Behavior of Dams Due to the Western Tottori Prefecture Earthquake in 2000

Total Page:16

File Type:pdf, Size:1020Kb

Behavior of Dams Due to the Western Tottori Prefecture Earthquake in 2000 Behavior of Dams due to The Western Tottori Prefecture Earthquake in 2000 By Shuji TAKASU1), Hitoshi YOSHIDA2), Yoshikazu YAMAGUCHI3), Takashi SASAKI4) and Tomoya IWASHITA5) ABSTRACT 2. SPECIFICATIONS OF EARTHQUAKE The Western Tottori Prefecture Earthquake The specifications of the earthquake of October 6, 2000 caused strong earthquake published by the Japan Meteorological motion over a wide area. Immediately after Agency are summarized in Table 1 the earthquake, dam management personnel carried out special safety inspections of dam This earthquake caused strong shaking in facilities in the region. Research engineers of the Chugoku, Kinki, and Shikoku regions in the Public Works Research Institute Japan. It recorded a seismic intensity of 6 performed field investigation of dams near (strong) in Sakaiminato City and Hino Town the epicenter and gathered the earthquake in Tottori Prefecture, 6 (weak) in Saihaku observation data of these dams. The results Town, Aimi Town, Kishimoto Town, Yodoe of the special safety inspections by the dam Town, Mizokuchi Town, and Hiezu Village in site offices and field investigation by the Tottori Prefecture, and 5 (strong) in Yonago PWRI have confirmed that no damage City in Tottori Prefecture, in Yasugi City, harming dam safety occurred. Nita Town, and Shinji Town in Shimane Prefecture, in Niimi City and Tetta Town in KEY WORDS: Western Tottori Prefecture Okayama Prefecture, and in Tonosho Town Earthquake, Dam, Special in Kagawa Prefecture. Safety Inspection, Acceleration Records 1) Leader, Hydraulic Engineering Research Group, 1. INTRODUCTION Independent Administrative Institution Public Works Research Institute (IAI-PWRI), 1-6 Minamihara Tsukuba Immediately after the Western Tottori City, 305-8516, JAPAN 2) Head, Water Management and Dam Division, River Prefecture Earthquake in 2000, dam Department, National Institute for Land and management personnel carried out special Infrastructure Management (NILIM), Ministry of Land, safety inspections of dam facilities in the Infrastructure and Transport, 1 Asahi, Tsukuba City, region shaken strongly. Research Engineers 305-0804, JAPAN 3) Principal Researcher, Hydraulic Engineering Research of the PWRI performed field investigation of Group, IAI-PWRI dams near the epicenter and gathered the 4) Senior Researcher, Hydraulic Engineering Research earthquake observation data of these dams. Group, IAI-PWRI This report summarizes the performance of 5) Senior Researcher, Water Management and Dam Division, River Department, NILIM the dams during the earthquake. 1 3. SPECIAL SAFETY INSPECTIONSINSPECTIONS OF of the guard gate house DAMS AFTER EARTHQUAKEARTHQUAKEE - Sliding of the mountain-side slope of the road on the right bank Immediately after the earthquake, the site - Settlement of pavement around the dam offices of the dams performed special safety management office building inspections within the river reaches administered under the River Act. The 2) Damages to the Sugesawa Dam inspections were conducted at dams which - Cracking of the walls and the floor of the recorded an acceleration of 25 gal or greater guard gate house by seismometers and dams where the - Chipped concrete on the downstream nearest station of the Japan Meteorological surface of the dam body (length of about Agency recorded a seismic intensity of 4 or 1 m and width of about 0.3 m) greater. The special safety inspection - Partial rupture of the foundation work of included a primary inspection that was a the mooring facility visual inspection immediately after the - V-shaped crack on the ground around the earthquake and a secondary inspection that garage on the right bank downstream was a detailed visual inspection accompanied from the dam (length of about 100 m) by analyzing the data measured by - Cracking of the wall of the garage shed instruments. on the right bank downstream from the dam A total of 180 dams were included in the - V-shaped cracking on the left bank slope special safety inspections: 119 dams in the upstream from the dam region of the Chugoku Regional Construction - Cracking of the surface of the wall of the Bureau, 31 dams in the region of the dam management office building on the Shikoku Regional Construction Bureau, and right bank 30 dams in the region of the Kinki Regional Construction Bureau. The special safety 4. FIELD INVESTIGATION inspections by dam site offices did not result in any reports of damage that could threaten (1) Dams the safety of a dam. But the slight damages We, research engineers of the PWRI, were reported from the Kasho Dam managed performed a field investigation of dams near by Tottori Prefecture (a concrete gravity dam the epicenter. The followings are a summary with a height of 46.4 m, completed in 1989) of the results of the investigation. and the Sugesawa Dam managed by the Ministry of