Defınıtıon of the Factors of
Defınıtıon of the Factors of
Passıng the Area-Pollutıon Radıo
Passıng the Area-Pollutıon Radıo
Nucleıds Soıl ın the Area
Nucleıds Soıl ın the Area
Orujova Jamala
Orujova Jamala
Institute of Radiation
•
On the settlement (village) Romani of the Absheron peninsula is On the settlement (village) Romani of the Absheron peninsula is situated a factory producing iodine. Boring water as used as a situated a factory producing iodine. Boring water as used as aprimary (raw) product in factory a long time. In doing so active coal primary (raw) product in factory a long time. In doing so active coal
was used as absorbent at the factory. was used as absorbent at the factory.
•
It is known boring water contains a certain amount of natural It is known boring water contains a certain amount of natural radionuclides having a long nuclear fission half period such as radionuclides having a long nuclear fission half period such asuranium -238, thorium-232, radium-226 and potassium- 40. uranium -238, thorium-232, radium-226 and potassium- 40.
•
After disintegration of the USSR the factory was closed. A lot of After disintegration of the USSR the factory was closed. A lot ofproduced coal was left at the factory yard. This coal makes a pile of produced coal was left at the factory yard. This coal makes a pile of
3 meters high and 600 square meters area. 3 meters high and 600 square meters area.
•
This coal pile creates at the territory a radiation field equal from This coal pile creates at the territory a radiation field equal from 700 to 1000 μR/h.700 to 1000 μR/h.
•
We have chosen this territory as an experiment area and studying We have chosen this territory as an experiment area and studying the impact of radiation on the grass formation here.the impact of radiation on the grass formation here.
•
In this work presented to your attention radionuclides polluting the In this work presented to your attention radionuclides polluting the area were identified and their vertical and horizontal distribution was area were identified and their vertical and horizontal distribution wasresearched. researched.
Slide 1
Slide 1
.
.
Distribution
Distribution
4040К
К
isotope in soil depending on depth
isotope in soil depending on depth
in area of experience.
in area of experience.
Slide 2. Distribution
Slide 2. Distribution
226226Ra isotope in soil depending on
Ra isotope in soil depending on
depth in area of experience.
depth in area of experience.
Slide 3. Distribution
Slide 3. Distribution
232232Th isotope in soil depending on
Th isotope in soil depending on
depth in area of experience.
depth in area of experience.
Pic.4 Distribution of radionuclides in soil by different
Pic.4 Distribution of radionuclides in soil by different
radiative background.
•
We can observe 35 - 40 sm deep maximum
We can observe 35 - 40 sm deep maximum
studying the results of vertical migration.
studying the results of vertical migration.
•
It will be noted that Chernobil radionuclides are
It will be noted that Chernobil radionuclides are
distributed mainly at 15– 20 sm deep in the
distributed mainly at 15– 20 sm deep in the
polluted territory.
polluted territory.
•
The detected distribution radionuclides on the
The detected distribution radionuclides on the
Absheron peninsula, apparently, connected with
Absheron peninsula, apparently, connected with
sandly composition of researched soil.
sandly composition of researched soil.
•
Studying the horizontal distribution we can see
Studying the horizontal distribution we can see
that moving away from the source of pollution
that moving away from the source of pollution
the amount of radionuclides diminishes and
the amount of radionuclides diminishes and
gets to background level at the distance of 70 -
gets to background level at the distance of 70 -
80 meter.
•
The coefficient of gathering of radionuclides in
The coefficient of gathering of radionuclides in
the plants and their different organs is identified
the plants and their different organs is identified
according to the results.
according to the results.
•
Gathering coefficient are identified by the
Gathering coefficient are identified by the
formula
formula
:
:
K
K
t t=
=
n
n
r,pr,p(Bk/kg) (Bk/kg) / /n
n
r,sr,s (Bk/kg) .(Bk/kg) .•
(Here (Here nnr,pr,p and and nnr,sr,s - shows the concentration of radionuclides - shows the concentration of radionuclidesin the plant and the soil).
in the plant and the soil).
•
The results about gathering coefficient are given
The results about gathering coefficient are given
in Slides 13-14.
Pic.
Pic. 5
5. Factors accumulation of radio nucleids in plants.
. Factors accumulation of radio nucleids in plants.
Kind of plant Quantity radio nucleids in soil Factors accumulation of radio nucleids in plants-Kt 40К 226Rа 232Th 40К 226Rа 232Th Alhagi pseudalhagi 120 - 1300 70 – 50000 30 - 4500 0.60 0.10 0.05 Zygophyllum L. 3.39 0.12 0.00 Turnefortia Sibirica 7.50 0.28 0.13 Juncus acutus L. 4.72 0.69 0.29
Pic.
Pic.
6
6
. Factors accumulation of radio nucleids in different
. Factors accumulation of radio nucleids in different
organs of plants.
organs of plants.
Kind of plant. (organs) Quantity radio nucleids in soil (Bk/kg) Factors accumulation of radio nucleids in different organs of plants - Кт
40К 226Rа 232Th 40К 226Rа 232Th Alhagi pseudalha gi Root 1 2 0 – 1 3 0 0 7 0 – 5 0 0 0 0 3 0 – 4 5 0 0 0.12 0.09 0.00 Stalk 0.47 0.01 0.05 Zygophyl lum L. Root 1.10 0.07 0.00 Stalk 2.25 0.05 0.00 Leaf 0.04 0.00 0.00 Turnefor tia Sibirica Root 2.43 0.05 0.00 Stalk 1.78 0.03 0.00 Leaf 3.28 0.20 0.13 Juncus Root 0.79 0.69 0.22