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Potential Explosion Hazard of Carbonaceous Nanoparticles:
Explosion Parameters of Selected Materials
Supplemental Material
Submitted to
Journal of Hazardous Materials
Leonid A. Turkevich*
Centers for Disease Control and PreventionNational Institute for Occupational Safety and Health,
Division of Applied Research and Technology,1090 Tusculum Avenue, MS-R7, Cincinnati, OH 45226 USA
and
Ashok G. Dastidar, Zachary Hachmeister, Michael Lim
Fauske & Associates, LLC16W070 83rd Street
Burr Ridge, IL 60527 USA
* corresponding author:
[email protected]: (513) 841 4518
Fax: (513) 841 4545
Keywords: explosion hazard, dust, carbon, nanoparticle, nanomaterials
Statistical Correlations of the Explosion Parameters
As discussed in our first paper [Turkevich et al. 2014], the explosion severity index, K(500), is
highly correlated with the maximum explosion overpressure, Pm(500) [Figure 5 of Turkevich et al.
2014]; this high degree of correlation is confirmed (R2 = 0.9) between the global explosion
severity index, KSt, and the global maximum explosion pressure, Pmax
6 6.2 6.4 6.6 6.8 7 7.2 7.4 7.6 7.8 850
100
150
200
R² = 0.892895616252253
Pmax [bar]
KSt
[bar
-m/s
]
The minimum explosive concentration, MEC, is also highly correlated with both Pmax (R2 = 0.7)
and with KSt (R2 = 0.8)
6 6.2 6.4 6.6 6.8 7 7.2 7.4 7.6 7.8 80
10
20
30
40
50
60
70
80
90
100
R² = 0.744399300809449
Pmax [bar]
MEC
[g/
m3]
50 100 150 2000
10
20
30
40
50
60
70
80
90
100
R² = 0.795127085541348
KSt [bar-m/s]
MEC
[g/
m3]
As expected, the more explosive powders (high Pmax, high KSt) exhibit a lower concentration
threshold (MEC) for explosion.
However, the minimum ignition energy, MIE, is poorly correlated with both Pmax (R2 = 0.2) and
with KSt (R2 = 0.3)
6 6.2 6.4 6.6 6.8 7 7.2 7.4 7.6 7.8 80
0.5
1
1.5
2
R² = 0.243924285381389
Pmax [bar]
MIE
[kJ]
50 100 150 2000
0.5
1
1.5
2
R² = 0.295794243863882
KSt [bar-m/s]
MIE
[kJ]
Although the correlation is poor, the trend is as expected, namely the more explosive materials
(high Pmax, high KSt) exhibit a lower ignition threshold (MIE) for explosion. It is not surprising that
there is a similar lack of correlation (R2 = 0.2) between MIE and MEC
10 20 30 40 50 60 70 80 90 1000
0.5
1
1.5
2
R² = 0.216823903755842
MEC [g/m3]
MIE
[kJ
]
Again, while the correlation is poor, the trend is as expected, namely, the materials with a
low concentration threshold (MEC) also exhibit a low ignition threshold (MIE).
Similar behavior obtains for the minimum ignition cloud temperature: MITcloud is
reasonably correlated with both Pmax (R2 ~ 0.6) and KSt (R2 ~ 0.7)
6 6.5 7 7.5 8525
550
575
600
625
650
675R² = 0.640303102060147
Pmax [bar]
MITcl
oud [
oC]
50 100 150 200525
550
575
600
625
650
675
R² = 0.704284272858267
KSt [bar-m/s]MI
Tclou
d [oC
]
with the more explosive powders (high Pmax, high KSt) exhibiting a lower temperature
threshold (MITcloud) for explosion. There is poor correlation (R2 ~ 0.3) between MITcloud
and MEC and also (R2 ~ 0.3) between MITcloud and MIE
10 20 30 40 50 60 70 80 90 100525
550
575
600
625
650
675
R² = 0.30350964072569
MEC [g/m3]
MITcl
oud [
oC]
0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2525
550
575
600
625
650
675
R² = 0.267334271226269
MIE [kJ]
MITcl
oud [
oC]
Again, while the correlation is poor, in both cases, the trend is as expected, namely, that
materials with low concentration (MEC) and ignition (MIE) thresholds for explosion also
exhibit a low temperature threshold (MITcloud) for explosion.
Statistical Correlation with Aggregate Particle Size.
We believe that aggregation of the primary particles is not a significant determinant of the
explosion parameters. As indicated in the main paper, there is no evidence of any tightly bound
aggregates from our electron micrographs (either before or after explosion). We believe that
aggregation has, at best, a minimal effect on the explosion parameters of the carbonaceous
nanomaterials.
