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JAEA Reports

A Modeling and numerical simulation for evaluating groundwater flow at the Horonobe coastal area (Contract research)

Maekawa, Keisuke; Saegusa, Hiromitsu; Inaba, Kaoru*; Shimogochi, Takafumi*

JAEA-Research 2010-001, 238 Pages, 2010/07

JAEA-Research-2010-001.pdf:30.2MB

In the design and safety assessment of the geological disposal system of the high-level radioactive waste (HLW), it is extremely important to improve the reliability of the evaluation of the investigation of the geological environment, which provides technical basis. Especially, the knowhow and the experience of groundwater flow modeling based on the data acquired in deep underground at the coastal area are needed to be enhanced because these are little. Against this background, we have carried out modeling and groundwater flow simulation of the Horonobe coastal area. The knowledge and the knowhow acquired through this work were accumulated and arranged as a knowledge base by executing the following items. (1)The discussion of applicability of the workflow of evaluation of the groundwater flow for the coast region, and extension and update according to need. (2)Understand of groundwater flow based on existing investigation result in Horonobe coastal area, (2-1)Estimation of distribution of salinity in groundwater, (2-2)Extraction and arrangement of knowhow and judgment basis in modeling and simulation works. As a result, the knowledge was expanded concerning the groundwater flow evaluation methodology needed in design and safety assessment of the geological disposal system that is able to correspond to various geological environments in our country.

JAEA Reports

Research on the Hydrogeological and Geochemical Conditions at the Coastal Area and Submarine Formations

Tokunaga, Tomochika*; Taniguchi, Makoto*; Shimada, Jun*; Zhang, J.*; Inaba, Kaoru; Saegusa, Hiromitsu; Iwatsuki, Teruki

JNC TY7400 2003-003, 142 Pages, 2003/05

JNC-TY7400-2003-003.pdf:6.85MB

One of the major concerns for the high-level radioactive waste disposal is the possibility of the radionuclides to reach biosphere by groundwater flow. Recent research results have shown that the fresh groundwater discharge from subsea formations are widespread phenomena, thus, it is necessary to evaluate the submarine groundwater discharge as possible pathways of contaminant discharge towards the biosphere. It is also important to unravel the groundwater flow and associated material transport at the coastal area and subsea formations. To better understand the groundwater flow processes and the submarine groundwater discharge, we have conducted the hydrological, hydrogeological, geochemical, and numerical modeling studies at the Kurobe alluvial fan and its offshore, Toyama Prefecture, Japan. In this report, the results of the following research activities are presented:1)Development and application of a method to detect the locations of the submarine groundwater discharge.2)Development and application of a method to collect uncontaminated groundwater samples from subesa formations.3)Measurements of submarine groundwater dischange fluxes by automated seepage meter.4)Hydrological and geochemical studies for groundwater flow at the coastal area.5)Geochemical studied to understand sources of fresh submarine groundwater discharge.6)Extamination of groundwater flow and submarine groundwater discharge using methane concentration and carbon isotope ratio.7)Numerical modeling studies for coastal groundwater flow system.

Journal Articles

Journal Articles

None

; ; Saegusa, Hiromitsu; Takeuchi, Shinji

Saikuru Kiko Giho, (16), p.137 - 148, 2002/09

None

Journal Articles

Research and development of HTTR hydrogen production systems

Shiozawa, Shusaku; Ogawa, Masuro; Inagaki, Yoshiyuki; Onuki, Kaoru; Takeda, Tetsuaki; Nishihara, Tetsuo; Hayashi, Koji; Kubo, Shinji; Inaba, Yoshitomo; Ohashi, Hirofumi

Proceedings of 17th KAIF/KNS Annual Conference, p.557 - 567, 2002/04

The research and development program on nuclear production of hydrogen was started on January in 1997 as a study consigned by Ministry of Education, Culture, Sports, Science and Technology. A hydrogen production system connected to the HTTR is being designed to be able to produce hydrogen of about 4000 m3/h by steam reforming of natural gas, using a nuclear heat of 10 MW supplied by the HTTR. In order to confirm controllability, safety and performance of key components in the HTTR hydrogen production system, the facility for an out-of-pile test was constructed on the scale of approximately 1/30 of the HTTR hydrogen production system. Essential tests are also carried out to obtain detailed data for safety review and development of analytical codes. Other basic studies on the hydrogen production technology of thermochemical water splitting called an iodine sulfur (IS) process, has been carried out for more effective and various uses of nuclear heat. This paper describes the present status and a future plan on the R&D of the HTTR hydrogen production systems in JAERI.

Journal Articles

Journal Articles

Hydrogen production from methane using nuclear energy

Ohashi, Hirofumi; Inagaki, Yoshiyuki; Ogawa, Masuro; Onuki, Kaoru; Takeda, Tetsuaki; Nishihara, Tetsuo; Hayashi, Koji; Inaba, Yoshitomo; Shiozawa, Shusaku

Suiso Enerugi Shisutemu, 26(2), p.23 - 28, 2001/12

no abstracts in English

JAEA Reports

Present status of research on hydrogen energy and perspective of HTGR hydrogen production system

Miyamoto, Yoshiaki; Ogawa, Masuro; Akino, Norio; Shiina, Yasuaki; Inagaki, Yoshiyuki; Shimizu, Saburo; Onuki, Kaoru; Ishiyama, Shintaro; Katanishi, Shoji; Takeda, Tetsuaki; et al.

JAERI-Review 2001-006, 147 Pages, 2001/03

JAERI-Review-2001-006.pdf:9.2MB

no abstracts in English

Oral presentation

Influence of topographic and climatic perturbations on groundwater flow conditions

Saegusa, Hiromitsu; Inaba, Kaoru*; Moriya, Toshifumi; Onoe, Hironori

no journal, , 

In the study, groundwater flow modeling has been performed in order to evaluate influence of topographic and climatic perturbations on groundwater flow conditions in the Tono area, Gifu, Japan. It was shown from the results of this study that the topographic and climatic perturbations influence hydraulic gradient, and groundwater flow path, path length and travel time. It is also found that these influences have spatial difference due to hydrogeological heterogeneity caused by faults with hydraulic contrast.

Oral presentation

Technical know-how and decision process for site characterization on the deep geological environment, 7; A Case study for groundwater flow analysis at coastal area

Maekawa, Keisuke; Saegusa, Hiromitsu; Inaba, Kaoru*; Shimogochi, Takafumi*

no journal, , 

no abstracts in English

Oral presentation

Technical know-how and decision process for groundwater flow analysis at coastal area

Maekawa, Keisuke; Saegusa, Hiromitsu; Inaba, Kaoru*; Shimogochi, Takafumi*

no journal, , 

no abstracts in English

Oral presentation

Extrusion behavior of bentonite buffer, 2; Analytical study on extrusion behavior

Takaji, Kazuhiko*; Inaba, Kaoru*; Matsumoto, Kazuhiro; Fujita, Tomoo

no journal, , 

no abstracts in English

12 (Records 1-12 displayed on this page)
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