1 Introduction
The study of turbulence-enhanced inertial particle collision in isotropic turbulence could improve our understanding and modelling of many particle-laden turbulent flows in nature. For example, water droplet development in the ‘size-gap’ in warm clouds is believed to be dominated by turbulence-induced particle collision (Shaw Reference Shaw2003). The formation of planetesimals in protoplanetary disks is believed to begin with small dust grains that collide and coalesce in turbulent protoplanetary nebulae (Dullemond & Dominik Reference Dullemond and Dominik2005; Zsom et al. Reference Zsom, Ormel, Guettler, Blum and Dullemond2010).
These phenomena are associated with high-Taylor-microscale Reynolds numbers (
$R_{\unicode[STIX]{x1D706}}$
) and a wide range of particle Stokes numbers (
$St$
). For example, in cumulus clouds,
$R_{\unicode[STIX]{x1D706}}=O(10^{5})$
and
$St\approx 0.01{-}2$
(Siebert, Lehmann & Wendisch Reference Siebert, Lehmann and Wendisch2006; Ayala et al.
Reference Ayala, Rosa, Wang and Grabowski2008), while in protoplanetary nebulae,
$R_{\unicode[STIX]{x1D706}}=O(10^{4}){-}O(10^{6})$
and
$St\approx O(1){-}O(10^{3})$
(Cuzzi et al.
Reference Cuzzi, Hogan, Paque and Dobrovolskis2001). However, since high
$R_{\unicode[STIX]{x1D706}}$
can neither be generated through typical laboratory facilities nor through high-performance computing, many researchers have studied inertial particle collisions in isotropic turbulence at relatively low Reynolds numbers (
$R_{\unicode[STIX]{x1D706}}=50{-}500$
). In order to understand whether findings from lower Reynolds numbers are applicable to naturally occurring high-Reynolds-number turbulent flows, it is necessary to quantify the effect of
$R_{\unicode[STIX]{x1D706}}$
on the particle collision rate in isotropic turbulence.
On the other hand, particle collision is also influenced by particle inertia in relation to turbulent flow, or the Stokes number
$St$
(Sundaram & Collins Reference Sundaram and Collins1997; Pan & Padoan Reference Pan and Padoan2013; Ireland, Bragg & Collins Reference Ireland, Bragg and Collins2016a
). In different
$St$
ranges, the effect of
$St$
on particle collision may be dominated by different mechanisms (Bragg & Collins Reference Bragg and Collins2014a
,Reference Bragg and Collins
b
; Bragg, Ireland & Collins Reference Bragg, Ireland and Collins2015b
). It is necessary to quantify, for a wide
$St$
range, the effect of
$St$
on particle collision in isotropic turbulence.
While particle collision itself is difficult to model numerically and capture experimentally, the collision rate of inertial particles is known to depend upon two distinct phenomena, namely particle clustering and particle-pair relative motion in isotropic turbulence. In the dilute limit, the collision kernel of monodispersed inertial particles can be expressed as (Sundaram & Collins Reference Sundaram and Collins1997; Wang, Wexler & Zhou Reference Wang, Wexler and Zhou2000)
where
$K(d)$
is the collision kernel,
$d$
is the diameter of the particle,
$g(r)$
is the radial distribution function (RDF) of the particles and
$\langle w_{r}(r)^{-}\rangle$
is the particle-pair mean inward radial relative velocity (RV). In (1.1), the separation distance
$r$
between two particles is taken at contact, i.e.
$r=d$
. The influence of
$R_{\unicode[STIX]{x1D706}}$
and
$St$
on particle collision rates can be investigated by considering how
$R_{\unicode[STIX]{x1D706}}$
and
$St$
affect the RDF and particle-pair RV.
Many studies have examined the RDF in isotropic turbulence (Eaton & Fessler Reference Eaton and Fessler1994; Collins & Keswani Reference Collins and Keswani2004; Salazar et al.
Reference Salazar, De Jong, Cao, Woodward, Meng and Collins2008; Bragg & Collins Reference Bragg and Collins2014a
; Bragg, Ireland & Collins Reference Bragg, Ireland and Collins2015a
; Wu et al.
Reference Wu, Soligo, Marchioli, Soldati and Piomelli2017) and, more recently, particle-pair RV (Bec et al.
Reference Bec, Biferale, Lanotte, Scagliarini and Toschi2010; Gustavsson & Mehlig Reference Gustavsson and Mehlig2011; Salazar & Collins Reference Salazar and Collins2012b
; Ireland et al.
Reference Ireland, Bragg and Collins2016a
). From these theoretical and numerical studies, a consensus has emerged concerning the effect of
$St$
on the RV, presented in Bragg & Collins (Reference Bragg and Collins2014b
) and Ireland et al. (Reference Ireland, Bragg and Collins2016a
), which we shall now summarize for the purposes of making the present paper self-contained (we refer the reader to the cited papers for more detailed and precise explanations).
Turbulence affects the particle relative motion through three mechanisms: preferential sampling, path-history and inertia filtering effects. Here, we define
$\unicode[STIX]{x1D70F}_{r}$
as the turbulence eddy turnover time scale at the particle-pair separation
$r$
, and
$\unicode[STIX]{x1D70F}_{p}$
as the particle response time. First, when
$\unicode[STIX]{x1D70F}_{p}\ll \unicode[STIX]{x1D70F}_{r}$
, the particle motion is only slightly perturbed relative to that of fluid particles. In this regime, the inertial particle-pair RV differs from the fluid particle RV only because of the preferential sampling mechanism, which describes the tendency of inertial particles to preferentially sample certain regions of the fluid velocity field, unlike fluid particles that uniformly (ergodically) sample the underlying velocity field. Except at low Reynolds numbers, the preferential sampling effect causes the inertial particle-pair RV to be reduced compared with those of fluid particles (Ireland et al.
Reference Ireland, Noda, Jarrett, Fujii, Nakamura, Wanless and Webber2016b
).
Second, when
$\unicode[STIX]{x1D70F}_{p}=O(\unicode[STIX]{x1D70F}_{r})$
, the inertial particle pairs retain a finite memory of the fluid velocity differences they have experienced along their path history. This gives rise to the path-history effect on particle-pair RV. At subintegral scales, the fluid velocity differences increase with increasing separation, on average (although in the dissipation regime this is true instantaneously). As a result, on average, there is an asymmetry in the nature of the turbulence experienced by particle pairs that approach compared with those that separate, and this asymmetry can strongly affect the inertial particle-pair RV statistics. In particular, it leads to an increase in their RVs compared with those of fluid particles. It should be noted, however, that the importance of this path-history mechanism depends not only upon the ratio
$\unicode[STIX]{x1D70F}_{p}/\unicode[STIX]{x1D70F}_{r}$
but also upon
$r$
. The effect is most profound in the dissipation range, and it decreases with increasing
$r$
. This is because the fluid velocity differences increase with
$r$
more weakly as
$r$
is increased, and indeed become independent of
$r$
for
$r\gg L$
, where the path-history mechanism vanishes at these scales. This path-history mechanism is the same mechanism that leads to ‘caustics’, ‘the sling effect’ and ‘random, uncorrelated motion’ (Wilkinson, Mehlig & Bezuglyy Reference Wilkinson, Mehlig and Bezuglyy2006; Falkovich & Pumir Reference Falkovich and Pumir2007; Ijzermans, Meneguz & Reeks Reference Ijzermans, Meneguz and Reeks2010; Bragg & Collins Reference Bragg and Collins2014b
).
Finally, when
$\unicode[STIX]{x1D70F}_{p}=O(\unicode[STIX]{x1D70F}_{r})$
, the particle inertia also gives rise to the filtering mechanism (Bec et al.
Reference Bec, Biferale, Boffetta, Celani, Cencini, Lanotte, Musacchio and Toschi2006; Ayyalasomayajula, Warhaft & Collins Reference Ayyalasomayajula, Warhaft and Collins2008; Ireland et al.
Reference Ireland, Bragg and Collins2016a
,Reference Ireland, Noda, Jarrett, Fujii, Nakamura, Wanless and Webber
b
), which describes the modulated response of the particles to fluctuations in the turbulent velocity field because of their inertia. This mechanism always causes the inertial particle-pair RV to decrease relative to that of fluid particles. The filtering mechanism operates at all
$r$
when
$\unicode[STIX]{x1D70F}_{p}\approx \unicode[STIX]{x1D70F}_{r}$
. However, its importance compared with the path-history effect depends upon
$r$
. For
$r\lesssim \unicode[STIX]{x1D702}$
, the path-history effect dominates the inertial particle-pair RV, while for
$r\gg L$
, the filtering effect completely dominates the inertial particle RV, since at large scales the path-history mechanism vanishes.
The ways in which the Stokes number and Reynolds number affect the inertial particle-pair RV are through their influence on these three mechanisms. The Stokes number, being a measure of the particle response time
$\unicode[STIX]{x1D70F}_{p}$
(normalized by the Kolmogorov time scale), affects the relative importance of these different mechanisms. At small
$St$
(
$St\ll 1$
), the preferential sampling effect dominates the particle-pair RV, leading to slightly lower RV values compared with fluid particles (Salazar & Collins Reference Salazar and Collins2012a
); at large
$St$
(
$St\approx O(1)$
), the path history dominates small
$r$
, while the inertia filtering dominates large
$r$
, resulting in an increase and decrease of the particle-pair RV respectively.
We note that when the path-history effect is weak, the inertial particle RVs may be estimated in terms of the correlation function of the particle and fluid RVs at separation
$r$
. This reflects the fact that in this case, the RVs of the particles are determined by how well correlated the particle motion is with the local fluid velocity field and its associated structure. The following models attempt to predict the particle-pair RV based on this idea: Laviéville, Deutsch & Simonin (Reference Laviéville, Deutsch and Simonin1995), Laviéville et al. (Reference Laviéville, Simonin, Berlemont and Chang1997), Simonin (Reference Simonin2000) and Zaichik & Alipchenkov (Reference Zaichik and Alipchenkov2009).
Compared with the effect of
$St$
