Quadrupolar solid-state NMR carries a wealth of structural information, including insights about chemical environments arising through the determination of local coupling parameters. Current methods can successfully resolve these parameters for individual sites using sample-spinning methods techniques applicable to quadrupolar I ≥ 1 nuclei, provided second-order central transition broadenings do not exceed by much the spinning rate. For large quadrupolar coupling (C Q) values, however, static acquisitions are often preferable, leading to challenges in extracting local structural information. This study explores the use of two-dimensional QUadrupolar Isotope Correlation SpectroscopY (QUICSY) experiments as a means to increase the NMR spectral resolution and enrich the characterization of quadrupolar NMR patterns under static conditions. QUICSY seeks to correlate the solid-state NMR powder line shapes for two quadrupolar isotopes belonging to the same element via a 2D experiment. In general, two isotopes of the same element will have different nuclear quadrupole moments, gyromagnetic ratios, and spin numbers but essentially identical chemical environments. The possibility then arises of obtaining sharp "ridges" in these 2D correlations, even in static samples showing large quadrupolar effects, which lead to second-order line shapes that are several kilohertz wide. Moreover, pairs of quadrupolar isotopes are recurrent in the periodic table and include important elements such as 35,37Cl, 69,71Ga, 79,81Br, and 85,87Rb. The potential of this approach is explored theoretically and experimentally on two rubidium-containing salts: RbClO4 and Rb2SO4. We find that each compound gives rise to distinctive 2D QUICSY line shapes, depending on the quadrupolar and chemical shift anisotropy (CSA) parameters of its sites. These experimental line shapes show good agreement with analytically derived 2D spectra relying on literature values of the quadrupolar and CSA tensors of these compounds. The approach underlined here paves the way toward better characterization of wideline NMR spectra of quadrupolar nuclei possessing different nuclear isotopes.
Quadrupolar solid-state NMR carries a wealth of structural information, including insights about chemical environments arising through the determination of local coupling parameters. Current methods can successfully resolve these parameters for individual sites using sample-spinning methods techniques applicable to quadrupolar I ≥ 1 nuclei, provided second-order central transition broadenings do not exceed by much the spinning rate. For large quadrupolar coupling (C Q) values, however, static acquisitions are often preferable, leading to challenges in extracting local structural information. This study explores the use of two-dimensional QUadrupolar Isotope Correlation SpectroscopY (QUICSY) experiments as a means to increase the NMR spectral resolution and enrich the characterization of quadrupolar NMR patterns under static conditions. QUICSY seeks to correlate the solid-state NMR powder line shapes for two quadrupolar isotopes belonging to the same element via a 2D experiment. In general, two isotopes of the same element will have different nuclear quadrupole moments, gyromagnetic ratios, and spin numbers but essentially identical chemical environments. The possibility then arises of obtaining sharp "ridges" in these 2D correlations, even in static samples showing large quadrupolar effects, which lead to second-order line shapes that are several kilohertz wide. Moreover, pairs of quadrupolar isotopes are recurrent in the periodic table and include important elements such as 35,37Cl, 69,71Ga, 79,81Br, and 85,87Rb. The potential of this approach is explored theoretically and experimentally on two rubidium-containing salts: RbClO4 and Rb2SO4. We find that each compound gives rise to distinctive 2D QUICSY line shapes, depending on the quadrupolar and chemical shift anisotropy (CSA) parameters of its sites. These experimental line shapes show good agreement with analytically derived 2D spectra relying on literature values of the quadrupolar and CSA tensors of these compounds. The approach underlined here paves the way toward better characterization of wideline NMR spectra of quadrupolar nuclei possessing different nuclear isotopes.
The
NMR of solids provides a valuable understanding of the local
structure and dynamics of a broad range of inorganic and biological
materials. Half-integer quadrupolar nuclei provide essential probes
in these characterizations as they constitute the majority of the
NMR-active elements[1] and make up key materials
including biominerals, glasses, ceramics, and solid electrolytes;
quadrupolar I ≥ 1 species are often also at
the reactive centers of biochemical events.[2,3] The
NMR of these species is often dominated by the quadrupolar interaction,
arising from the electrostatic coupling between the quadrupolar moment
of these nuclei and an electric field gradient (EFG). The EFG is defined
by the electronic environment surrounding the species in the solid;
it carries rich structural information and is highly sensitive to
changes in local atomic environments.[1,2,4] Besides these advantages, quadrupolar effects can
bring about substantial anisotropic broadenings, challenging the elucidation
of NMR spectra on polycrystalline samples and precluding a clear interpretation
of overlapping patterns in the presence of multiple chemical sites.
For this reason, quadrupolar NMR is often circumscribed to half-integer I ≥ 3/2 spins, which presents a relatively narrow
central transition (CT). These −1/2 ↔ +1/2 CTs will
be solely affected by quadrupolar broadenings up to the second order,
yielding linewidths of the order of CQ2/ω0, where CQ is the quadrupolar coupling constant and ω0 is the spin’s Larmor frequency.
