Open Access Article
Reece
Nixon-Luke
a,
Jochen
Arlt
b,
Wilson C. K.
Poon
b,
Gary
Bryant
*a and
Vincent A.
Martinez
*b
aSchool of Science, RMIT University, Melbourne, Victoria 3000, Australia. E-mail: gary.bryant@rmit.edu.au
bSUPA, School of Physics and Astronomy, The University of Edinburgh, Peter Guthrie Tait Road, Edinburgh, EH9 3FD, UK. E-mail: vincent.martinez@ed.ac.uk
First published on 11th February 2022
Few techniques can reliably measure the dynamics of colloidal suspensions or other soft materials over a wide range of turbidities. Here we systematically investigate the capability of Differential Dynamic Microscopy (DDM) to characterise particle dynamics in turbid colloidal suspensions based on brightfield optical microscopy. We measure the Intermediate Scattering Function (ISF) of polystyrene microspheres suspended in water over a range of concentrations, turbidities, and up to 4 orders of magnitude in time-scales. These DDM results are compared to data obtained from both Dynamic Light Scattering (DLS) and Two-colour Dynamic Light Scattering (TCDLS). The latter allows for suppression of multiple scattering for moderately turbid suspensions. We find that DDM can obtain reliable diffusion coefficients at up to 10 and 1000 times higher particle concentrations than TCDLS and standard DLS, respectively. Additionally, we investigate the roles of the four length-scales relevant when imaging a suspension: the sample thickness L, the imaging depth z, the imaging depth of field DoF, and the photon mean free path
. More detailed experiments and analysis reveal the appearance of a short-time process as turbidity is increased, which we associate with multiple scattering events within the imaging depth of the field. The long-time process corresponds to the particle dynamics from which particle-size can be estimated in the case of non-interacting particles. Finally, we provide a simple theoretical framework, ms-DDM, for turbid samples, which accounts for multiple scattering.
On the other hand, scattering techniques are ideal for characterising suspended nanoparticles: they are non-destructive and suitable for a variety of solvents, including physiologically relevant media. Static light scattering (SLS), small angle X-ray scattering (SAXS) and small angle neutron scattering (SANS) all rely on the fact that the angle-dependent scattered intensity is sensitive to the particle composition, size and shape.8 They have been used to characterise a broad range of complex particles in solution such as drug delivery systems2 and solid-lipid nanoparticles.3 However, these techniques require specialised instrumentation and considerable expertise in analysis.
Unlike the methods mentioned so far, dynamic light scattering (DLS) measures particle size via particle dynamics.9,10 Standard DLS does so by measuring the temporal autocorrelation function (ACF) of the far-field scattered intensity at a specified scattering vector
, which specifies the length scale l = 2π/q (with q = ‖
‖) at which the particle dynamics are being probed.
For diffusive monodisperse spheres, the ACF decays exponentially with a characterisitic time that depends inversely on the particle size provided that the detected photons have only been scattered once. Thus conventional DLS only works when the turbidity is negligible either because the concentration is low, or because the solvent and particles have very similar refractive indices. Dynamics in concentrated samples may also be probed, but only after care is taken to eliminate multiple scattering by refractive index matching.11 This is not possible for most samples, so methods have been developed to suppress the signal from multiple scattering, such as two-colour DLS (TCDLS)12 and 3D DLS.13,14 The synchrotron-based analogue of DLS, XPCS, does not suffer from multiple scattering, but is only available at central facilities and suffers from beam-damage problems.15 Finally, diffusing wave spectroscopy (DWS) deals with multiple scattering by seeking to model it explicitly to extract particle mean squared displacements from turbid systems, but requires knowledge of the hard-to-measure photon mean free path and gives no information on the q-dependant dynamics.16
Differential dynamic microscopy (DDM) is a relatively new technique for characterising particle dynamics in solution.17,18 The method extracts dynamical information by measuring the spatio-temporal intensity fluctuations from microscopy movies. Interestingly, recent studies have shown that DDM5,19–22 and related techniques such as heterodyne near-field scattering23 and confocal DDM24,25 appear to be less affected by multiple scattering than DLS, making it possible to investigate concentrated suspensions of colloids22 or micro-organisms26 without index matching.
