Christoffer Olsson1, Jan Swenson1. 1. Department of Physics, Chalmers University of Technology, SE-412 96 Göteborg, Sweden.
Abstract
The two sugar molecules sucrose and trehalose are both considered as stabilizing molecules for the purpose of preserving biological materials during, for example, lyophilization or cryo-preservation. Although these molecules share a similar molecular structure, there are several important differences in their properties when they interact with water, such as differences in solubility, viscosity, and glass transition temperature. In general, trehalose has been shown to be more efficient than other sugar molecules in preserving different biological molecules against stress, and thus by investigating how these two disaccharides differ in their water interaction, it is possible to further understand what makes trehalose special in its stabilizing properties. For this purpose, the structure of aqueous solutions of these disaccharides was studied by using neutron and X-ray diffraction in combination with empirical potential structure refinement (EPSR) modeling. The results show that there are surprisingly few differences in the overall structure of the solutions, although there are indications for that trehalose perturbs the water structure slightly more than sucrose.
The two sugar molecules sucrose and trehalose are both considered as stabilizing molecules for the purpose of preserving biological materials during, for example, lyophilization or cryo-preservation. Although these molecules share a similar molecular structure, there are several important differences in their properties when they interact with water, such as differences in solubility, viscosity, and glass transition temperature. In general, trehalose has been shown to be more efficient than other sugar molecules in preserving different biological molecules against stress, and thus by investigating how these two disaccharides differ in their water interaction, it is possible to further understand what makes trehalose special in its stabilizing properties. For this purpose, the structure of aqueous solutions of these disaccharides was studied by using neutron and X-ray diffraction in combination with empirical potential structure refinement (EPSR) modeling. The results show that there are surprisingly few differences in the overall structure of the solutions, although there are indications for that trehalose perturbs the water structure slightly more than sucrose.
In a previous study
we examined the structural properties of an
aqueous trehalose solution for the purpose of investigating its role
as a protein stabilizer.[1] The main results
showed that trehalose forms multiple (although weak) bonds with water,
avoiding direct trehalose–trehalose interactions (clustering),
and had a destructuring effect on the water. However, the results
obtained in that study did not include any comparisons with other
sugar molecules. Thus, the question is whether our findings are unique
for trehalose and therefore may explain its special stabilizing properties
or if similar results would be obtained for other sugar molecules,
such as sucrose.Sucrose and trehalose are both disaccharide
molecules with the
same chemical formula (C12H22O11)
but with different geometrical structures (see Figure ). The sucrose molecule consists of one glucose
ring, and one fructose ring, connected by a glycosidic linkage, whereas
the trehalose molecule consists of two glycosidic-linked glucose rings.
Figure 1
Simple
molecular sketches of sucrose (left) and trehalose (right).
The carbon-bound hydrogens (labeled “M”) have been omitted
from the drawings for clarity.
Simple
molecular sketches of sucrose (left) and trehalose (right).
The carbon-bound hydrogens (labeled “M”) have been omitted
from the drawings for clarity.Both sucrose and trehalose are often used as a stabilizing agent
for different storing purposes, and it is commonly known that disaccharides
in general have stabilizing effects both for the purpose of stabilization
during cryo-storage and for the purpose of anhydrobiotic preservation
(e.g., freeze-drying).[2] When comparing
the disaccharidestrehalose and sucrose, however, it is found that
trehalose is superior for many different biological preservation purposes,[3,4] such as stabilization against thermal stress[5,6] or
during lyophilization.[7−9] It is therefore of interest to determine what aspects
of these rather similar molecules are important for biological stabilization.
There have been plenty of studies comparing the two types of molecules
for different purposes.[5,10−16] On a macroscopic level there are some obvious differences: For example,
sucrose has an exceptionally high solubility in water of 2.14 g of
sucrose per 1 g of water (which implies that only 9 water molecules
per sucrose molecule are required to dissolve the sugar), whereas
trehalose can only be dissolved up to 1.1 g of trehalose per 1 g of
water.[17] Possibly one of the most important
differences of these two sugar molecules, for preservation purposes,
is the larger glass transition temperature (Tg) of trehalose compared to sucrose.[5,18,19] This difference relates to the higher ability
of trehalose to form a homogeneous amorphous network[14,20] which, in turn, leads to a slowing down of the water dynamics[21] and perhaps, more importantly, to its larger
capability to incorporate water molecules into its network, thus preventing
water from crystallizing.[5] Furthermore, Tg of a trehalose–water matrix has been
shown to decrease less with an addition of small amounts of water
compared to, for example, sucrose.[22−24] This implies that trehalose
provides a more stable environment for the biological molecules and
is better at maintaining a more rigid vitrified surrounding.[25]The questions are, however, what the structural
differences are
that produce these differences in macroscopic properties. Several
groups have examined the number of bonds formed between the different
disaccharides, and some of them have concluded that trehalose forms
more and stronger hydrogen bonds with water than, for example, sucrose.