As second-order effects can challenge the acquisition of solid-state
quadrupolar NMR spectra numerous routes to improve the interpretation
and resolution of CT spectra have been developed. These include methods
that rely on multiple sample-spinning axes[5−9] as well as on fixed spinning at the magic angle of
54.7°, but call for 2D correlations between central and multiple-quantum
(MQMAS) or between central and satellite (STMAS) transitions.[10−14] Although these experiments are widely used to study materials,[2,11−15] they may still fail when tackling quadrupolar sites characterized
by large C values, particularly
when the CT second-order broadenings are so large that they substantially
exceed the rates of MAS sample spinning. Species characterized by
a large CQ are therefore best measured
under static, low-resolution conditions,[16−19] thus preventing the sensitivity
losses associated with MQMAS/STMAS as well as the numerous overlapping
spinning sidebands that may otherwise arise. Approaches to discern
quadrupolar-broadened sites under static conditions have thus been
discussed based on variable-field acquisitions[20] and on differing nutation behaviors;[21] the use of multi-quantum 2D correlations to enrich the
information of static NMR has also been explored.[22] This study discusses an alternative route based on 2D correlations.A common characteristic of spinning-based 2D NMR experiments used
for resolving quadrupolar second-order powder patterns is a reliance
on two consecutive periods where spins are subject to anisotropic
evolutions that are, in some way, “proportional” to
one another for every crystallite in the sample. It is owing to this
proportionality that echoes refocusing the residual quadrupolar broadening
arise in the (t1, t2) time domain. In dynamic-angle spinning,[8,9] a
judicious choice of the two different spinning axes and evolution
times imparts a proportionality that aligns the various CT powder
line shapes along (F1,F2); in MQMAS and STMAS experiments, the proportionality
arises from Clebsch–Gordan coefficients, which make the evolution
of the anisotropies left over by the MAS proportional to one another
for every crystallite in the powder. Similarly, this study was motivated
by the realization that a certain “proportionality”
between the anisotropic quadrupolar broadenings could be imposed if
correlations were performed among CTs of different isotopes of the
same element: quadrupolar second-order shifts in such isotopes will
be given by EFG properties that are virtually independent of the nature
of the isotope, modulated by orientation-independent scalar parameters,
i.e., gyromagnetic ratios, spin numbers, and nuclear quadrupole moments,
which scale the strength of the interaction. In such cases, the possibility
could arise of yielding one-to-one correlations for the CT frequencies
of every crystallite in a powder so as to arrive at high-resolution
2D correlations even in the absence of MAS. On the other hand, in
the presence of multiple magnetically or crystallographically (chemically)
inequivalent sites, such powdered 2D correlations should feature off-diagonal
peaks containing rich information. Moreover, quite a few elements
in the periodic table possess two quadrupolar isotopes in relatively
high abundances, including 35,37Cl, 69,71Ga, 79,81Br, 63,65Cu, 135,137Ba, and 85,87Rb; out of these, halogens are often present in active
pharmaceutical ingredients,[23,24] whereas species such
as Ga are present in semiconductors and metal–organic frameworks.[25,26]Based on such considerations, the present study explores static
NMR versions of what we denominate as QUadrupolar Isotope Correlation
SpectroscopY (QUICSY), a 2D experiment correlating the CTs of different
quadrupolar isotopes of the same element. To this end, we treat a
number of theoretical scenarios pertaining to static spectra acquired
on nuclei broadened by second-order quadrupolar effects: first in
the absence and then in the presence of the chemical shift interaction.
Following these considerations, we explore the static 2D QUICSY approach
on the isotope pair 85Rb and 87Rb for compounds
bearing one and two chemically inequivalent crystallographic sites.
For each case, a unique pattern is achieved containing rich information
regarding the interaction tensors and their relative orientations.
The experimental results arising from these considerations matched
well with analytical 2D calculations based on existing literature
parameters, validating the use of theoretical arguments to estimate
the benefits and insight arising from this approach.
Materials and Methods
Samples
Polycrystalline
RbClO4 and Rb2SO4 (Strem Chemicals,
99.9%)
were used as received, after grinding them into fine powders and packing
into 4 mm zirconia NMR rotors, for measurement under static conditions.
In these samples, the natural abundance of 85Rb is 72.17%
and that of 87Rb is 27.83%.
Solid-State
NMR Spectroscopy
NMR
experiments were performed using a Varian VNMRS console interfaced
to an Oxford 14.1 T (ω0(1H) = 600 MHz)
wide-bore magnet. A Varian 4 mm triple-resonance HXY probe was used
for this study, with the X and Y channels tuned to the high- and low-frequency-correlated
isotopes, respectively. Chemical shift referencing was performed for 87Rb and 85Rb using a dilute RbNO3 solution.