Land, Infrastructure and At the Kasho Dam (Photograph 1), the Transport (main dam: a concrete gravity dam earthquake caused peak accelerations at the with a height of 73.5 m, saddle dam: concrete lower inspection gallery of 529 gal face rockfill dam with a height of 17.0 m, (north/south direction), 531 gal (east/west completed in 1968). Figure 1 shows the direction), and 485 gal (vertical direction). At locations of the epicenter and the two dams. the elevator tower at the crest elevation (Photograph 2), the peak accelerations were 1) Damages to the Kasho Dam 2,051 gal (north/south direction), 1,406 gal - Cracking of the walls and the foundation (east/west direction), and 884 gal (vertical 2 direction). The stream direction is 20 degrees has been monitoring the situation and east from north. At this dam, the wall counter-measures will be conducted by the (Photograph 3) and the foundation of the end of this year. guard gate house that was a cantilever structure projecting upstream from the dam The Uh Dam (Photograph 9) is a regulating crest were cracked. But the drainage from reservoir for the Ohmiya Dam that is for the foundation, dam body leakage, and power generation and owned by the Chugoku displacement of the dam body had stabilized Electric Power Co. and located upstream so that there were no problems threatening from the Sugesawa Dam. This dam is a the dam’s safety. The water level in the concrete gravity dam with a height of 14 m reservoir dropped abruptly by 6 cm and a crest length of 34 m. Figure 2 shows its immediately after the earthquake. The standard cross section. It is located about 1 level measurement, conducted at a later time, kilometer from the fault estimated by the revealed that the upper end of the reservoir Geographical Survey Institute, Japan1) subsided about 20 cm as compared with the (hereafter called the “earthquake source dam by the quake. It would be a possible fault”). During the earthquake, its reservoir reason for the dropping of water level of the water level was about 2 m below the full reservoir. water level. The Hino Observation Station of the Digital Strong-Motion Seismograph The repairing works are planned to come Network (KiK-net) 2) owned by the National into force shortly by Tottori Prefecture. Research Institute for Earth Science and Disaster Prevention is located 20 m from the At the Sugesawa Dam (Photograph 4), in the Uh Dam. At this location, seismographs lower inspection gallery of the dam, the peak installed at the surface (S wave velocity of accelerations were 158 gal 210 m/s) and the underground (100 m below (downstream/upstream direction), 126 gal the surface, S-wave velocity of 790 m/s) (right bank/left bank direction), and 109 gal recorded earthquake motion with a peak (vertical direction). On the walls and the accelerations (combination of 3 constituents) floor of the guard gate house that is a of 1,135 gal and 607 gal respectively. cantilever structure projecting upstream Although the dam was subjected to this from the dam crest (Photograph 5), there strong earthquake motion, the only damage were cracks that appeared to be extensions of to the dam was cracking with a width of 1 to the transversal joints of the dam 2 cm on the spillway channel near the foot of (Photograph 6), and concrete on the dam’s the downstream slope (Photographs 10). The downstream surface was partially chipped embankment along the lakeside had slips (Photograph 7), but the no trouble of dam caused small cracks. In addition, because of body was observed. Although the drainage damage to the water supply facilities for from the foundation increased slightly power generation, after the earthquake, the immediately after the earthquake, it later water supply from the Ohmiya Dam to the stabilized. Near the dam and in the natural Uh Dam was shut off and discharged into the ground surrounding the reservoir, ground reservoir of the Sugesawa Dam. deformation caused cracking (Photograph 8). The Chugoku Regional Construction Bureau 3 (2) Small earth dams for irrigation Figure 4 shows the attenuation by distance It was reported that this earthquake from the earthquake source fault of the peak damaged about 40 small earth dams for horizontal acceleration measured at dam irrigation in Tottori Prefecture. Thirty-six of foundations (at the lower inspection gallery these small earth dams were in Saihaku in a concrete dam or at the inspection gallery Town, Hino Town and Mizokuchi Town that beneath an embankment dam). Where, the are close to the epicenter. Main damage of peak horizontal acceleration indicates about half of them was damage to inclined composing the two horizontal components. sluiceways, bottom sluiceways and spillways. The figure also shows the composite of peak horizontal accelerations recorded under the We performed a field investigation of 18 ground at a depth of 100 m at the Hino small earth dams that were assumed to have Observation Station and Hakuta suffered relatively serious damage or were Observation Station of the KiK-net2).