, the effect of the Reynolds number on the particle-pair RV is far less understood. There are essentially two kinds of Reynolds number effect. One is the ‘trivial’ effect which describes the fact that as the Reynolds number is increased, the scale separation (spatial and temporal) of the turbulence increases. Theoretical models of inertial particle-pair RV have captured this trivial effect (Zaichik & Alipchenkov Reference Zaichik and Alipchenkov2009; Pan & Padoan Reference Pan and Padoan2010). However, the more complex question concerns how the RV statistics might be affected by the ‘non-trivial’ Reynolds-number effects, e.g. through internal intermittency and potential modifications to the spatial–temporal structure of the flow. Theoretical studies by Falkovich, Fouxon & Stepanov (Reference Falkovich, Fouxon and Stepanov2002) conjectured that an increase of the Reynolds number could lead to larger particle-pair RV through the enhanced intermittency of the fluid velocity field. Although this is undoubtedly true for higher-order statistical quantities (associated with ‘extreme events’ in the turbulence), for the lower-order quantities relevant to particle collisions in turbulence, recent numerical studies by Bec et al. (Reference Bec, Biferale, Lanotte, Scagliarini and Toschi2010), Rosa et al. (Reference Rosa, Parishani, Ayala, Grabowski and Wang2013) and Bragg, Ireland & Collins (Reference Bragg, Ireland and Collins2016) have found that the effect of the Reynolds number is very weak.
However, those numerical simulations or theoretical interpretations were obtained under simplified and limited conditions, i.e. the particle size was monodispersed, the particle–turbulence interaction was one-way coupling, the Basset history forces, nonlinear drag and hydrodynamic interactions were ignored. In natural phenomena or real engineering applications, these terms may not be avoidable. In order to know whether the findings from simulations are applicable under more complex circumstances, experimental investigation of these findings is clearly needed.
These findings from theoretical and numerical studies have not yet been verified experimentally, except for one case – particle-pair RV at
$R_{\unicode[STIX]{x1D706}}\approx 180$
in a small range of low
$St$
(
$0.05{-}0.5$
) (Saw et al.
Reference Saw, Bewley, Bodenschatz, Ray and Bec2014). Using high-speed particle tracking in an enclosed turbulence chamber, Saw et al. (Reference Saw, Bewley, Bodenschatz, Ray and Bec2014) experimentally found that
$\langle w_{r}^{-}\rangle$
increases with
$St$
when
$r$
is comparable to
$\unicode[STIX]{x1D702}$
, the Kolmogorov length scale, which agreed with their direct numerical simulation (DNS) results. However, systematic experimental explorations of
$R_{\unicode[STIX]{x1D706}}$
and
$St$
effects on particle-pair RV are still lacking, and it is important to comprehensively verify these findings from theory and simulation through experiment.
The limited availability of high-speed particle tracking instruments and the challenging nature of these experiments account for the dearth of experimental measurements of particle-pair RV. In our preliminary study, de Jong et al. (Reference de Jong, Salazar, Woodward, Collins and Meng2010) measured particle-pair RV using double-exposure holographic particle imaging in a cubic turbulence chamber. Their measurement exhibited large errors at large RV values due to particle positioning uncertainty along the depth direction caused by the limited angular aperture of digital holography, as well as due to particle pairing error based on only two exposures to track particles (Dou et al.
Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017). More recently, Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017) demonstrated greatly improved particle-pair RV measurement using a novel planar four-frame particle tracking velocimetry (planar 4F-PTV) technique in a new fan-driven ‘soccer ball’ shaped homogeneous and isotropic turbulence (HIT) chamber. They measured particle-pair RV at two
$St$
values (
$St=0.09$
and 3.46) and a fixed
$R_{\unicode[STIX]{x1D706}}=357$
, and reported an excellent match between experimental and DNS results in the range
$10<r/\unicode[STIX]{x1D702}<60$
. Both experiment and DNS show that the particle-pair RV increases with
$St$
in the dissipation range and decrease with
$St$
in the inertial range. However, when
$r/\unicode[STIX]{x1D702}\lesssim 10$
, the experimentally measured
$\langle w_{r}^{-}\rangle$
was higher than the value from DNS. They attributed this difference to the measurement uncertainty caused by polydispersion of particles and finite light sheet thickness in the experiment, with the DNS being run for 3D and monodispersed particles. These authors only examined two
$St$
conditions at a single
$R_{\unicode[STIX]{x1D706}}$
and did not address the effect of changing
$R_{\unicode[STIX]{x1D706}}$
on particle-pair RV.
In this paper, we report a systematic experimental investigation of the effects of the Reynolds number and Stokes number on the mean inward particle-pair RV, based upon the pilot study by Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017). Using the 4F-PTV technique and the HIT chamber described by Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017), we systematically but independently vary
$R_{\unicode[STIX]{x1D706}}$
and
$St$
over wide ranges and measure
$\langle w_{r}^{-}\rangle$
under a large number of experimental conditions. Furthermore, in order to examine whether the findings from numerical simulations and theoretical interpretations still stand in more complex circumstances, we compare experimental results for variance of RV
$\langle w_{r}^{2}\rangle$
and mean inward RV
$\langle w_{r}^{-}\rangle$
with DNS by Ireland et al. (Reference Ireland, Bragg and Collins2016a
) and theoretical predictions by Pan & Padoan (Reference Pan and Padoan2010).
2 Experimental method
2.1 Flow facility and measurement technique
Our experiments were conducted in an enclosed one-metre-diameter truncated icosahedron chamber, which generates high-Reynolds-number homogeneous and isotropic turbulence in the centre region through 20 symmetrically distributed actuators along 10 axes (Dou et al.
Reference Dou, Pecenak, Cao, Woodward, Liang and Meng2016; Dou Reference Dou2017). This flow chamber produces homogeneous and isotropic turbulence (with near zero-mean flow and a maximum
$R_{\unicode[STIX]{x1D706}}$
of 384) in a spherical volume in the centre of at least 48 mm in diameter with minimal gravitational effects on the particles. A 0.2 in. diameter hole was placed at the bottom of the facility to allow particle injection through an attached injector, and compressed air was employed for particle injection before each test run. A thermocouple probe (type K) was inserted into the chamber near the back of a fan to monitor temperature fluctuations. We further modified the chamber to remove static electric charge buildup on particles by coating the interior surfaces of the chamber with carbon conductive paint (Dou et al.
Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017).
We used an in-house developed planar 4F-PTV technique for the measurement of particle-pair RV in this study, as shown in figure 1. The detail of the 4F-PTV has been described by Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017). Briefly, the 4F-PTV system employs two double-exposure particle image velocimetry (PIV) cameras and two double-pulse PIV lasers. The PIV systems are combined together spatially and temporally. Spatially, the two PIV laser beams are overlapped to illuminate the same flow region, and the two PIV cameras are placed orthogonally next to a polarized beam splitter to focus on the same flow region. Temporally, a timing unit synthetizes the two PIV lasers and cameras. The two PIV lasers each generate two short laser pulses, leading to four consecutively generated laser pulses with the same time interval. The first PIV camera captures the first and second particle images, while the second PIV camera captures the third and fourth particle images. Since polarized beam splitters are used and the laser pulses from the two PIV lasers are horizontally and vertically polarized, these two double exposures are not contaminated with each other. This high-speed planar 4F-PTV technique has the advantage of a very short time interval (of the order of microseconds) and accurate particle pairing capability which enables high-speed particle tracking over four consecutive frames using routine laboratory equipment (i.e. regular PIV systems).
2.2 Experimental conditions
The turbulence Taylor-microscale Reynolds number is expressed as
where
$u^{\prime }$
is the turbulence strength,
$\unicode[STIX]{x1D710}$
is the kinematic viscosity and
$\unicode[STIX]{x1D700}$
is the turbulence kinetic energy dissipation rate. The inertia of particles in isotropic turbulence is quantified by the particle Stokes number,
$St\equiv \unicode[STIX]{x1D70F}_{p}/\unicode[STIX]{x1D70F}_{\unicode[STIX]{x1D702}}$
, the ratio of the particle response time,
$\unicode[STIX]{x1D70F}_{p}=\unicode[STIX]{x1D70C}_{p}d^{2}/(18\unicode[STIX]{x1D710}\unicode[STIX]{x1D70C}_{f})$
, to the turbulence Kolmogorov time scale,
$\unicode[STIX]{x1D70F}_{\unicode[STIX]{x1D702}}=\sqrt{\unicode[STIX]{x1D710}/\unicode[STIX]{x1D700}}$
. It can be shown that
Here,
$\unicode[STIX]{x1D70C}_{p}$
and
$\unicode[STIX]{x1D70C}_{f}$
are the particle and fluid densities respectively and
$d$
is the particle diameter.
The set-up for measuring the inertial particle-pair RV using planar 4F-PTV in a homogeneous and isotropic turbulence chamber.
In order to generate a wide range of
$St$
values at different
$R_{\unicode[STIX]{x1D706}}$
values in our HIT chamber, we used two types of commercial particles: low-density glass bubbles (3M Inc., K25,
$\unicode[STIX]{x1D70C}_{p}=0.25~\text{g}~\text{cm}^{-3}$
) and high-density glass bubbles (3M Inc., S60,
$\unicode[STIX]{x1D70C}_{p}=0.60~\text{g}~\text{cm}^{-3}$
). Both the low- and the high-density glass bubbles were run through a series of sieves (ASTM E161 compliant) to generate diameter ranges (5–
$10~\unicode[STIX]{x03BC}\text{m}$
,
$15{-}20~\unicode[STIX]{x03BC}\text{m},25{-}32~\unicode[STIX]{x03BC}\text{m}$
,
$32{-}38~\unicode[STIX]{x03BC}\text{m}$
and
$38{-}45~\unicode[STIX]{x03BC}\text{m}$
) in a particle separation instrument (GilSonic UltraSiever GA-8). Based on the available flow conditions in the fan-driven HIT chamber (
$R_{\unicode[STIX]{x1D706}}=246,277,324,334$
and 357), as well as the obtainable particle densities and diameters, we list all possible experimental conditions in table 1. It should be noted that the particle samples in the experiments were narrowly polydispersed, and the effective
$St$
of a group of polydispersed particles could be slightly different from their mean
$St$
(Zaichik, Simonin & Alipchenkov Reference Zaichik, Simonin and Alipchenkov2006).
The experimental conditions for the particle-laden turbulence in the HIT chamber used in this study. In some particle size ranges, two particle densities were required. In total, 40 unique experimental conditions were used.