Pulse-width calibrations were performed on solid RbBr: directly for 87Rb and indirectly for 85Rb, which was calibrated
via its cross-polarization (CP) to 87Rb. All used sequences
relied on such 85Rb → 87Rb CPs and included
either a 1D CP[27,28] with Carr–Purcell–Meiboom–Gill
(CPMG) acquisition[29−33] or 2D constant-time[34−36] CP-CPMG with whole-echo acquisition for an absorptive
line shape.[37,38] The phase-cycling used for the
1D CP-CPMG was as follows: ϕ1 = x,–x, ϕ3 = y, ϕ4 = x,x,–x,–x,y,y,–y,–y,
ϕ4 = x,–x,x,–x,y,–y,y,–y, and ϕrec = ϕ1 + ϕ4 = x,–x,–x,x,y,–y,–y,y. The phase-cycling of the 2D constant-time CP-CPMG was altered to
select a single CT-detected evolution pathway in the indirect dimension:
ϕ1 = x,y,–x,–y, ϕ2 = 4*{x}, 4*{y}, 4*{−x}, 4*{−y}, ϕ3 = 16*{x}, 16*{y}, 16*{−x}, 16*{−y}, ϕ4 = x, ϕ5 = x, and ϕ = ϕ1 – 2ϕ2 + ϕ3. In all cases, a converging double-frequency
sweep (DFS) pulse was applied on the 85Rb channel prior
to the 85Rb → 87Rb CP for signal enhancement,[55,56] with the following parameters: 1.9 ms duration; initial/final frequencies
(from the CT center): 6600/200 kHz; number of steps: 27,000; and RF
amplitude: 20 kHz. The same DFS parameters were used for both Rb2SO4 and RbClO4. For processing the 2D
CP-CPMG QUICSY data, CPMG echoes were spliced and co-added in the
direct dimension. Unless otherwise specified, a symmetric whole echo
was also collected in the t1-domain. As
no dispersive component arises from such fully t1/t2 echoed acquisitions, all 2D
data are presented in the magnitude mode. No line-broadening was added,
and a zero-filling of 2048 points in F2 and 512 points in F1 was used. For more
details, see the following text and Supporting Information.
Simulations
All
calculations/simulations
focused on the CT of half-integer quadrupolar nuclei. Analytical calculations
to describe 2D correlation spectra of two isotopes affected by second-order
quadrupolar interactions and by isotropic/anisotropic chemical shifts
(CSA) were coded in MATLAB. All of these 2D spectral calculations
assumed ideal correlations among the evolution frequencies of the
two isotopes for each crystallite orientation: i.e., equal efficiencies
for the information transferred during the mixing. The orientation-dependent
CSA effects were calculated on powdered samples by first transforming
their tensors from a CSA principal axis system (PAS) to the PAS of
the EFG tensor and then onto the laboratory frame. In the case of
two or more magnetically inequivalent sites per crystallographic unit,
an additional transformation was added to relate the PAS of one of
the EFG tensors to the PAS of the other EFG tensor. All transformations
and conventions used are described in the Appendix. The full expressions of the orientation dependencies were calculated
with Mathematica,[39] and the accuracy of
these lab-written codes was verified by comparisons against 1D numerical
simulations arising from the Simpson[40] programming
software (not shown). Throughout the text and the Supporting Information, frequency-based calculations were
used; for comparisons with the experimental data, equivalent time-domain
calculations were performed to obtain comparable spectral resolutions
upon processing. All MATLAB scripts are available upon request; the
Mathematica scripts used in this study can also be found in the Supporting Information.
Theoretical Background
This study considers two different
isotopes of the same element;
each of these is a half-integer quadrupolar species described by a
distinct spin I, gyromagnetic ratio γ defining
both the Larmor frequency ωo and the chemical shift
ωcs, and nuclear quadrupole moment eQ. Disregarding isotope effects, one can assume that for a certain
compound, these two isotopes will be subject to identical surroundings,
and thus their EFG and shielding anisotropy will, for a given magnetically
and chemically equivalent site, be the same. In consequence, for a
given crystallite orientation, the Hamiltonians of the two isotopes
will be affected by the same orientation-dependent terms.[41] Their difference will thus be given by eQ and γ-driven scalings of their quadrupolar and
chemical shift frequencies, respectively. Figure presents a number of scenarios that will
then arise when considering 2D QUICSY correlations, taking the 85Rb and 87Rb isotopes as prototypical examples.
In these cases, the correlated frequencies will be given by the orientation-dependent
frequency of each isotope’s central transitionwhere the second-order quadrupolar shift is
given by[42] (see Appendix)and the chemical shift is
represented as[41,43,44]In these
equations, α and β are
Euler angles that define the orientation of the static magnetic field
in the PAS of the EFG tensor. The CSA and quadrupolar interaction
tensors need not be coincident and, in general, will have their respective
PASs related by Euler angles ((ψ,χ,ξ); see Appendix for more details). For sites that are
affected solely by a quadrupolar interaction (ωCS = 0), the result of such an inter-isotope correlation would be a
narrow ridge, even for a powder pattern (see Figure a). The proportionality constant between
the second-order quadrupolar effects of the correlated CTs will dictate
the slope of the ensuing ridge; on the basis of eq , it will beHere, the subscripts 1 and 2 denote the two
isotopes being correlated, assumed in Figure to involve 87Rb and 85Rb, respectively. Adding an isotropic chemical shift does not affect
the high resolution of these correlations but only shifts the ridge
in both dimensions (Figure b). Under these premises, multiple sites with different isotropic
chemical shifts could in principle still be resolved. The addition
of a collinear, axially symmetric chemical shift anisotropy interaction
alters the proportionality between the F1 and F2 frequencies over the powder;
yet, as long as ηQ is close to zero, the correlation
retains a narrow parabola-like contour (Figures c and S1). Upon
considering axially asymmetric and noncoincident quadrupolar/CSA tensors,
however, the nature of the 2D correlation is further altered and the
narrow ridge becomes broader, with the exact shape of this contour
containing a wealth of information regarding the coupling parameters. Figure d depicts such a
line shape for a case based on RbClO4;[45] the contour’s dependence on the relative orientation
and symmetry of the two interaction tensors is further illustrated
in Supporting Figure S1.
