The Transition of Sabo Works for Disaster Mitigation in Japan
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Preliminary Survey on the Tetori Group in Southern Ishikawa, Japan 石川
石川県立自然史資料館研究報告 第3号 Bulletin of the Ishikawa Museum of Natural History, 3: 49-62 (2013) Preliminary survey on the Tetori Group in southern Ishikawa, Japan Yoshihiro KATSURA 石川県南部に分布する手取層群に対する予備調査 桂嘉志浩 Abstract The Lower Cretaceous Itoshiro and overlying Akaiwa subgroups of the Tetori Group are distributed in the Shiramine Area of Hakusan City, Ishikawa Prefecture, Japan. The Kuwajima Formation, the upper division of the lower subgroup, is considered to have been deposited under lacustrine and associated alluvial environments. It has yielded a reasonable number of vertebrate remains that are small, allochthonous, and mostly disarticulated. The Akaiwa Formation, the lower division of the upper subgroup, is suggested to have been formed by fluvial systems with strong currents and rapid deposition. Except for plant fragments, fossils are uncommon. Vertebrates, including dinosaurs, occur in the Kitadani Formation, the upper division of the upper subgroup, in northeastern Fukui Prefecture, and this formation crops out in the Shiramine Area. Therefore, there is a chance that articulated large vertebrate fossils are preserved in the subgroups exposed in the area. However, the indurated nature of the rocks, precipitous topology, thick vegetation cover, and overall poor exposures represent significant challenges to making such a discovery. Further, based on the taphonomy of the observed vertebrates, finding well-preserved large vertebrates in the area will be difficult and require much time and financial support. Organizing a survey group of trained -
Vol2 Case History English(1-206)
Renewal & Upgrading of Hydropower Plants IEA Hydro Technical Report _______________________________________ Volume 2: Case Histories Report March 2016 IEA Hydropower Agreement: Annex XI AUSTRALIA USA Table of contents㸦Volume 2㸧 ࠙Japanࠚ Jp. 1 : Houri #2 (Miyazaki Prefecture) P 1 㹼 P 5ۑ Jp. 2 : Kikka (Kumamoto Prefecture) P 6 㹼 P 10ۑ Jp. 3 : Hidaka River System (Hokkaido Electric Power Company) P 11 㹼 P 19ۑ Jp. 4 : Kurobe River System (Kansai Electric Power Company) P 20 㹼 P 28ۑ Jp. 5 : Kiso River System (Kansai Electric Power Company) P 29 㹼 P 37ۑ Jp. 6 : Ontake (Kansai Electric Power Company) P 38 㹼 P 46ۑ Jp. 7 : Shin-Kuronagi (Kansai Electric Power Company) P 47 㹼 P 52ۑ Jp. 8 : Okutataragi (Kansai Electric Power Company) P 53 㹼 P 63ۑ Jp. 9 : Okuyoshino / Asahi Dam (Kansai Electric Power Company) P 64 㹼 P 72ۑ Jp.10 : Shin-Takatsuo (Kansai Electric Power Company) P 73 㹼 P 78ۑ Jp.11 : Yamasubaru , Saigo (Kyushu Electric Power Company) P 79 㹼 P 86ۑ Jp.12 : Nishiyoshino #1,#2(Electric Power Development Company) P 87 㹼 P 99ۑ Jp.13 : Shin-Nogawa (Yamagata Prefecture) P100 㹼 P108ۑ Jp.14 : Shiroyama (Kanagawa Prefecture) P109 㹼 P114ۑ Jp.15 : Toyomi (Tohoku Electric Power Company) P115 㹼 P123ۑ Jp.16 : Tsuchimurokawa (Tokyo Electric Power Company) P124㹼 P129ۑ Jp.17 : Nishikinugawa (Tokyo Electric Power Company) P130 㹼 P138ۑ Jp.18 : Minakata (Chubu Electric Power Company) P139 㹼 P145ۑ Jp.19 : Himekawa #2 (Chubu Electric Power Company) P146 㹼 P154ۑ Jp.20 : Oguchi (Hokuriku Electric Power Company) P155 㹼 P164ۑ Jp.21 : Doi (Chugoku Electric Power Company) -
Flood Loss Model Model
GIROJ FloodGIROJ Loss Flood Loss Model Model General Insurance Rating Organization of Japan 2 Overview of Our Flood Loss Model GIROJ flood loss model includes three sub-models. Floods Modelling Estimate the loss using a flood simulation for calculating Riverine flooding*1 flooded areas and flood levels Less frequent (River Flood Engineering Model) and large- scale disasters Estimate the loss using a storm surge flood simulation for Storm surge*2 calculating flooded areas and flood levels (Storm Surge Flood Engineering Model) Estimate the loss using a statistical method for estimating the Ordinarily Other precipitation probability distribution of the number of affected buildings and occurring disasters related events loss ratio (Statistical Flood Model) *1 Floods that occur when water overflows a river bank or a river bank is breached. *2 Floods that occur when water overflows a bank or a bank is breached due to an approaching typhoon or large low-pressure system and a resulting rise in sea level in coastal region. 3 Overview of River Flood Engineering Model 1. Estimate Flooded Areas and Flood Levels Set rainfall data Flood simulation Calculate flooded areas and flood levels 2. Estimate Losses Calculate the loss ratio for each district per town Estimate losses 4 River Flood Engineering Model: Estimate targets Estimate targets are 109 Class A rivers. 【Hokkaido region】 Teshio River, Shokotsu River, Yubetsu River, Tokoro River, 【Hokuriku region】 Abashiri River, Rumoi River, Arakawa River, Agano River, Ishikari River, Shiribetsu River, Shinano -
