Darren C Peets1, Maxim Avdeev2,3, Marein C Rahn1, Falk Pabst4, Sergey Granovsky1,5, Markus Stötzer6, Dmytro S Inosov1,7. 1. Institut für Festkörper- und Materialphysik, Technische Universität Dresden, 01069 Dresden, Germany. 2. Australian Nuclear Science and Technology Organisation, Lucas Heights, NSW 2234, Australia. 3. School of Chemistry, The University of Sydney, Sydney, NSW 2006, Australia. 4. Anorganische Chemie II, Technische Universität Dresden, 01069 Dresden, Germany. 5. Faculty of Physics, M.V. Lomonossow Moscow State University, Moscow 119991, Russia. 6. Anorganische Chemie I, Technische Universität Dresden, 01069 Dresden, Germany. 7. Würzburg-Dresden Cluster of Excellence on Complexity and Topology in Quantum Matter-ct.qmat, Technische Universität Dresden, 01069 Dresden, Germany.
Abstract
The rare mineral cyanochroite, K2Cu(SO4)2·6H2O, features isolated Cu2+ ions in distorted octahedral coordination, linked via a hydrogen-bond network. We have grown single crystals of cyanochroite as large as ∼0.5 cm3 and investigated structural and magnetic aspects of this material. The positions of hydrogen atoms deviate significantly from those reported previously based on X-ray diffraction data, whereas the magnetic response is fully consistent with free Cu2+ spins. The structure is not changed by deuteration. Density functional theory calculations support our refined hydrogen positions.
The rare mineral cyanochroite, K2Cu(SO4)2·6H2O, features isolated Cu2+ ions in distorted octahedral coordination, linked via a hydrogen-bond network. We have grown single crystals of cyanochroite as large as ∼0.5 cm3 and investigated structural and magnetic aspects of this material. The positions of hydrogen atoms deviate significantly from those reported previously based on X-ray diffraction data, whereas the magnetic response is fully consistent with free Cu2+ spins. The structure is not changed by deuteration. Density functional theory calculations support our refined hydrogen positions.
Natural minerals offer
a wealth of crystal structures and magnetic
sublattices, and populating these sublattices with quantum spins,
notably Cu2+, is expected to reveal exotic magnetic ground
states and quantum spin dynamics.[1,2] In a few materials,
the Cu2+ ions are well-separated by large anions, aquo
or hydroxo ligands, and alkali-metal ions, resulting in large Cu–Cu
distances with long and convoluted superexchange paths. This is the
case, in particular, in the Tutton salts, which have the general formula
A2M(XO4)2·6H2Oa where A is an alkali metal or NH4+, M is a 3d transition metal,
and X is sulfur or selenium, as well as in kröhnkite Na2Cu(SO4)2·2H2O[3] and related minerals. This is expected to result
in exceedingly weak magnetic interactions and in spin dynamics restricted
to very low energies and temperatures.The exchange pathways
in the Tutton salts, two of which are shown
in Figure b for cyanochroite,
K2Cu(SO4)2·6H2O,
pass through a minimum of five intermediate atoms via two hydrogen
bonds. This would not be expected to support strong magnetic interactions,
and no magnetic entropy is visible down to 2 K.[4] The paramagnetic nature of the Tutton salts down to very
low temperatures has been known for quite some time and led to these
materials being well-studied decades ago by electron paramagnetic
resonance (see ref (5) on cyanochroite) and for use in adiabatic demagnetization refrigeration,[6] which led to hints of a transition around 10 mK[7] in K2Cu(SO4)2·6H2O. The magnetic transition in cyanochroite has
since been identified at 29.6 mK by ac susceptibility and specific
heat measurements.[8−10] The quest of late in condensed matter physics has
been for strong electron correlations and magnetic frustration, but
these families offer a useful baseline of maximally noninteracting
Cu2+ ions.
Figure 1
(a) Crystal structure of cyanochroite from our structure
refinement
at 293 K. Thinner lines indicate hydrogen bonds. (b) View along b of a slice showing the networks responsible for two magnetic
exchange pathways.