However, the physical origins of DDM's insensitivity to multiple scattering remain unclear. The sample turbidity is, as in DWS, characterised by the photon mean free path
, which is a function of the particle size and shape, refractive indices of the particles and solvent, and the particle volume fraction ϕ. However, there are three other relevant length scales characterising the experimental implementation of DDM: the sample thickness L, the imaging depth z, the imaging depth of field, DoF, Fig. 1. The range of turbidities over which DDM is applicable must depend on the three dimensionless ratios (L/
, z/
, DoF/
).
Here, we investigate this dependence systematically in dilute colloids by tuning L and
, in the latter case via the particle radius R and volume fraction ϕ. We first compare DDM with DLS and TCDLS and discuss its advantages and limitations. We find that DDM can reliably size particles at up to ≈25× higher particle concentrations than TCDLS. We then investigate the roles of the length scales mentioned above, extending previous studies18,27,28 to turbid samples. We find the emergence of a short-time decay process that appears as ϕ increases, which we associate with multiple-scattering events. We examine the source of this process and provide a simple theoretical framework for DDM that accounts for multiple scattering.
to the relevant sample dimension L. The mean free path scales with the scattering cross-section of individual scatterers σ and their number density as
∝ 1/(σϕ). For simple spherical scatterers, as considered here, σ can be computed from Mie theory in terms of the particles' radius, their (complex) refractive index and that of the suspending medium, and the incident wavelength.29,30
Scattering can be considered as a Poisson process, and the probability that a photon gets scattered n times can be estimated from the mean number of scattering events
= L/ = −ln(T/T0), | (1) |
≪ 1 it is sufficient to consider only single scattering events. In general, however, singly-scattered photons (P1) represent only a fraction of the total scattered light (Psc):![]() | (2) |
= L/
= 1/5, multiple scattering already contributes ≈10%, and becomes dominant for L/
≳ 1.3. Multiple scattering speeds up the decay of the intensity ACF measured in DLS.31 However, this effect is difficult to quantify except in the extreme DWS limit.16
| gDLS(q, τ) = 1 + β2|f(q, τ)|2 | (3) |
is the magnitude of the scattering vector
defined by θ, with λ the laser wavelength and n the refractive index of the solvent. For non-interacting mono-disperse Brownian spheres,| f(q, τ) = exp(−τ/τr) | (4) |
| D0 = kBT/6πηR, | (5) |
. Cross-correlation of the two scattered intensities (XCF) allows suppression of the multiple scattering and yields the ISF:| gTCDLS(q, τ) = 1 + β2βOV2βMS2|f(q,τ)|2, | (6) |
g(s)DDM ( , τ) = 〈|I( , t + τ) − I( , t)|2〉t | (7) |
, t) is the Fourier transform of the recorded image I(
, t), with
the pixel position in the image, and brackets denote averaging over t. In transmission microscopy, the image is formed by the incident light I0 traversing the pure solvent minus the light scattered by particles in the object plane, Is, giving rise to a spatio-temporally varying measured intensity I:34I( , t) = I0( , t) − Is( , t) | (8) |
, t). Note that for bright field microscopy Is can be locally negative but is positive when averaged over the field of view. Using eqn (8), eqn (7) becomes![]() | (9) |
) = 2〈|ΔI0(
)|2〉. In practice, B represents the instrumental noise and is a combination of the incident light and camera uncorrelated noises. For isotropic motion and under appropriate optical conditions, so that the scattered intensity fluctuations are proportional to the density fluctuations (ΔIs ∝ Δρ), eqn (7) yields the ISF via33,34| g(s)DDM(q, τ) = A(q)[1 − f(q, τ)] + B(q). | (10) |
(q)|2S(q) is the amplitude of the static signal of the sample, where S(q) is the structure factor and
(q) is the single particle amplitude combining the effects of the particle form factor P(q) and the optical transfer function T(q) of the imaging system, which can be seen as the contrast of the particles in the image. For non-interacting particles and negligible turbidity, A ∝ ϕ as previously demonstrated.26
I( , t) = I0( , t) − Is( , t) − Im( , t) | (11) |
![]() | (12) |
| g(m)DDM(q, τ) = A(m)(q)[1 − αf(q, τ) − (1 − α)f(m)(q, τ)] + B(m)(q) | (13) |
the normalised correlation function of the multiply-scattered intensity fluctuations, and B(m)(q) = B(q) + B×. The signal amplitude A(m)(q) = 2(〈|ΔIs(q)|2〉 + 〈|ΔIm(q)|2〉) can be independently estimated using eqn (1), which accounts for the attenuation of the intensity reaching the detector, and the definition of A(q) from eqn (10):![]() | (14) |
Most of the videos were recorded using a frame rate of 100 fps, but for some of the samples we also acquired movies at 1000 fps in order to investigate the emergence of short-time processes. A table showing the conditions used for all experiments is in the ESI† (Table S2). A bespoke LABVIEW program was used to calculate the DICFs from the videos based on eqn (7), which were then fitted using eqn (4) and (10). The resulting fitted D(q) were then averaged over the range 1.5 < q < 4 μm−1, where reliable fitting were obtained, to yield the averaged diffusion coefficient D. The amplitude of the signal 〈A〉 (ϕ) was obtained by normalising the fitted A(q, ϕ) to an arbitrary reference sample A(q, ϕ0) and then averaged over the above q range.