Figure 1
Calculated 2D QUICSY
spectra of a single site affected by either
a second-order quadrupolar interaction alone (a) or by both chemical
shift and quadrupolar interactions (b–d). (a) 2D QUICSY for
an 85Rb/87Rb isotope pair subjected solely to
a quadrupolar interaction with CQ = 3.3
MHz and ηQ = 0.21 for 87Rb (ω0 = 196.26 MHz). The CQ of 85Rb was scaled by the ratio of quadrupole moments of the nuclei.[41] (b) The same as in panel (a) but upon introducing
an isotropic chemical shift δiso = −13.7ppm.
(c) The same as in panel (b) but upon introducing a CSA with δaniso = −13.8 ppm. The CSA tensor is collinear with
the quadrupolar tensor and is axially symmetric, i.e., ηCS = 0. (d) The same as in panel (c) but for a non-coincident
CSA tensor with ηCS = 0.61, ψ = 94°, χ
= 28°, and ξ = 87° (i.e., the literature-given quadrupole
and chemical shift anisotropy parameters of RbClO4[45,46]). The insets depict pictorially the relative orientation of the
PAS of the quadrupolar tensor (brown ellipsoid) and the CSA tensor
(green ellipsoid).
Calculated 2D QUICSY
spectra of a single site affected by either
a second-order quadrupolar interaction alone (a) or by both chemical
shift and quadrupolar interactions (b–d). (a) 2D QUICSY for
an 85Rb/87Rb isotope pair subjected solely to
a quadrupolar interaction with CQ = 3.3
MHz and ηQ = 0.21 for 87Rb (ω0 = 196.26 MHz). The CQ of 85Rb was scaled by the ratio of quadrupole moments of the nuclei.[41] (b) The same as in panel (a) but upon introducing
an isotropic chemical shift δiso = −13.7ppm.
(c) The same as in panel (b) but upon introducing a CSA with δaniso = −13.8 ppm. The CSA tensor is collinear with
the quadrupolar tensor and is axially symmetric, i.e., ηCS = 0. (d) The same as in panel (c) but for a non-coincident
CSA tensor with ηCS = 0.61, ψ = 94°, χ
= 28°, and ξ = 87° (i.e., the literature-given quadrupole
and chemical shift anisotropy parameters of RbClO4[45,46]). The insets depict pictorially the relative orientation of the
PAS of the quadrupolar tensor (brown ellipsoid) and the CSA tensor
(green ellipsoid).When approaching systems
with multiple chemical sites (Figure a), the situation
becomes more complex as both same-site and inter-site correlations
are possible. Same-site correlations refer to situations where the
cross-peaks between the different isotopes arise from a single magnetically
(and thereby chemically) equivalent site in the unit cell. Although
such same-site correlations will still retain a high resolution (Figure b), isotopological
correlations among inequivalent sites will not preserve the high resolution.
They will, however, lead to distinctive patterns containing potentially
valuable information about the quadrupolar and CSA components of each
site as well as the tensors of the two sites (Figure b,d). The probability of all of these correlations
is expected to scale according to the dipolar interaction strength
among the sites, scaled by the polarization transfer efficiency between
the two isotopes.