Recommended publications
  • Groundwater Oxygen Isotope Anomaly Before the M6.6 Tottori Earthquake
    www.nature.com/scientificreports OPEN Groundwater oxygen isotope anomaly before the M6.6 Tottori earthquake in Southwest Japan Received: 13 December 2017 Satoki Onda1, Yuji Sano 1, Naoto Takahata 1, Takanori Kagoshima1, Toshihiro Miyajima1, Accepted: 8 March 2018 Tomo Shibata2, Daniele L. Pinti 3, Tefang Lan4, Nak Kyu Kim5, Minoru Kusakabe5 & Published: xx xx xxxx Yoshiro Nishio6 Geochemical monitoring of groundwater in seismically-active regions has been carried out since 1970s. Precursors were well documented, but often criticized for anecdotal or fragmentary signals, and for lacking a clear physico-chemical explanation for these anomalies. Here we report – as potential seismic precursor – oxygen isotopic ratio anomalies of +0.24‰ relative to the local background measured in groundwater, a few months before the Tottori earthquake (M 6.6) in Southwest Japan. Samples were deep groundwater located 5 km west of the epicenter, packed in bottles and distributed as drinking water between September 2015 and July 2017, a time frame which covers the pre- and post-event. Small but substantial increase of 0.07‰ was observed soon after the earthquake. Laboratory crushing experiments of aquifer rock aimed to simulating rock deformation under strain and tensile stresses were carried out. Measured helium degassing from the rock and 18O-shift suggest that the co-seismic oxygen anomalies are directly related to volumetric strain changes. The fndings provide a plausible physico- chemical basis to explain geochemical anomalies in water and may be useful in future earthquake prediction research. Hydro-geochemical precursors of major earthquakes have attracted the attention of researchers worldwide, because they are not entirely unexpected1,2.
    [Show full text]
  • Ffe
    JP9950127 ®n m&?. mti HBA\ /j^¥ m** f «ffe#«i^p^fe«j:y f^± (top-soii) frbzarm (sub-son) '\<Dm$tm*wfeLtz0 i37 ,37 ®mmm(nmij\c£^ffi'Pi-& cs(DfrMim%¥mmmm7^mT\ ££>c cs<z)fe , i3, !^«££1ffiIELfc&JK0*£«fc^«'> tS Cs<Dn<Dffi8¥tmffil*4l~-42Spk%-3tz0 ffi^f.^CTi'N© 137Cs©*»4^iMf^±fc*)1.6~1.7%/^-C&o^o £fc* 1996^K t3, &\fZ Cs<Dft±£*<DTm<D%ttm&*mfeLfcm%\*¥ftX-6:4t1i-it:0 Residence half-time of 137Cs in the top-soils of Japanese paddy and upland fields Misako KOMAMURA, Akito TSUMURA*. Kiyoshi K0DA1RA** National Institute of Agro-Environmental Sciences, *ex-National Institute of Agro-Environmental Sciences, **Prof. Em. Ashikaga Institute of Technology A series of top-soil samples of 14 paddy fields and 10 upland fields in Japan, were annually collected during more than 30 years, to be examined in the contents of ,37Cs. The data, which were obtained by the use of a gamma spectrometric system, received some statistical treatments to distinguish the annual decline of 137Cs contents from deviations. Then the authors calculated "residence half-time of137Cs" within top-soil, and "eluviation rate of 137Cs" from top to the sub-layer of the soil. The following nationwide results were obtained irrespective of paddy or upland fields: (1) The "apparent residence half-time" was estimated as 16—-17 years. This one consists of both effects of eluviation and nuclear disintegration. (2) The "true residence half-time" was reported as 41~~42 years. This one depends on the eluviation speed of 137Cs exclusively, because the influence of nuclear disinte• gration has been compensated.
