Dam, Construction, Red Tide, Surface Area, Bay, Estuary
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Biogeography and Evolution of the Carassius Auratus-Complex in East
Takada et al. BMC Evolutionary Biology 2010, 10:7 http://www.biomedcentral.com/1471-2148/10/7 RESEARCH ARTICLE Open Access Biogeography and evolution of the Carassius auratus-complex in East Asia Mikumi Takada1,2*, Katsunori Tachihara1, Takeshi Kon2, Gunji Yamamoto2, Kei’ichiro Iguchi3, Masaki Miya4, Mutsumi Nishida2 Abstract Background: Carassius auratus is a primary freshwater fish with bisexual diploid and unisexual gynogenetic triploid lineages. It is distributed widely in Eurasia and is especially common in East Asia. Although several genetic studies have been conducted on C. auratus, they have not provided clear phylogenetic and evolutionary descriptions of this fish, probably due to selection bias in sampling sites and the DNA regions analysed. As the first step in clarifying the evolutionary entity of the world’s Carassius fishes, we attempted to clarify the phylogeny of C. auratus populations distributed in East Asia. Results: We conducted a detailed analysis of a large dataset of mitochondrial gene sequences [CR, 323 bp, 672 sequences (528 sequenced + 144 downloaded); CR + ND4 + ND5 + cyt b, 4669 bp in total, 53 sequences] obtained from C. auratus in East Asia. Our phylogeographic analysis revealed two superlineages, one distributed mainly among the Japanese main islands and the other in various regions in and around the Eurasian continent, including the Ryukyus and Taiwan. The two superlineages include seven lineages with high regional specificity that are composed of endemic populations indigenous to each region. The divergence time of the seven lineages was estimated to be 0.2 million years ago (Mya) by a fossil-based method and 1.0-1.9 Mya by the molecular clock method. -
Muko City, Kyoto
Muko city, Kyoto 1 Section 1 Nature and(Geographical Environment and Weather) 1. Geographical Environment Muko city is located at the southwest part of the Kyoto Basin. Traveling the Yodo River upward from the Osaka Bay through the narrow area between Mt. Tenno, the famous warfield of Battle of Yamazaki that determined the future of this country, and Mt. Otoko, the home of Iwashimizu Hachimangu Shrine, one of the three major hachimangu shrines in Japan, the city sits where three rivers of the Katsura, the Uji and the Kizu merge and form the Yodo River. On west, Kyoto Nishiyama Mountain Range including Mt. Oshio lays and the Katsura River runs on our east. We share three boundaries with Kyoto city - the northern and western boundaries with Nishikyo-ku, and the eastern boundary with Minami-ku and Fushimi-ku. Across the southern boundary is Nagaokakyo city abutting Oyamazaki-cho which is the neighbor of Osaka Prefecture. The city is approximiately 2km from east to west and approximiately 4km from south to north covering the 7.72km2 area. This makes us the third smallest city in Japan after Warabi city and Komae city. Figure 1-1-1 Location of Muko city (Right figure (Kyoto map) : The place of red is Muko city) (Lower figure (Japan map) : The place of red is Kyoto) N W E S 1 Geographically, it is a flatland with the northwestern part higher and the southwestern part lower. This divides the city coverage into three distinctive parts of the hilly area in the west formed by the Osaka Geo Group which is believed to be cumulated several tens of thousands to several million years ago, the terrace in the center, and the alluvial plain in the east formed by the Katsura River and the Obata River. -
List of Previous Grant Projects
Toyota Environmental Activities Grant Program 2019 Recipients Grant Catego Theme Project Description Organization Country ry "Kaeng Krachan Forest Complex: Future Conference of Earth Creation Project Through Local Knowledge Environment from Thailand and Traditional Knowledge" for Sustainable Akita Environmental Innovation Japan International Orangutan Conservation Activity in Forestry Promotion Collaboration with the Government and Indonesia and Cooperation Residents in East Kalimantan, Indonesia Center Environmental Conservation Activity Through the Production Support of Organic Fertilizers from Palm Oil Waste and the Agricultural Kopernik Japan Indonesia Education for Farmers to Receive the Roundtable on Sustainable Palm Oil (RSPO) Certification in Indonesia Biodiversi Nippon Practical Environmental Education Project in ty International Collaboration with Children, Women, and the Cooperation for India Government in a Rural Village in Bodh Gaya, Community India Development Star Anise Peace Project Project -Widespread Adoption of Agroforestry with a Barefoot Doctors Myanmar Overse Focus on Star Anise in the Ethnic Minority Group as Regions in Myanmar- Sustainable Management of the Mangrove Forest in Uto Village, Myanmar, as well as Ramsar Center Share Their Experiences to Nearby Villages Myanmar Japan and Conduct Environmental Awareness Activities for Young Generations Patagonian Programme: Restoring Habitats Aves Argentinas Argentina for Endemic Wildlife Conservation Beautiful Forest Creation Activity at the Preah Pride of Asia: Preah -