Figure 2
Calculated 2D QUICSY spectra of two crystallographic sites
inspired
by Rb2SO4. (a) Orthorhombic structure of Rb2SO4 (space-group Pnam(47)), with the Rb atoms displayed in brown and marked
as Rb1 or Rb2 to describe the two Rb sites, oxygen atoms in light
pink, and S atoms in yellow (image generated with the VESTA program[48]). (b) 2D QUICSY for two 85Rb/87Rb pairs, characterized by intrasite correlations: Rb1–Rb1
and Rb2–Rb2. The two sites are affected by the quadrupolar
interaction and isotropic chemical shift of the following parameters
for 87Rb: CQ,1=2.72 MHz, ηQ,1 = 0.93, δ = 42.6
ppm; CQ,2=5.29 MHz, η = 0.12, δiso,2 = 15.5 ppm. (c)
2D QUICSY including same and inter-site correlation terms between
the two sites, with equal probabilities: Rb1–Rb1, Rb1–Rb2,
Rb2–Rb1, and Rb2–Rb2. (d) The same as in panel (c) but
with the addition of the following CSA parameters: δaniso,1 = 2.7 ppm, ηCS,1 = 0.26, ψ1 =
76°, χ1 = 17°, ξ1 = 110°;
δaniso,2 = −25 ppm, ηCS,2 = 0.54, ψ2 = 9°, χ2 = 37°,
and ξ2 = 270°. The parameters taken are based
on the literature values of Rb2SO4.[45,49]
Calculated 2D QUICSY spectra of two crystallographic sites
inspired
by Rb2SO4. (a) Orthorhombic structure of Rb2SO4 (space-group Pnam(47)), with the Rb atoms displayed in brown and marked
as Rb1 or Rb2 to describe the two Rb sites, oxygen atoms in light
pink, and S atoms in yellow (image generated with the VESTA program[48]). (b) 2D QUICSY for two 85Rb/87Rb pairs, characterized by intrasite correlations: Rb1–Rb1
and Rb2–Rb2. The two sites are affected by the quadrupolar
interaction and isotropic chemical shift of the following parameters
for 87Rb: CQ,1=2.72 MHz, ηQ,1 = 0.93, δ = 42.6
ppm; CQ,2=5.29 MHz, η = 0.12, δiso,2 = 15.5 ppm. (c)
2D QUICSY including same and inter-site correlation terms between
the two sites, with equal probabilities: Rb1–Rb1, Rb1–Rb2,
Rb2–Rb1, and Rb2–Rb2. (d) The same as in panel (c) but
with the addition of the following CSA parameters: δaniso,1 = 2.7 ppm, ηCS,1 = 0.26, ψ1 =
76°, χ1 = 17°, ξ1 = 110°;
δaniso,2 = −25 ppm, ηCS,2 = 0.54, ψ2 = 9°, χ2 = 37°,
and ξ2 = 270°. The parameters taken are based
on the literature values of Rb2SO4.[45,49]Even when dealing with chemically
identical sites, crystallographic
symmetry operations such as reflections or glide planes may still
lead to magnetically inequivalent sites; this is illustrated for the
RbClO4 unit cell in Figure a.[45,50−52] Here, all four
Rb atoms in the unit are crystallographically equivalent, but they
are composed of two pairs of magnetically inequivalent Rb atoms related
by glide planes perpendicular to the a and c crystallographic axes.[45] It
follows that two different orientation-dependent frequencies are present
per single crystallite orientation, leading to single-site QUICSY
correlations such as the one shown in Figure b. It should be noted that the relative orientations
of the CSA and quadrupolar tensors remain the same for the two magnetically
inequivalent sites since both tensors are related by the same symmetry
operations.[45] The ensuing correlations
will contain in this case a redundancy regarding the relative orientation
of the quadrupolar tensors of the chemically identical yet magnetically
inequivalent sites, of the type that typically arises in single-crystal
NMR measurements.[50] Even further features
will arise if chemically as well as magnetically inequivalent sites
are present in the unit cell, as illustrated in Figure c.
Figure 3
Calculated 2D QUICSY spectra of magnetically
inequivalent sites
inspired by RbClO4. (a) Orthorhombic structure of RbClO4 (space-group Pnma(53)), with the Rb atoms displayed in brown, oxygen atoms in light pink,
and Cl atoms in green (image generated with the VESTA program[48]). Pairs of crystallographically equivalent yet
magnetically inequivalent Rb atoms are related by glide planes (shown
in light blue); the NMR tensors of these sites are related by a symmetry
operation. (b, c) Analytical calculations of 2D correlation experiments
between 85Rb and 87Rb with two magnetically
inequivalent sites for each crystallographic site. (b) 2D spectrum
of a crystallographic unit consisting of two magnetically inequivalent
sites, with a relative orientation of ϕ = −112°,
κ = 103°, and ζ = 24° based on the single-crystal
data of RbClO4.[45] Other NMR
parameters are identical to those shown in Figure d. (c) 2D spectrum with two crystallographic
sites, each of them consisting of two magnetically inequivalent sites
with relative orientations of ϕ1 = 84°, κ1 = 174°, and ζ1 = −100°
and ϕ2 = 39°, κ2 = 43°,
and ζ2 = 97°, based on the single-crystal data
of Rb2SO4 (see Appendix for details of the calculation).[45] Other
NMR parameters are as shown in Figure d.
Calculated 2D QUICSY spectra of magnetically
inequivalent sites
inspired by RbClO4. (a) Orthorhombic structure of RbClO4 (space-group Pnma(53)), with the Rb atoms displayed in brown, oxygen atoms in light pink,
and Cl atoms in green (image generated with the VESTA program[48]). Pairs of crystallographically equivalent yet
magnetically inequivalent Rb atoms are related by glide planes (shown
in light blue); the NMR tensors of these sites are related by a symmetry
operation. (b, c) Analytical calculations of 2D correlation experiments
between 85Rb and 87Rb with two magnetically
inequivalent sites for each crystallographic site. (b) 2D spectrum
of a crystallographic unit consisting of two magnetically inequivalent
sites, with a relative orientation of ϕ = −112°,
κ = 103°, and ζ = 24° based on the single-crystal
data of RbClO4.[45] Other NMR
parameters are identical to those shown in Figure d. (c) 2D spectrum with two crystallographic
sites, each of them consisting of two magnetically inequivalent sites
with relative orientations of ϕ1 = 84°, κ1 = 174°, and ζ1 = −100°
and ϕ2 = 39°, κ2 = 43°,
and ζ2 = 97°, based on the single-crystal data
of Rb2SO4 (see Appendix for details of the calculation).[45] Other
NMR parameters are as shown in Figure d.