    [Show full text]
  • China Russia
    1 1 1 1 Acheng 3 Lesozavodsk 3 4 4 0 Didao Jixi 5 0 5 Shuangcheng Shangzhi Link? ou ? ? ? ? Hengshan ? 5 SEA OF 5 4 4 Yushu Wuchang OKHOTSK Dehui Mudanjiang Shulan Dalnegorsk Nongan Hailin Jiutai Jishu CHINA Kavalerovo Jilin Jiaohe Changchun RUSSIA Dunhua Uglekamensk HOKKAIDOO Panshi Huadian Tumen Partizansk Sapporo Hunchun Vladivostok Liaoyuan Chaoyang Longjing Yanji Nahodka Meihekou Helong Hunjiang Najin Badaojiang Tong Hua Hyesan Kanggye Aomori Kimchaek AOMORI ? ? 0 AKITA 0 4 DEMOCRATIC PEOPLE'S 4 REPUBLIC OF KOREA Akita Morioka IWATE SEA O F Pyongyang GULF OF KOREA JAPAN Nampo YAMAJGATAA PAN Yamagata MIYAGI Sendai Haeju Niigata Euijeongbu Chuncheon Bucheon Seoul NIIGATA Weonju Incheon Anyang ISIKAWA ChechonREPUBLIC OF HUKUSIMA Suweon KOREA TOTIGI Cheonan Chungju Toyama Cheongju Kanazawa GUNMA IBARAKI TOYAMA PACIFIC OCEAN Nagano Mito Andong Maebashi Daejeon Fukui NAGANO Kunsan Daegu Pohang HUKUI SAITAMA Taegu YAMANASI TOOKYOO YELLOW Ulsan Tottori GIFU Tokyo Matsue Gifu Kofu Chiba SEA TOTTORI Kawasaki KANAGAWA Kwangju Masan KYOOTO Yokohama Pusan SIMANE Nagoya KANAGAWA TIBA ? HYOOGO Kyoto SIGA SIZUOKA ? 5 Suncheon Chinhae 5 3 Otsu AITI 3 OKAYAMA Kobe Nara Shizuoka Yeosu HIROSIMA Okayama Tsu KAGAWA HYOOGO Hiroshima OOSAKA Osaka MIE YAMAGUTI OOSAKA Yamaguchi Takamatsu WAKAYAMA NARA JAPAN Tokushima Wakayama TOKUSIMA Matsuyama National Capital Fukuoka HUKUOKA WAKAYAMA Jeju EHIME Provincial Capital Cheju Oita Kochi SAGA KOOTI City, town EAST CHINA Saga OOITA Major Airport SEA NAGASAKI Kumamoto Roads Nagasaki KUMAMOTO Railroad Lake MIYAZAKI River, lake JAPAN KAGOSIMA Miyazaki International Boundary Provincial Boundary Kagoshima 0 12.5 25 50 75 100 Kilometers Miles 0 10 20 40 60 80 ? ? ? ? 0 5 0 5 3 3 4 4 1 1 1 1 The boundaries and names show n and t he designations us ed on this map do not imply of ficial endors ement or acceptance by the United N at ions.