This has been shown by the use of, for example, ultrasonic velocity
measurements,[26] quasi-elastic neutron scattering
(QENS) measurements,[27] and molecular dynamics
(MD) simulations.[14] Lerbret et al.[14] have furthermore pointed out that trehalose,
compared to sucrose and maltose, retains a less folded structure when
dehydrated and tends to avoid cluster formation in an aqueous solution
(which was also found in ref (1)), thus exposing more of its moieties to the surrounding
water molecules. However, other groups point out that the total hydration
numbers of sucrose and trehalose are actually quite similar.[12,13]Another important property of disaccharides is that they tend
to
have a destructuring effect on the natural tetrahedral structure of
water.[10,12] This destructuring effect has been found
to be particularly strong for trehalose,[10,14,21,28−32] and this observation is often used to explain parts of the extraordinary
stabilizing properties of trehalose. However, Soper and co-workers
have disputed this argument by showing very small destructuring effects
on the water by the use of neutron and X-ray diffraction combined
with empirical potential structure refinement (EPSR) modeling.[33,34]In this paper we extend
our previous study[1] on an aqueous trehalose
solution by also studying sucrose at the
same solution concentration (33 wt %) also with the use of both neutron
and X-ray diffraction combined with EPSR modeling. From this we can
directly compare the effect the two sugars have on their aqueous environment
and also how the sugars themselves interact and structure in water.
The purpose of this is to elucidate the aspects that make trehalose
better at, for example, stabilizing proteins. However, the present
results indicate very small structural differences between the sucrose
and the trehalose solutions. A new EPSR model for trehalose has been
produced, which showed a slightly smaller effect on the water structure
than what was found in our previous study,[1] thus more in line with the similar studies made by Pagnotta et al.[33] and Soper et al.[34] However, by comparison with sucrose, it was found that the presence
of trehalose appears to have a stronger effect on the structure of
bulk water than sucrose. A similar abundance of water–disaccharide
bonds was found in this study as in our previous study on only trehalose.[1]
Experimental Section
Sample Preparation
All sucrose samples were prepared
in the same way as trehalose in ref (1). Six samples with different deuterations were
made with the same molar concentration of 38 water molecules per sucrose
(corresponding to a sugar content of 33 wt% for the fully hydrogenous
sample). The sucrose was dissolved in either H2O, D2O, or a 1:1 molar concentration mixture of the two (HDO).
Two different isotope conformations of sucrose were used: either regular
hydrogenated sucrose (purchased in crystalline form from Sigma-Aldrich,
with >99.5% purity), which will be denoted as H-Sucrose (or H-Suc),
or deuterated sucrose, in which the 14 carbon-bound hydrogens had
been exchanged for deuterium (purchased in crystal form from Omicrometer
Biochemicals Inc.) which will be denoted as D-Sucrose (or D-Suc).
The hydrogens at the hydroxyl groups are exchangeable in water, and
therefore these hydrogens were replaced with deuterium by repeatedly
dissolving and drying (under vacuum at 70 °C) the sucrose in
either D2O or HDO (depending on what solvent they were
to be finally dissolved in). This procedure was used to ensure that
the exchangeable sucrosehydrogens always had the same isotope composition
as the solvent. The six different isotope compositions were either
D-Sucrose in H2O, D2O, or HDO (D-Suc D2O, D-SucH2O, and D-SucHDO), or H-Sucrose in H2O, D2O, or HDO (H-Suc D2O, H-SucH2O, and H-SucHDO). The neutron diffraction data of trehalose (α,α-trehalose)
was taken from our previous study;[1] however,
we now added X-ray diffraction data of fully protonated trehalose
in H2O (H-Tre in H2O), prepared in the same
way as described in ref (1).