(a) Crystal structure of cyanochroite from our structure
refinement
at 293 K. Thinner lines indicate hydrogen bonds. (b) View along b of a slice showing the networks responsible for two magnetic
exchange pathways.The Tutton salts including
cyanochroite, the structure of which
is shown in Figure a, have also been investigated for use in Li and Na batteries[11] and for a unique interplay between their hydrogen-bonding
networks and their Jahn–Teller-distorted Cu coordination spheres.
Although most Tutton salts form in the same crystal structure, the
copper members of the family can form in two different structures,
determined by a competition between cooperative Jahn–Teller
distortions and the hydrogen-bonding network.[12−15] The copper-based Tutton salts
can be tuned between these structures by pressure,[16,17] by doping, or by substitution on the Cu,[18] X,[19] or A site.[20] (NH4)2Cu(SO4)2·6H2O is even known to adopt different structures depending on
the degree of deuteration.[21,22]We find a magnetic
response in K2Cu(SO4)2·6H2O consistent with free Cu2+ spins at all fields
and temperatures accessible to us. Our crystal
structure refinement provides updated hydrogen positions, which differ
significantly from earlier values extracted from X-ray diffraction,[23] and establishes that deuteration does not significantly
alter the crystal structure or magnetic response of K2Cu(SO4)2·6H2O. Our hydrogen positions
will be useful for modeling the magnetic interactions, internal electric
fields, and octahedral distortions.
Results
and Discussion
Diffraction
Neutron
white-beam Laue
diffraction was performed on cyanochroite at room temperature and
4 K and in multiple orientations to ensure reflection coverage.
One of the Laue images for a measurement at room temperature is shown
in Figure a, and the
top inset in Figure b shows the crystal mounted in the beam. The corresponding |F2|calc versus |F2|obs plot from the refinement of these data is shown in Figure b. The points remain close
to a unit slope, indicating that the refined structure describes the
data well.
Figure 2
Neutron white-beam Laue diffractometry on cyanochroite. (a) Laue
pattern at 293 K, showing sharp spots. (b) Comparison of observed
and calculated structure factors, demonstrating the quality of the
refinement. The top inset shows the crystal used, and the bottom inset
shows several representative crystals on millimeter-ruled graph paper.
Neutron white-beam Laue diffractometry on cyanochroite. (a) Laue
pattern at 293 K, showing sharp spots. (b) Comparison of observed
and calculated structure factors, demonstrating the quality of the
refinement. The top inset shows the crystal used, and the bottom inset
shows several representative crystals on millimeter-ruled graph paper.The results of refinements at 293 and 4 K
are summarized
in Table . With the
exception of hydrogen positions, our refined crystal structure is
consistent with that previously reported, but we were additionally
able to refine anisotropic thermal parameters. The hydrogen positions
are significantly different from their previously reported positions,[23] exhibiting shifts of 0.11 to 0.25 Å
at room temperature. At 4 K, our atomic positions shift slightly,
and the displacements relative to ref (23) range from 0.14 to 0.25 Å. The hydrogen
positions refined from our data are compared with those from ref (23) in Figure to more clearly demonstrate the significance
of these shifts. The work of ref (23) was based on single-crystal X-ray diffraction,
which is sensitive to electron density and thus has far poorer sensitivity
to H than does neutron diffraction, so the hydrogen positions reported
here more closely represent the location of the nuclei. This is supported
by a visual examination of the shifts in hydrogen positions—the
X-ray-derived hydrogen positions are all significantly closer to the
covalently bonded oxygen atom, as that covalent bond is where the
electron density is.
