FY2013 Radioactivity Concentration of Iodine 131 in Soil Sample through the Analysis of
Iodine 129 ( Decay correction: June 14, 2011 )
- In order to elaborate the map of iodine 131, this data was created in "Establishment of A
Comprehension Approach of Long Term Effects by Radioactive Substances Due to Fukushima Daiichi
Nuclear Power Plant Accident" lead by the Secretariat of the Nuclear Regulation Authority.
This year, the area of analyses for the iodine 129 was expanded for areas where data had been
barely obtained and deposition data of iodine 131 was reconstructed.
- This data shows radiation (Bq) per unit area (m2) i.e., "Deposition".
- In the Second Distribution Survey, a good correlation between iodine 129 and iodine 131
concentrations in soil was observed. In this data, iodine 131 deposition density at each
sampling point was derived by multiplying iodine 129 concentrations obtained in this survey
and the (iodine 131)/(iodine 129) ratio "9368" (as of June 14, 2011) obtained in the Second
Distribution Survey. Note: (iodine131)/(iodine129) ratio should be adjusted when more analyses
are performed in the future.
- One sample at each sampling point was used for analysis because the analysis of iodine 129
is time consuming. In this data, the average of each sampling point was calculated by the
following method.
A conversion factor was derived as (Deposition density)/(Average
deposition density of 5 sampling points) of cesium 137. The average deposition density
(Bq/m2) of iodine 131 was calculated by dividing deposition density of iodine 131
by the conversion factor.
- Measurement procedure of iodine 129 deposition densities.
First, soil sample was taken
out from the U-8 container and stirred in the plastic bag till being uniform. A part of the
soil sample in the plastic bag was taken out and triturated in an agate ball mill to use as a
powder sample for analysis. The powder sample was heated up in 1000 degree C and then
volatilized radioactive iodine was collected in an alkaline solution. Using a part of the
solution, iodine 127 (stable iodine) was measured by a ICP-MS(Agilent 7700 or 8800). Using the
leftover trap solution, the radioactive iodine was separated and refined by solvent extraction
and back extraction, and then silver iodide (AgI) was made by adding caustic silver. Using the
AgI as a target, ratio of iodine 129 atomicity to iodine 127 atomicity (hereafter, (iodine
129)/(iodine 127) ratio ) was measured by AMS (Accelerator Mass Spectrometry). The chemical
separation method of iodine was based on the reference-I. The measurement conditions of AMS
were based on the reference-II. The radioactivity concentration (Bq/kg) of iodine 129 in the
soil sample was derived using radioactivity concentration of iodine 127 and (iodine
129)/(iodine 127) ratio. Considering the weight and volume of the relevant soil sample, iodine
129 deposition densities per a unit area (Bq/m2) was derived. The detection limit
was approximately 0.001Bq/m2.
- Reference I. Muramatsu, Y., Y. Takada, H. Matsuzaki, S. Yoshida: AMS analysis of 129I
in Japanese soil samples collected from background areas far from nuclear facilities.
Quaternary Geochronology, 3, 291-297 (2008)
- Reference II. Matsuzaki, H.,Y. Muramatsu, K. Kato, M. Yasumoto and C. Nakano.
Development of 129I-AMS system at MALT and measurements of 129I concentrations in several
Japanese soils. Nuclear Instruments and Methods in Physics Research Section B, 259,
721-726 (2007)
- The analysis results show estimated iodine 131 deposition density and measured iodine 131
deposition density in the first distribution survey as reference.
FY2012 Concentration of Iodine 131 in Soil Samples through the Analysis of Iodine 129 ( Decay
correction: June 14, 2011 )
- In order to elaborate the map of iodine 131, this data was created in "Establishment of A
Comprehension Approach of Long Term Effects by Radioactive Substances Due to Fukushima Daiichi
Nuclear Power Plant Accident" lead by the Ministry of Education, Culture, Sports, Science and
Technology in Japan..
- This data shows radiation (Bq) per unit area (m2) i.e., "Deposition" .
- In the Second Distribution Survey, a good correlation between iodine 129 and iodine 131
concentrations in soil was observed. In this data, iodine 131 deposition density at each
sampling point was derived by multiplying iodine 129 concentrations obtained in this survey
and the (iodine 131)/(iodine 129) ratio "9368" obtained in the Second Distribution Survey".
Note: (iodine131)/(iodine129) ratio should be adjusted when more analyses are performed in the
future.
- One sample at each sampling point was used for analysis because the analysis of iodine 129
is time consuming. In this data, the average of each sampling point was calculated by the
following method.
A conversion factor was derived as (Deposition density)/(Average
deposition density of 5 sampling points) of cesium 137. The average deposition density
(Bq/m2) of iodine 131 was calculated by dividing deposition density of iodine 131
by the conversion factor.
- Measurement procedure of iodine 129 deposition densities.