Neutron Diffraction Experiments
The neutron diffraction
measurements and data corrections were performed by using the same
method as described in ref (1). The samples were placed, using a syringe, inside 1 mm
thick Ti0.676Zr0.324 containers, which were
sealed with a PTFE O-ring. These containers were mounted on a sample
changer with a water bath temperature control set to 298 K. The measurements
were performed on the NIMROD diffractometer[35] at the ISIS neutron spallation source (Rutherford Appleton Laboratory,
UK).Once the data were collected, it was corrected (e.g., background
subtraction and inelastic scattering corrections) by using the GUDRUN
suite (2015 version).[36] From these corrections
the interference differential cross sections (I(Q)) for the sample were obtained:where Q is the neutron momentum
transfer, cα is the number density
of atom type α, bα is the
corresponding scattering length of that atom, and Sα,β(Q) is the partial structure
factor of atom types α and β, i.e., describing the correlations
between these two atoms.
X-ray Experiments
The samples taken
for X-ray measurements
were prepared in the same way as for the fully protonated neutron
diffraction samples (H-Sugar and H2O). Samples were placed
in 2 mm wide silica glass capillaries and placed in an Empyrean X-ray
diffractometer (using an Ag anode) with an X-ray beam with a wavelength
of 0.5609 Å. The data were corrected for background scattering,
multiple scattering, and attenuation and converted to an interference
differential cross section scale with the use of GUDRUN-X, which is
extensively explained in ref (37).
EPSR Modeling
The corrected data
were fitted by using
EPSR modeling.[38] In this method, a molecular
simulation box is created with the identical chemical composition
as the measured sample. The user also assigns an appropriate reference
potential for the different atom types (typically based on known force-field
parameters), and then the software calculates the theoretical I(Q) for the different isotope compositions
and compares those to the experimental data. An empirical potential,
based on the difference between supplied and simulated I(Q), is then added to the reference potential, which
subsequently reconfigures the molecular model.Theoretical details
regarding the empirical potential structure refinement (EPSR) method
are well described in, for examle, ref (38). The simulation was set up in a similar way
as in ref (1), although
with some important differences. The simulation box was doubled in
size, with 4000 water molecules and 104 sucrose molecules. For comparison,
the previously produced trehalose simulation from ref (1) was rerun with the same
increased box size and with the addition of X-ray data. The reference
potential for sucrose was set identical to that of trehalose, which
was based on the parameters used in ref (33) (which in turn was based on the OPLS-AA force
field[39] for trehalose and the SPC/E model
for the water molecules[40]). The reference
potential for the new trehalose EPSR model was set identical to our
previous study.[1] Details regarding the
force field parameters for the reference potential can be seen in
Table S1 of the Supporting Information.
The atomic labeling of sucrose was mainly set analogous to that of
trehalose in ref (1) (see Figure ) and
ref (33); however,
an additional oxygen type (O4) was defined for the hydroxymethyl groups
on the fructose ring of the sucrose molecule. This was introduced
to be able to distinguish between the two sugar rings (glucose and
fructose) for at least one atom type. The number density of the model
for the sucrose sample was set to 0.106439, as determined by a density
measurement of the fully hydrogenated sucrose sample, and 0.10677
for the trehalose model, as previously used in ref (1).After the simulation
box was equilibrated by using the reference
potential, the diffraction data were introduced to refine the empirical
potential. The influence of the empirical potential was increased
until the fit with the diffraction data was no longer improved. When
the fit reached this point, statistics about the systems was gathered
by collecting ∼1000 molecular configurations. Average molecular
properties presented in the results originate from these configurations.
EPSR Analysis
From the obtained molecular model, different
coordination numbers from atom α to atom β (see Table S2) were calculated via the following equation:where gα,β(r) is the partial pair correlation function of
atoms α and β and cβ is the atomic number density of atom β. The integration is
done between the center of the atom α (r1 = 0) and a certain distance (r2, where r2 depends on which coordination
number is of interest).Hydrogen bonds were also calculated
by three different hydrogen-bond criteria. In criteria 1 a hydrogen
bond is defined as soon as the distance of a hydrogen and an oxygen
is <2.5 Å (as used in e.g. refs (41−43)) and thus contains
no constraint regarding the bond angles of relevance. Criteria 2 and
3 define a hydrogen bond when the distance between two oxygen atoms
is <3.4 Å and the angle between donor–hydrogen–acceptor
is above 120° and 160°, respectively. Criteria 2 was used
in, for example, refs (12, 14, and 40), and the more strict definition of a hydrogen bond, criteria 3,
was also used in ref (14). The hydrogen bond analysis for criteria 2 and 3 was done by creating
a “pseudo-trajectory” from the EPSR model of ∼500
configurations and analyzing this trajectory by using the molecular
dynamics trajectory analysis software VMD.[45]
SANS Fits
To determine the size distribution of the
two different disaccharides, a separate fit was made to the small-angle
scattering part (the Q-range 0.05–1 Å–1) of the diffraction data. Specifically, the fits
were made on either D-Suc in H2O or D-Suc in HDO (and D-Tre
in H2O and D-Tre in HDO) because these data sets have the
strongest form factor contribution to the signal. The fits were made
with the help of the SasView software (v. 4.1.2).[46] Simultaneous fits of the two different isotope compositions
were performed by using a spherical hard-sphere model with a Gaussian
distribution of the radius. The scattering length densities for the
solute and the solvent for the two different isotope compositions
were fixated, and similarly, the volume fraction of the disaccharide
molecules was fixed and approximated to 0.2467, based on the macroscopic
densities of the two components in the solution. The Q-range was selected so that it captures the steep descent of the I(Q) signals, which was assumed to originate
mainly from the form factor of the disaccharides.