![[small script l]](https://www.rsc.org/images/entities/h3_char_e146.gif)
(eqn (1)), and thus the volume fraction ϕ. Fig. 2 shows the visual appearance of the SYS250 suspensions in cylindrical tubes (4 mm diameter) used for DLS and TCDLS measurements and of the SYS210 suspensions in 400 μm-height capillaries used for DDM measurements, both as a function of concentration.
![]() | ||
| Fig. 2 Pictures of (top) SYS250 particle suspensions in cylindrical tubes (4 mm diameter) used for DLS & TCDLS measurements and (bottom) SYS210 in 400 μm-height capillaries used for DDM measurements, both with increasing ϕ from left to right. See Table S2 (ESI†) for values of concentration. Top image: Highest ϕ ≈ 1.6%. Pictures were recorded using a Huawei Mate 10 Pro camera with a blue background. | ||
We quantified the turbidity by measuring the light transmitted through the sample (eqn (1)), which can be estimated from the mean intensity of microscope images, provided that these are recorded with the same illumination settings.5 We therefore recorded sets of movies covering a wide range of ϕ using identical illumination settings (but tuning the exposure time to compensate for the limited dynamic range of our camera). These movies allowed us to estimate transmission as well as the relative amplitude of the DDM signal as a function of ϕ (Section S2, ESI†). The transmission measurements were validated using an additional custom-made setup based on laser-light rather than white light (Section S4, ESI†).
![]() | ||
| Fig. 3 Typical DICFs, gDDM(q, τ), obtained from DDM as a function of delay time τ at q ≈ 1 μm−1 measured for several volume fractions of SYS250. Lines are fits using eqn (10) and (4). The corresponding movies (100 fps, 1024 × 1024 pixels, 20) were recording at variable incident intensity to maximise the signal amplitude. | ||
We find four regimes of behaviour as ϕ increases. Regime 1 is the single-scattering regime, where the TCDLS intercept remains at its nominal value of ≈0.6, i.e., only singly-scattered light is being detected. In this regime, all techniques return similar D(ϕ).
In regime 2, the intercept drops as ϕ increases, indicating an increase in multiple scattering. This produces faster intensity fluctuations, so that D(ϕ) measured by DLS increases. As TCDLS suppresses contributions from multiple scattering, it still returns a valid (constant) D(ϕ) in this regime.
In regime 3, the TCDLS intercept drops to zero as there are not enough single-scattered photons reaching the detector. Note that TCDLS now measures noise and delivers a null rather than false result, contrasting with DLS in regime 2. In this regime, DDM carried out using glass capillaries with L = 400 μm (blue open symbols) is able to return an accurate D(ϕ) up to ϕ = 2.5%. This limit is 25× higher than for TCDLS, and will be discussed further in Section 4.3. The multiple scattering contribution to DDM in this regime will be discussed in Section 4.2.
In regime 4, samples in L = 400 μm DDM capillaries appear extremely turbid, Fig. 2, and only a small fraction of incident light is transmitted. Even with the microscope light source set to maximum, only a very low signal is detected on the camera. The resulting DICFs are approximately τ-independent: the noise term B(m)(q) overwhelms the amplitude of the DDM signal A(q), eqn (13).
