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Integrated Water Resources Management of Maetang Sub
lobal f G Ec o o Sucharidtham et al., J Glob Econ 2015, 3:3 l n a o n m DOI: 10.4172/2375-4389.1000150 r u i c o s J $ Journal of Global Economics ISSN: 2375-4389 Research Article OpenOpen Access Access Integrated Water Resources Management of Maetang Sub Watershed, Chiang Mai Province Thunyawadee Sucharidtham1*, Thanes Sriwichailamphan2 and Wichulada Matanboon3 1Department of Applied Economics, National Chung Hsing University, Taiwan 2School of Economics, Chiang Mai University, Thailand 3Social Research Institute, Chiang Mai University, Thailand Abstract Thailand has been managing water in order to solve the water problem in the country for a long time. In 2011, however, Thailand suffered a severe flood, and that means the country’s water management was not successful. Maetaeng watershed is another area that has been receiving a lot of funding to develop and solve the problem of water resources in the area continuously. Still, it was also found that the projects and budgets spent still cannot fix the problems of water resources in the area. This study aims to analyze the events, problems, and factors that can lead to the process development of integrated water resources management in Mae Taeng watershed area, Chiang Mai province. This qualitative study workshop was conducted by collecting basic information, setting a discussion panel for water users, and a workshop to brainstorm for the ideas of water management. The findings showed important factors positively affect the strength of the community, cooperation in water management of the community, and the sacrifices of strong community leaders. The negative impacts include the deforestation of certain ethnic groups, cultural diversity, a lack of awareness in the role of community leaders, as well as insufficient funding. -
Chiang Mai Lampang Lamphun Mae Hong Son Contents Chiang Mai 8 Lampang 26 Lamphun 34 Mae Hong Son 40
Chiang Mai Lampang Lamphun Mae Hong Son Contents Chiang Mai 8 Lampang 26 Lamphun 34 Mae Hong Son 40 View Point in Mae Hong Son Located some 00 km. from Bangkok, Chiang Mai is the principal city of northern Thailand and capital of the province of the same name. Popularly known as “The Rose of the North” and with an en- chanting location on the banks of the Ping River, the city and its surroundings are blessed with stunning natural beauty and a uniquely indigenous cultural identity. Founded in 12 by King Mengrai as the capital of the Lanna Kingdom, Chiang Mai has had a long and mostly independent history, which has to a large extent preserved a most distinctive culture. This is witnessed both in the daily lives of the people, who maintain their own dialect, customs and cuisine, and in a host of ancient temples, fascinating for their northern Thai architectural Styles and rich decorative details. Chiang Mai also continues its renowned tradition as a handicraft centre, producing items in silk, wood, silver, ceramics and more, which make the city the country’s top shopping destination for arts and crafts. Beyond the city, Chiang Mai province spreads over an area of 20,000 sq. km. offering some of the most picturesque scenery in the whole Kingdom. The fertile Ping River Valley, a patchwork of paddy fields, is surrounded by rolling hills and the province as a whole is one of forested mountains (including Thailand’s highest peak, Doi Inthanon), jungles and rivers. Here is the ideal terrain for adventure travel by trekking on elephant back, river rafting or four-wheel drive safaris in a natural wonderland. -
Planning and Managing Water Resources Development in Thailand Page 1 of 8