Results
and Discussion
Figure presents
pulse sequences developed to test the 2D QUICSY correlation experiment.
To tune the experiment, a 1D CP-CPMG sequence (Figure a) was utilized to find the optimal DFS pulse,[54−56] and good CP matching conditions linking the CTs of the two Rb isotopes.
Given the different spin numbers of the Rb isotopes, I(87Rb) = 3/2 and I(85Rb) = 5/2,[57,58] and the selective ω1 ≪ ω irradiation conditions under which experiments were
performed, optimal CP was found when 2ω1(87Rb) ≈ 3ω1(85Rb). After suitable
tuning, varying the flip angle of 85Rb clearly reflected
in the phased CPMG signal of the 87Rb spectrum, verifying
the direct correlation of both isotopes (Figure a). Notice that complexities associated with
CP between half-integer quadrupoles undergoing MAS[57,59−61] will be absent under QUICSY’s static conditions,
which are compatible with conventional CP transfer protocols. Still,
bandwidth and relaxation limitations may arise, particularly given
the short T1s and relatively low B1s for low-γ
nuclei such as 85Rb. As a part of this study, we tested
the effect of these factors by monitoring the 85Rb CT line
shapes and intensities following spin-lock for both RbClO4 and Rb2SO4 under static conditions (Figures b,5c, and S2). During a spin-locking
pulse applied on the 85Rb channel at a single offset, the
line shape of 85RbClO4 was slightly altered
as a function of the pulse length, but its main features were preserved.
The rapid anisotropic relaxation of 85Rb (in RbClO4 T1(85Rb) = 80 ms[41]) also meant that after 70 ms of spin-lock, a reduction
in the intensity and some distortions became visible. The limited
CP bandwidth problem could be overcome by frequency-stepped acquisitions:
a Rb2SO4 pattern arising from the summation
of CP traces collected using three different offsets on the 85Rb channel yielded a faithful preservation of the overall line shape
(Figures c and S2).[62−65] In contrast, owing to the longer T1 and
T1ρ (T1(87Rb) = 210–220
ms[41,46]), the spin-lock on 87Rb maintained
the line shapes for all of the compounds examined in this study (Figure S3). It should be noted that reverting
the direction of the transfer used, i.e., going from 87Rb to 85Rb, resulted in diminished efficiency; this is
likely due to the short T1 and T1ρ of 85Rb,[41] which were in the order
of the contact times used. It is worth noting that other variants
for establishing this kind of correlation were also tested, including
intermediate transfer through 1Hs for protonated compounds.
Although some of these proved feasible, the regular CP version described
above appeared to be the most advantageous option in terms of the
signal-to-noise ratio (SNR) for all of the compounds studied (Figures S4 and S5).
Figure 4
Sequences used in this
study. (a) 1D CP-CPMG acquisition preceded
by a double-frequency sweep (DFS) block on 85Rb for signal
enhancement. (b) 2D QUICSY sequence involving a constant-time CP-CPMG
with whole-echo acquisitions in t1 and t2, preceded by a DFS block (see Materials and
Methods for the phase-cycling employed). (c) Coherence transfer pathways
for the sequence in (b): after the first excitation pulse on 85Rb, a constant-time acquisition enables the sampling of a
full SQC echo in t1, which is then transferred
by CP to 87Rb. On 87Rb, only a single (−1)
SQC is then detected throughout a CPMG train. Note that the four-step
phase-cycling executed in t1 will also
allow a Δp = + 3 (marked in light gray) to
evolve, but this contribution is likely negligible under static conditions.
Figure 5
(a) 1D CP-CPMG nutation experiment on RbClO4, showing
that the phased CPMG signal of 87Rb followed the 85Rb nutation. The contact time for CP was 45 ms, with an RF amplitude
of ca. 30 kHz on the 85Rb channel and 45 kHz on the 87Rb channel. (b,c) 85Rb CT line shapes and intensities
as a function of the spin-lock (SL) duration given in milliseconds
for (b) RbClO4 and (c) Rb2SO4 using
an RF amplitude of ca. 26 kHz. The Rb2SO4 spectrum
is a sum of sub-spectra collected at three different transmitter frequency
offsets (18, −10, and −35 kHz), marked by yellow arrows
(for the separate sub-spectra, see Figure S2). The RbClO4 spectrum was collected at a single frequency
offset marked by a yellow arrow. The acquisition was carried out with
CPMG to overcome the dead time for 85Rb. The phase-cycling
employed was ϕ1 = x,x,–x,–x,y,y,–y,–y, ϕ2 = −y,–y,y,y,x,x,–x,–x, ϕ3 = y,–y,y,–y,x,–x,x,–x, and ϕ = x,x,–x,–x,y,y,–y,–y.