Relationship Between Estuarine Shellfish Fauna and Physical Environmental Characteristics for Estuary Conservation in Kyushu, Japan
Current World Environment Vol. 10(3), 715-728 (2015) Relationship Between Estuarine Shellfish Fauna and Physical Environmental Characteristics for Estuary Conservation in Kyushu, Japan REI ITSUKUSHIMA1* and YUKIHIRO SHIMATANI2 1Department of Decision Science for Sustainable Society, Kyushu University, 744, Motooka, Nishi-ku, Fukuoka 819-0395, Japan. 2Department of Urban and Environmental Engineering, Kyushu University, 744, Motooka, Nishi-ku, Fukuoka 819-0395, Japan. http://dx.doi.org/10.12944/CWE.10.3.01 (Received: November 29, 2015; Accepted: December 13, 2015) ABSTRACT The establishment of a conservation strategy or restoration goal for river estuaries requires knowledge of potential biota or possible habitat characteristics. In this study, we investigated the relationship between estuarine fauna and macro scale physical indicators on Kyushu Island, Japan to provide basic information for estuarine conservation. As a result of the classification of shellfish fauna by similarity, the Kyushu region was divided into three groups, namely, 1) southern Kyushu with high wave exposure, long fetch, and low tidal variation; 2) the Ariake and Yatsushiro seas with low wave exposure, short fetch, and high tidal variation; and 3) northern Kyushu with an intermediate fetch and tidal variation. In addition, a number of sites, such as Nakatsu Port, Sone tideland, and the Honmyou River, were classified into geographically different groups. This is because the physical characteristics of these sites were similar to classified groups or shellfish fauna were significantly altered by artificial impacts. As a result of discriminant analysis, the discrimination hit rate of species inhabiting the inner bay or tidal flat was high, whereas that for species using a wide variety of bottom sediment environment was low. -
Volki (Annelida: Clitellata: Propappidae) from Japan
JapaneseJapaneseSociety Society ofSystematicof Systematic Zoology Species Diversity, 2006, 11, 359-365 New Record of Propappus volki (Annelida: Clitellata: Propappidae) from Japan Takaaki Torii ll)Et`I CDnsuttants inc., 1334-5Riemon, Oigawa. Shida, Shizuoka, 421-CL212 .lapan E-mail: [email protected] (Received 1 November 2005; Accepted 11 July 2006) A species of freshwater oligochaete, PrQpoppus volki Michaelsen, 1916, is newly recorded from sand and gravel bottoms of several unpolluted streams in Honshu, Japan. The present material agrees well with the previous de- scriptiens of this species except that the spermathecal ampulla is shorter and the proboscis is more elomgate than those described earlier. This is the first record of the family Propappidae Coates, 1986 (New Japanese name: Ko- himemimizu-ka) and the genus Prql)qppus Miehaelsen, 1905 (New Japanese narne: Ko-himemimizu-zoku) in Japan. It provides evidence that the oligochaete fauna in Japan is more closely related to the Holarctic than to the Sino-Indian zoogeographical region, PrQpqppus votici can be regarded as a good bio-indicator fbr unpolluted water. Key Words: oligochaetes, Clitellata, Propappidae, Propappus volki, new record, Japan. Introduction The genus PrQpqppus was erected by Michaelsen (1905) fbr PrQpappus gtandu- losus Michaelsen, 1905 in the family Enchytraeidae. Afterwards Coates (1986) cre- ated the family Propappidae for the single genus PrQpappus on the basis of a unique combination of setal and genital characteristics distinctly different from those ef the Enchytraeidae. Only three species of Propampus have so far been described from freshwater habitats of the Palaearctic region, Among them, Prqpqppus glandulosus has been recorded from Lake Baikal and the Angara and Yenisey Rivers in central Russia (Michaelsen 1905; Coates 1986), PrQpqppus arhynchotus Sokolskaja, 1972 has been recorded only from the Kamchatka Peninsula and Amur basin in the Russian Far East (Timm 1994, 1999a). -