Table 1
Parameters of the
Neutron Structure
Refinement of K2Cu(SO4)2·6H2O and K2Cu(SO4)2·6D2O (“D”) in Space Group P21/a (No. 14) at 293 K and Low Temperature,
and the X-ray Structure Refinement of K2Cu(SO4)2·6D2O at Room Temperaturea
temperature
293 K
4 K
293 K (D)
5 K (D)
293 K (D, XRD)
space group
P21/a
P21/a
P21/a
P21/a
P21/a
a
9.090 Å
9.082 Å
9.085 Å
9.092 Å
9.0647(5) Å
b
12.121 Å
12.108 Å
12.137 Å
12.106 Å
12.0875(7) Å
c
6.167 Å
6.182 Å
6.162 Å
6.173 Å
6.1516(4) Å
β
104.55°
104.43°
104.36°
104.31°
104.453(5)°
unit cell
volume
657.68 Å3
658.36 Å3
658.22 Å3
658.37 Å3
652.70(7) Å3
Z
2
2
2
2
2
density
2.232 g/cm3
2.229 g/cm3
2.288 g/cm3
2.287 g/cm3
2.310 1 g/cm3
reflections
4412
4389
4424
3271
1302
reflections, I > 3σ
2154
3253
1396
2348
1256
parameters
143
143
143
143
95
θ range
2.86–51.20°
3.40–51.09°
3.80–51.62°
3.98–51.21°
2.87–27.25°
coverage
0 ≤ h ≤ 18
0 ≤ h ≤ 18
0 ≤ h ≤ 15
0 ≤ h ≤ 15
–10 ≤ h ≤ 11
0 ≤ k ≤ 24
0 ≤ k ≤ 24
0 ≤ k ≤ 26
0 ≤ k ≤ 26
–15 ≤ h ≤ 12
–12 ≤ l ≤ 11
–13 ≤ l ≤ 11
–10 ≤ l ≤ 11
–10 ≤ l ≤ 11
–7 ≤ l ≤ 7
R, I > 3σ
5.41%
4.39%
6.21%
5.55%
4.51%
wR, I > 3σ
4.23%
3.95%
4.75%
4.83%
5.93%
Lattice parameters
from the neutron
Laue measurements were estimated at the data reduction stage.[24]
Figure 3
Our refined
hydrogen positions (50% probability ellipsoids, green)
at (a) 293 and (b) 4 K compared with the room temperature hydrogen
positions (gray) of ref (23). The shifts are significant at all sites. Shifts on the
oxygen sites at 4 K reflect the lower measurement temperature
in our data. Blue is oxygen, and yellow is copper. Our refined deuterium
positions (magenta) at (c) 293 and (d) 5 K are compared with
our respective hydrogen positions. Oxygen ellipsoids for the deuterated
structure are drawn darker.
Lattice parameters
from the neutron
Laue measurements were estimated at the data reduction stage.[24]Our refined
hydrogen positions (50% probability ellipsoids, green)
at (a) 293 and (b) 4 K compared with the room temperature hydrogen
positions (gray) of ref (23). The shifts are significant at all sites. Shifts on the
oxygen sites at 4 K reflect the lower measurement temperature
in our data. Blue is oxygen, and yellow is copper. Our refined deuterium
positions (magenta) at (c) 293 and (d) 5 K are compared with
our respective hydrogen positions. Oxygen ellipsoids for the deuterated
structure are drawn darker.Several deuterated crystals were also measured, by both neutron
and X-ray single-crystal diffraction, to determine whether the structure
changes with deuteration as it does in (NH4)2Cu(SO4)2·6H2O. The X-ray structure
solution algorithm reproducibly converged to the (Cu, K, S, O) atomic
arrangement previously reported.[19,23,25] This measurement is not sensitive to the presence
of deuterium ions due to their weak X-ray scattering amplitude, so
positional parameters for D were fixed to those determined by neutron
diffraction at the same temperature. Excluding D entirely produced
significantly worse results, and refining these positional parameters
led to insignificant improvements. Non-hydrogen structural parameters
were refined using Jana2006; the refinement is summarized in Table . Both X-ray and neutron
diffraction indicated that the structure does not change with deuteration,
and the atomic positions are essentially unchanged.In the harmonic
approximation, the ratio of atomic displacement
parameters Ueq(H)/Ueq(D) should be inversely proportional to the square root of
the ratio of their masses, that is, √2 ∼ 1.4. The fact
that the refined ratio is significantly lower—1.063(12) and
1.15(2) at 293 and 4 K, respectively—suggests anharmonicity
and/or local static disorder. The latter is also supported by the
fact that, although the thermal displacement parameters for Cu, K,
S, and O decrease by a factor of ∼5 on cooling from room temperature
to 4 K, those of H and D decrease only by a factor of ∼2.
