Refine your search:     
Report No.
 - 
Search Results: Records 1-4 displayed on this page of 4
  • 1

Presentation/Publication Type

Initialising ...

Refine

Journal/Book Title

Initialising ...

Meeting title

Initialising ...

First Author

Initialising ...

Keyword

Initialising ...

Language

Initialising ...

Publication Year

Initialising ...

Held year of conference

Initialising ...

Save select records

Journal Articles

Advection-dispersion modelling of tritium and chloride migration in the Lake233 drainage basin

Klukas, M. H.*; Moltyaner, G. L.*; Takeda, Seiji; Yamazaki, L. S.*; Kozter, T. G.*

AECL-RC-2132, p.1 - 42, 1998/08

no abstracts in English

Oral presentation

Numerical modeling of pore water migration and water quality evolution due to compaction and diagenesis processes of sedimentary rock

Komura, Yuto*; Kashiwaya, Koki*; Miyakawa, Kazuya; Nakata, Kotaro*; Koike, Katsuaki*

no journal, , 

no abstracts in English

Oral presentation

A Numerical modeling of groundwater evolution due to compaction and diagenesis of sedimentary rock at Horonobe area

Komura, Yuto*; Kashiwaya, Koki*; Miyakawa, Kazuya; Nakata, Kotaro*; Koike, Katsuaki*

no journal, , 

no abstracts in English

Oral presentation

Analysis of environmental fate of radiocesium in the Abukuma River basin for 30 years after the Fukushima Dai-ichi Nuclear Power Plant accident

Ikenoue, Tsubasa; Shimadera, Hikari*; Kondo, Akira*

no journal, , 

We evaluated the environmental fate of $$^{137}$$Cs in the Abukuma River Basin from 2011 to 2040 by using a distributed radiocesium prediction model. The model well reproduced interannual variations in the concentration of $$^{137}$$Cs in the suspended sediment and the total outflow of $$^{137}$$Cs at Iwanuma near the estuary. Thirty years after the Fukushima Daiichi Nuclear Power Plant accident, it was estimated that the concentration of $$^{137}$$Cs in the suspended sediment decreased to 1.9% of the concentration in the earliest phase after the accident and the total outflow of $$^{137}$$Cs was equivalent to 4.6% of the initial deposition in the Abukuma River basin.

4 (Records 1-4 displayed on this page)
  • 1