    [Show full text]
  • Local Dishes Loved by the Nation
    Sapporo 1 Hakodate 2 Japan 5 3 Niigata 6 4 Kanazawa 15 7 Sendai Kyoto 17 16 Kobe 10 9 18 20 31 11 8 ocal dishes Hiroshima 32 21 33 28 26 19 13 Fukuoka 34 25 12 35 23 22 14 40 37 27 24 29 Tokyo loved by 41 38 36 Nagoya 42 44 39 30 Shizuoka Yokohama 43 45 Osaka Nagasaki 46 Kochi the nation Kumamoto ■ Hokkaido ■ Tohoku Kagoshima L ■ Kanto ■ Chubu ■ Kansai 47 ■ Chugoku ■ Shikoku Naha ■ Kyushu ■ Okinawa 1 Hokkaido 17 Ishikawa Prefecture 33 Okayama Prefecture 2 Aomori Prefecture 18 Fukui Prefecture 34 Hiroshima Prefecture 3 Iwate Prefecture 19 Yamanashi Prefecture 35 Yamaguchi Prefecture 4 Miyagi Prefecture 20 Nagano Prefecture 36 Tokushima Prefecture 5 Akita Prefecture 21 Gifu Prefecture 37 Kagawa Prefecture 6 Yamagata Prefecture 22 Shizuoka Prefecture 38 Ehime Prefecture 7 Fukushima Prefecture 23 Aichi Prefecture 39 Kochi Prefecture 8 Ibaraki Prefecture 24 Mie Prefecture 40 Fukuoka Prefecture 9 Tochigi Prefecture 25 Shiga Prefecture 41 Saga Prefecture 10 Gunma Prefecture 26 Kyoto Prefecture 42 Nagasaki Prefecture 11 Saitama Prefecture 27 Osaka Prefecture 43 Kumamoto Prefecture 12 Chiba Prefecture 28 Hyogo Prefecture 44 Oita Prefecture 13 Tokyo 29 Nara Prefecture 45 Miyazaki Prefecture 14 Kanagawa Prefecture 30 Wakayama Prefecture 46 Kagoshima Prefecture 15 Niigata Prefecture 31 Tottori Prefecture 47 Okinawa Prefecture 16 Toyama Prefecture 32 Shimane Prefecture Local dishes loved by the nation Hokkaido Map No.1 Northern delights Iwate Map No.3 Cool noodles Hokkaido Rice bowl with Tohoku Uni-ikura-don sea urchin and Morioka Reimen Chilled noodles
    [Show full text]
  • Chugoku・Shikoku Japan
    in CHUGOKU・SHIKOKU JAPAN A map introducing facilities related to food and agriculture in the Chugoku-Shikoku Tottori Shimane Eat Okayama Hiroshima Yamaguchi Stay Kagawa Tokushima Ehime Kochi Experience Rice cake making Sightseeing Rice -planting 疏水のある風景写真コンテスト2010 Soba making 入選作品 題名「春うらら」 第13回しまねの農村景観フォトコンテスト入賞作品 第19回しまねの農村景観フォトコンテスト入賞作品 Chugoku-shikoku Regional Agricultural Administration Office Oki 26 【Chugoku Region】 7 13 9 8 Tottori sand dunes 5 3 1 Bullet train 14 2 25 4 16 17 11 Tottori Railway 36 15 12 6 Izumo Taisha 41 Matsue Tottori Pref. Shrine 18 Kurayoshi Expressway 37 10 Shimane Pref. 47 24 45 27 31 22 42 43 35 19 55 28 Iwami Silver Mine 48 38 50 44 29 33 34 32 30 Okayama Pref. 39 23 20 54 53 46 40 49 57 Okayama 21 Okayama 52 51 Kurashiki Korakuen 59 Hiroshima Pref. 60 64 79 75 76 80 62 Hiroshima Fukuyama Hagi 61 58 67 56 Atom Bomb Dome Great Seto Bridge 74 Yamaguchi Pref.Yamaguchi Kagawa Pref. 77 63 Miyajima Kintaikyo 68 69 Bridge Tokushima Pref. Shimonoseki 66 65 72 73 Ehime Pref. 70 71 78 Tottori Prefecture No. Facility Item Operating hours Address Phone number・URL Supported (operation period) Access language Tourism farms 1206Yuyama,Fukube-cho,Tottori city Phone :0857-75-2175 Mikaen Pear picking No holiday during 1 English 味果園 (Aug.1- early Nov.) the period. 20 min by taxi from JR Tottori Station on the Sanin http://www.mikaen.jp/ main line 1074-1Hara,Yurihama Town,Tohaku-gun Phone :0858-34-2064 KOBAYASHI FARM Strawberry picking 8:00~ 2 English 小林農園 (early Mar.- late Jun.) Irregular holidays.