FY2017 Results of the Radioactive Material Monitoring in the Water Environment
FY2017 Results of the Radioactive Material Monitoring in the Water Environment March 2019 Ministry of the Environment Contents Outline .......................................................................................................................................................... 5 1) Radioactive cesium ................................................................................................................... 6 (2) Radionuclides other than radioactive cesium .......................................................................... 6 Part 1: National Radioactive Material Monitoring Water Environments throughout Japan (FY2017) ....... 10 1 Objective and Details ........................................................................................................................... 10 1.1 Objective .................................................................................................................................. 10 1.2 Details ...................................................................................................................................... 10 (1) Monitoring locations ............................................................................................................... 10 1) Public water areas ................................................................................................................ 10 2) Groundwater ......................................................................................................................... 10 (2) Targets .................................................................................................................................... -
FY2018 Results of the Radioactive Material Monitoring in the Water Environment
FY2018 Results of the Radioactive Material Monitoring in the Water Environment March 2020 Ministry of the Environment Contents Outline .......................................................................................................................................................... 1 Part 1: National Radioactive Material Monitoring in the Water Environment throughout Japan (FY2018) . 6 1 Objective and Details ............................................................................................................................. 6 1.1 Objective .................................................................................................................................... 6 1.2 Details ........................................................................................................................................ 6 2 Survey Methods and Analysis Methods .............................................................................................. 19 2.1 Survey methods ....................................................................................................................... 19 2.2 Analysis methods ..................................................................................................................... 20 3 Results ................................................................................................................................................. 22 3.1 Detection of total β radioactivity and γ-ray emitting radionuclides .......................................... 22 (1) Public water -
A Synopsis of the Parasites from Cyprinid Fishes of the Genus Tribolodon in Japan (1908-2013)