First, soil sample was taken
out from the U-8 container and stirred in the plastic bag till being uniform. A part of the
soil sample in the plastic bag was taken out and triturated in an agate ball mill to use as a
powder sample for analysis. The powder sample was heated up in 1000 degree C and then
volatilized iodine was collected in an alkaline solution. Using a part of the solution, iodine
127 (stable iodine) was measured by a ICP-MS(Agilent 7700). Using the leftover trap solution,
the radioactive iodine was separated and refined by solvent extraction and back extraction,
and then silver iodide (AgI) was made by adding silver nitrate. Using the AgI as a target,
ratio of iodine 129 to iodine 127 (hereafter, (iodine 129)/(iodine 127) ratio ) was measured
by AMS (Accelerator Mass Spectrometry). The chemical separation method of iodine was based on
the reference-I. The measurement conditions of AMS were based on the reference-II. The
radioactivity concentration (Bq/kg) of iodine 129 in the soil sample was derived using
radioactivity concentration of iodine 127 and (iodine 129)/(iodine 127) ratio. Considering the
weight and volume of the relevant soil sample, iodine 129 deposition densities per a unit area
(Bq/m2) was derived. The detection limit was approximately
0.001Bq/m2.
- Reference I. Muramatsu, Y., Y. Takada, H. Matsuzaki, S. Yoshida: AMS analysis of 129I
in Japanese soil samples collected from background areas far from nuclear facilities.
Quaternary Geochronology, 3, 291-297 (2008)
- Reference II. Matsuzaki, H.,Y. Muramatsu, K. Kato, M. Yasumoto and C. Nakano.
Development of 129I-AMS system at MALT and measurements of 129I concentrations in several
Japanese soils. Nuclear Instruments and Methods in Physics Research Section B, 259,
721-726 (2007)
- In this database, results for the deposition density of estimated iodine 131 are listed
together with those of measured cesium 137 obtained from the first deposition survey as
reference.
FY2011 Concentration of Iodine 131 in Soil Samples through the Analysis of Iodine 129 ( Decay
correction: June 14, 2011 )
- This data was created to study if the deposition densities of iodine 131 and iodine 129 are
correlated and then if deposition density of iodine 131 is derived by deposition density of
iodine 129 using said correlation between iodine 131 and iodine 129
- This data shows radiation (Bq) per unit area (m2) i.e., "Deposition" .
- This published data was prepared based on the results of iodine 129 deposition densities
obtained in the soil samples that iodine 131 were measured in the first distribution survey.
- Measurement procedure of iodine 129 deposition density
First, soil sample was taken out
from the U-8 container and stirred in the plastic bag till being uniform. A part of the soil
sample in the plastic bag was taken out and triturated in an agate ball mill to use as a
powder sample for analysis. The powder sample was heated up in 1,000 degree C and then
volatilized iodine was collected in an alkaline solution. Using a part of the solution, iodine
127 (stable iodine) was measured by a ICP-MS(Agilent 7,700). Using the leftover trap solution,
the radioactive iodine was separated and refined by solvent extraction and back extraction,
and then silver iodide (AgI) was made by adding caustic silver. Using the AgI as a target,
ratio of iodine 129 atomicity to iodine 127 atomicity (hereafter, (iodine 129)/(iodine 127)
ratio ) was measured by AMS (Accelerator Mass Spectrometry). The chemical separation method of
iodine was based on the reference-II. The measurement conditions of AMS were based on the
reference-I. The radioactivity concentration (Bq/kg) of iodine 129 in the soil sample was
derived using radioactivity concentration of iodine 127 and (iodine 129)/(iodine 127) ratio.
Considering the weight and volume of the relevant soil sample, iodine 129 deposition density
per a unit area (Bq/m2) was derived. The detection limit was approximately 0.001
Bq/m2.
- Reference I. Matsuzaki, H.,Y. Muramatsu, K. Kato, M. Yasumoto and C. Nakano.
Development of 129I-AMS system at MALT and measurements of 129I concentrations in several
Japanese soils. Nuclear Instruments and Methods in Physics Research Section B, 259,
721-726 (2007)
- Reference II. Muramatsu, Y., Y. Takada, H. Matsuzaki, S. Yoshida: AMS analysis of 129I
in Japanese soil samples collected from background areas far from nuclear facilities.
Quaternary Geochronology, 3, 291-297 (2008)
- Estimation method of deposition density of iodine 131
The deposition density ratio of
(iodine 131)/(iodine 129) was 9368 (as of June 14, 2011), as a result of comparison between
iodine 129 deposition measured in this survey and iodine 131 deposition obtained in the first
distribution survey. Iodine 131 deposition density was estimated by multiplying iodine 129
deposition density and (iodine131)/(iodine129) ratio. The data show estimated iodine 131
deposition density and measured iodine 131 deposition density in the first distribution survey
as reference. Note: (iodine131)/(iodine129) ratio should be adjusted when more analyses are
performed in the future.