Table 2 (cont'd).
c. Detonation number 3.
Sample
M3-S4
M3-S3
M3-S2
M3-S1
Distance from crater (m)
5.46.2
9.410.1
14.615.3
20.020.8
Area sampled (m2)
1.16
1.16
1.16
1.16
Analytes detected:
RDX
Mass-aqueous (g)
44.0
14.0
10.1
4.5
Mass-soot (g)
0.8
2.9
26.4
1.1
Mass-total (g)
45
17
37
5.6
Concentration (g/m2)
39
15
31
4.8
HMX
Mass-aqueous (g)
2.2
2.1
1.4
0.7
Mass-soot (g)
7.8
15.6
62.6
4.1
Mass-total (g)
10
18
64
4.7
Concentration (g/m2)
9
15
55
4.1
NG
Mass-aqueous (g)
664
915
372
165
Mass-soot (g)
90
24
38
0.1
Mass-total (g)
754
939
410
165
Concentration (g/m2)
649
808
353
142
TNT
Mass-aqueous (g)
<d
<d
<d
<d
Mass-soot (g)
0.17
0.20
0.22
0.29
Mass-total (g)
0.17
0.20
0.22
0.29
Concentration (g/m2)
0.15
0.17
0.19
0.25
and it can potentially sorb to the aluminum tail fins. NG
the same factor as RDX and HMX, but they remained
is also present in the ignition cartridge within the round.
several orders of magnitude lower than RDX. The con-
NG is frequently found in post-blast propellant residue
centrations of NG were about the same as that found
(Yinon and Zitrin 1993) and it has been detected on
for round detonation 1, which implies that the source
demolition ranges (Fine et al. 1984). The concentra-
of the NG is different from that for RDX, HMX, and
tions of NG in the snow cover were sufficiently high to
TNT. Surface concentrations of RDX, HMX, and TNT
saturate the ECD, but the NG peaks were minor in the
for round detonation 3 were intermediate between those
HPLC-UV chromatograms at 254 nm. The NG concen-
found for rounds 1 and 2, while the concentrations found
trations were sufficiently high in some of the samples
for NG remained similar to that found for rounds 1 and
to obtain confirmatory spectra using the Photodiode Ar-
2 (Table 2c).
ray. NG is apparently less completely consumed in the
The lowest concentrations in these surface snow
detonation than TNT and RDX, based on the mass of NG
samples were generally found for samples collected the
found versus the amount of NG present in the round.
farthest away from the detonation; however, the oppo-
site was not true for the highest concentrations, which
sequent detonations varied considerably (Tables 2b and
were generally found at some intermediate distance.
c). The residues found in the surface snow collected
The surface areas where residues were deposited for
from the second detonation (Table 2b) were much
these three detonations were estimated from the visual
deposition of soot: 158 m2 for area 1, 81 m2 for area 2,
greater than those observed for the first one. In addi-
and 74 m2 for area 3. The larger area of deposition for
tion to the four analytes detected for the first detona-
tion (RDX, HMX, NG, and TNT), four additional
the first detonation may be a result of using the steel
plate under the round, thereby deflecting a greater per-
2-ADNT, and 4-ADNT) were detected in some or all
centage of the debris upward and out. The surface areas
of the samples from the second detonation. Surface con-
sampled for these three plumes were 24, 6.0, and 4.7
centrations of RDX ranged from 369 to 4430 g/m2;
m2, respectively. Thus, the percentages of the contam-
this is over 300 times the concentrations found for the
inated surface area that were sampled were 15, 7.4 and
first detonation. The concentrations of HMX were also
6.3%, respectively.
much greater than those found near the first detona-
If the mean surface concentrations that were
tion; concentrations ranged from 13 to 20% of the RDX.
obtained for each of these three areas are representa-
The concentrations of TNT were also higher by about
tive of the total surface area in which deposition was
9
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