    [Show full text]
  • Sakai Port Tourist Information
    Sakai Port Tourist Information http://www.mlit.go.jp/kankocho/cruise/ Sakai's kaisen-don (fresh seafood rice bowl) The Sakai Port is one of the best fishing ports in Japan. Sakai has large volume of fresh bluefin tuna and crab catch in Japan. In addition, there are also various fresh seafood caught more fresh on a daily depending on the season such as shiroika (white squid), aji (horse mackerel), snow crab, Silver Salmon and other seafood. Sakai's kaisen-don (fresh seafood rice bowl) is as good as one would expect for a port town with such fresh seafood. Location/View Access 5 min. via car from port(2km) Parking for Season Year-round tour buses 24 buses The city of fish and Kitaro Sakaiminato Guide for Related links Sightseeing http://www.sakaiminato.net/foreign/ Contact Us [Tottori Prefecture Tourism and Exchange Bureau International Tourism Attraction Division ] TEL:+18-857-26-7421 l E-MAIL:[email protected] l Website:http://www.pref.tottori.lg.jp/kokusaikankou/ Izumo Soba ( Buckwheat Noodles) Izumo soba is made from unhusked buckwheat soba grains which are freshly ground into a powder. The husks are used in the process, making the color darker and the aroma stronger compared to other types of soba found in Japan. Some of the ways you can enjoy it include the "warigo" style which involves three round bowls stacked on each other where you add your toppings individually to each bowl and the "kama-age" style where noodles come served in the water that the noodles were boiled in.
    [Show full text]
  • Simulation of the Transition Metal-Based Cumulative Oxidative
    www.nature.com/scientificreports OPEN Simulation of the transition metal‑based cumulative oxidative potential in East Asia and its emission sources in Japan Mizuo Kajino1,2*, Hiroyuki Hagino3, Yuji Fujitani4, Tazuko Morikawa3, Tetsuo Fukui5, Kazunari Onishi6, Tomoaki Okuda7 & Yasuhito Igarashi8,9 The aerosol oxidative potential (OP) is considered to better represent the acute health hazards of aerosols than the mass concentration of fne particulate matter (PM2.5). The proposed major contributors to OP are water soluble transition metals and organic compounds, but the relative magnitudes of these compounds to the total OP are not yet fully understood. In this study, as the frst step toward the numerical prediction of OP, the cumulative OP (OPtm*) based on the top fve key transition metals, namely, Cu, Mn, Fe, V, and Ni, was defned. The solubilities of metals were assumed constant over time and space based on measurements. Then, the feasibility of its prediction was verifed by comparing OPtm* values based on simulated metals to that based on observed metals in East Asia. PM2.5 typically consists of primary and secondary species, while OPtm* only represents primary species. This disparity caused diferences in the domestic contributions of PM2.5 and OPtm*, especially in large cities in western Japan. The annual mean domestic contributions of PM2.5 were 40%, while those of OPtm* ranged from 50 to 55%. Sector contributions to the OPtm* emissions in Japan were also assessed. The main important sectors were the road brake and iron–steel industry sectors, followed by power plants, road exhaust, and railways. Te aerosol oxidative potential (OP), the potential to generate reactive oxygen species (ROS) in cells that induce airway oxidative stress and infammation, is considered to better represent the health hazards of aerosols than the 1–3 mass concentration of very fne particulate matter (PM 2.5) .