Sequences used in this
study. (a) 1D CP-CPMG acquisition preceded
by a double-frequency sweep (DFS) block on 85Rb for signal
enhancement. (b) 2D QUICSY sequence involving a constant-time CP-CPMG
with whole-echo acquisitions in t1 and t2, preceded by a DFS block (see Materials and
Methods for the phase-cycling employed). (c) Coherence transfer pathways
for the sequence in (b): after the first excitation pulse on 85Rb, a constant-time acquisition enables the sampling of a
full SQC echo in t1, which is then transferred
by CP to 87Rb. On 87Rb, only a single (−1)
SQC is then detected throughout a CPMG train. Note that the four-step
phase-cycling executed in t1 will also
allow a Δp = + 3 (marked in light gray) to
evolve, but this contribution is likely negligible under static conditions.(a) 1D CP-CPMG nutation experiment on RbClO4, showing
that the phased CPMG signal of 87Rb followed the 85Rb nutation. The contact time for CP was 45 ms, with an RF amplitude
of ca. 30 kHz on the 85Rb channel and 45 kHz on the 87Rb channel. (b,c) 85Rb CT line shapes and intensities
as a function of the spin-lock (SL) duration given in milliseconds
for (b) RbClO4 and (c) Rb2SO4 using
an RF amplitude of ca. 26 kHz. The Rb2SO4 spectrum
is a sum of sub-spectra collected at three different transmitter frequency
offsets (18, −10, and −35 kHz), marked by yellow arrows
(for the separate sub-spectra, see Figure S2). The RbClO4 spectrum was collected at a single frequency
offset marked by a yellow arrow. The acquisition was carried out with
CPMG to overcome the dead time for 85Rb. The phase-cycling
employed was ϕ1 = x,x,–x,–x,y,y,–y,–y, ϕ2 = −y,–y,y,y,x,x,–x,–x, ϕ3 = y,–y,y,–y,x,–x,x,–x, and ϕ = x,x,–x,–x,y,y,–y,–y.With the optimization of the heteroisotopic correlation thus established,
constant-time 2D experiments incorporating the DFS, the CP, and a
CPMG acquisition block to improve the SNR (Figure b) were executed. Whole-echo acquisitions
were utilized for obtaining absorptive 2D line shapes as they yielded
higher sensitivities than hypercomplex (or States[38]) acquisitions; although the whole-echo CPMG t2 acquisitions meant that full t1 echoes were not needed
for avoiding 2D mixed-phase line shapes, we found whole-echo t1 acquisitions advantageous sensitivity-wise. (see Supporting Figure S6). All 2D spectra are thus
presented in magnitude mode. The phase-cycling for these 2D correlation
experiments included a full four-step nested phase cycle of the first
three pulses ϕ1–ϕ3 (for a
total 64-step phase-cycling) to select a single SQC pathway on 85Rb (see Materials and Methods and Figure b,c).Figure a,c shows
representative 2D QUICSY spectra of RbClO4 and Rb2SO4. The experimental 2D spectra bear a close resemblance
to analytically calculated 2D correlations based on the literature
values despite the fact that the calculated spectra disregard the
inefficiencies and heterogeneities of the DFS, CP, or CPMG processes
(Figure b,d). As for
the literature values employed, different sources list somewhat different
chemical shift parameters, particularly with regard to the relative
chemical shift tensor orientation (Tables S1 and S2). A good match was found between the experimental 2D QUICSY
spectrum of RbClO4 and the literature set in ref (45), with the exception that
δ’s sign had to be reversed
for achieving this (δaniso = −13.8 ppm; a
negative value of δaniso was also reported in a previous
study[46]). It can be seen that the experimental
spectrum is slightly asymmetric as compared with the ideal analytical
calculation; this could reflect the offset-dependent CP efficacy mentioned
earlier. Differences between experimental and calculated spectra may
also arise due to the simplified assumption of equal probability for
all transfers regardless of orientation; still, differences between
experiments and analytical expectations are too small to enable their
refinement. Notice how the extensive cross-peak structure in the RbClO4 spectrum clearly indicates more than one magnetically inequivalent
site per single crystallographic unit (Figure ); this is a type of information that arises
in homonuclear correlations[66,67] and in single-crystal
NMR, but it is not usually available from correlations among different
NMR species. Rb2SO4 2D QUICSY experiments acquired
at three different 85Rb offsets (Figure c, see Supporting Figure S7 for the separate 2Ds) also show a clear fine structure.
Literature sources differ somewhat with regard to the chemical shift
parameters and orientation of the two different sites of Rb2SO4 (Table S2); however, again,
our data show a good match with the literature values in ref (45) (Figure d). Figures S9 and S10 further explore this potential by providing difference maps between
the theoretical and experimental data as well as a fitting procedure
attempting to extract the coupling parameters from the RbClO4 data, respectively. From these and other tests, we conclude that
although QUICSY can be a useful tool for extracting this kind of tensorial
information, dealing with multiple correlated sites might demand the
acquisition of higher-quality experimental data as well as more optimized
fitting procedures compared with those assayed hereby for a reliable
extraction of the parameters involved. Alternatively, however, QUICSY
might provide a relatively straightforward experimental confirmation
of parameters as estimated by other means (e.g., DFT calculations).