Water Budgets and Water Regions: Planning and Managing Water Resources Development in Thailand Page 1 of 8 Published in TDRI Quarterly Review Vol. 9 No. 4 December 1994, pp. 14-23 Editor: Linda M. Pfotenhauer Water Budgets and Water Regions: Planning and Managing Water Resources Development in Thailand Donald Alford* addresses some long-held notions about water supply and water use, gives hydrological analyses of the Chao Phraya river system, and provides recommendations for improved water planning and management in Thailand "It is important to distinguish between what 'everybody knows' and what is empirically established. 'Everybody knows' that ... population pressure has been increasing rapidly; that people need fuel and animals need fodder; that too many trees have been felled and that, as a result, runoff rates have accelerated, silt loads have increased, downstream canals and rivers have been clogged, flooding has had greater destructive effect, and the topsoil of the mountains has been washed into the seas...... In a few places, no doubt, all of this is true. Yet much of what 'everybody knows' is not scientifically documented, and some of it is probably not true" (Cool, 1983). Water, together with soil, is a life support resource. As long as both are protected and conserved, a country retains options for future development. When either, or both, are degraded by misuse, a country loses these options. Water enters into all aspects of human life—social, cultural, economic, legal, and technical, and is thus perceived by various segments of society in very different ways, depending upon the primary interest of the various user groups. -
Floodplain Sediment from a 30-Year-Recurrence Flood in 2005 of the Ping River in Northern Thailand S
Floodplain sediment from a 30-year-recurrence flood in 2005 of the Ping River in northern Thailand S. H. Wood, A. D. Ziegler To cite this version: S. H. Wood, A. D. Ziegler. Floodplain sediment from a 30-year-recurrence flood in 2005 of the Ping River in northern Thailand. Hydrology and Earth System Sciences Discussions, European Geosciences Union, 2007, 4 (5), pp.3839-3868. hal-00298904 HAL Id: hal-00298904 https://hal.archives-ouvertes.fr/hal-00298904 Submitted on 18 Oct 2007 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Hydrol. Earth Syst. Sci. Discuss., 4, 3839–3868, 2007 Hydrology and www.hydrol-earth-syst-sci-discuss.net/4/3839/2007/ Earth System HESSD © Author(s) 2007. This work is licensed Sciences 4, 3839–3868, 2007 under a Creative Commons License. Discussions Papers published in Hydrology and Earth System Sciences Discussions are under Floodplain sediment, open-access review for the journal Hydrology and Earth System Sciences 30-year flood, Ping River, Thailand S. H. Wood and A. D. Ziegler Floodplain sediment from a Title Page 30-year-recurrence flood in 2005 of the Abstract Introduction Ping River in northern Thailand Conclusions References Tables Figures S. -
Small Hydropower Development and Legal Limitations in Thailand
Small Hydropower Development and Legal Limitations in Thailand Thanaporn Supriyasilp 1,*, Kobkiat Pongput 2, Challenge Robkob3 1 Department of Civil Engineering, Faculty of Engineering, Chiang Mai University. Thailand. 50200. Science and Technology Research Institute, Chiang Mai University. Thailand. 50200. 2 Water Resources Engineering Department of Kasetsart University, Bangkhen, Bangkok, Thailand. 10900. 3 Biodiversity-based Economy Development Office (Public Organization), Laksi, Bangkok, Thailand. 10210. * Corresponding author. Tel: +66 53942461, Fax: +66 53942478, E-mail: [email protected], [email protected] Abstract: The northern region of Thailand which consists of the Ping, Wang, Yom, and Nan river basins has potential for small hydropower development. The Ping and Wang River Basins are used as case studies. Apart from technical aspects such as electricity generation, engineering and economic aspects, the socio-economics, environment, law and regulation, and stakeholder involvement aspects are also taking into consideration. There are 64 potential projects in the Ping River Basin. The overall electricity potential is about 211 MW with annual power generation of about 720 GWh. For the Wang River Basin, there are 19 potential projects with about 6 MW and an annual power generation of about 30 GWh. However, most of these potential projects are located in forested areas with legal limitations. The various types of forests can result in different levels of legal obstacles. Therefore, the procedure required for permission is varied and is dependent on both the desired development and the forest in question. The laws and regulations related to project development in forested areas are reviewed and are summarized on a case by case basis in a way that is easily understood and accessible for others to use as a reference for other areas. -
Did the Construction of the Bhumibol Dam Cause a Dramatic Reduction in Sediment Supply to the Chao Phraya River?