As discussed in the main paper, we have measured aggregate particle size distributions with
light scattering (CILAS 1064). We have attempted to correlate the various parameters that
characterize those distributions with the measured explosion parameters. The aggregate size
distributions are all broad and multimodal (main paper, Figure 1). Statistically, we may identify
a mean size, dmean, and the size of the mode (cumulant midpoint), d50; qualitatively, we may also
identify the size, ddom, of the dominant mode, as well as the sizes, dmax and dmin, of the largest and
smallest modes, respectively. As most of the weight is at the upper end of the distributions,
the parameters, dmean, d50, ddom, dmax are essentially equivalent.
There are weak statistical correlations (R2 ~ 0.6) of Pmax with dmean, d50, ddom, dmax
0 10 20 30 40 50 60 70 80 90 1006
6.5
7
7.5
8
R² = 0.619846400266592
d50 [micron]
Pmax
[ba
r]
0 20 40 60 80 1006
6.5
7
7.5
8
R² = 0.625585067270943
dmean [micron]
pmax
[bar]
0 20 40 60 80 100 1206
6.5
7
7.5
8
R² = 0.570021942174034
ddom [microns]
pmax
[bar]
0 20 40 60 80 100 1206
6.5
7
7.5
8
R² = 0.628707439388697
dmax [micron]
pmax
[bar]
There are similar weak statistical correlations (R2 ~ 0.6) of KSt with dmean, d50, ddom, dmax
0 20 40 60 80 10050
100
150
200
R² = 0.63476243026339
dmean [micron]
KSt [
bar-m
/s]
0 20 40 60 80 1000
50
100
150
200
250
R² = 0.645382997206696
d50 [micron]
KSt
[bar-m
/s]
0 20 40 60 80 100 12050
100
150
200
R² = 0.579519871402134
ddom [microns]
KSt [
bar-m
/s]
0 20 40 60 80 100 12050
100
150
200
R² = 0.603660166557892
dmax [micron]
KSt [
bar-m
/sec]
Statistically, the smaller the aggregate, the less explosive is the material—i.e. smaller Pmax and
smaller KSt. However, under the NanoSafe hypothesis, the smaller aggregates should be more
explosive. Thus the NanoSafe model is not supported by the statistical correlation.
With such a limited data set, it is impossible to deconvolute the effect of aggregate particle size
from the effect of allotrope on explosion severity; e.g. on the above correlation plots, the most
explosive material, fullerene (Pmax = 8 bar, KSt = 199 bar-m/s), is always upper right, and the least
explosive material, graphite (Pmax = 6.3 bar, KSt = 64 bar-m/s), is always lower left. Given the
established dependence of explosion severity on allotrope [Turkevich et al. 2014], it is difficult to
extract any additional influence of aggregate particle size on the severity of the carbonaceous
explosions.
For completeness, we have also examined the potential correlation with the lower end of the
distribution, dmin; there is poor correlation of both Pmax (R2 ~ 0.1) and KSt (R2 ~ 0.2) with dmin
.
0 2 4 6 8 10 12 14 16 18 206
6.5
7
7.5
8
R² = 0.0551443901744411
dmin [micron]
pmax
[bar]
0 5 10 15 2050
100
150
200
R² = 0.231259065983268
dmin [micron]
KSt [
bar-m
/sec]
Similarly, we have attempted to correlate MEC with aggregate particle size. The correlation is weak (R2 ~ 0.6) for
dmean, d50, ddom, dmax
0 20 40 60 80 1000
10
20
30
40
50
60
70
80
90
100
R² = 0.605699535555657
dmean [micron]
MEC [
g/m3
]
0 10 20 30 40 50 60 70 80 90 1000
10
20
30
40
50
60
70
80
90
100
R² = 0.622554170370054
d50 [micron]
MEC [
g/m3
]
0 20 40 60 80 100 1200
10
20
30
40
50
60
70
80
90
100
R² = 0.515696295380343
ddom [microns]
MEC [
g/m3
]
0 20 40 60 80 100 1200
10
20
30
40
50
60
70
80
90
100
R² = 0.565799154980731
dmax [micron]
MEC [
g/m3
]
Again, the weak statistical correlation contradicts the NanoSafe hypothesis, namely, while the
smaller aggregates should be more explosive, statistically, the smaller aggregates exhibit a
higher threshold MEC for explosion.
There is no correlation of MEC with dmin (R2 ~ 0.1)
0 5 10 15 200
10
20
30
40
50
60
70
80
90
100
R² = 0.0630170208584863
dmin [micron]
MEC
[g/m
3]
We have not attempted to correlate the more limited data sets for MIE, MITcloud with the
aggregate particle size distribution parameters.