生物圏科学 Biosphere Sci. 52:87-115 (2013) A synopsis of the parasites from cyprinid fishes of the genus Tribolodon in Japan (1908-2013) Kazuya Nagasawa and Hirotaka Katahira Graduate School of Biosphere Science, Hiroshima University Published by The Graduate School of Biosphere Science Hiroshima University Higashi-Hiroshima 739-8528, Japan December 2013 生物圏科学 Biosphere Sci. 52:87-115 (2013) REVIEW A synopsis of the parasites from cyprinid fishes of the genus Tribolodon in Japan (1908-2013) Kazuya Nagasawa1)* and Hirotaka Katahira1,2) 1) Graduate School of Biosphere Science, Hiroshima University, 1-4-4 Kagamiyama, Higashi-Hiroshima, Hiroshima 739-8528, Japan 2) Present address: Graduate School of Environmental Science, Hokkaido University, N10 W5, Sapporo, Hokkaido 060-0810, Japan Abstract Four species of the cyprinid genus Tribolodon occur in Japan: big-scaled redfin T. hakonensis, Sakhalin redfin T. sachalinensis, Pacific redfin T. brandtii, and long-jawed redfin T. nakamuraii. Of these species, T. hakonensis is widely distributed in Japan and is important in commercial and recreational fisheries. Two species, T. hakonensis and T. brandtii, exhibit anadromy. In this paper, information on the protistan and metazoan parasites of the four species of Tribolodon in Japan is compiled based on the literature published for 106 years between 1908 and 2013, and the parasites, including 44 named species and those not identified to species level, are listed by higher taxon as follows: Ciliophora (2 named species), Myxozoa (1), Trematoda (18), Monogenea (0), Cestoda (3), Nematoda (9), Acanthocephala (2), Hirudinida (1), Mollusca (1), Branchiura (0), Copepoda (6 ), and Isopoda (1). For each taxon of parasite, the following information is given: its currently recognized scientific name, previous identification used for the parasite occurring in or on Tribolodon spp.; habitat (freshwater, brackish, or marine); site(s) of infection within or on the host; known geographical distribution in Japan; and the published source of each locality record. -
Impact Analysis of the Decline of Agricultural Land-Use on Flood Risk
Changes in Flood Risk and Perception in Catchments and Cities (HS01 – IUGG2015) Proc. IAHS, 370, 39–44, 2015 proc-iahs.net/370/39/2015/ Open Access doi:10.5194/piahs-370-39-2015 © Author(s) 2015. CC Attribution 3.0 License. Impact analysis of the decline of agricultural land-use on flood risk and material flux in hilly and mountainous watersheds Y. Shimizu1, S. Onodera2, H. Takahashi3, and K. Matsumori3 1JSPS Research Fellow, Western Region Agricultural Research Centre, National Agriculture and Food Research Organization, Fukuyama, Japan 2Graduate School of Integrated Arts and Sciences, Hiroshima University, Higashi-Hiroshima, Japan 3Western Region Agricultural Research Centre, National Agriculture and Food Research Organization, Fukuyama, Japan Correspondence to: Y. Shimizu ([email protected]) Received: 11 March 2015 – Accepted: 11 March 2015 – Published: 11 June 2015 Abstract. Agricultural land-use has been reduced by mainly urbanization and devastation in Japan. The objec- tive of this study is to evaluate the impact of the decline of agricultural land-use on flood risk and material flux in hilly and mountainous watersheds using Soil Water Assessment Tool. The results indicated that increase of flood risk due to abandonment of agricultural land-use. Furthermore, the abandonment of rice paddy field on steep slope areas may have larger impacts on sediment discharges than cultivated field. Therefore, it is suggested that prevention of expansion of abandonment of rice paddy field is an important factor in the decrease of yields of sediment and nutrients. 1 Introduction ing of the most of farmers. Even though the aged farmers have will to continue to cultivate crops, they no longer can do The changes in increasing of magnitude of flood events it on the agricultural land-use with a steep slope such as hilly which have been observed all over the world could be af- and mountainous area. -
Hakusan Tedorigawa, Japan
