yamauchi et al: effect of the ionizing radiation on the rain-time atmospheric electric field (pg)
DESCRIPTION
Yamauchi et al: Effect of the ionizing radiation on the rain-time atmospheric electric field (PG). Fukushima. Chernobyl. Helsinki PG. rain. PICO 09:36 (EGU2013-3064). 2 week. Rain time peaks. - PowerPoint PPT PresentationTRANSCRIPT
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Yamauchi et al: Effect of the ionizing radiation on the rain-time atmospheric electric field (PG)
2 week
rainChernobyl
PICO 09:36 (EGU2013-3064)
Fukushima
Helsinki PG
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Rain time peaks (a) Distribution of PG peak values every 15 min in logarithmic bins (25% stepping in horizontal axis).
(b) Relative PG values compared to the peak during 5 min before (right) and 5 min after (left) the negative peaks (when peak PG < -0.2 kV/m).
The same period of the year (14 March to 30 April) is plotted for 2006-2010 (gray triangles), 2006-2010 average (black line) and 2011 (red cross).
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Effect of the ionizing radiation on the rain-time atmospheric electric field
M. Yamauchi1, M. Takeda2, M. Makino3, and T. Owada4
(1) Swedish Institute of Space Physics (IRF), Kiruna, Sweden(2) Kyoto University, Japan (3) National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan(4) Kakioka Magnetic Observatory, Japan Meteorological Agency, Ishioka, Japan
PICO (EGU2013-3064) / GI1.4
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Effect of ionizing radiation
ionization
Electric field reduction
Instrument to measure E-field
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Extra ionization causes the atmospheric E-field (PG) decrease
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Atmospheric E-field (PG) after the accident (EGU-2012)
2 week
rain
Chernobyl
Fukushima
Helsinki PG
PG suddenly decreased!
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Combine with dose rate and rain data
Interpretation: PG obs for different contamination
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At Kakioka, 150 km SW of the FNPP1 (EGU-2012)(A) 14-20 March = floating radionuclide• 14 March: Dry deposition on 14 March at Kakioka, 150 km. •16-20 March: Strong re-suspension by wind.
(B) - 20 April = some re-suspension• 20-21 March: Wet deposition at Kakioka by the first substantial rain. • - 20 April : Re-suspension by daily wind. Transport from highly-contaminated to moderately-contaminated areas.
(C) afterward• - summer: minor plumes from the FNPP-1.
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Today, we examine rain-time PG
• Analyses is not possible without < 5 min resolution PG data (i.e., impossible for Chernobyl).
• Case-study is very difficult for very variable phenomenon
Difficulty: PG under rain-cloud is highly variable and dynamic.
Therefore, we examine statistically(Kakioka PG sampling is 1 Hz. Data is calibrated and compared with backup measurement)
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PG vs. rain (hourly value)
Less spread of <PG> right after FNPP accident?
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Is “less spread” real? Statistic of all peaks • We used 1-min value instead of hourly value • We examine all positive and negative peaks in 15-min bins• Remove double-counted peaks between neighboring 15-min bins• Remove even minor peaks (see illustration)
We removed this type of small peaks from the statistics
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Result: distribution of the peaks (a) Distribution of PG peak values every 15 min in logarithmic bins (25% stepping in horizontal axis).
(b) Relative PG values compared to the peak during 5 min before (right) and 5 min after (left) the negative peaks (when peak PG < -0.2 kV/m).
The same period of the year (14 March to 30 April) is plotted for 2006-2010 (gray triangles), 2006-2010 average (black line) and 2011 (red cross).
![Page 13: Yamauchi et al: Effect of the ionizing radiation on the rain-time atmospheric electric field (PG)](https://reader035.vdocuments.us/reader035/viewer/2022062409/568146c2550346895db3f9da/html5/thumbnails/13.jpg)
• Quick decay & development for March-April 2011 (red/black) .
• May (blue) and March/April is different because of different types of rain cloud (seasonal effect).
• May is already back to normal (consistent with the end of re-suspension).
The characteristic time of the negative peaks
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Summary For the first time, effect of the floating radioactive materials on the rain-time PG was examined, using PG data at Kakioka (150 km SW of FNPP1). (1) one-hour averaged rain-time PG after the accident is not as much scattered to the negative side as those during the same season at different years. (2) The range/distribution of the peak value is not changed very much. (3) But the time scale of negative peaks after the accident is shortened compared to those before the accident.
The observed short time scale can be interpreted in two ways: (1) Quick development and decay of the electric charges in the cloud nuclei.(2) Shielding of the charge of horizontally moving cloud when the charges are not exactly the above the PG measurement.
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extra slides for questions
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Low PG even after 1 year because of radiocesium (half-life is 134Cs = 2 yr, 137Cs = 30 yr).
seasonal effect
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weather
2011-3-14 (00 UT) 2011-3-16 (00 UT)
2011-3-20 (00 UT)
2011-3-21 (00 UT)
2011-3-15 (00 UT)
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Fallout
(a)
(b)
(c)Three types of fallout
(a) (b) (c)
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PG drops after nuclear test (Harris, 1955) and Chernobyl Accident (Tuomi, 1988)
24 hours
2 weeks
PG at Tuscon after Navada Test
12 16 20 24 4 8
Shower
Harris, 1955 (JGR)
Shower
26/4 29/4 1/5 10/5
PG at Helsinki after Chernobyl AccidentRain
Past (wet deposition)
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detailed analyses (EGU-2012)
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q: production (by cosmic ray, radon, and -ray)α : neutralization , β : attaching to aerosol (density N)
Ion density n: dn/dt = q - αn2 - βnN
aerosol
+
positive ion+
+
++
+
+
++
molecule
negative ion
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With atmospheric electric field
aerosol
+
+
+
++
+
+
++
negative ion
positive ion
E
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Main Sub Electrometer Electrostatic sensor type Field mill type
Collector
Type Water-dropper Mechanical Height 2.55 m 1.00m
Separation from the wall 1.17 m
Sampling 1 sec 1sec
Latitude Longitude
3613'56"N 14011'11"E
PG measurement at Kakioka