Geomorphological Evolution and Sediment Budget Analysis with the Uji River, Kyoto
D-7 Fourth International Conference on Scour and Erosion 2008 GEOMORPHOLOGICAL EVOLUTION AND SEDIMENT BUDGET ANALYSIS WITH THE UJI RIVER, KYOTO Ryoukei AZUMA1 and Hideo SEKIGUCHI2 1Member of ISSMGE, Assistant Professor, Disaster Prevention Research Institute, Kyoto University (Shimomisu, Yoko-oji, Fushimi-ku, Kyoto 612-8235, Japan) E-mail:[email protected] 2 Member of ISSMGE, Professor, Disaster Prevention Research Institute, Kyoto University (Shimomisu, Yoko-oji, Fushimi-ku, Kyoto 612-8235, Japan) E-mail:[email protected] This paper starts with presenting field evidences that illustrate the occurrence of significant bank erosion in a reach of the Uji River. It then demonstrates that the resulting escarpment was not a mere local adjustment, but is an indicator as to how extensively the Uji River has undergone appreciable amounts of channel erosion over the entire 15.2km-long section. The datasets on which the discussion is based include: the cross-channel topographical data (200m intervals along the river course) in 1967, 1979 and 2006 made available from the Yodogawa Office, MLIT. A careful geomorphological analysis of the datasets in terms of GIS, permitted the determination of tempo-spatial changes of areal sediment storage in the Uji River. When integrated over the entire river course, the overall volume of sediment loss due to erosion proved to amount to 3.1 ×106 m3 in the period from 1967 up to 2006. A discussion is made to identifying its practical implications for future riverine management. Furthermore, a discussion is made of the linkage between the extent of the channel erosion and the depositional environments of the sediment that constitutes the boundary of the river channel. -
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 -
How Is the Gap Between the Concept and Practice of Integrated Sediment Management Bridged?
K-3 Fourth International Conference on Scour and Erosion 2008 HOW IS THE GAP BETWEEN THE CONCEPT AND PRACTICE OF INTEGRATED SEDIMENT MANAGEMENT BRIDGED? Koh-ichi FUJITA Member of JSCE, Research Coordinator for Environmental Affairs, Environment Dept., National Institute for Land and Infrastructure Management (NILIM), Ministry of Land, Infrastructure, Transport and Tourism (MLIT) (Asahi 1, Tsukuba-shi, Ibaraki-ken, 305-0804, Japan) E-mail: [email protected] In Japan, various and intensive modifications to river systems through projects for sediment/flood control, water resources development, electric power supply, river improvement and so on have played extremely important roles in mitigating flood/sediment related disasters and improving our lives and society. At the same time, they have changed river-basin-scale sediment transport systems, bringing new problems with their system soundness in terms of continuity, sustainability and ecological functions. Perceiving that this shows limitations of a locally optimized approach by the area and purpose, which had been taken because of its efficiency, the government has already laid out the concept of “integrated management of a sediment transport system” as a new national policy direction. However, there still appears to be the gap between the concept and its practice, which may retard sweeping development of the new policy. Instead of seeking for “magic technology” that alone can bridge the gap, this overview paper stresses three keys to firmly establishing integrated sediment management: (a) grasping and sharing an overall image of a sediment transport system by using a “common language” that macroscopically describes sediment transport phenomena, not being limited to excessively precise analysis; (b) appropriately performing a diagnosis to identify the structure of problems through a scenario-driven approach, not being preoccupied by stereotyped thoughts; (c) prioritizing the development of component technologies and linking them with policy setting & implementation processes. -
PICES-2012 Program and Abstracts
