チェルノブイリでの内部被ばくと土壌

IAEA (2006) Radiological Conditions in the Dnieper River Basin http://www-pub.iaea.org/MTCD/publications/PDF/Pub1230_web.pdf チェルノブイリの土壌についての覚え書き:http://togetter.com/li/474705
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Seiichi Ushikubo @sushikubo

@myen IAEA(2006) p138 "effective internal doses received by the rural population strongly depend on the dominating soil type in the village"

2013-03-20 08:31:23

低汚染のチェルノーゼム土壌(black soil)の地域に住む人が、最初の15年間で受けた被ばく量は、ほどんどゼロ。

Seiichi Ushikubo @sushikubo

@myen IAEA (2006) p138 "in black soil areas people received during the first 15 years after the accident ..."

2013-03-20 08:33:31
Seiichi Ushikubo @sushikubo

@myen IAEA (2006) p138 "exposures ranging from almost zero in low contaminated areas ..."

2013-03-20 08:34:14

Cs137の土壌汚染が 37 kBq/m2 のチェルノーゼム土壌の地域では、1 mSv (そのほとんどは 1986年分)。

Seiichi Ushikubo @sushikubo

@myen IAEA (2006) p138 "... up to 1 mSv (most of it in 1986) in rural settlements with 37 kBq/m2 of 137Cs in the soil."

2013-03-20 08:34:49

チェルノーゼム土壌に住む人たちに比べて、ジョールンポドゾル土壌(sandy, soddy–podzolic soils)に住む人たちの内部被ばくは、2から3倍。

Seiichi Ushikubo @sushikubo

@myen IAEA (2006) p138 "In areas with sandy, soddy–podzolic soils, the dose was two to three times as much"

2013-03-20 08:35:40

チェルノーゼム土壌の地域に住む人に比べ、泥炭土壌(peaty)に住む人が受ける内部被ばくは、桁の変化で多くなる。

Seiichi Ushikubo @sushikubo

@myen IAEA(2006) "in areas with dominating peaty soils, internal dose was typically an order of magnitude larger than in black soil areas."

2013-03-20 08:37:20

現時点で食物からの内部被ばく
 チェルノーゼム:0.004 mSv/a
 ジョールンポドゾル:0.04 mSv/a
 泥炭:0.1 mSv/a

Seiichi Ushikubo @sushikubo

@myen IAEA (2006) p138 "At present, the inhabitants of low contaminated areas are receiving from ingestion of local food .."

2013-03-20 08:40:13
Seiichi Ushikubo @sushikubo

@myen IAEA (2006) "... up to 0.004 mSv/a in black soil areas, up to 0.04 mSv/a in sandy soil areas ..."

2013-03-20 08:40:52
Seiichi Ushikubo @sushikubo

@myen IAEA (2006) "... and about 0.1 mSv/a in villages located in peaty soil areas."

2013-03-20 08:41:29

1986年から2000年までの 0.04 - 0.6 MBq/m2 の地域での積算の内部被ばく
 チェルノーゼム土壌:1 - 12 mSv
 ジョールンポドゾル土壌:3 - 30 mSv
 泥炭土壌:8-120 mSv

Seiichi Ushikubo @sushikubo

@myen IAEA (2006) p139 "For assessment purposes, soils are classified into three major soil types: ..."

2013-03-20 08:47:52
Seiichi Ushikubo @sushikubo

@myen IAEA(2006) ".. black or chernozem soil; podzol soil (including both podzol sandy and podzol loamy soils); and peat–bog or peat soil.

2013-03-20 08:50:18
Seiichi Ushikubo @sushikubo

@myen IAEA (2006) "In the settlements with 137Cs soil deposition of 0.04 – 0.6 MBq/m2, ..."

2013-03-20 08:51:20
Seiichi Ushikubo @sushikubo

@myen IAEA (2006) "the mean internal effective doses accumulated from 1986 to 2000 ..."

2013-03-20 08:52:00
Seiichi Ushikubo @sushikubo

@myen IAEA (2006) "... are in the range of about 1–12 mSv for black soil, 3–30 mSv for podzol soil and 8–120 mSv for peat soil."

2013-03-20 08:52:31