    [Show full text]
  • Daisen-Oki National Park Boasts Diverse Sceneries, Comprising a Mountainous Area Stretching from Mt
    Mountains where the gods reside, and a series of volcanoes and islands that breathe with ancient memories Daisen-Oki National Park boasts diverse sceneries, comprising a mountainous area stretching from Mt. Daisen, the highest Daisen-Oki peak of the Chugoku region, to Mt. Hiruzen and Mt. Kenashi, the Mt. Mitoku area, the coastal portion of the Shimane 15 Peninsula, the Mt. Sanbe area and the Oki Islands. This Park and its surrounding areas include places of mountain worship National Park and stages of a number of Japanese myths such as the Kunibiki Shinwa (“land-pulling myth”), and retain culture and livelihood deeply connected to nature. In the Park’s mountainous region, volcanic topography, forests and grasslands are part of a varied landscape where each area possesses distinct scenery. Amidst this majesty, Mt. Daisen is revered as Japan’s oldest kami-yama —mountain of gods—while Mt. Mitoku is said to be sacred ground for mountain asceticism. On the Shimane Peninsula along with Izumo Grand Shrine, one of the most important shrines in Japan, you will find scenic and historic locations associated with myths in every direction. At Miho Shrine, situated on the eastern tip of the Shimane Peninsula, Shinto rituals associated with two ancient accounts of Japanese history, the Kojiki and the Nihon- Shoki, are passed down as regional events, while the main hall of Izumo Grand Shrine, constructed in the oldest style of Shinto shrine architecture, is a designated National Treasure. The Oki Islands are celebrated for their spectacular islands and coastal scenery. In acknowledgement of the geohistory that dynamic forces created them, their isolated and unique ecosystem, and the lifestyle and traditions that this environment nurtured, the Islands have been designated as a UNESCO Global Geopark.
    [Show full text]
  • Overview of Local Implementation Support
    Overview of Local Implementation Support In the SIP "Infrastructure maintenance, renovation, and management technologies", an initiative to support implementation of these new technologies in local governments is being promoted through locally-based universities, etc. (Local Implementation Support Team). ■Support Activities ●Verification test for introduction of new technology for solving the problems of local governments, initiatives to provide technical advice, etc. Verification of application of advanced magnetic non-destructive testing Gifu University (Professor Rokugo) Verification of the use of robotic Verification of the performance on site of a bridge inspection robotic device for evaluation of degradation of the bottom of columns for signage technology on site (Gifu University, Kakamigahara City) camera (Nagasaki Prefecture, Saikai City) (Osaka city, Osaka Prefecture) ●Initiatives to spread information regarding the introduction of new technologies, for training of engineers ●Initiatives to introduce database systems for managing inspection data, etc. Public symposium by Hokkaido University and officials from local governments (Sapporo City, Hokkaido) Nagasaki University (Professor Matsuda) Providing information to members of the media regarding verification activities at Nakato Bridge (Saikai City, Nagasaki Prefecture) Explanation of database systems by Tohoku University for managers in the 35 cities, towns, and villages of Yamagata Prefecture (Yamagata City, Yamagata Prefecture) Technology explanatory meeting for members of
    [Show full text]
  • Justice and Humanity JCG - Keeping the Oceans Safe and Enjoyable for Future Generations! 120°E 130°E 140°E 150°E 160°E 170°E
    Justice and Humanity JCG - Keeping the oceans safe and enjoyable for future generations! 120°E 130°E 140°E 150°E 160°E 170°E Territorial sea 165° East Approx. 430,000 km2 (Including inland waters) 5 0 °N Territorial sea + EEZ Approx. 4,470,000 km2 (Japan’s Land area x 12) Etorofu Island Land area Japan Sea 2 Approx. 380,000 km 4 0 °N Takeshima Pacific Ocean Exclusive Economic Zone (EEZ) 2 East China Sea Approx. 4,050,000 km 3 0 °N Senkaku Islands Ogasawara Islands Io To Island Yonagunijima Island Minami-Tori Shima Island 2 0 °N Oki-no-Tori Shima Island 17° North Extended continental shelves* Japan's search responsibility area Approx. 180,000 km2 under the U.S.-Japan SAR Agreement * Areas of the sea as defined in Article 2 (2) of the Exclusive Economic Zone and Continental Shelf Act. For illustration purposes, this map also shows geographical intermediate lines in waters in which borders with neighboring countries have yet to be demarcated. Despite ranking only 61st in the world in terms of land area (380,000 km2), Japan’s territorial waters and exclusive economic zone combined are 12 times larger (4,470,000 km2) than its land area. In December 1986, the Agreement between the Government of the United States of America and the Government of Japan on Maritime Search and Rescue (U.S.-Japan SAR Agreement) was concluded, under which Japan is responsible for coordinating search and rescue activities in the vast expanse of ocean that extends northward from 17° North and westward from 165° East.
