Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Miyakawa, Kazuya; Hayano, Akira; Sato, Naomi; Nakata, Kotaro*; Hasegawa, Takuma*
JAEA-Data/Code 2023-009, 103 Pages, 2023/09
This borehole investigation was carried out to confirm the validity of the distribution of low flow areas deep underground estimated based on the geophysical survey in FY 2020, as a part of an R&D supporting program titled "Research and development on Groundwater Flow Evaluation Technology in Bedrock" under contract to the Ministry of Economy, Trade and Industry (2021, 2022 FY, Grant Number: JPJ007597). The borehole name is Horonobe Fossil seawater Boring-1 and is referred to as HFB-1 borehole. HFB-1 is a vertical borehole drilled adjacent to the Horonobe Underground Research Laboratory (URL), which was drilled from the surface to a depth of 200 m in FY2021 and from a depth of 200 m to 500 m in FY2022. This report summarizes information related to the drilling of HFB-1 and various data (rock core description, geophysical logging, chemical analysis, etc.) obtained from the borehole investigation.
Sato, Naomi; Hayano, Akira; Teshima, Minoru*; Negi, Tateyuki*; Yamane, Terumasa*; Kawasaki, Shinji*
no journal, ,
This paper reports the preliminary results of the magnetotelluric (MT) survey aiming to evaluate the three-dimensional distribution of fossil seawater in the Horonobe area. The MT survey was conducted in the area of 3 km square adjacent to the Horonobe Underground Research Laboratory at 60 points. Our results showed that the distribution of the resistivity varied in accordance with the geological structure. This survey was funded by the Ministry of Environment, Trade and Industry.
Sato, Naomi; Hayano, Akira; Kashihara, Koji*; Teshima, Minoru*; Negi, Tateyuki*
no journal, ,
The objective of this study was to assess the effect of borehole siting on collocated cokriging (COK) for estimating the three-dimensional distribution of chloride ion concentration (Cl) and stable isotope (O, D) compositions of groundwater in the Horonobe area, which are indicators of paleo-saline water. When compared to the full model consisting of ten borehole surveys, COK with a partial dataset consisting of 1-3 borehole surveys covering the entire range of resistivity from the electromagnetic survey in the study area performed better than other datasets. The results suggested that a borehole survey at a site with the representative geochemical feature in the region could yield adequate coefficients in the COK and, as a result, produce reasonable estimates with a cost-effective procedure. This survey was funded by the Ministry of Environment, Trade and Industry.
Hayano, Akira; Sato, Naomi
no journal, ,
no abstracts in English