Environmental Engineering Reference
In-Depth Information
6
Cs-137
Long-lived beta-activity
Pb-212
Pb-214
5
4
3
2
1
0
30.11
5.12
10.12
15.12
Data of sampling
20.12
25.12
30.12
FIGURE 18.12
AMAD of aerosol carriers of
137
Cs, long-lived beta-active nuclides,
212
Pb, and
214
Pb in room
207/5 of the “Shelter” in December 2000.
submicrometer particles with small amounts of even dry particles can be formed. It should be noted
that during welding work, sizes of radiocesium were AMAD = 1.02 μm.
Aerosols of radon and thoron daughters belong to condensation aerosols. They form due to
deposition of atoms of metals (Po, Pb, Bi) that arise during radioactive decay of gaseous mater-
nal substances on very small aerosol particles, called condensation nuclei. These aerosols can be
formed both inside the “Shelter” due to emanation of radon and thoron from building constructions
and from the free atmosphere. The AMAD values of such particles are in the range of 0.08-0.8 μm.
Important data were received on December 9 in room 207/5, when aerosol concentration was
the highest. Three methods were used: beta-radiation radiometry, gamma-spectrometry, and
beta-spectrometry. It was found that all radionuclides (
90
Sr,
134
Cs,
137
Cs,
241
Am) were disposed on
the same particles with AMAD values near 1.5 μm. The ratio of
137
Cs/
90
Sr was near 1.15 and was
practically equal to the data presented in Ref. [45] for average nuclear fuel of the fourth block at the
moment of the accident.
During the study of ejection from the “Shelter” from 1996 to 2000, a ive-cascade impactor of the
Institute of Biophysics (Russia) and an Andersen impactor PM-10 were used.
A majority of the measurements were provided for
137
Cs (22 samples) and
241
Am (16 samples). It
was found that the AMAD for aerosols of
137
Cs was 2.9 ± 1.5 μm, and for
241
Am it was 1.4 ± 0.4 μm.
No systematically measured AMAD values of aerosols of
90
Sr and
239 + 240
Pu were in the range
of 3.1-4.5 and 6.0-9.3 μm, respectively. It should be noted that these data are similar to the data
obtained by the MMF. Unfortunately, in Ref. [46] there were no comments on the substantial differ-
ence in the size of Pu and Am, which is a DP of
241
Pu.
18.9.6 r
adioactive
a
erosol
d
isPersity
in
tHe
“b
yPass
”
s
ysteM
oF
tHe
“s
Helter
”
in
2002-2010
Over 300 samples taken on three-layer ilters at the “Bypass” system enabled us to determine the
size distribution of aerosols. It was established that the radioactive products of Chernobyl accident
had been leaving the “Shelter” on particles with AMAD > 1 μm and DPs of radon and thoron—on
submicron particles.
Search WWH ::
Custom Search