Results
Q-Space Analysis
I(Q) of
both sucrose and trehalose solutions of all
isotope compositions are shown in Figure . It should be noted that some of the differences,
namely, the overall level of these curves, may differ slightly due
to inaccuracies in the data correction steps, such as in the inelasticity
correction. This particularly becomes more problematic with higher
fractions of hydrogens and at lower Q’s. The
data sets coming from the two different disaccharides are, however,
very similar, although some features are noticeably different. In Figure , these differences
are amplified and are plotted in comparison to bulk water (H2O, HDO, or D2O). These bulk–water data were obtained
from ref (47) and were
converted to the same scale as the sugar data sets. The most obvious
feature differences between the different data sets are listed in
the following points:
Figure 2
Differential cross sections, I(Q), of both sucrose and trehalose in a 1.1 M aqueous
solution. Full
lines show I(Q) of sucrose solutions
of different isotope compositions, and black dashed lines show I(Q) for the same isotope compositions
of the trehalose solutions.
Figure 3
Zoomed-in
differential scattering cross sections for different
isotope compositions compared with different isotope compositions
of bulk water at the same temperature. Blue lines represent sucrose,
black dashed lines represent trehalose, and red dashed-dotted lines
represent bulk water. Corresponding differential scattering cross
section from X-ray measurement can be found in Figure S1.
In the H-SucH2O data (Figure A), there are few
clear differences. Trehalose exhibits a slightly larger peak than
sucrose around 3 Å–1.In the D-SucH2O data (Figure B), sucrose shows
a steeper descent in the region 0.2–1 Å–1 and exhibits a small peak around 1.25 Å–1, which is not present in the trehalose data.In the H-SucHDO data (Figure C), there are few clear differences.
Trehalose exhibits a slightly larger peak than sucrose around 2 Å–1.In
the D-SucHDO data (Figure D), sucrose exhibits a small
shoulder between 1.2 and 1.6 Å–1, which is
not present in the trehalose data. Furthermore, the sucrose data show
a stronger peak at 2 Å–1, but trehalose exhibits
a more pronounced peak at 2.7 Å–1. In this
latter case, sucrose has a similar curve as the bulk water.In the H-Suc D2O data (Figure E),
sucrose features
a more pronounced peak at 3.9 Å–1 than trehalose.
An even more pronounced peak, although quite similar to sucrose, is
observed for bulk water at a similar Q-value.In the D-Suc D2O data (Figure F),
sucrose exhibits
a weak peak at 3.65 Å–1, which is not present
in the trehalose data. A similar peak is present in the bulk water
data.Differential cross sections, I(Q), of both sucrose and trehalose in a 1.1 M aqueous
solution. Full
lines show I(Q) of sucrose solutions
of different isotope compositions, and black dashed lines show I(Q) for the same isotope compositions
of the trehalose solutions.Zoomed-in
differential scattering cross sections for different
isotope compositions compared with different isotope compositions
of bulk water at the same temperature. Blue lines represent sucrose,
black dashed lines represent trehalose, and red dashed-dotted lines
represent bulk water. Corresponding differential scattering cross
section from X-ray measurement can be found in Figure S1.The steeper descent (point
3) is most likely due to differences
in the form factors between the different samples, which are related
to the size of the individual sugar molecules (see the Results and Discussion sections).
In general, however, it should be pointed out that the differences
between the I(Q)’s of the
sucrose and trehalose solutions are quite small, but where they differ,
it appears that the features of the sucrose solution are closer to
those of bulk water compared to the corresponding features of the
trehalose solution. These results indicate that the trehalose has
a stronger effect on perturbing the structure of the water from its
bulk-like properties.