2.3 Experimental design
In order to independently study the effects of
$R_{\unicode[STIX]{x1D706}}$
and
$St$
on particle-pair RV statistics, we conducted two series of experiments: experiment A (sweeping
$R_{\unicode[STIX]{x1D706}}$
at fixed
$St$
) and experiment B (sweeping
$St$
at fixed
$R_{\unicode[STIX]{x1D706}}$
). The two variables were controlled independently by changing the flow conditions and particle characteristics. To compare with the DNS results of particle-pair RV by Ireland et al. (Reference Ireland, Bragg and Collins2016a
), ideally we should match the
$R_{\unicode[STIX]{x1D706}}$
and
$St$
of our experiments with their DNS conditions. In practice, the available
$R_{\unicode[STIX]{x1D706}}$
values for experiments are determined by the flow facility (table 1), and the whole range of experimental
$R_{\unicode[STIX]{x1D706}}$
(247–357) fell between two of the
$R_{\unicode[STIX]{x1D706}}$
values in the DNS by Ireland et al. (Reference Ireland, Bragg and Collins2016a
), namely 224 and 398. Since there was essentially no difference in mean inward RV,
$\langle w_{r}^{-}\rangle$
, and variance of RV,
$\langle w_{r}^{2}\rangle$
, under these two
$R_{\unicode[STIX]{x1D706}}$
values over the range (small and intermediate
$St$
and
$r$
) of interest in the DNS results (see figure 15 of Ireland et al.
Reference Ireland, Bragg and Collins2016a
), we used their DNS results under
$R_{\unicode[STIX]{x1D706}}=398$
and
$St=0,0.05,0.3,0.5,1,2,3$
and
$10$
to compare with our experimental measurements.
Experiment A: Sweeping
$R_{\unicode[STIX]{x1D706}}$
at fixed
$St$
. To study the effect of
$R_{\unicode[STIX]{x1D706}}$
on the particle-pair RV, we experimentally swept
$R_{\unicode[STIX]{x1D706}}$
at six target
$St$
values, namely
$St=0.05$
, 0.3, 0.5, 1, 2 and 3. In practice, it is difficult to sweep
$R_{\unicode[STIX]{x1D706}}$
while keeping
$St$
constant, since an increase of
$R_{\unicode[STIX]{x1D706}}$
is accompanied by a decrease of
$\unicode[STIX]{x1D70F}_{\unicode[STIX]{x1D702}}$
and thereby an increase of
$St$
for the same particles. To maintain a nominal
$St$
value, increasing
$R_{\unicode[STIX]{x1D706}}$
requires decreasing particle time scale
$\unicode[STIX]{x1D70F}_{p}$
accordingly. This requires either the particle diameter (
$d$
) or the density (
$\unicode[STIX]{x1D70C}$
) or both to be reduced accordingly as well. Since the available particle densities and diameter ranges were limited, we had to choose different particles for different
$R_{\unicode[STIX]{x1D706}}$
in order to get
$St$
as close to the nominal
$St$
values as possible.
For this purpose, some of the experimental conditions in table 1 were reorganized by the nominal
$St$
value, with
$R_{\unicode[STIX]{x1D706}}$
being the variable, and were denoted as A1, A2, A3, A4, A5 and A6, as shown in table 2. Each test group held nominal
$St$
constant while changing
$R_{\unicode[STIX]{x1D706}}$
from 246 to 357. Figure 2 graphically illustrates the conditions of these test groups, showing that the fluctuations of the actual
$St$
values were within 20 % of the nominal
$St$
values except for test group A1.
Graphical representation of table 2: experimental conditions for test groups A1–A6. Each colour represents one sweeping
$R_{\unicode[STIX]{x1D706}}$
test group at a certain
$St$
, while each point represents one unique experimental condition.