    [Show full text]
  • Distributions of a Halophilous and a Riparian Species of Harvestmen Along Sendai River, Tottori City, with the First Records of Harvestmen in Tottori Sand Dunes
    Acta Arachnologica, 69 (2): 95–103, December 20, 2020 Distributions of a halophilous and a riparian species of harvestmen along Sendai River, Tottori City, with the first records of harvestmen in Tottori Sand Dunes Nobuo Tsurusaki1, 2*, Minako Kawaguchi2,3, Yamato Funakura2,4, Toru Matsumoto2,5 & Yuito Obae6 1 Laboratory of Animal Taxonomy, Faculty of Agriculture, Tottori University, Tottori 680-8551, Japan 2Department of Regional Environment, Faculty of Regional Sciences, Tottori University, Tottori 680-8551, Japan and 6Faculty of Environmental Studies, Tottori University of Environmental Studies, Wakabadai-kita 1-1-1, 689-1111, Japan E-mail: [email protected], *Corresponding author Abstract ― Distributions of a maritime harvestman, Psathyropus tenuipes and a riparian harvestman Paraum- bogrella pumilio were investigated along the Sendai River, Tottori City, Honshu, Japan. Psathyropus tenuipes was found from the mouth of the river to the site 4 km upstream where slight salinity (0.1 PPT) was detected in the river. On the other hand, no specimens were found from the upstream sites where no salinity was detect- ed. This indicates that the species needs at least a slight salinity for its occurrence. Paraumbogrella pumilio was found at five sites from the dry riverbed near the Shobu floodgate to a site on the right bank of Sendai River just upstream of Yachiyo Bridge. Occurrence of this species seems to be related to presence of open ground covered with lower grasses on the banks. Recently, the both species were also found from the right bank of the river mouth of Sendai River that is also a part of Tottori Sand Dunes.
    [Show full text]
  • By Municipality) (As of March 31, 2020)
    The fiber optic broadband service coverage rate in Japan as of March 2020 (by municipality) (As of March 31, 2020) Municipal Coverage rate of fiber optic Prefecture Municipality broadband service code for households (%) 11011 Hokkaido Chuo Ward, Sapporo City 100.00 11029 Hokkaido Kita Ward, Sapporo City 100.00 11037 Hokkaido Higashi Ward, Sapporo City 100.00 11045 Hokkaido Shiraishi Ward, Sapporo City 100.00 11053 Hokkaido Toyohira Ward, Sapporo City 100.00 11061 Hokkaido Minami Ward, Sapporo City 99.94 11070 Hokkaido Nishi Ward, Sapporo City 100.00 11088 Hokkaido Atsubetsu Ward, Sapporo City 100.00 11096 Hokkaido Teine Ward, Sapporo City 100.00 11100 Hokkaido Kiyota Ward, Sapporo City 100.00 12025 Hokkaido Hakodate City 99.62 12033 Hokkaido Otaru City 100.00 12041 Hokkaido Asahikawa City 99.96 12050 Hokkaido Muroran City 100.00 12068 Hokkaido Kushiro City 99.31 12076 Hokkaido Obihiro City 99.47 12084 Hokkaido Kitami City 98.84 12092 Hokkaido Yubari City 90.24 12106 Hokkaido Iwamizawa City 93.24 12114 Hokkaido Abashiri City 97.29 12122 Hokkaido Rumoi City 97.57 12131 Hokkaido Tomakomai City 100.00 12149 Hokkaido Wakkanai City 99.99 12157 Hokkaido Bibai City 97.86 12165 Hokkaido Ashibetsu City 91.41 12173 Hokkaido Ebetsu City 100.00 12181 Hokkaido Akabira City 97.97 12190 Hokkaido Monbetsu City 94.60 12203 Hokkaido Shibetsu City 90.22 12211 Hokkaido Nayoro City 95.76 12220 Hokkaido Mikasa City 97.08 12238 Hokkaido Nemuro City 100.00 12246 Hokkaido Chitose City 99.32 12254 Hokkaido Takikawa City 100.00 12262 Hokkaido Sunagawa City 99.13
    [Show full text]