Small-Angle Data Fitting
To determine
the size of the
individual sugar molecules, we fitted the small-angle data (in the
range 0.05–1 Å–1) of D-SucH2O and D-SucHDO (same isotope compositions for trehalose). The resulting
fits can be seen in Figure and resulted in a radius of 4.0 Å for sucrose and 4.2
Å for trehalose.
Figure 4
Small-angle data fitted for samples containing deuterated
disaccharides
in either H2O or HDO. Dotted lines show the fits to the
data.
Small-angle data fitted for samples containing deuterated
disaccharides
in either H2O or HDO. Dotted lines show the fits to the
data.Furthermore, no significant clustering
of either of the disaccharide
molecules was found, as also obtained in our previous study on only
trehalose.[1] This can be seen directly from Figure by the lack of any
significant small-angle scattering except that from the individual
disaccharide molecules (as highlighted in Figure ). We also calculated cluster distributions
from the EPSR models as seen in Figure . For this cluster distribution calculation two disaccharides
were classified as clustered if any of the disaccharideoxygens reside
within 2.5 Å of any other disaccharidehydrogen. Noticeably,
both disaccharides have a similar cluster distribution, where most
(∼80%) of the molecules are only bonding to water molecules.
A hard-sphere model was produced in EPSR, where all potential parameters
were set to zero (except from a minimum atom–atom distance
constraint of 0.8 Å to avoid atomic overlaps), for comparison.
The hard-sphere model represents a system where all disaccharides
are distributed randomly in the solution and can be seen to exhibit
more “clustering”a than the actual
EPSR models. This finding indicates that there is a preference against
the formation of clusters of disaccharide molecules in both solutions.
Figure 5
Cluster
size distribution of sucrose and trehalose in water. Cluster
criteria is defined here as when any of the hydroxyl oxygens of the
disaccharide is within 2.5 Å of an exchangeable hydrogen of any
other disaccharide. Dashed lines represent a hard-sphere model of
both disaccharides in water.
Cluster
size distribution of sucrose and trehalose in water. Cluster
criteria is defined here as when any of the hydroxyl oxygens of the
disaccharide is within 2.5 Å of an exchangeable hydrogen of any
other disaccharide. Dashed lines represent a hard-sphere model of
both disaccharides in water.
EPSR Fits
The resulting EPSR fits to the total differential
scattering cross sections are shown in Figure S2 for sucrose and in Figure S3 for
trehalose. We furthermore also fitted the model to the first order
difference of IDDD(Q)
– IHDD(Q), which
is shown in Figure (Fourier transformed to a real space representation). This differential
scattering cross section only contains correlations to the nonexchangeable
hydrogen atoms (M atoms), as discussed in greater detail below. Because
of the dominating signal of water–water interactions in the
total differential cross sections, this added differential scattering
cross section forces the EPSR model to also take the relatively small
signal of the M atoms into account.
Figure 6
Correlation functions obtained from the
Fourier transform of the
difference between the differential scattering cross sections from
D-Sug in D2O and H-Sug in D2O (red solid line
for sucrose and black solid line for trehalose). Red and black dashed
lines represent the Fourier transform of the corresponding EPSR fits
for sucrose and trehalose, respectively. The first peak in f(r) at about 1.1 Å is entirely due
to intramolecular C–M correlations and consequently not related
to the hydration of the disaccharides.
Correlation functions obtained from the
Fourier transform of the
difference between the differential scattering cross sections from
D-Sug in D2O and H-Sug in D2O (red solid line
for sucrose and black solid line for trehalose). Red and black dashed
lines represent the Fourier transform of the corresponding EPSR fits
for sucrose and trehalose, respectively. The first peak in f(r) at about 1.1 Å is entirely due
to intramolecular C–M correlations and consequently not related
to the hydration of the disaccharides.Although the fits capture most features of the experimentally obtained
diffraction data and are in relatively good agreement (compared to
e.g. previous mentioned studies on trehalose[1,33,34,41]), there are
still several discrepancies with the experimental data. These discrepancies
are definitely larger than the experimentally measured differences
between sucrose and trehalose. In fact, the total root-mean-square
deviation between the EPSR fits and sucrose or trehalose is 0.23 and
0.27 respectively, whereas the total root-mean-square deviation between
sucrose and trehalose is 0.13. For this reason, we stress that no
clear conclusions can be drawn from only EPSR modeling regarding structural
differences of the two solutions. However, despite this accuracy problem,
it is clear from the analysis presented below that EPSR can at least
qualitatively reproduce the experimentally observed structural differences
between the two solutions. The reason for this is most likely that
the experimental data contain some experimental (or data correction)
errors which makes it impossible to obtain full quantitative agreement
with the data obtained for all the isotopically different samples
(including X-ray diffraction data). Thus, the fits to the experimental
data are not excellent, but nevertheless the produced models seem
to be able to qualitatively reproduce most of the experimentally observed
structural differences between the two solutions. Furthermore, both
disaccharide solution models have been rerun several times, giving
almost identical results. For example, the models consistently produce
a larger distortion of the water structure in the case of trehalose
(as seen in Figures S4 and S5), in agreement
with direct experimental observations, as seen from the analysis of Figure given above. However,
because of the small structural differences between the two solutions
in relationship to the uncertainties in the models, all the observed
differences between the two sugar models cannot be regarded to be
fully established and conclusive.Nonetheless, quantitative
results are valuable to obtain to allow
us to compare our findings to previous works, such as those in refs (1, 33, 34, and 41). Within
the limits of the error bars, our hydration numbers of trehalose (Table S2) are consistent with these previous
studies,[1,33,34,41] although our interpretation of the experimental results
and models differs somewhat from those studies as further discussed
below.