Experiment A (sweeping
$R_{\unicode[STIX]{x1D706}}$
): list of the nominal
$St$
, actual
$St$
and swept
$R_{\unicode[STIX]{x1D706}}$
conditions for the six test groups (A1–A6).

It should be noted that for
$St\sim 2.0$
, the lowest
$R_{\unicode[STIX]{x1D706}}$
that can be obtained is 277, and for
$St\sim 3.0$
, the lowest
$R_{\unicode[STIX]{x1D706}}$
that can be obtained is 324.
Experiment B: Sweeping
$St$
at fixed
$R_{\unicode[STIX]{x1D706}}$
. To study the effect of
$St$
on the particle-pair RV, we experimentally swept
$St$
at five
$R_{\unicode[STIX]{x1D706}}$
values, namely
$R_{\unicode[STIX]{x1D706}}=246$
, 377, 324, 334 and 357. To change
$St$
at fixed
$R_{\unicode[STIX]{x1D706}}$
, the flow condition was held constant and different particles were used. For each flow condition and thus
$R_{\unicode[STIX]{x1D706}}$
, all particle size and density permutations listed in table 1 were used to acquire eight
$St$
values. The test groups for five different
$R_{\unicode[STIX]{x1D706}}$
values are denoted as B1, B2, B3, B4 and B5, and are shown in table 3 and figure 3.
Graphical representation of table 3: experimental conditions for test groups B1–B5. Each colour represents one sweeping
$St$
test group at a certain
$R_{\unicode[STIX]{x1D706}}$
, while each point represents one unique experimental condition.

2.4 Experimental procedure
For all of the 40 experimental conditions (table 1), we performed particle-pair RV measurement using the planar 4F-PTV technique in the HIT chamber. Statistics of the particle motion were only collected and computed once the turbulence had reached a statistically stationary state plus an additional 10 large-eddy time scales. Furthermore, the particle number density in the turbulence chamber was estimated to be below 50 per centimetre cubed (particle volume fraction of order
$10^{-6}$
), such that the system could be considered to be dilute. Under each test condition, we obtained 10 000 quadruple-exposure particle images in 20 runs of 500 consecutive quadruple pulses, repeated at 5–9.5 Hz. The time interval in the quadruple exposure varied between 38
$\unicode[STIX]{x03BC}\text{s}$
and 91
$\unicode[STIX]{x03BC}\text{s}$
for different values of
$R_{\unicode[STIX]{x1D706}}$
. In each quadruple exposure, we obtained individual particle positions and velocities. We calculated the particle-pair RV as
where
$\boldsymbol{v}_{A}$
and
$\boldsymbol{v}_{B}$
are the velocity vectors of particles A and B respectively, and
$\boldsymbol{r}$
is the distance vector from particle A to particle B. The calculated particle-pair RVs,
$w_{r}(r)$
, were binned with the particle separation distance,
$r$
, at increments of
$\unicode[STIX]{x1D702}$
. Particle-pair RV statistics of mean inward particle-pair RV,
$\langle w_{r}^{-}\rangle$
, and variance of particle-pair RV,
$\langle w_{r}^{2}\rangle$
, were obtained over a wide range of
$r$
. We calculated all experimental uncertainties following the procedure reported in appendix B of Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017). In the final calculation, we normalized
$r$
,
$\langle w_{r}^{-}\rangle$
and
$\langle w_{r}^{2}\rangle$
by the Kolmogorov length scale
$\unicode[STIX]{x1D702}$
, the Kolmogorov velocity scale
$u_{\unicode[STIX]{x1D702}}$
and the square of the Kolmogorov velocity scale
$u_{\unicode[STIX]{x1D702}}^{2}$
respectively. We then plotted these normalized quantities based on the test groups in experiments A and B.
Experiment B (sweeping
$St$
): list of the fixed
$R_{\unicode[STIX]{x1D706}}$
and swept
$St$
conditions for the five test groups (B1–B5).

