The 13th International Conference on Environmental ... - Events
The 13th International Conference on Environmental ... - Events
The 13th International Conference on Environmental ... - Events
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Abstracts<br />
various percentage saturated test pieces to be dissolved in 4wt% NaCl soluti<strong>on</strong>. <str<strong>on</strong>g>The</str<strong>on</strong>g> time for 47% saturated <strong>on</strong>e was<br />
shorter than 1 Hr, but the time for 67% was l<strong>on</strong>ger than 5 Hrs. In case of 88%, it had not been dissolved yet in 7Hrs, but<br />
after drying the test piece it could be easily dissolved in 5 minutes. <str<strong>on</strong>g>The</str<strong>on</strong>g> results from the laboratory tests indicate that the<br />
unsaturated buffer material can be easily dissolved in NaCl 4wt% soluti<strong>on</strong>, and the wet buffer material can be dissolved<br />
by immersing in NaCl 4wt% soluti<strong>on</strong> after process of dry-hot-air blowing. Finally, in order to c<strong>on</strong>firm the effect of<br />
removal processes, simulated experiments were executed using small scale (1/14 scale) specimens. <str<strong>on</strong>g>The</str<strong>on</strong>g> 47% saturated<br />
buffer material specimen was easily removed by the process of immersing in NaCl soluti<strong>on</strong>, flushing NaCl soluti<strong>on</strong>,<br />
removing slurry by vacuum device, and re-using NaCl soluti<strong>on</strong> after depositi<strong>on</strong>. In the nearly saturated case, it was<br />
removed in cyclic process of dry-hot-air blowing and immersing in NaCl 4wt% soluti<strong>on</strong>.<br />
SESSION H10: Site Characterizati<strong>on</strong> and Modeling of Geological Envir<strong>on</strong>ment (2)<br />
1) 40135 – Dry-run of Site Investigati<strong>on</strong> Planning using the Manual for Preliminary Investigati<strong>on</strong> in Japan<br />
Shigeki Akamura, Tadashi Miwa, NUMO (Japan); Tatsuya Tanaka, Obayashi Corporati<strong>on</strong> (Japan);<br />
Hiroshi Shiratsuchi, Tokyo Electric Power Service Co.,Ltd. (Japan);<br />
Atsushi Horio, DIA CONSULTANTS CO., Ltd. (Japan)<br />
A stepwise site selecti<strong>on</strong> process has been adopted for geological disposal of HLW in Japan. Literature surveys,<br />
followed by preliminary investigati<strong>on</strong>s (PI) and, finally, detailed investigati<strong>on</strong>s in underground facilities will be carried<br />
out in the successive selecti<strong>on</strong> stages. In the PI stage, surface-based investigati<strong>on</strong>s such as borehole surveys and<br />
geophysical prospecting will be implemented.<br />
NUMO recognizes that sustained improvement of internal expertise is very important to ensure that the PI will be<br />
implemented rigorously and efficiently. <str<strong>on</strong>g>The</str<strong>on</strong>g>refore existing knowledge and experience in the planning and management<br />
of site investigati<strong>on</strong>s were compiled in the form of two manuals: the Preliminary Investigati<strong>on</strong> Planning Manual (PIPM)<br />
and the Preliminary Investigati<strong>on</strong> Management Manual (PIMM). <str<strong>on</strong>g>The</str<strong>on</strong>g> manuals were based <strong>on</strong> the experience in overseas<br />
site investigati<strong>on</strong> programs, and has further been refined by taking experience from site investigati<strong>on</strong>s in Japan (e.g. from<br />
generic URLs) into account. NUMO has applied them in its own R&D programs, such as the dry-run studies for various<br />
geological envir<strong>on</strong>ments (e.g. coastal and island).<br />
This paper outlines the process and the results of a dry-run study which applied the revised PIPM to the Yokosuka<br />
area where the dem<strong>on</strong>strati<strong>on</strong> and validati<strong>on</strong> project for PI technologies has been c<strong>on</strong>ducted. <str<strong>on</strong>g>The</str<strong>on</strong>g> planning of the PI was<br />
performed according to the eight steps in the PIPM. <str<strong>on</strong>g>The</str<strong>on</strong>g> GET (Geosphere Evaluati<strong>on</strong> Team) c<strong>on</strong>sisting of staffs from site<br />