First-Order Difference Method
To compare more detailed
information about the data with the model, a first-order difference
analysis method (as described in e.g. refs (48 and 49)) was also
used. In this method, the differential scattering cross sections of
(presumably) identical chemical composition with differing isotope
compositions are subtracted from each other. If the isotopes of a
specific atom pair of the two different samples are identical, these
are subsequently removed by the subtraction. In Figure , the differential scattering cross section
of H-Sug in D2O was subtracted from that of D-Sug in D2O and Fourier transformed to a real space representation;
because all atoms except the M atoms of the sugars are identical,
the only remaining pair correlations are those with the M atoms. The
resulting correlation function thus hides water–water correlations
and yields more information regarding water–sugar (54% scattering
contribution from M–Hw and 23% from M–Ow) and sugar–sugar
correlations (23%). Although this method adds plenty of specific information
regarding correlations with the M atoms, which otherwise would be
neglected by fitting the total scattering cross sections, it should
be pointed out that this method is unfortunately quite sensitive to
small errors in the data, which might come from the data corrections.
Therefore, the small differences between the two experimentally obtained
difference functions cannot be considered to be significant, but rather
the small differences indicate that the sugar–water interactions
are similar for the two solutions. The results from the EPSR modeling
are in this case not fully consistent with the experimental findings,
since the second and third peaks are stronger for trehalose due to
stronger M–water correlations.A similar, second-order
difference method was used to highlight the exchangeable hydrogen
atoms in the sample, which is shown in Figure S5 (red and black dashed lines), compared to the Hw–Hw
pair correlations obtained from EPSR for both sugar solutions and
with the Hw–Hw pair correlation of bulk water (as obtained
from refs (36 and 50)). The pair correlations of the exchangeable hydrogen
atoms were obtained by taking the Fourier transform of (IDDD(Q) + IDHH(Q)) – 2(IDHD(Q)). By performing this slightly more complex subtraction,
all correlations cancel out, except for the exchangeable hydrogen
atoms (Hw and H). The majority (90%) of this signal does, however,
originate from the Hw–Hw atoms (since they are more abundant).
Discussion
Throughout this section the reader should keep
in mind that the I(Q)’s indicate
very minor differences
between sucrose and trehalose (details on differences between the
data sets can be seen in Figure ), and, furthermore, the EPSR models are not able to
reproduce the experimental data in all details. This means that there
may be important features which the models fail to capture or, conversely,
that features may be obtained that are not present in the data. That
being said, if the models capture features that can be seen by a direct
analysis of the experimental data (see Figure ), it is a good indicator that the models
have captured “true” features, and they can thus be
used to quantify these features. Furthermore, these differences can
also be corroborated by other studies, such as measurements of glass
transitions, viscosity, and dynamical measurements, as discussed below.