2.5 Monte Carlo analysis to account for out-of-plane components of the particle-pair RV
The planar 4F-PTV technique measures the particle-pair RV within a laser light sheet that has a finite thickness of
$8\unicode[STIX]{x1D702}$
. The laser thickness is required to contain a sufficient number of particles within the light sheet over the four consecutive exposures for accurate particle tracking. However, the planar PTV measures only the in-plane particle-pair separation and plane RV, omitting the out-of-plane components, which brings about uncertainty in the RV measurement when the particle separation distance is small. Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017) evaluated the finite laser thickness effect and showed that it causes an overestimation of the particle-pair RV at small
$r$
. When the in-plane particle separation distance
$r$
is larger than the laser thickness, the difference in
$\langle w_{r}^{-}\rangle$
drops down to below 10 %. They further attempted to correct the omission of the out-of-plane components of the RV using Monte Carlo analysis (MCA) on their experimental data, assuming the same particle distribution in the out-of-plane direction as in the transverse directions based on isotropy. This correction procedure was able to eliminate the finite laser thickness effect on RV measurements for
$r\gtrsim 5\unicode[STIX]{x1D702}$
.
We have applied the MCA correction to all of the experimental results for
$\langle w_{r}^{-}\rangle$
in both experiments A and B to account for the finite laser thickness, and compared the results after and before the out-of-plane correction.
3 Results and discussion
We present all of the raw experimental data from experiments A and B in this section. After the MCA correction for the out-of-plane components, all of the plots of
$\langle w_{r}^{-}\rangle$
against
$r$
remained the same for
$r\geqslant 15\unicode[STIX]{x1D702}$
(indicating negligible effect), moved down by 5 %–10 % for
$r=5{-}15\unicode[STIX]{x1D702}$
(successful correction) and by 3 %–5 % for
$r\leqslant 5\unicode[STIX]{x1D702}$
(limited correction), which is consistent with report by Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017). Because the MCA correction method itself contains assumptions and simulation, and because the difference after correction is minimal and not enough to change the trends of
$\langle w_{r}^{-}\rangle$
versus
$r$
,
$\langle w_{r}^{-}\rangle$
versus
$R_{\unicode[STIX]{x1D706}}$
and
$\langle w_{r}^{-}\rangle$
versus
$St$
, we chose to present the raw experimental data without the MCA correction.
3.1 Mean inward particle-pair RV
In figures 4 and 5, we plot the mean inward particle-pair RV,
$\langle w_{r}^{-}\rangle$
, versus the particle-pair separation distance
$r$
for some of the experimental conditions to give an overview of the general trend using both linear and log scales. The rows represent the sweeping of
$R_{\unicode[STIX]{x1D706}}$
in experiment A while the columns represent the sweeping of
$St$
in experiment B. Thirteen unique experimental conditions of experiment B (sweeping
$St$
) are not shown due to limited space. The DNS data from Ireland et al. (Reference Ireland, Bragg and Collins2016a
) are plotted at
$St$
matching the experiment, but solely at
$R_{\unicode[STIX]{x1D706}}=398.$
As stated earlier, since
$\langle w_{r}^{-}\rangle$
from DNS is insensitive to
$R_{\unicode[STIX]{x1D706}}$
between
$R_{\unicode[STIX]{x1D706}}=88$
and 598 in the
$St$
and
$r$
ranges we are interested in (and, specifically, DNS results between
$R_{\unicode[STIX]{x1D706}}=224$
and 398 are near-identical), DNS data at
$R_{\unicode[STIX]{x1D706}}=398$
with
$St$
matching experimental conditions are sufficient for comparison.
The mean inward particle-pair RV
$\langle w_{r}^{-}\rangle$
(normalized by the Kolmogorov velocity scale
$u_{\unicode[STIX]{x1D702}}$
) versus the particle-pair separation distance
$r$
(normalized by the Kolmogorov length scale) at different values of
$R_{\unicode[STIX]{x1D706}}$
and
$St$
from experimental measurements (data points with error bars) and DNS (curves). The rows (A1–A6) represent the sweeping of
$R_{\unicode[STIX]{x1D706}}$
in experiment A while the columns (B1–B5) represent the sweeping of
$St$
in experiment B. For clarity, only 27 experimental conditions between experiments A and B are plotted, and we omit every other experimental data point in each plot. The DNS was taken from Ireland et al. (Reference Ireland, Bragg and Collins2016a
) under
$R_{\unicode[STIX]{x1D706}}=398$
and the matching nominal
$St$
values.

Replot of figure 4 using a logarithmic scale: mean inward particle-pair RV
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
versus particle-pair separation distance
$r/\unicode[STIX]{x1D702}$
at different values of
$R_{\unicode[STIX]{x1D706}}$
and
$St$
from experiment and DNS.

From figure 4, we notice that the experimental data for
$\langle w_{r}^{-}\rangle$
versus
$r$
closely match with the DNS data within the experimental uncertainty (5 %
${\sim}$
10 %) at all experimental conditions, provided that
$r\gtrsim 10\unicode[STIX]{x1D702}$
. In each case,
$\langle w_{r}^{-}\rangle$
increases with decreasing slope when
$r$
increases. When
$r\lesssim 10\unicode[STIX]{x1D702}$
, the experimental results are consistently higher than the DNS for all experimental conditions. In order to visualize this discrepancy more clearly, we plot the same experimental conditions as those in figure 4 using logarithmic scales in figure 5. From figure 5, we see that the value of
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
in the experiment is around 0.37 (with
$\pm 0.12$
fluctuations) higher than the DNS values when
$r=\unicode[STIX]{x1D702}$
for all experimental conditions. This difference does not have a preferred trend when
$R_{\unicode[STIX]{x1D706}}$
or
$St$
is swept in experiment A or B respectively.
The persistent discrepancy between experimental and DNS results for
$\langle w_{r}^{-}\rangle$
at small
$r$
through all test conditions recapitulates the observation by Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017) at two test conditions (
$St=0.09$
and 3.46, both at
$R_{\unicode[STIX]{x1D706}}=357$
). As explained in Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017), particle polydispersity and finite light sheet thickness effects were the two main contributors to this discrepancy, and the contributions from these two effects were comparable. In addition, we noticed that the magnitudes of the discrepancies were very similar for all experimental conditions. This further indicates that the polydispersity and light sheet thickness effects may be the main contributors to the discrepancy, as these two effects could be approximately uniform between different test conditions, given the factor that the particle size distributions in different size ranges and light sheet thicknesses in different experimental runs were similar to each other.
3.2 Reynolds number effect on particle-pair RV
In test groups A1–A6, we are able to examine the behaviour of
$\langle w_{r}^{-}\rangle$
versus
$r$
as we sweep
$R_{\unicode[STIX]{x1D706}}$
under similar
$St$
in figure 4. To more clearly visualize any effect of the Reynolds number on
$\langle w_{r}^{-}\rangle$
, we superimpose all curves of the same nominal
$St$
but different
$R_{\unicode[STIX]{x1D706}}$
together, and show the results in figures 6 and 7, where each plot is a combination of all plots in one row in figures 4 and 5 respectively. The DNS data at
$St$
values matching the nominal
$St$
values and
$R_{\unicode[STIX]{x1D706}}=398$
are also plotted along with the experimental data. In general, the experimental data points do not show any systematic variation with the Reynolds number. Some of the results in figure 7 do seem to reveal a weak trend with
$R_{\unicode[STIX]{x1D706}}$
at small
$r$
, e.g. groups A5 and A6 in figure 7 seem to reveal a decrease in
$\langle w_{r}^{-}\rangle$
as
$R_{\unicode[STIX]{x1D706}}$
is increased for fixed
$St$
. However, such apparent trends should be interpreted with caution since the variation with
$R_{\unicode[STIX]{x1D706}}$
falls within the experimental uncertainty.
Superimposition of the experimental results for all
$R_{\unicode[STIX]{x1D706}}$
values under the same nominal
$St$
value for test groups A1–A6. The DNS data are plotted as a solid line at an
$St$
value matching the nominal
$St$
value of the test group with
$R_{\unicode[STIX]{x1D706}}=398$
. For clarity, we omit every other experimental data point in each plot.