Significantly, using a thinner capillary, L = 100 μm, allowed measurements of D(ϕ) up to ϕ ≈ 10%, which is the undiluted stock solution, Fig. 4a (open blue symbol). This finding will be discussed in detail later (Section 4.2).
Results collected using a smaller particle size (SYS140), Fig. 4b, confirms these findings, although regime boundaries shift to higher ϕ. This is consistent with eqn (1), as one expects
to increase when R decreases (see Section 4.2). Now, regime 4 is beyond the highest concentration studied, so DDM is able to deliver reliable D(ϕ) over the whole of our concentration regime. Note that, as expected, D increases slightly with ϕ due to particle interactions.35
These results demonstrate that the maximum ϕ measurable with DDM is a function of both the sample thickness L/
and the particle radius R/
. They highlight the importance of measuring the photon mean free path
to fully identify and understand the limitations of DDM and its practical use for turbid samples.
![[small script l]](https://www.rsc.org/images/entities/h3_char_e146.gif)
(ϕ) using eqn (1), shown in Fig. 5b together with validating values extracted using a laser-based experimental setup (see Section S4, ESI†). Our measured
are also in good agreement with values predicted from Mie theory (Section S4, ESI†) up to ϕ ≈ 0.7%. At ϕ ≥ 0.7%, the relative transmission increasingly deviates from an exponential decay, Fig. 5a, suggesting significant contributions from multiple scattering and leading to an over-estimation of
, Fig. 5b.
![]() | ||
Fig. 5 (a) Transmission, measured directly from DDM movies, as a function of volume fraction ϕ for SYS210 with L = 400 μm. Dotted line: Guide to the eye. Solid line: Exponential fit with exponent −L/ = −ϕ/(0.49%). Dashed line: Estimated transmission for a thinner capillary with L = 100 μm. Inset: Corresponding measured diffusion coefficient D/D0, with D0 = 2.14 μm2 s−1. Arrows show the last volume fraction for which D was measurable. Grey area: Limit in transmission (≈6–7%) above which DDM delivers reliable measurements. (b) photon mean free path obtained from transmission measurements of (circles) DDM movies and (diamonds) laser-based setup as a function of ϕ for SYS210. Lines are predictions of from Mie scattering theory for the three particle size as indicated. The red horizontal lines indicate the sample thickness for our light scattering (dotted – L = 4 mm) and DDM experiments (dashed – L = 400 μm). Inset: Normalised signal amplitude 〈A〉 versus ϕ using ϕ0 ≈ 0.1% as reference. Line is fit to the data using eqn (14). The red and blue areas define the regimes of single scattering and emerging multiple scattering, respectively, for DDM experiments with L = 400 μm. | ||
Our results indicate that DDM measurements of D are reliable up to ϕ = 4% (inset Fig. 5a), corresponding to L/
≈ 10 (using predicted
values). In other words, although most of the detected light has been scattered more than once, DDM can still deliver reliable D values down to ≈6–7% transmission (grey area in Fig. 5a).
To further understand DDM for turbid samples, it is useful to identify the volume fraction ϕs, corresponding to the ϕ-boundary between single scattering regime and when multiple scattering emerges.
At low ϕ, where particle interactions are negligible and S(q) → 1, we expect from eqn (14) that 〈A〉 ∝ ϕ if multiple scattering can be neglected. This is indeed the case, Fig. 5b (inset). However, non-linearity, and indeed non-monotonicity, is observed at higher ϕ. These deviations arise from multiple scattering, which start to emerge at the threshold of ϕs ≈ 0.1%, corresponding to
(ϕs) ≈ 1.6 mm for SYS210, Fig. 5b. In other words, multiple scattering starts to affect the (static) DDM signal amplitude when L/
→ 1/4, where single scattering constitutes ≈88% of the signal. This value agrees with that found by a second approach based on TCDLS data (Section S5, ESI†).
∝ 1/ϕ, we expect the multiple-scattering threshold to scale as ϕs ∝ 1/L. Fig. 6 shows that this is at least qualitatively correct: 〈A〉 deviates from a linear ϕ-dependency at increasing ϕs values when L is reduced from 400 to 100 μm. As a consequence, DDM is able to measure D reliably at concentrations up to that of the stock solutions, ϕ ≈ 10%, when using L = 100 μm (inset). Fitting the normalised 〈A〉 with eqn (14) gives good quantitative agreement, so that the increase in overall signal is indeed due to a reduction in multiple scattering events.