Applicant UNESCO Global Geopark Hakusan Tedorigawa, Japan Geographical and geological summary 1. Physical and human geography The aUGGp is located on the west coast of Japan, in Ishikawa Prefecture. It covers all of Hakusan City, with a total area of 754.93 km2. It includes Mt. Hakusan (2,702m elevation), and the Tedori River basin flowing from Mt. Hakusan to the Sea of Japan. The plains by the sea have a relatively mild climate, averaging 13-14oC. Annual precipitation is 2,000 to 3,000mm – higher than the Japan average. The mountains have an average temperature about 2oC lower, and annual rainfall exceeds 4,000mm. Mt. Hakusan is the highest peak, and the surrounding area is one of the world’s high snowfall areas. Up to 10m of snowfall can be seen, with surrounding villages receiving about 2.5m on average. Much snow melts in spring, with almost all melted by autumn. The abundance of moving water has brought many blessings to the residents, and shaped the topography. The Tedori River is one of the steepest in the world, with an average gradient of 1/27. This formed many erosive features such as V-shaped valleys and gorges in the upper to mid-river, and transports sediment downstream. Mt. Hakusan’s flora and fauna are considered some of the best in Japan, and are protected through the Mount Hakusan Biosphere Reserve, and the Hakusan National Park, etc. Mt. Hakusan is the western-most alpine area of Japan, and as such is the western most distribution of many alpine species. Furthermore, with the golden eagle at the top of the ecosystem, Mt. -
Assessment of Factors Influencing Groundwater-Level Change
Assessment of factors influencing groundwater-level change using groundwater flow simulation, considering vertical Title infiltration from rice-planted and crop-rotated paddy fields in Japan Iwasaki, Yumi; Nakamura, Kimihito; Horino, Haruhiko; Author(s) Kawashima, Shigeto Citation Hydrogeology Journal (2014), 22(8): 1841-1855 Issue Date 2014-12 URL http://hdl.handle.net/2433/199679 The final publication is available at Springer via Right http://dx.doi.org/10.1007/s10040-014-1171-8.; 許諾条件によ り本文ファイルは2016-01-01に公開. Type Journal Article Textversion author Kyoto University Assessment of factors influencing groundwater-level change using groundwater flow simulation, considering vertical infiltration from rice-planted and crop-rotated paddy fields in Japan Yumi Iwasaki*, Kimihito Nakamura, Haruhiko Horino, Shigeto Kawashima Y. Iwasaki, K. Nakamura, S. Kawashima Graduate School of Agriculture, Kyoto University Kitashirakawa Oiwake-cho, Sakyo-ku, Kyoto 606-8502, Japan e-mail: [email protected] H. Horino Graduate School of Life and Environmental Sciences, Osaka Prefecture University 1-1 Gakuen-cho, Naka-ku, Sakai, Osaka 599-8531, Japan *Corresponding author:[email protected] Tel: +81-75-753-6175 Fax: +81-75-753-6476 1 Abstract Assessing factors, such as land use and pumping strategy, that influence groundwater levels is essential to adequately manage groundwater resources. A transient numerical model for groundwater flow with infiltration was developed for the Tedori River alluvial fan (140 km2), Japan. The main water input into the groundwater body in this area is irrigation water, which is significantly influenced by land use, namely paddy and upland fields. The proposed model consists of two models, a one-dimensional (1-D) unsaturated-zone water flow model (HYDRUS-1D) for estimating groundwater recharge and a 3-D groundwater flow model (MODFLOW). -
New View of the Stratigraphy of the Tetori Group in Central Japan
Memoir of the Fukui Prefectural Dinosaur Museum 14: 25–61 (2015) REVIEW © by the Fukui Prefectural Dinosaur Museum NEW VIEW OF THE STRATIGRAPHY OF THE TETORI GROUP IN CENTRAL JAPAN Shin-ichi SANO Fukui Prefectural Dinosaur Museum Terao, Muroko, Katsuyama, Fukui 911-8601, Japan ABSTRACT The stratigraphy of the Tetori Group (sensu lato) and other Early Cretaceous strata in the Hakusan Region in the Hida Belt, northern Central Japan, is reviewed based on recent advances in ammonoid biostratigraphy, U-Pb age determination of zircons using inductively coupled plasma-mass spectrometry with laser ablation sampling (LA-ICPMS), recognition of marine influence, and climatic change inferred from the occurrences of thermophilic plants and pedogenetic calcareous nodules. Four depositional stages (DS) are recognized: DS1 (Late Bathonian–Middle Oxfordian)̶mainly marine strata characterized by the occurrences of ammonoids; DS2 (Berriasian–Late Hauterivian)̶mainly brackish strata characterized by the occurrences of Myrene (Mesocorbicula) tetoriensis and Tetoria yokoyamai; DS3 (Barremian– Aptian)̶fluvial strata characterized by the occurrence of abundant quartzose gravels and freshwater molluscs, such as Trigonioides, Plicatounio and