Density Functional Theory Calculations
Density functional theory (DFT) calculations were used to model the
crystal structure of cyanochroite, using all van der Waals density
corrections and functionals available in VASP.[26] DFT is, in principle, a zero-temperature approximation,
so results were compared against our 4 K results, which were collected
specifically for this comparison. All calculations produce a crystal
structure consistent with our refinements and previous X-ray diffraction
results, but with deviations in the atomic positions. These deviations
from our 4 K neutron refinement are shown in Figure , where the X-ray results of Bosi et al.[23] are also included. Atomic positions here were
converted to angstrom units using the experimental 4 K unit cell.
Figure 4
Comparison
of the deviations in Å between the positions from
our neutron structure refinement and the atomic positions determined
by Bosi et al.,[23] by Rauw et al.,[25] and by DFT calculations using all available
van der Waals density functionals.
Comparison
of the deviations in Å between the positions from
our neutron structure refinement and the atomic positions determined
by Bosi et al.,[23] by Rauw et al.,[25] and by DFT calculations using all available
van der Waals density functionals.Excluding hydrogen positions, the atomic positions reported previously
based on room-temperature X-ray diffraction[23] are roughly an order of magnitude closer to our current results
than those of any DFT model or the neutron single-crystal refinement
under 1.4 kbar of pressure reported in ref (25), despite the very different
temperature. The X-ray lattice parameters are also very close to ours
(not shown), again despite the temperature difference, but here, the
others are not significantly worse. The X-ray refinement fares poorly
when it comes to hydrogen positions because X-ray diffraction probes
electron density rather than the position of the nucleus, and the
electron density around H+ is both extremely low and shifted
by typically 0.1–0.2 Å toward the nearest anion.Among the van der Waals functionals, BEEF-vdW consistently produced
the least accurate results, whereas rPW86-vdW2 gave the best results
for 8 of the 15 refineable sites. In particular, rPW86-vdW2 came far
closer to the experimental O2 and O3 positions than any other functional.
The O6 site seemed particularly difficult to model accurately through
DFT, although interestingly, the otherwise inaccurate BEEF-vdW functional
described this site better than the other functionals.
UV–Vis Spectroscopy
The absorption spectrum
of K2Cu(SO4)2·6H2O in the near-infrared, visible, and ultraviolet
range is shown in Figure . This spectrum was fit to three Gaussians in the frequency
domain to obtain peak positions. The first two peaks are found at
212 and 279 nm (47 255 and 35 862 cm–1), whereas the third peak is in the infrared range
beyond our measurement window.
Figure 5
UV–vis–NIR spectrum of cyanochroite,
with a fit to
three Gaussians.
UV–vis–NIR spectrum of cyanochroite,
with a fit to
three Gaussians.In a conventional Jahn–Teller
picture considering only the
ligands directly bonded to Cu, the sole hole in elongated octahedrally
coordinated Cu2+ would be expected to be in the d antibonding orbital, and excitations would only be possible into
this orbital. Transitions would be possible, in order of increasing
energy, from d3, d, and
the doubly degenerate d and d. However, recent work has shown that the Cu coordination
sphere in Tutton salts is best described as a compressed octahedron with an orthorhombic instability, where electric fields
from more distant ions play a crucial role .[27] In this picture, the d3 antibonding orbital
is shifted to higher energy than d, and the lowest-energy
transition is from d to d3. This transition is
not within our measurement window, and we cannot comment on the veracity
of this picture based on our spectroscopic data. However, our structure
refinements find three different Cu–O bond lengths, consistent
with the scenario described in ref (27).Returning to the optical spectrum, at
significantly higher energy,
additional excitations would be expected from bonding orbitals having
significant ligand sp3 character, commonly referred to
as “charge-transfer” bands. We attribute absorptions
toward the 200 nm end of our spectrum as the latter charge-transfer
excitations, involving transitions out of the highest-energy filled
bonding orbitals. The gap in the optical range corresponds to the
gap between these bonding orbitals and the nonbonding d, d, and d, whose excitations appear at and beyond the infrared
end of our spectrum. Previous studies on this and similar Cu(H2O)62+ compounds have found d–d
excitations exclusively in the infrared, starting at ∼850 nm.[28,29]
Magnetization
Magnetization measurements
in fields applied along selected directions for both protonated and
deuterated crystals are shown in Figure . No anisotropy is observed. The temperature-dependent
data are well-described below 100 K by a Curie–Weiss
law with an offset, i.e., M/H = A + B/(T – ΘCW), as shown in the right inset. The Curie–Weiss temperatures
extracted from the zero-field-cooled (ZFC) and field-cooled (FC) data
range from 33 to 205 mK, and the paramagnetic moments range
from 1.59 to 1.62 μB. No evidence for a magnetic
transition is observable in these data or their derivative (left inset),
consistent with the extremely small Curie–Weiss temperatures.