water Article Did the Construction of the Bhumibol Dam Cause a Dramatic Reduction in Sediment Supply to the Chao Phraya River? Matharit Namsai 1,2, Warit Charoenlerkthawin 1,3, Supakorn Sirapojanakul 4, William C. Burnett 5 and Butsawan Bidorn 1,3,* 1 Department of Water Resources Engineering, Chulalongkorn University, Bangkok 10330, Thailand; [email protected] (M.N.); [email protected] (W.C.) 2 The Royal Irrigation Department, Bangkok 10300, Thailand 3 WISE Research Unit, Chulalongkorn University, Bangkok 10330, Thailand 4 Department of Civil Engineering, Rajamangala University of Technology Thanyaburi, Pathumthani 12110, Thailand; [email protected] 5 Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA; [email protected] * Correspondence: [email protected]; Tel.: +66-2218-6455 Abstract: The Bhumibol Dam on Ping River, Thailand, was constructed in 1964 to provide water for irrigation, hydroelectric power generation, flood mitigation, fisheries, and saltwater intrusion control to the Great Chao Phraya River basin. Many studies, carried out near the basin outlet, have suggested that the dam impounds significant sediment, resulting in shoreline retreat of the Chao Phraya Delta. In this study, the impact of damming on the sediment regime is analyzed through the sediment variation along the Ping River. The results show that the Ping River drains a mountainous Citation: Namsai, M.; region, with sediment mainly transported in suspension in the upper and middle reaches. By contrast, Charoenlerkthawin, W.; sediment is mostly transported as bedload in the lower basin. Variation of long-term total sediment Sirapojanakul, S.; Burnett, W.C.; flux data suggests that, while the Bhumibol Dam does effectively trap sediment, there was only a Bidorn, B. -
Flood Effects on Water Quality and Benthic Fauna Diversity in the Upper Chao Phraya River and the Lower Ping and Nan Rivers, Thailand
eJBio Electronic Journal of Biology, 2014, Vol. 10(4):113-117 Flood Effects on Water Quality and Benthic Fauna Diversity in the Upper Chao Phraya River and the Lower Ping and Nan Rivers, Thailand Tinnapan Netpae* Faculty of Science and Technology, Nakhon Sawan Rajabhat University, Thailand. * Corresponding author. Tel: +66 (0)5621 9100; Fax: +66 (0)5622 1237; E-mail: [email protected] this research will provide information on the water Abstract qualities and the diversity of benthic fauna in the upper Chao Phraya River, the lower Ping and Nan The final quarter of the year 2011, wide space Rivers. The results of this research will also be flooding in Thailand was heavily affected to compared with other research done before the to ecosystem in rivers. This research aims to compare determine any characteristic changes of water water quality and benthic fauna diversity of the quality and the diversity of benthic fauna. upper Chao Phraya River and the lower Ping and Nan Rivers in Nakhon Sawan Province between 2. Methods before and after the flood. The parameters including water temperature, turbidity, pH, conductivity, DO, Study Area - 3- BOD5, NO3 -N, NH3-N, PO4 , coliform bacteria and fecal coliform bacteria were measured. In the Nakhon Sawan Province is the place where Ping aftermath of flood situation, the results indicate that and Nan Rivers combine together to form Chao water quality of rivers after the flood is lower than Phraya River. In 2011, more than 5,300 cubic before the flood but both of them not lower than the meters of flood water per second flow into the Chao surface water quality standard. -
Development of Flood Routing Models for Wang River Basin