Replot of figure 6 using a logarithmic scale: superimposition of experimental results for all
$R_{\unicode[STIX]{x1D706}}$
values under the same nominal
$St$
value for test groups A1–A6.

Furthermore, we plot
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
versus
$R_{\unicode[STIX]{x1D706}}$
directly at four different particle separation distances (
$r=1\unicode[STIX]{x1D702},10\unicode[STIX]{x1D702},30\unicode[STIX]{x1D702}$
and
$60\unicode[STIX]{x1D702}$
) in figure 8 for all six different
$St$
values. It is seen that
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
is nearly independent of
$R_{\unicode[STIX]{x1D706}}$
, showing no systematic variation of
$\langle w_{r}^{-}\rangle$
with increasing
$R_{\unicode[STIX]{x1D706}}$
.
Normalized mean inward particle-pair RV
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
against
$R_{\unicode[STIX]{x1D706}}$
at four different particle separation distances, namely
$r=1\unicode[STIX]{x1D702},10\unicode[STIX]{x1D702},30\unicode[STIX]{x1D702}$
and
$60\unicode[STIX]{x1D702}$
. Here,
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
has no preferred change when
$R_{\unicode[STIX]{x1D706}}$
increases, regardless of
$St$
.

The weak Reynolds number dependence in the range of experimental observations supports previous conclusions from numerical simulations (Bec et al.
Reference Bec, Biferale, Lanotte, Scagliarini and Toschi2010; Ireland et al.
Reference Ireland, Bragg and Collins2016a
). Explanations for this behaviour were given in Ireland et al. (Reference Ireland, Bragg and Collins2016a
), which we now summarize. For
$St\leqslant O(1)$
, the memory time scale of the inertial particles is sufficiently small such that when
$r$
lies in the dissipation range, the inertial particles are only weakly affected by their memory of their interaction with the inertial range turbulence. As such,
$St\leqslant O(1)$
particles are only weakly affected by the trivial Reynolds-number effect when
$r$
lies in the dissipation range, whereas
$St>O(1)$
particles will be affected since they retain a memory of the inertial range scales, whose properties (such as extent) strongly depend upon
$R_{\unicode[STIX]{x1D706}}$
.
Outside the dissipation range, for sufficiently large
$St$
, the filtering mechanism plays an important role in determining the RV behaviour. For a given
$r$
, the effect of filtering depends upon the local Stokes number
$St$
, and this is directly affected by the trivial
$R_{\unicode[STIX]{x1D706}}$
effect (i.e. scale separation). In particular, for fixed
$r$
,
$St$
(and hence the filtering effect) decreases as
$R_{\unicode[STIX]{x1D706}}$
is increased (fixed
$\unicode[STIX]{x1D708}$
), as observed in Ireland et al. (Reference Ireland, Bragg and Collins2016a
). This variation is not apparent in our experimental results, which is most likely because outside the dissipation range, the response times of the particles,
$\unicode[STIX]{x1D70F}_{p}$
, in our experiment are too small compared with the local eddy turnover time,
$\unicode[STIX]{x1D70F}_{r}$
, for the filtering mechanism to be effective (Ireland et al. (Reference Ireland, Bragg and Collins2016a
) considered particles with
$St\leqslant 30$
, whereas we only have
$St\leqslant 3$
in our experiment).
Concerning the non-trivial
$R_{\unicode[STIX]{x1D706}}$
effect, since the low-order moments of the fluid velocity difference field are (when normalized by the Kolmogorov scales) essentially independent of
$R_{\unicode[STIX]{x1D706}}$
in the dissipation range (implying that they are weakly affected by intermittency), the low-order inertial particle RV statistics are also essentially independent of
$R_{\unicode[STIX]{x1D706}}$
. For the higher-order RV statistics, not investigated in this paper, this is probably not the case because of the increased intermittency of the turbulent velocity field as
$R_{\unicode[STIX]{x1D706}}$
is increased.
Ireland et al. (Reference Ireland, Bragg and Collins2016a
) did detect a weak
$R_{\unicode[STIX]{x1D706}}$
trend in the dissipation range low-order particle-pair RV using DNS with monodispersed particles. For example, they found a slight decrease of the mean inward particle-pair RV with
$R_{\unicode[STIX]{x1D706}}$
when
$St\approx O(1)$
. They attributed this to the fact that the effect of the path-history mechanism depends not only upon the value of
$St$
, but also the size of the Lagrangian correlation time scales of the fluid velocity gradient measured along the inertial particle trajectories. Their DNS results showed that these time scales decrease slightly with increasing
$R_{\unicode[STIX]{x1D706}}$
when
$St\approx O(1)$
(a non-trivial
$R_{\unicode[STIX]{x1D706}}$
effect resulting from changes to the spatiotemporal structure of the turbulence when
$R_{\unicode[STIX]{x1D706}}$
is changed), which decreases the effect of the path-history mechanism, leading to the observed reduction in the RV in this regime.
The experimental uncertainty of our results in this regime (5 %–10 %) is larger than the change of
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
observed in the DNS, and as such we are not able to conclude whether or not our experiments corroborate the weak
$R_{\unicode[STIX]{x1D706}}$
dependence observed in the DNS when
$St\approx O(1)$
. We believe that studies on further reducing the experimental uncertainty and increasing the acquirable
$R_{\unicode[STIX]{x1D706}}$
range would be very helpful to support the weak
$R_{\unicode[STIX]{x1D706}}$
dependence observed in the DNS. Of course, other factors are the particle polydispersity and laser thickness effects in our experiment, which are absent in the DNS results of Ireland et al. (Reference Ireland, Bragg and Collins2016a
). How these affect the
$R_{\unicode[STIX]{x1D706}}$
dependence of the inertial particle RV statistics is currently unknown, which is an important question that we intend to address in future work.
3.3 Stokes number effect on particle-pair RV
In test groups B1–B5, we are able to examine the trend of the curve of
$\langle w_{r}^{-}\rangle$
versus
$r$
as we sweep
$St$
vertically under the same
$R_{\unicode[STIX]{x1D706}}$
value in figures 4 and 5. In order to compare the curves at different
$St$
values, we superimpose all curves in each test group of the same
$R_{\unicode[STIX]{x1D706}}$
from experiment B and plot the vertically combined plots in figures 9 and 10 respectively. This allows us to further visualize the overall change of the curve slopes. On the combined
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
versus
$r/\unicode[STIX]{x1D702}$
plot for each test group, we also plot two curves from DNS of
$St$
near the upper and lower
$St$
bounds of the experimental conditions for that group. Comparing the two simulation curves, and comparing between the experimental curves, we notice that the curves of
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
versus
$r/\unicode[STIX]{x1D702}$
change when
$St$
changes, but no obvious relationship can be obtained due the discernibility.
Superimposed experimental results of all
$St$
values under the same
$R_{\unicode[STIX]{x1D706}}$
value for test groups B1–B5. Two DNS curves are plotted as solid and dashed lines at conditions approximating to the highest and lowest
$St$
values in each test group with
$R_{\unicode[STIX]{x1D706}}=398$
. For clarity, we omit every other experimental data point in each plot.