The slightly positive ΘCW suggests a tendency toward
ferromagnetism. Earlier ac susceptometry measurements to lower temperature
found a Curie–Weiss temperature of 31.3 mK,[9] with our higher values likely due to our higher
measurement field, and a slightly higher paramagnetic moment of 1.91 μB.
Figure 6
Magnetization of K2Cu(SO4)2·6H2O (cyanochroite). (a) Temperature-dependent magnetization
under a 1000 Oe field H∥[001] and H∥[011] in a deuterated crystal shows Curie–Weiss
behavior (right inset), with Curie–Weiss temperatures ranging
from 33 to 205 mK. The left inset shows the derivative of the
magnetization data, with no peak that could suggest a magnetic phase
transition. (b) M–H loop
at 2 K for field along [100], fit to the behavior expected
for noninteracting S = 1/2 spins with only the electron g factor as a free parameter.
Magnetization of K2Cu(SO4)2·6H2O (cyanochroite). (a) Temperature-dependent magnetization
under a 1000 Oe field H∥[001] and H∥[011] in a deuterated crystal shows Curie–Weiss
behavior (right inset), with Curie–Weiss temperatures ranging
from 33 to 205 mK. The left inset shows the derivative of the
magnetization data, with no peak that could suggest a magnetic phase
transition. (b) M–H loop
at 2 K for field along [100], fit to the behavior expected
for noninteracting S = 1/2 spins with only the electron g factor as a free parameter.Field-dependent magnetization is shown in Figure b. As expected, no hysteresis is observed.
The curve is well-described by that of free S = 1/2
spins, i.e., M = −NAnSgμB tanh(−SgμBB/kBT), where there is n = 1 Cu spin
per formula unit and S = 1/2, with only the electron g factor as an adjustable parameter. The g factor extracted from this fit is 2.34, suggesting an orbital component,
as proposed previously.[9] The argument of
the tanh function reaches unity for our 1000 Oe M(T) measurement field at a temperature of 79 mK,
indicating that our Curie–Weiss temperatures reflect the temperature
scale at which the moments would align with the applied field for
statistical reasons, with no significant contribution due to exchange
interactions. This would lead to an apparent ferromagnetic contribution
as found in our fits.The free-spin-like behavior in the temperature
range probed and
Curie–Weiss temperatures consistent with a near-absence of
exchange interactions reflect that the material’s tortuous
exchange pathways (see Figure b) prevent any significant exchange coupling among the Cu2+ moments. The Cu spins in cyanochroite behave as free and
noninteracting to a very good approximation well down into the milliKelvin
regime.
Conclusion
We have
refined the structure of cyanochroite, K2Cu(SO4)2·6H2O, finding hydrogen positions
which differ significantly from those previously reported. These positions
are key for modeling of the hydrogen-bonding network, the internal
electric fields, and their complex interplay with the Cu2+ octahedral distortions. Unlike its NH4+ analogue, K2Cu(SO4)2·6H2O retains the same structure upon
deuteration. The hydrogen positions are also crucial for modeling
the extremely weak exchange interactions coupling the Cu spins in
what remains a model system for studying essentially noninteracting
quantum (i.e., S = 1/2) spins.