Disaccharide–Water
Interactions
A greater water-destructuring
effect of trehalose compared to sucrose has been previously shown
in the literature.[10,14,21,28−32] This issue is important to explain the superior cryo-protective
effect of trehalose. For example, a stronger destructuring effect
should in principle lead to less crystallizable water, which could
otherwise damage biological materials during cooling, and indeed it
has been shown by, for example, calorimetric measurements that trehalose
prevents more water from crystallization than sucrose.[5] The results presented in Figure clearly show that the intermediate structure
(in the range 1–4 Å–1) of these solutions
is more similar to that of bulk water in the case of sucrose than
in the case of trehalose, which is also supported from the EPSR model,
as seen in Figure S4, for example. These
results support the idea that trehalose perturbs the network structure
of bulk water more efficiently than sucrose. The reason for this stronger
destructuring effect has been suggested to be coupled to a couple
of different, not necessarily opposing, ideas. One of these is that
trehalose binds to more water molecules, as suggested by, for example,
ref (26). Another common
hypothesis is that the way water binds to trehalose alters the three-dimensional
structure of bulk water more than in the case of sucrose.[16] Because the present experimental and EPSR results
are not giving support for that there is any substantial difference
in the number of water molecules trehalose and sucrose bind to, the
latter explanation for the stronger destructuring effect of trehalose
seems most plausible. Thus, the specific water–disaccharide
interactions determine how the water molecules rearrange themselves
around the disaccharide, which in turn determines how the water structure
is perturbed. This observation has also been indicated in previous
studies.[12,13]Another important related aspect regarding
how trehalose interacts with water is how it changes the dynamics
of water. It has been shown, by multiple different studies, that trehalose
exhibits a stronger dynamical coupling (i.e., longer residence times
of a water–trehalosehydrogen bond and slower diffusion of
water for trehalose than for other disaccharides).[21,25,31,51] A stronger
dynamic coupling indicates more and/or stronger hydrogen bonds between
the two molecular species. From the present results it is, however,
surprisingly difficult to determine any such differences since both
disaccharides exhibit similar hydration numbers and similar hydrogen
bonding distances to the atoms of the water molecules (see Figure , Figure S6, and Table S2). Thus,
there is no obvious structural reason for the different dynamical
properties[21,25,31,51] of the two different sugar types.
A Note
on the New EPSR Model of Trehalose and Water Structure
The
new trehalose model produced in this work differs somewhat
from our previous paper on trehalose in aqueous solution.[1] As pointed out by Soper et al.,[34] X-ray diffraction data contain complementary information
to neutron diffraction data, and particularly oxygen–oxygen
correlations become more strongly weighted in X-ray diffraction data.
Thus, the inclusion of X-ray diffraction data produces a more accurate
model of the water structure in each sugar solution. Other differences
for the present trehalose model are that we used a larger simulation
box (4000:104 water:trehalose molecules instead of 2000:52) and that
the influence of the empirical potential was constrained to a lower
value in the current work. The main difference between this new model
and our previous model is that the current model produced a slightly
smaller effect on the structure of water than was previously obtained;
thereby this result agrees more with what was obtained by Pagnotta
et al.[33] Soper et al. (coauthors of ref (33)) performed a new study
on aqueous trehalose which included the data provided from our own
previous study[1] and with the addition of
X-ray data for the two trehalose concentrations provided in their
previous paper.[33] In their new study,[34] they came to the same conclusion again that
trehalose forms weak bonds with water and does not significantly perturb
the water structure. Their obtained pair correlation functions are
very similar to those presented for trehalose in this paper, and therefore
we agree with their presented molecular model (see, for example, Figure
7b of ref (34) compared
to Figure S5 for water–water correlations).
We also partly agree with their conclusion that trehalose (and sucrose
as seen here) form relatively weak bonds with water. However, their
conclusions about the minor destructuring effect of trehalose differs
somewhat from that presented here.The partial pair correlation
functions presented here for both trehalose and sucrose (Figure S6) are quite similar compared to those
of previous studies on mannose[52] or cellobiose[43] but indicate less bonding than compared to glucose.[52] It should however be pointed out that the concentrations
in those studies differ from the one presented here, and therefore
the results are not directly comparable. Nonetheless, compared to
other sugar molecules neither trehalose nor sucrose exhibits extraordinary
weak or strong water interactions. Furthermore, Soper et al.[34] refer to a paper by Towey et al.[42] in which the correlations between water and
glycerol were found to be strong in comparison to the disaccharides
presented here. However, Towey et al. claim in a later study[53] that glycerol perturbs the typical tetrahedral
structure of bulk water less than trehalose. They found that trehalose,
which data were obtained from Pagnotta et al.,[33] shifts the second peak position of gOwOw more than glycerol (for about 20 water molecules per glycerol)
and should thus be even more efficient in perturbing the tetrahedral
water structure.Soper et al.[34] also
bring up the issue
that the first peak of gOwOw increases
with the addition of trehalose. Indeed, such an effect can be seen
also for sucrose, and it was brought up in ref (1), too; however, it was pointed
to that it is precisely this additional water in the first coordination
shell of a water molecule which was proposed to give rise to the water
destructuring effect. This is highlighted by Figure S4, showing that the addition of trehalose (and sucrose) promotes
O–O–O triplet angles of 60°, corresponding to an
equilateral triangular formation,[54] rather
than the tetrahedral structure at 109°. This is suggested to
be due to the presence of an interstitial water molecule in the first
coordination shell of the water. If some of the water molecules become
relatively more packed, this should be associated with an increase
in density, which indeed is indicated by the fact that the density
of the aqueous trehalose solution is slightly higher than that of
the sucrose solution at the same concentration and temperature (1.1296
and 1.1270 g/mL for trehalose and sucrose, respectively).