![]() | ||
| Fig. 6 Effect of thickness L on DDM measurements (100 fps) for SYS250. (main) amplitude of DDM signal 〈A〉 normalised to an arbitrary reference sample A0 at ϕ ≈ 0.1% and L = 400 μm versus ϕ for L = 100, 200, 400 μm. All Movies were recorded with fixed illumination and varying exposure time, except for (△) for which exposure time was fixed and illumination adjusted. Note that the normalisation takes into account differences in exposure time. Dotted line shows a slope of 1. Inset shows the corresponding measured D/D0 for the higher ϕ. Arrows define the highest ϕ at which DDM delivered a successful measurement. Lines are fits using eqn (14). | ||
![]() | ||
| Fig. 7 DDM measurements (100 fps) as a function of focal depth z of the imaging plane for SYS210. (left-axis) D and (right-axis) amplitude 〈A〉 and mean intensity 〈I〉, normalised to their corresponding value at z = 0, versus z for L = 400 μm at ϕ = 1.6%. Continuous line is an exponential fit to the normalised amplitude using eqn (14) for z ≤ 200 μm yielding a characteristic length-scale of z0 ≈ 380 μm. | ||
This does not, however, mean that DDM should be performed at as small z as possible to maximise signal. Fig. 7 shows that the measured diffusivity remains constant throughout the central region of the sample, but starts to decrease from z ≈ 50 μm, dropping by ≲5% close to the bottom interface. As we show in Section S6 (ESI†), this drop in diffusivity is far too large and long range to be explained by hydrodynamic interactions with the wall, but instead is mostly caused by sedimenting aggregate clusters. Thus experimental constraints, such as sample purity, might require a fairly large ‘safe distance’ from the sample edges. Selecting a sample twice as high and imaging near its mid plane18 will optimise DDM performance for turbid samples.
To show this, we recorded movies at 1000 fps, 10× higher than in any experiment reported so far, giving access to DICFs at one decade shorter τ. This reveals a second correlated process at short time, as shown for q = 0.65 μm−1 in Fig. 8. We identify this as the f(m)(q, τ) term in our ms-DDM result, eqn (13) due to correlated fluctuations in the multiply-scattered intensity.
![]() | ||
| Fig. 8 DICFs of SYS250 at q = 0.65 μm−1 recorded at a higher frame rate (1000 fps) with L = 100 μm revealing a 2nd decorrelation process at short delays, which at this q is much faster than diffusion and has a very low amplitude (note log scale for amplitude). Lines are fits based on eqn (15). | ||
We fit these DICFs with a double generalised exponential:
| g(q, τ) = A(q)[1 − αe−(τ/τr1)β1 − (1 − α)e−(τ/τr2)β2] + B(q) | (15) |
Fig. 9 shows the q-averaged values, 〈tr2〉 and 1 − 〈α〉, as functions of ϕ at three values of L. Over this ϕ range, we find a constant β2 ≈ 0.8 ± 0.1. As ϕ (and therefore turbidity) increases, we find that the short-time process speeds up (main figure) and its relative amplitude increases (inset). This is consistent with our identification of this short-time process with the f(m)(q, τ) term eqn (13).
![]() | ||
| Fig. 9 Average decay time of the short-time process (main) and relative fractional contribution (inset) as a function of volume fraction for data presented in Fig. 8. Error bars are standard deviation of the mean obtained in the range 0.3 ≤ q ≤ 1 μm−1. | ||
Interestingly, the time-scale, 〈τr2〉, and amplitude, 1 − 〈α〉, of the fast process do not seem to change with the sample thickness L, Fig. 9; nor do they depend on the imaging depth z, Fig. 10. This suggests that the short-time process mainly depends on the thickness of the imaged sample region, i.e. the DoF.
The depth of field, DoF, defines the imaging region (II) centred around the object plane. The intensity fluctuations, ΔI, in the images captured by the camera are dominated by scattering within this region. As such, only light scattered in this region and reaching the camera contributes to the DDM signal, as was already pointed out in the earliest discussion of the technique.18 Increasing the sample thickness L beyond the DoF (and thus introducing regions I and III) generates no extra useful DDM signal. For dilute samples, there is no detrimental effect of these regions either, and larger sample thickness can offer experimental advantages such as ease of loading, handling and focusing, avoidance of boundary effects and signal distortions due to sedimenting ‘impurities’ within the sample.
