Following the occurrence of the Niigata-Chuetsu-Oki Earthquake on July 16, 2007, the
Tokyo Electric Power Company, Inc. (TEPCO) received an instruction from the Nuclear
and Industrial Safety Agency (NISA) of the Ministry of Economy, Trade, and Industry
(METI) to ensure safety at the Kashiwazaki-Kariwa Nuclear Power Station (NPS)[*1].
In response to this, TEPCO submitted an interim report on the results of the geological
survey in areas adjoining the NPS to NISA on May 12, 2008.
Subsequently, this interim report was revised mainly with respect to assessment of
active faults in areas adjoining the NPS, in light of feedback from the national
council[*2]. The revised report, which additionally includes the results of geological
and tectonic evaluation of the NPS site and its adjoining areas, was submitted to NISA
today.
At the same time, TEPCO submitted a supplementary document to its previous report
on the revision of the design-basis seismic motion for the Kashiwazaki-Kariwa NPS,
which was submitted to NISA on September 22. As suggested by NISA's notification
on the issues to be incorporated into the seismic safety evaluation[*3], this
supplementary report describes the evaluation results of the exceedance probability
of the design-basis seismic motion.
1. Brief outline the reports (see appendices for their summaries)
(1) Report on geological survey results
The estimated length of the F-B fault that takes account of uncertainties has been
changed to approximately 36 km. Major additions to the initial report are (i) the
results of geological and tectonic evaluation of the NPS site and its adjoining
areas, (ii) the fact that no indications of activity of the Madonosaka and other
faults are observed at the NPS site and its adjoining areas, and (iii) assessment
results suggesting that there are no active faults or folds that should be
considered in seismic design.
(2) Supplementary report on the design-basis seismic motion
The results of the evaluation of the exceedance probability of the design-basis
seismic motion show that the probability of occurrence of any seismic motion in
excess of the defined design-basis seismic motion is about once every 10,000 to
100,000 years.
For reference purposes, TEPCO evaluated the confirmation seismic motion that has been
defined in consideration of the draft view of the Nuclear Safety Commission (NSC)[*4].
The results show that the properties of the confirmation seismic motion are roughly
the same as those of the design-basis seismic motion Ss-2, which has been obtained
from the results of the seismic motion evaluation using the fault model of an earthquake
that could be caused by the F-B fault.
2. Our future actions
In consideration of the survey results compiled into these reports, TEPCO will continue
the seismic safety evaluation of its facilities, based on the design-basis seismic motion.
- Appendices
(Appendix 1)
Summary of the Report on the Geology and Tectonics of the Kashiwazaki-Kariwa NPS Site
and its Adjoining Areas (PDF 86.4KB)
(Appendix 2)
Summary of the Supplementary Report on the Analysis of Seismic Observation Data Acquired
at the Kashiwazaki-Kariwa NPS during the 2007 Niigata-Chuetsu-Oki Earthquake and the
Design-Basis Seismic Motion (PDF 282KB)
*1 Instruction to ensure safety at the Kashiwazaki-Kariwa NPS
"[TEPCO] should continue the analysis of the seismic observation data obtained during
the [Niigata-Chuetsu-Oki] Earthquake and the confirmation of the seismic safety of its
safety-critical facilities."
An excerpt from "On Ensuring Safety at the Kashiwazaki-Kariwa Nuclear Power Station,
which Sustained Damages by the 2007 Niigata-Chuetsu-Oki Earthquake," issued on July
16, 2007 (NISA No. 2, 19-07-16)
*2 National council
Joint Working Group on Earthquake, Tsunami, Geology, and Ground Foundation under the
Seismic and Structural Design Subcommittee, Nuclear and Industrial Safety Subcommittee,
Advisory Committee for Natural Resources and Energy
*3 Notification on the issues to be incorporated into the seismic safety evaluation
"[TEPCO] should define the design-basis seismic motion Ss, based on seismic motion
that considers source characteristics and subsurface structural characteristics and
should refer to the exceedance probability of the design-basis seismic motion that
has been defined considering uncertainties."
An excerpt from "Issues to Be Incorporated into the Seismic Safety Evaluation of
Nuclear Power Stations in Light of the Niigata-Chuetsu-Oki Earthquake," issued on
September 4, 2008 (NISA No. 10, 20-08-29)
*4 Draft view of NSC
"[TEPCO] should define, in addition to the design-basis seismic motion, the confirmation
seismic motion using a fault model based on the F-B fault and confirm the validity of
the design-basis seismic motion. For evaluation, the recipe for strong motion prediction
proposed by the Headquarters for Earthquake Research Promotion in 2008 should be used
for setting fault parameters. However, in setting stress drops and the number and location
of asperities, the data obtained during the Niigata-Chuetsu-Oki Earthquake should be
used as much as possible."
An excerpt from the "Draft View on the Review by the Nuclear and Industrial Safety
Agency on the Formulation of the Design-Basis Seismic Motion for the Kashiwazaki-Kariwa
Nuclear Power Station," issued by the Investigatory Advisory Board on Assessment of
Seismic Safety on September 25, 2008
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