Replot of figure 9 using a logarithmic scale: superimposition of experimental results of all
$St$
values under the same
$R_{\unicode[STIX]{x1D706}}$
value for test groups B1–B5.

To clearly visualize this trend, we plot
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
directly against
$St$
at single values of
$r/\unicode[STIX]{x1D702}$
in figure 11, using experimental and DNS results. Four representative particle separation distances are shown, namely
$r=1\unicode[STIX]{x1D702}$
,
$10\unicode[STIX]{x1D702}$
,
$30\unicode[STIX]{x1D702}$
and
$60\unicode[STIX]{x1D702}$
. The experimental values are higher than the DNS values at
$r=1\unicode[STIX]{x1D702}$
. When
$r$
increases, the experimental and DNS results tend to agree with each other to a greater degree, and at
$r=30$
and
$60\unicode[STIX]{x1D702}$
, an excellent match between experiment and DNS is achieved until
$St\approx 2$
. The improved agreement as
$r$
is increased is probably due to the fact that the influence of the particle polydispersity and finite light sheet thickness effects becomes less important as
$r$
is increased. Furthermore, both the experimental and the DNS results indicate that
$\langle w_{r}^{-}\rangle$
depends more weakly upon
$St$
as
$r$
is increased. This is again simply a consequence of the fact that for fixed
$St$
values,
$\unicode[STIX]{x1D70F}_{r}$
become larger than
$\unicode[STIX]{x1D70F}_{p}$
as
$r$
is increased, so that the effect of inertia becomes less and less important.
Normalized mean inward particle-pair RV
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
against
$St$
at four different particle separation distances, namely
$1\unicode[STIX]{x1D702},10\unicode[STIX]{x1D702},30\unicode[STIX]{x1D702}$
and
$60\unicode[STIX]{x1D702}$
. The black lines represent the DNS results at each corresponding
$r/\unicode[STIX]{x1D702}$
and
$R_{\unicode[STIX]{x1D706}}=398$
. At small
$r/\unicode[STIX]{x1D702}$
values,
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
increases when
$St$
increases. At large
$r/\unicode[STIX]{x1D702}$
values,
$\langle w_{r}^{-}\rangle /u_{\unicode[STIX]{x1D702}}$
slightly decreases when
$St$
increases. The value of
$R_{\unicode[STIX]{x1D706}}$
does not affect the trend of the data points.

The dependence of
$\langle w_{r}^{-}\rangle$
on
$St$
measured from experiment is consistent with previous numerical studies (Salazar & Collins Reference Salazar and Collins2012b
; Bragg & Collins Reference Bragg and Collins2014b
) as well as the precursor of the current experimental study by Dou et al. (Reference Dou, Ireland, Bragg, Liang, Collins and Meng2017). At small
$r$
,
$\langle w_{r}^{-}\rangle$
increases with the particle inertia. This is because in this regime the path-history mechanism dominates. At large
$r$
, the particle-pair RV decreases with increasing
$St$
. This decrease is because as
$r$
increases, the filtering mechanism begins to dominate over the path-history mechanism, and the filtering mechanism always reduces the RV.
3.4 Comparison between experiment, DNS and theoretical model
As discussed by Bragg & Collins (Reference Bragg and Collins2014b
), the analytical model of particle-pair RV by Pan & Padoan (Reference Pan and Padoan2010) provides a more accurate prediction of the DNS results than previous theoretical models. In order to calculate the mean inward particle-pair RV,
$\langle w_{r}^{-}\rangle$
, Pan & Padoan (Reference Pan and Padoan2010) adopted the assumption that the probability distribution function (PDF) of the particle-pair RV is Gaussian, which leads to
$\langle w_{r}^{-}\rangle =\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
. We would like to examine this theoretical model using experimental and DNS results. This will be done in two steps: (1) a comparison of the theoretical predicted
$\langle w_{r}^{2}\rangle$
and
$\langle w_{r}^{-}\rangle$
with experimental and DNS results; (2) validation of the Gaussian assumption of the particle-pair RV, which underlines the relation
$\langle w_{r}^{-}\rangle =\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
using experimental data.
Following Pan’s theory, we first calculated
$\langle w_{r}^{2}\rangle$
by solving (3.5) from Pan & Padoan (Reference Pan and Padoan2010) numerically. We then calculated
$\langle w_{r}^{-}\rangle$
using the relation
$\langle w_{r}^{-}\rangle =\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
. These quantities were obtained at
$St=[0.01-5.0]$
,
$R_{\unicode[STIX]{x1D706}}=398$
and four particle separation values (
$r=1\unicode[STIX]{x1D702},10\unicode[STIX]{x1D702},30\unicode[STIX]{x1D702}$
and
$60\unicode[STIX]{x1D702}$
). We also obtained
$\langle w_{r}^{2}\rangle$
versus
$St$
and
$\langle w_{r}^{-}\rangle$
versus
$St$
at similar conditions using experimental and DNS data. Results from the theoretical, numerical and experimental calculations are normalized by the Kolmogorov velocity scale and shown in figure 12.
Comparison between experimental data, simulation results and theoretical predictions of the normalized variance of the particle-pair RV and the normalized mean inward particle-pair RV versus
$St$
. Here, the red lines are the theoretical model predictions, the blue curves are the DNS simulation results and the discrete dots are the experimental data. Results are plotted at particle separation distances of
$r=1\unicode[STIX]{x1D702},10\unicode[STIX]{x1D702},30\unicode[STIX]{x1D702}$
and
$60\unicode[STIX]{x1D702}$
. (a) Normalized variance of the particle-pair RV; (b) normalized mean inward particle-pair RV.