However, once the suspension is turbid enough, a significant fraction of light scattered by the sample is no longer collected by the objective. The light detected by the camera is reduced by its passage through the complete sample thickness L. Our measurements for different sample thickness (Fig. 6) confirm that the drop of DDM signal amplitude with increasing volume fraction is controlled by the sample thickness L and is in quantitative agreement with eqn (14). Thus both regions I and III introduce extra attenuation, which can lead to premature failure of DDM measurements.
Our measurements for varying imaging depth z (Fig. 7) reveal a secondary effect of the near-objective region III, as z controls the thickness of the layer through which light from the object plane has to propagate to reach the camera. Apart from scattered light no longer reaching the camera, this region of the sample can also scatter light which had been scattered in the object plane (region II) to reach the camera at random positions (e.g. orange ray (d) in Fig. 1). This reduces the contrast,
(q), of the particles in the image. We observe an exponential reduction of the DDM signal amplitude with the thickness of region III, z (Fig. 7), with a characteristic length scale z0 ≈ 380 μm ≈ 4
.
Our experimental investigation of the emergent short-time process highlights that the ‘extraneous’ sample regions I and III only affect the static DDM signal (〈A〉), but have no measurable effect on the dynamic DDM signal (g(q, τ)). This might at first appear surprising, especially when noticing that the short-time process is detectable at volume fractions where
is still much larger than the depth of field (i.e. ≲10 μm) visually perceived from direct imaging. However, the DoF strongly depends on the Fourier wavenumber q and typically increases with decreasing q.18 We have verified, using a recently introduced experimental protocol,36 that our measured DoF is indeed a strongly decreasing function of q (Section S7, ESI†). For example, we find DoF ≈ 20 μm at q = 0.5 μm−1 and DoF ≈ 4 μm at (q = 3 μm−1). These values are comparable to
values (Fig. 5) at the higher volume fractions considered in this study. We may therefore expect that the f(m)(q, τ) term in eqn (13) should become important at low q (large DoF). Observation of the DICFs at ϕ = 1.6% for several q values (Section S8, ESI†) suggests the short-time process emerges at q ≲ 1.2 μm−1 for which DoF ≈ 10 μm, i.e. DoF(q)/
> 1/7, using
(ϕ = 1.6%, SYS250) ≈ 70 μm (Fig. 5).
Interestingly, this ‘dynamical’ threshold DoF/
≈ 1/7 for the emergence of the short-time process corresponds to 7% multiple scattering contribution to the overall signal, eqn (2), in good agreement with the 12% static threshold (Section 4.2).
From a TCDLS perspective, the relevant length-scale is the sample thickness L (or diameter of the DLS tube) because a DLS measurement relies on a well defined scattering angle. Assuming multiple scattering affects TCDLS and DDM measurements in a similar way, we would expect the ratio of the highest concentration measurable by DDM and TCDLS to corresponds approximately to the ratio LTCDLS/LDDM. However, we found a significantly higher ratio of ≈25 for LTCDLS/LDDM = 10 (see Section 4.1). This finding suggests that DDM is indeed more efficient than a DLS-based setup in its capability to work at smaller relevant length-scales, here (L, z, DoF).
While this discussion and our current study pertains entirely to scattering, the same analysis should also be applicable to strongly absorbing particles. In this case, the light absorbed by the particles is equivalent to the scattering events in regions I and III that give rise to light not being collected by the camera.
Multiple scattering effects do still affect the practice of DDM. In particular, we have shown that it contributes a short-time process that complicates data interpretation. Our results suggest that the length scale that controls the emergence of this process is the depth of field rather than the sample thickness L. In practice, these complications can be avoided by only using data at sufficiently high q, say ≳1 μm−1, and long enough delay time, say ≳0.01 s. With these provisos, we conclude that DDM should be a robust method for characterising turbid suspensions.
Footnote |
| † Electronic supplementary information (ESI) available. See DOI: 10.1039/d1sm01598b |
| This journal is © The Royal Society of Chemistry 2022 |