characterizati<strong>on</strong>, performance assessment and repository design groups in NUMO, was established for the PI planning.<br />
This task force team has resp<strong>on</strong>sibility not <strong>on</strong>ly for the planning but also for making key decisi<strong>on</strong>s regarding the<br />
performance of the program. <str<strong>on</strong>g>The</str<strong>on</strong>g> SDMT (Site Descriptive Modeling Team) was formed for site modeling activities.<br />
Initial geoscientific c<strong>on</strong>ceptual models were established based <strong>on</strong> the interpretati<strong>on</strong> of existing site informati<strong>on</strong> around<br />
the area. Various c<strong>on</strong>ceptual models were c<strong>on</strong>structed due to the limited amount of existing informati<strong>on</strong>. Site descriptive<br />
models were derived taking such variati<strong>on</strong>s in the c<strong>on</strong>ceptual models into account. <str<strong>on</strong>g>The</str<strong>on</strong>g> main targets for the PI planning<br />
were specified c<strong>on</strong>sidering the uncertainties in the models, requests from the repository c<strong>on</strong>cept as well as legal<br />
requirement. <str<strong>on</strong>g>The</str<strong>on</strong>g> integrated PI program set out the sequence of investigati<strong>on</strong>s and characterizati<strong>on</strong> activities to achieve<br />
the main targets. Less<strong>on</strong>s learned in the PI planning and the applicability of the revised PIPM were addressed as the<br />
c<strong>on</strong>clusi<strong>on</strong> of the dry-run.<br />
2) 40070 – Evaluati<strong>on</strong> of the l<strong>on</strong>g-term evoluti<strong>on</strong> of the groundwater system in the Mizunami area, Japan<br />
Takashi Mizuno, Teruki Iwatsuki, JAEA (Japan); Ant<strong>on</strong>i E. Milodowski, British Geological Survey (UK)<br />
This study aimed to develop a methodology for assessing the evoluti<strong>on</strong> of the l<strong>on</strong>g-term groundwater system, using<br />
fracture-filling calcite. Fracture-filling calcite mineralizati<strong>on</strong>, closely associated with groundwater flow paths, in deep (to<br />
ca. 1000 m) granitic rocks in and around Mizunami area, Japan, was studied by optical and cathode-luminescence<br />
microscopy, SEM, laser ablati<strong>on</strong> microprobe-ICP MS, stable isotope geochemistry, and fluid inclusi<strong>on</strong> analysis. As the<br />
results, four generati<strong>on</strong>s (I to IV) of calcite precipitati<strong>on</strong> can be differentiated based <strong>on</strong> their morphological and isotopic<br />
characteristics. Calcite I - calcite with indistinct morphology including the wall rock fragments (d13CPDB -31.4 ‰ ~<br />
-7.5 ‰, d18OPDB -32.7 ‰ ~ -8.0 ‰); Calcite II -calcite with euhedral rhombohedral and hexag<strong>on</strong>al crystal forms<br />
(d13CPDB 22.5 ‰ ~ -1.8 ‰, d18OPDB -15.5 ‰ ~ -6.5 ‰); Calcite III - calcite forming c-axis el<strong>on</strong>gated rhombohedral<br />
overgrowths seeded <strong>on</strong> top of Calcite II (d13CPDB -18.0 ‰ ~ 5.8 ‰, d18OPDB -11.1 ‰ ~ -2.3 ‰); Calcite IV - calcite<br />
forming small rhombohedral crystals nucleated <strong>on</strong> the surface of Calcite III (d13CPDB -12.5 ‰ ~ -1.7 ‰, d18OPDB<br />
-12.7 ‰~7.8 ‰). Carb<strong>on</strong> and oxygen isotopic ratios suggests that the Calcite I is of hydrothermal origin. On the other<br />
hand, Calcite II, IV and III were precipitated from freshwater and marine water, respectively. From the geohistorical<br />
point of view, depositi<strong>on</strong>al setting in Mizunami area was changed during Tertiary and Quaternary. Mizunami Group<br />
overlying above Toki granite is changed from lacustrine strata to marine strata. In additi<strong>on</strong>, upper Seto Group is a<br />
lacustrine stratum. <str<strong>on</strong>g>The</str<strong>on</strong>g> change of depositi<strong>on</strong>al setting corresp<strong>on</strong>ds to groundwater system assumed by mineralogical<br />
study. As there is no other evidence linked to penetrati<strong>on</strong> of high-salinity water into deep envir<strong>on</strong>ment in this area, it is<br />
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