From figure 12, we observe that, in the range
$0<St\lesssim 1.0$
, the theoretical prediction for
$\langle w_{r}^{2}\rangle$
matches the DNS data well across the range of
$r$
. The slight discrepancies observed are a consequence of slight errors in the empirical formula used as input to the theory for the fluid second-order structure function. Both the theoretical model and the DNS results are smaller than the experimental results at
$r\lesssim 10\unicode[STIX]{x1D702}$
but match the experimental results at larger
$r$
. This is again a result of particle polydispersity and finite light sheet thickness in the experiment, whose effects are only observable for
$r\lesssim 10\unicode[STIX]{x1D702}$
. However, when
$St\gtrsim 1.0$
, the theoretical prediction for
$\langle w_{r}^{2}\rangle$
departs from both the experimental and the DNS results for all
$r$
values. Indeed, the theoretical results are 20 %–100 % smaller than the DNS and experimental results.
As discussed in Bragg & Collins (Reference Bragg and Collins2014b
), a possible explanation for this disagreement is that in Pan’s theoretical model, the particle backward-in-time dispersion is approximated using its forward-in-time counterpart. The need to specify the backward-in-time dispersion arises in their model through their approximation for the fluid RVs experienced by the inertial particles along their path history. In this way, the quality of the closure they prescribe for the backward-in-time dispersion will determine, in a significant way, the degree to which their model can describe the path-history mechanism affecting the RV statistics. It was suggested in Bragg & Collins (Reference Bragg and Collins2014b
) that since inertial particles may disperse backward-in-time faster than forward-in-time, the approximation of their equivalence in the Pan theory may explain its underprediction of the particle-pair RV. In a recent study (Bragg et al.
Reference Bragg, Ireland and Collins2016), it was in fact demonstrated, both theoretically and numerically, that inertial particles separate faster backward-in-time than forward-in-time, and that they may differ by orders of magnitude in the dissipation regime when
$St\gtrsim O(1)$
. This then supports the explanation given by Bragg & Collins (Reference Bragg and Collins2014b
) for the cause of the underpredictions by the Pan theory.
The ratio of
$\langle w_{r}^{-}\rangle$
and
$\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
calculated from experimental data. (a) Ratio calculated from test group A4 and (b) ratio calculated from test group B5. It should be noted that regardless of the
$R_{\unicode[STIX]{x1D706}}$
or
$St$
, the result varies between 0.8 and 0.97 consistently.

Despite the discrepancy observed in figure 12 for
$\langle w_{r}^{2}\rangle$
, the theoretical predictions for
$\langle w_{r}^{-}\rangle$
compare more favourably with the DNS results. A possible explanation for this is related to the Gaussian assumption used in the theory to obtain a prediction for
$\langle w_{r}^{-}\rangle$
from
$\langle w_{r}^{2}\rangle$
, namely
$\langle w_{r}^{-}\rangle =\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
. This relationship is exact when the PDF of
$w_{r}$
is Gaussian; however, we expect that this PDF will be non-Gaussian (Ireland et al.
Reference Ireland, Bragg and Collins2016a
). To test the validity of
$\langle w_{r}^{-}\rangle =\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
, we plot the ratio
$\langle w_{r}^{-}\rangle /\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
as a function of
$r$
from test groups A4 and B5 in figures 13(a) and 13(b) respectively. It is evident that the value of
$\langle w_{r}^{-}\rangle /\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
is always less than unity based on our experimental data, and it monotonically decreases with decreasing
$r$
from 0.97 to 0.80. Our experiment is not able to obtain reliable data for
$r<\unicode[STIX]{x1D702}$
, but the DNS results reported by Ireland et al. (Reference Ireland, Bragg and Collins2016a
) reveal that this ratio will be even lower when
$r<\unicode[STIX]{x1D702}$
(
$\langle w_{r}^{-}\rangle /\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}\approx 0.4$
when
$r=0.25\unicode[STIX]{x1D702}$
). The conclusion then is that the Gaussian result
$\langle w_{r}^{-}\rangle =\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
would lead to an overprediction of
$\langle w_{r}^{-}\rangle$
when the correct value for
$\langle w_{r}^{2}\rangle$
is prescribed, especially at small
$r$
.
Therefore, although Pan’s theory underpredicts the variance
$\langle w_{r}^{2}\rangle$
at
$St\gtrsim 1$
, this underprediction is compensated for through its use of the Gaussian assumption to compute
$\langle w_{r}^{-}\rangle$
from
$\sqrt{\langle w_{r}^{2}\rangle /2\unicode[STIX]{x03C0}}$
, leading to a much better prediction for
$\langle w_{r}^{-}\rangle$
than
$\langle w_{r}^{2}\rangle$
when
$St\gtrsim 1$
.
In addition, by improving the spatial resolution (e.g. a higher-magnification camera lens), the experimental method used in this study offers a potential for exploring the influence of
$R_{\unicode[STIX]{x1D706}}$
on particle-laden flows at high
$R_{\unicode[STIX]{x1D706}}$
values and large particle separations that cannot be reached by DNS in the near future.
4 Conclusion
We systematically studied, for the first time, the effect of the Reynolds number and the particle inertia on the particle-pair RV through experiments in homogeneous isotropic turbulence. In experiments A and B,
$R_{\unicode[STIX]{x1D706}}$
and
$St$
respectively were independently varied, and we obtained an excellent match of the mean inward particle-pair RV,
$\langle w_{r}^{-}\rangle$
, between experimental and DNS results throughout the range of experiment conditions, except for particle-pair separations in the dissipation range. The discrepancies in the dissipation range are probably due to particle polydispersity and finite light sheet thickness effects, which were absent in the DNS. We found that the Reynolds number has essentially no effect on
$\langle w_{r}^{-}\rangle$
except within a small region of the parameter space. In this small region, the experimental results show a weak dependence of
$\langle w_{r}^{-}\rangle$
on the Reynolds number; however, the variation falls within the range of experimental uncertainty, and so must be viewed with caution. We observed that the particle inertia enhances the particle-pair RV at small particle separation distances due to the ‘path-history’ mechanism, but the particle inertia decreases the particle-pair RV at large particle separation distances due to the ‘inertial filtering’ mechanism. The findings are all qualitatively consistent with previous theoretical and numerical results. Lastly, through the comparison between experiment, DNS and theory, we found that the variance of the particle-pair RV,
$\langle w_{r}^{2}\rangle$
, predicted by Pan’s theoretical model is smaller than the experimental or DNS results when
$St\gtrsim 1$
. In contrast, the model predictions for
$\langle w_{r}^{-}\rangle$
compare more favourably with experimental and DNS results when
$St\gtrsim 1$
. This occurs because the model uses a Gaussian approximation to relate
$\langle w_{r}^{2}\rangle$
to
$\langle w_{r}^{-}\rangle$
, which overestimates
$\langle w_{r}^{-}\rangle$
(when the correct value of
$\langle w_{r}^{2}\rangle$
is prescribed), but since the model underpredicts
$\langle w_{r}^{2}\rangle$
, the two errors cancel each other out, leading to good predictions for
$\langle w_{r}^{-}\rangle$
.
Acknowledgements
This work was supported by the National Science Foundation through Collaborative Research grants CBET-0967407 (H.M.) and CBET-0967349 (L.R.C.). We thank Dr P. Ireland for providing DNS data for comparison with our experimental results. We acknowledge the support provided by the Center for Computational Research at the University at Buffalo for Monte Carlo analysis.