Nippononaia; DS4 (Albian–Cenomanian)̶volcanic/plutonic rocks which unconformably covered or intruded into the Tetori Group. I here propose new interpretation that 1) the Tetori Group (s.l.) in the Hakusan Region in the Hida Belt is divided into Middle–Late Jurassic Kuzuryu Group (corresponding to DS1) and unconformably overlying Early Cretaceous Tetori Group (sensu stricto) (corresponding to DS2–3); and 2) the Tetori Group (s.l.) in other areas is separated from the Tetori Group (s.s.), and divided into the Late Jurassic strata of the Kuzuryu Group (corresponding to the upper part of the same group in the Hakusan Region) and the Early Cretaceous Jinzu Group in the Jinzu Region in the Hida Belt, and the Late Jurassic–Early Cretaceous Managawa Group in the Hida Gaien Belt. -
The Development of Highly Durable Concrete Using Classified Fine Fly Ash in Hokuriku District Tohru Hashimoto1 and Kazuyuki Torii2
The Development of Highly Durable Concrete Using Classified Fine Fly Ash in Hokuriku District Tohru Hashimoto, Kazuyuki Torii, Journal of Advanced Concrete Technology, volume 11 ( 2013 ), pp. 312-321 Early Age Stress Development, Relaxation, and Cracking in Restrained Low W/B Ultrafine Fly Ash Mortars Akhter B Hossain, Anushka Fonseka, Herb Bullock Journal of Advanced Concrete Technology, volume 6 ( 2008 ), pp. 261-271 Hydration Kinetics of a Low Carbon Cementitious Material Produced by Physico-Chemical Activation of High Calcium Fly Ash Monower Sadique, Hassan Al-Nageim Journal of Advanced Concrete Technology, volume 10 ( 2012 ), pp. 254-263 Experimental Investigation on Reaction Rate and Self-healing Ability in Fly Ash Blended Cement Mixtures Seung Hyun Na , Yukio Hama, Madoka Taniguchi, Takahiro Sagawa Journal of Advanced Concrete Technology, volume 10 ( 2012 ), pp. 240-253 Journal of Advanced Concrete Technology Vol. 11, 312-321, November 2013 / Copyright © 2013 Japan Concrete Institute 312 Scientific paper The Development of Highly Durable Concrete Using Classified Fine Fly Ash in Hokuriku District Tohru Hashimoto1 and Kazuyuki Torii2 Received 7 October 2013, accepted 5 November 2013 doi:10.3151/jact.11.312 Abstract In the Hokuriku district, the effort toward the production of highly durable concrete mixtures using classified fine fly ash has just started as a part of ongoing countermeasures for the chloride attack and the alkali silica reaction (ASR). At a time when ASR deterioration phenomena are still progressing, the use of fly ash cement in concrete should be recommended and assertively be adopted as a regional approach for the mitigation of ASR problem especially in the Hokuriku District. -
OFFICIAL GAZETTE GOVERNMENT Pfilniing Biremf ENGLISH EDITION Ib* ~"F-4* I-N^+B O^Bbwrnmn- No
OFFICIAL GAZETTE GOVERNMENT PfilNIINg BIREMf ENGLISH EDITION iB* ~"f-4* i-n^+B o^BBwrnmn- No. 654 TUESDAY, JUNE 8, 1§48 Price 28.00 yen Att orney- Gener al OFFICE ORDINANCE SUZUKI Yoshio Minister of Finance Attorney-General' s Office Ordinance KITAMURA Tokutaro , No. 29 Name of Debenture Name of Registry Jtine 8, 1948 Tokyo-to Bond (No, Chi) ' Industrial Bank of Ja- The following amendment shall be made to pan,^ Ltd; part of the^ Examination Regulations for Bar -Apprentice (Ministry Gf -Justice Ordinatice No. il of 1936) : Ministry of Finance' Notiffcation No. 174 fc* Attorney-General SUZUKI.Yosfaio June 8, 1948 In Articles-1, 4,.5 and 12, " Minister of Jus- A part of the Notification designating the day tice " shall read il Attorney-General." of submitting the financial statements or trans- In Article 2, "Chief"of Division" shall be ferring the business ,of new account of the dis- deleted. solved financial institutions in accordance with In Paragraph 1 of Article 3, " Vice-Minister the provisions of Paragraph 2 of Article 8, Article ' of Justice" shall read " Secretary-General " and 21 and Paragraph 2 of Article 26 of the Financial Paragraph 2 shall fce deleted. Institutions Reconstruction gnd Reorganization Tn Article 4, " 4 persons"' shall read " 6 per- Law (Ministry of Finance Notification No. 255, sons" anjl *'Ministry of Justice" shall read October, 1947) shall be amended &s follows, and " Attorney-General's Office." it shall be applied as from March 27, 1948: In Article 5, "Court of Appeal" shall foe Minister of Finance deleted. ' KITAMURA Tokutaro Article 6.