) |
![]() | (9) |
![]() | (10) |
Disregarding again the fast-decaying e−δt terms in eqn (10) and collecting all the terms that in eqn (8) and (10) contribute to a solute precession frequency Δω, yields after some algebra to
![]() | (11) |
It follows from this expression that the phase of the observed solute signal is determined by a product of the evolving magnetization times a complex factor
, that will impart on the solute peaks phase distortions vs. a conventionally phased purely-absorptive peak, of
. Thus, if the peak offset exceeds the effects of the RD-broadened water
, the phase distortion will be negligible; otherwise, the phase distortions of the solute peaks will be sizable, and have opposite signs on either side of the water peak. Fig. 6 presents simulations that, based on this analytical description and utilizing the values of λRD and Mw enhancement obtained in the previous Paragraph, are expected for the various solutes introduced in Fig. 1 and 2. Notice that these simulations kept fixed the offsets and the absolute magnitudes of the solute magnetizations, and attention was solely focused on predicting solute peak phases as a function of solvent hyperpolarization. Notice that these simulations also include one of glycerol's 1H peaks which, despite arriving at the sample with a positive hyperpolarization, exhibits an inverted phase that generates “a hole” in water's RD-broadened peak, at the early post-dissolution stages. This transient phase inversion might be misassigned as negative glycerol polarization, yet is in fact consequence of the phase distortions introduced by water's RD effects, superimposing on a broadened water resonance.
![]() | ||
| Fig. 6 Experimental (top) vs. analytically predicted (bottom) spectra focusing on the solute resonances appearing in Fig. 1 and 2. Analytical spectra were calculated based on eqn (11) after applying an apodization of 40 Hz. Solute magnetizations M were considered positive or negative as per exchange or NOE transfers from the hyperpolarized water (solutes) or from the direct hyperpolarization process (alanine's –NH3+ plus glycerol peak at ≈3.6 ppm). See text for further details. | ||
Notice that in addition to phase distortions, solutes dissolved in hyperpolarized water show changing 1H peak intensities, which vary non-monotonically with post-dissolution time. These intensity changes also originate in water's time-dependent RD effects, as can be appreciated from theoretical expectations that only considered such effects (Fig. 6, bottom). Indeed, in a similar way as RD shortens water's transverse magnetization lifetime, water-derived RF fields will also suppress the lifetimes associated to solute's transverse magnetizations that fall within water's line width. Solute signal intensities will thus progressively increase and sharpen as water's hyperpolarization decays. For similar reasons, solute signal intensities increase and sharpen progressively as a solute's resonance moves away from the water frequency.
In addition to these RD-derived effects, solute intensities will also be influenced by magnetization transfers from the hyperpolarized water via intermolecular NOEs for the non-labile solute protons, and via chemical exchanges for the labile ones. As the solutes involved are small molecules, NOEs will induce negative magnetization enhancements for a positive water hyperpolarization (i.e., for propanol aliphatic and pyridine protons in Fig. 1, and for alanine's methyl in Fig. 2), while alanine's NH3 signal will undergo positive – and, depending on the pH, more significant – polarization transfers as driven by water chemical exchanges. Unfortunately, an accurate quantitative interpretation of these absolute signal intensity changes is limited by data processing and experimental constraints. Data processing-wise, the accurate integration of the weak solute signals is hampered by the changing baselines arising from the much more intense hyperpolarized water resonance. At an experimental level, the solutes’ mixed phase line shapes coupled to receiver deadtime effects, further complicate the analyses. Consequently, parameters related to enhancements, cross-relaxation, and chemical exchange rates could only be extracted from solute signal integrals at semi-quantitative levels.
To proceed with the solute intensity quantification, Gaussian best fits were first made to the overall water line shape, and these were used as baseline for calculating the solute's post-dissolution intensities (see SI Section S3 for further details). Thereafter, the aforementioned RD-induced phase and intensity distortions affecting the solute signals were compensated, using a correction corresponding to the inverse magnitude of the prefactor in eqn (11):
![]() | (12) |
With these provisions at hand, analyses of the post-dissolution solute signal intensities in the spectra introduced in Fig. 1 and 2, led to the data points (circles) illustrated in Fig. 7. These data points were then fitted with classical Bloch–McConnell–Solomon equations relating the z-magnetizations of the water and solute protons
![]() | (13) |
![]() | ||
| Fig. 7 Experimentally observed (circles) and best-fit enhancements (lines) deriving from the results obtained for sample I and sample II in the dissolution experiments shown in Fig. 1 and 2, after accounting for RD-driven amplitude and phase distortions (eqn (12)) and then solving eqn (13). | ||
Based on these relations, the best fits of the water and solute (labile and nonlabile) signals introduced in Fig. 1 and 2, were obtained as summarized in Fig. 7. For the NOE-mediated transfer, non-labile protons in all samples exhibit weak intermolecular cross-relaxation rates from the hyperpolarized water – with values of ∼0.5 × 10−4 s−1 and ∼2 × 10−4 s−1 for propanol's and pyridine's protons, respectively, and of ∼1.1 × 10−4 s−1 for alanine's methyl group. These values are comparable to reported heteronuclear 19F–1H intermolecular NOE rates,21 as could be expected from 1H–1H intermolecular NOEs happening under comparable conditions. Alanine's NH3 signal exhibited ca. 100-fold larger enhancements than the non-labile protons, arising from direct exchanges with the hyperpolarized water. Best fit of alanine's NH3 enhancements resulted in an exchange rate kex ≈ 17 s−1; to further characterize this, complementary measurements on the same sample performed using chemical exchange saturation transfer (CEST) resulted in an exchange rate kex ≈ 20 s−1 (SI, Section S3). Both of these values are consistent with previously reported exchange rates for alanine under comparable experimental conditions;56 see Supporting Information for further details regarding these fits.
The present study focused on line shapes arising from short, single-pulse 1D 1H NMR acquisitions. However, also other experiments can be significantly affected by RD effects in hyperpolarized systems. A large body of recent research has focused on hyperpolarized metastable states leading to spontaneous, pulse-free maser-like emissions;58,59 gradient applications on hyperpolarized systems can also lead to chaotic dynamics in simple one-pulse acquisitions.60 These are all interesting instances where RD-mediated interactions between solutes and hyperpolarized water, remain to be researched. Another significant area waiting to be explored involves 2D homo- and heteronuclear HyperW experiments, where hitherto neglected effects like those described in this study are also expected to arise. Also the use of selective excitation pulses may result in an additional suppression or enhancement of solute signals due to the RD field, and therefore to exacerbate or attenuate the effects here described. Complex RD interactions are also expected when applying dissolution DNP on systems more complicated than water, where multiple chemically inequivalent sites might couple to one another non-linearly via the receiving circuit. We have also found that rapid repetitive pulsing along the lines often used in hyperpolarized NMR imaging acquisitions,61,62 may also elicit interesting RD-related effects. Investigations on some of these interesting phenomena will be reported in an upcoming publication.
The raw data are available from the corresponding author upon reasonable request.
Footnotes |
| † In ref. 52 ψ is the angle between the feedback field and the transverse magnetization, whereas here it is being used as a phase related to the detuning. Both are simply related by a 90° difference. |
| ‡ Also the phase ψ should show changes upon dissolution; however, to first order these can be included in a redefinition of the λ0. |
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