Experimental
Section
Materials and Synthesis
Cyanochroite
crystals were grown from aqueous solutions. CuSO4·5H2O (Alfa Aesar, 99%) and K2SO4 (Grüssing
GmbH, 99%) were each fully dissolved in distilled water; these solutions
were then mixed in a glass beaker, and the water was allowed to slowly
evaporate. In some cases, a watchglass was added as a lid, and the
crystals were grown at 60 °C in a convection drying oven
or on a hot plate; in other cases, the beaker was left to evaporate
at room temperature with no lid. After several days, pale blue crystals
several millimeters in size grew on the bottom of the beaker. The
growth process proceeded somewhat more quickly at 60 °C
due to the more rapid evaporation even with a lid present, but no
significant difference was found among crystals grown by these approaches.
Deuterated crystals were grown from D2O (Acros Organics,
99.8%D) instead of H2O, and these growths were performed
in a desiccator with silica gel to exclude the replacement of deuterium
with protons from the water vapor in air.Best results were
obtained with copper-rich cation ratios, typically Cu/K ∼ 2:1,
to control nucleation—mixtures closer to the ideal stoichiometry
produced clusters of small crystals. Copper-rich mixtures initially
produced small clusters of slow-growing green kaliochalcite crystals,
KCu2(SO4)2[(OH)(H2O)],
which were readily collected at one side of the beaker by swirling
the liquid. Segregation of the solid phases was also achieved using
a horizontal temperature gradient—kaliochalcite grows predominantly
on the hot side, whereas cyanochroite grows on the cold side. Thermal
gradients were achieved most effectively by cantilevering the beaker
off the edge of a hot plate.
Crystal Structure Determination
and Modeling
A roughly 1.5 × 1.5 × 2 mm3 single
crystal of K2Cu(SO4)2·6H2O was measured using the KOALA white-beam neutron Laue diffractometer
at the OPAL Research Reactor at ANSTO, in Australia,[30] with a 3 mm aperture to fully illuminate the sample.
Due to a very high signal-to-background ratio, analyzable data can
be obtained by this technique without deuteration. Data were collected
at room temperature and at 4 K for multiple
orientations. Deuterated crystals were also measured to verify that
the structure did not change. Image data processing, including indexing,
intensity integration, and wavelength distribution normalization,
was performed using LaueG.[24] Crystal structure
refinement was carried out using Jana2006.[31]Room-temperature single-crystal X-ray diffraction was carried
out on a deuterated sample using a Bruker-AXS KAPPA APEX II CCD diffractometer
with graphite-monochromated Mo Kα X-ray radiation. The Rigaku
CrysAlisPro package was used to index the observed Bragg reflections
and perform the necessary data reduction.[32] Various crystallites with dimensions on the order of 100 μm
were investigated, and the results were found to be fully reproducible.
The structure was solved using the Superflip charge flipping[33] and EDMA[34] Fourier
peak search approach as implemented in Jana2006.[31,35]Density functional theory calculations were performed in VASP[26] using all the van der Waals corrections and
functionals available to optimize the structure for comparison with
diffraction results.
Magnetization Measurements
Magnetization
was measured on both protonated and deuterated crystals as a function
of temperature using a Cryogenic Ltd. cryogen-free measurement system
using the vibrating-sample magnetometry option in both ZFC warming
and FC cooling conditions. Four- or five-quadrant M–H loops were measured at several temperatures.
The single crystals were mounted either to a plastic straw or to a
plastic rod sample holder, and temperature-dependent measurements
were performed in 1000 Oe fields applied along the [100], [001], and
[011] directions.
UV–Vis Spectroscopy
Absorption
spectra in the ultraviolet, visible, and near-infrared range from
200 to 800 nm were collected at room temperature on a Varian
Cary 4000 spectrophotometer with a scan rate of 600 nm/min,
a step of 1 nm, a spectral bandwidth of 2 nm, and averaging
time of 0.1 s. Fifteen milligrams of cyanochroite crystal
was ground together with 200 mg of BaSO4 to avoid
excessive absorption.
Authors: Inés Sánchez-Movellán; David Carrasco-Busturia; Juan M García-Lastra; Pablo García-Fernández; José A Aramburu; Miguel Moreno Journal: Chemistry Date: 2022-06-14 Impact factor: 5.020