In this regard, it shows some parallels with static 2D nutation line
shape experiments that have been proposed in the literature.[68,69]
Figure 6
Experimental
and calculated 2D QUICSY spectra of RbClO4 (a, b) and Rb2SO4 (c, d). (a) Experimental
parameters: CP contact time of 45 ms; CP RF amplitude ∼30 kHz
on the 85Rb channel and ∼45 kHz on the 87Rb channel; whole-echo acquisition performed with the CPMG echo time
TE = 720 μs (7 μs dead time before and after each π
pulse, sw = 100 kHz); and a total of 23 t1 increments sampling
a symmetric t1 echo (sw1 = 50 kHz). The SNR of the lowest contour
level is 7. (b) Analytical calculation with the same parameters as
in Figure b. The calculation
was performed with 36 points in F2 (sw
= 100 kHz) and 12 points in F1 (sw1 = 50 kHz). (c) Experimental QUICSY spectrum of Rb2SO4 acquired at three different 85Rb offsets
(−35, −10, and 18 kHz) and subsequently summed up (see Figure S7). The 2D spectrum was acquired with
a CP contact time of 70 ms and the same matching conditions as those
for RbClO4. The CPMG echo acquisition time was TE = 320
μs (7 μs dead time before and after each π pulse,
sw=100 kHz) and a total of 49 t1 increments
constituting a symmetric t1-echo (sw1 = 150 kHz). The SNR of the lowest
contour lever is 12. It is possible to collect a slightly asymmetric
t1-echo without compromising the 2D contour as well as to reduce sw1
(Figure S8). (d) Analytical calculation
with literature parameters of Rb2SO4 identical
to those in Figure c. Simulations used 16 points in F2 (sw
= 100 kHz) and 25 points in F1 (sw1 = 150 kHz).
Experimental
and calculated 2D QUICSY spectra of RbClO4 (a, b) and Rb2SO4 (c, d). (a) Experimental
parameters: CP contact time of 45 ms; CP RF amplitude ∼30 kHz
on the 85Rb channel and ∼45 kHz on the 87Rb channel; whole-echo acquisition performed with the CPMG echo time
TE = 720 μs (7 μs dead time before and after each π
pulse, sw = 100 kHz); and a total of 23 t1 increments sampling
a symmetric t1 echo (sw1 = 50 kHz). The SNR of the lowest contour
level is 7. (b) Analytical calculation with the same parameters as
in Figure b. The calculation
was performed with 36 points in F2 (sw
= 100 kHz) and 12 points in F1 (sw1 = 50 kHz). (c) Experimental QUICSY spectrum of Rb2SO4 acquired at three different 85Rb offsets
(−35, −10, and 18 kHz) and subsequently summed up (see Figure S7). The 2D spectrum was acquired with
a CP contact time of 70 ms and the same matching conditions as those
for RbClO4. The CPMG echo acquisition time was TE = 320
μs (7 μs dead time before and after each π pulse,
sw=100 kHz) and a total of 49 t1 increments
constituting a symmetric t1-echo (sw1 = 150 kHz). The SNR of the lowest
contour lever is 12. It is possible to collect a slightly asymmetric
t1-echo without compromising the 2D contour as well as to reduce sw1
(Figure S8). (d) Analytical calculation
with literature parameters of Rb2SO4 identical
to those in Figure c. Simulations used 16 points in F2 (sw
= 100 kHz) and 25 points in F1 (sw1 = 150 kHz).
Conclusions
and Outlook
This study discussed 2D QUICSY, an experiment
with the potential
to improve the resolution and information content of static NMR spectroscopy
on half-integer quadrupoles. This type of correlations should thus
find usefulness in cases characterized by a large second-order broadening,
which render MAS less effective and are best measured under static
conditions. The approach is aimed at exploiting the proportionality
between the anisotropic broadenings of two isotopes belonging to the
same element. The defining difference among these isotopes arises
from different nuclear quadrupole and magnetic moments, which will
shift the overall center of the patterns and scale their anisotropies.
Calculations showed that 2D QUICSY spectra quickly gained complexity
when considering multiple magnetically inequivalent sites endowed
with sizable chemical shift anisotropies. The ensuing correlations
led to off-diagonal patterns even for single sites. Sequences based
on CP transfers were utilized to test these experiments on compounds,
focusing on the 85Rb/87Rb isotope pair as the
paradigm. Experimental results validated QUICSY’s ability to
convey information on the size and relative orientations of the quadrupolar
and chemical shift interaction tensors. The experiments also demonstrated
that straightforward analytical 2D calculations that assumed ideal
polarization transfers presented a good framework to describe and
match the experimental data. From all of this, we conclude that the
use of such correlation experiments could also yield an understanding
of the structure of new compounds with unknown parameters. Numerous
potential developments could be imparted based on the basic experiments
performed here. The achievable resolution could be improved over the
one shown, which was limited by a low SNR and the rapid ensuing decay
of the signal in the indirect domain into noise; combining this experiment
with hyperpolarization methods could hence be beneficial. Variations
of the sequences that combine broadband excitations as well as broadband
polarization transfers, including swept pulses (Figure S4), are also under study. Moreover, for species for
which both isotopes possess low gyromagnetic ratios, such as 35,37Cl, where direct polarization transfer is expected to
present a larger challenge, sequences mediated by protons as a source
of spin diffusion and polarization transfer are also being considered.
Authors: Frédéric A Perras; Jasmine Viger-Gravel; Kevin M N Burgess; David L Bryce Journal: Solid State Nucl Magn Reson Date: 2012-12-10 Impact factor: 2.293