Intra-
and Interdisaccharide Interactions
Lerbret et
al.[14] have performed a set of simulations
which suggest that trehalose has a more open structure in aqueous
solutions than sucrose, that is, that sucrose forms more intramolecular
hydrogen bonds. This has also previously been shown by X-ray diffraction,[55] where the authors showed that sucrose forms
more intramolecular hydrogen bonds, exhibiting a closer more compact
structure, as the concentration is increased above ∼22 wt%
sucrose (below this concentration no intramolecular hydrogen bonds
are formed). Here we study a sucrose solution of 33 wt% sucrose and
thus expect, according to ref (55), that some, but few, intramolecular hydrogen bonds exist.
The only clear indication of this was seen from the form factor analysis
(see Figure ), which
shows that, on average, sucrose has a slightly smaller radius of gyration
than trehalose, which indicates that the sucrose molecules are slightly
more folded than the trehalose molecules.The idea that sucrose
forms more intramolecular bonds with increasing disaccharide concentration
can also explain why sucrose has a significantly higher solubility
than trehalose. In the low water limit, sucrose forms multiple intramolecular
hydrogen bonds,[55] whereas trehalose remains
unfolded, and thus has more of its hydrogen-bonding sites available
for interactions with other molecules.[14] For this reason, sucrose only requires about 8.9 water molecules
to cover its smaller interactive surface, whereas 17.3 water molecules
are required to prevent trehalose molecules from directly interacting
with each other. However, in this study, the disaccharide solutions
were too diluted for these effects to be evident, and we can only
conclude that if such a structural difference is present, it is more
prominent at lower water concentrations.
Conclusion
It
may be expected that the structural differences between aqueous
sucrose and trehalose should be large due to their different macroscopic
and dynamical properties. However, the diffraction data clearly exhibited
only small discrepancies in the overall structures of the two solutions
(see Figure ). On
the basis of the isotope subtraction method to highlight interactions
with the carbon-bound hydrogen atoms (M atoms), as shown in Figure , it could be seen
that the M atoms of the two sugars bind to similar numbers of water
molecules in the two solutions. Although the structural EPSR models,
based on the differential scattering cross-section data, suggest that
sucrose binds slightly more water molecules in total, the difference
is so small that it cannot be established due to the uncertainties
in the EPSR produced structural models. Furthermore, directly from
the diffraction data, as seen in Figure , it was evident that there are no clear
differences in intermolecular clustering of the sugar molecules, since
neither sucrose nor trehalose shows a preference of forming clusters.
The differences that were observed in the experimentally obtained
scattering data do, however, provide key insights into the subtle
differences these molecules exhibit. First of all, it was shown that
the structure factor of bulk water is more similar to that of sucrose
than to trehalose, thus indicating that trehalose has a stronger perturbing
effect on the structure of water. Second, the overall radius of gyration
was slightly larger for trehalose than for sucrose, and, finally,
the water molecules seem to interact slightly differently with the
different atomic sites of the two disaccharides. All these observations
are in line with what has previously been shown by others[10,14,21,28−31,55] and can partly explain why the
solubility of sucrose is higher than for trehalose and, more importantly,
provides possible explanations for why trehalose is superior to sucrose
as a biological stabilizer.
Authors: Philip E Mason; George W Neilson; John E Enderby; Marie-Louise Saboungi; Gabriel Cuello; John W Brady Journal: J Chem Phys Date: 2006-12-14 Impact factor: 3.488
Authors: Alan K Soper; Maria Antonietta Ricci; Fabio Bruni; Natasha H Rhys; Sylvia E McLain Journal: J Phys Chem B Date: 2018-07-17 Impact factor: 2.991
Authors: Wafaa Alabsi; Maria F Acosta; Fahad A Al-Obeidi; Meredith Hay; Robin Polt; Heidi M Mansour Journal: Pharmaceutics Date: 2021-08-17 Impact factor: 6.321