PICES-2012 Program & Abstracts Image: “The Itsukushima Shrine from the sea”, November 25, 2010, watercolour, by Satoshi Arima, retiree of the National Research Institute of Fisheries and Environment of Inland Sea, Hiroshima, Japan. Permission to reproduce this artwork was kindly granted by Mr. Arima. Prepared and published by: North Pacific Marine Science Organization PICES Secretariat P.O. Box 6000 Sidney, BC PICES-2012 V8L 4B2 Canada Tel: 1-250-363-6366 Fax: 1-250-363-6827 Program and Abstracts E-mail: [email protected] Website: www.pices.int October 12-21, 2012 Hiroshima, Japan PICES-2012 Effects of natural and anthropogenic stressors in the North Pacific ecosystems: Scientific challenges and possible solutions North Pacific Marine Science Organization October 12-21, 2012 Hiroshima, Japan Table of Contents Notes for Guidance � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �vi International Conference Center Floor Plan � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � vii Meeting Timetable � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �viii Map of the International Conference Center Area � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � xii Keynote Lecture � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 1 Schedules and Abstracts S1: Science Board Symposium Effects of natural and anthropogenic stressors in -
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 .................................................................................................................................... -
資料29-4 Ihpトレーニングコース2014概要,2013
International Hydrological Programme International Hydrological Programme Forest Hydrology Conservation of Forest, Soil, and Water Resource The Twenty-fourth IHP Training Course 24 November - 7 December, 2014 Nagoya, Japan Hydrospheric Atmospheric Research Center, Nagoya University Supported by Water Resources Research Center, Disaster Prevention Research Institute, Kyoto University Outline A short training course “Forest Hydrology Conservation of Forest, Soil, and Water Resource” will be programmed for participants from Asia-Pacific regions as a part of Japanese contribution to the International Hydrological Program (IHP). The course is composed of a series of lectures and practice sessions. Objectives Incident rainwater is firstly intercepted by foliage and branches and evaporates from their surface to the atmosphere. From the surface full of rainwater, the rainwater conducts to soils along the plant body, and also, some of incident rainwater directly reaches the soils without touching foliage and branches. These rainwaters coming to the soils infiltrate into the soils with being influenced by the soil pore structure, and reaching to groundwater table. During the slow soil water movement, some of the soil water is absorbed by plant roots. It conducts through stem conduits, reaches leaves, and evaporates to the atmosphere through stomata. The ground water flows to a river. This is an outline of water cycling in the forest ecosystems, and science on this water cycling is “Forest Hydrology”. As one can see above, Forest Hydrology has two major scientific aspects, i.e., discharge from forested watershed and water use by trees (evaporation from the forest canopy). Soils in the forested watershed have a high hydraulic conductivity at the ground surface, which prevents from soil erosion, and functions to make soil water flow slow, resulting in a behavior like a dam. -
Japan: Tokai Heavy Rain (September 2000)
WORLD METEOROLOGICAL ORGANIZATION THE ASSOCIATED PROGRAMME ON FLOOD MANAGEMENT INTEGRATED FLOOD MANAGEMENT CASE STUDY1 JAPAN: TOKAI HEAVY RAIN (SEPTEMBER 2000) January 2004 Edited by TECHNICAL SUPPORT UNIT Note: Opinions expressed in the case study are those of author(s) and do not necessarily reflect those of the WMO/GWP Associated Programme on Flood Management (APFM). Designations employed and presentations of material in the case study do not imply the expression of any opinion whatever on the part of the Technical Support Unit (TSU), APFM concerning the legal status of any country, territory, city or area of its authorities, or concerning the delimitation of its frontiers or boundaries. WMO/GWP Associated Programme on Flood Management JAPAN: TOKAI HEAVY RAIN (SEPTEMBER 2000) Ministry of Land, Infrastructure and Transport, Japan 1. Place 1.1 Location Positions in the flood inundation area caused by the Tokai heavy rain: Nagoya City, Aichi Prefecture is located at 35° – 35° 15’ north latitude, 136° 45’ - 137° east longitude. The studied area is Shonai and Shin river basin- hereinafter referred to as the Shonai river system. It locates about the center of Japan including Nagoya city area, 5th largest city in Japan with the population about 3millions. Therefore, two rivers flow through densely populated area and into the Pacific Ocean and are typical city-type rivers in Japan. Shin Riv. Border of basin Shonai Riv. Flooding area Point of breach ●Peak flow rate in major points on Sept. 12 (app. m3/s) ← Nagoya City, ← ← ino ino Aichi Prefecture j Ku ← 1,100 Shin Riv. ← 720 ← → ← ima Detention j Basin Shinkawa Araizeki Shidami Biwa (Fixed dam) Shin Riv.