DEVELOPMENT OF FLOOD ROUTING MODELS FOR WANG RIVER BASIN Atchara Komsai 1, Winai Liengcharernsit 2, and Tsuyoshi Kinouchi 3 1 Department of Environmental Science and Technology, Tokyo Institute of Technology, Yokohama, Japan, e-mail: [email protected] 2 Department of Environmental Engineering, Kasetsart University, Bangkok, Thailand, e-mail: [email protected] 3 Department of Environmental Science and Technology, Tokyo Institute of Technology, Yokohama, Japan, e-mail: [email protected] Received Date: March 31, 2014 Abstract Nowadays, severe flooding frequently occurs in various parts of Thailand resulted from changes in climatic condition and land use patterns. The flooding has caused great damages to properties and lives and affects country economy. Experience from the most severe flooding in the northern and central regions of Thailand in the year 2011 reveals that reliable flood warning system is still lagging. For flood warning purpose, it is necessary to have an accurate flood routing system. This study is aimed at developing mathematical models for flood routing so as to provide data for flood warning. Two different models are developed, i.e., kinematic overland flow model and kinematic stream flow model. The finite element method with Galerkin’s weighted residual technique is used in model development. The second-order Runge-Kutta method is applied to solve the set of differential equations obtained from finite element formulation. The developed models are applied to simulate flows in the Wang river basin in the northern region of Thailand during July 1 – October 31, 2011 when severe flooding occurred in this region. Model calibration is made by adjusting some parameters in the models and comparing the obtained results with measured data recorded by RID at 5 stream flow gauge stations along the Wang river. -
The Borneo Company Limited Does
Adventurous and entrepreneurial Englishmen known as the Wild Men of Borneo formed The Borneo Company Limited in 1856 (or 2399 according to the Thai solar calendar known as Suriyakati which counts from the year of the Buddha’s birth 543 years before Christ) initially to develop, or some say exploit, the natural resources of Borneo. The world’s third largest island at 290,000 square miles (750,000 square kilometers), Borneo is cradled by the Indonesian archipelago in the Java Sea. Over the company’s hundred plus years of existence, its activities extended to other islands in that archipelago now unified as Indonesia as well as the Malayan Peninsula, China and to the kingdom of Thailand, then known to foreigners as Siam. 137 Pillars House © First published in 2011. Acknowledgements All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior written permission of the 137 Pillars House. Designed & Produced by Shrimp Asia. We are indebted to Professor Julaporn Nantapanit from Chiang Mai University who gave us the inspiration to restore this historical building. Printed in Thailand. We are also thankful for the dedication and passion of the following people: Khun Vipavadee Pattanapongpibul Interior Design, P49 Co. Khun Wanaporn Pornprapa Landscape Design, Plandscape Co. Joseph Polito & Ativa Hospitality Consultants Hotel Architects, Habita Co. Ltd. Mechanical and Electrical Engineering, March Co. Ltd. We would especially like to thank Mr. Jack Chaerdjareewattananan, Mrs. Praneet Bain Chaerdjareewattananan and Cynthia Rosenfeld for their contribution of ideas, concepts and historical facts pertaining to the project and the contents of this book. -
Chao Ph Raya River Basin, Thailan D
WWAP Chapter 16/6 27/1/03 1:37 PM Page 387 Table of contents General Context 390 16 Location 390 Map 16.1: Locator map 390 Map 16.2: Basin map 391 River Basin, Thailand Chao Phraya Major physical characteristics 390 Table 16.1: Hydrological characteristics of the Chao Phraya basin 390 Major socio-economic characteristics 391 Population characteristics 391 Economic activities 391 Table 16.2: Population, per capita income and Gross Provincial Product (GPP) in the sub-basins in 1996 392 Water Resources: Hydrology and Human Impacts 392 Surface water 392 Riverine resources 392 Surface water storage 392 Table 16.3: Annual average runoff in the sub-basins 393 Table 16.4: Characteristics of major reservoirs 393 Barrages 393 Groundwater 393 Aquifer distribution 393 Table 16.5: Groundwater storage and renewable water resources of the sub-basins 394 Recharge, flow and discharge 394 Water quality 394 Surface water quality 394 Groundwater quality 394 Rainfall variation 394 Flooding 394 Human impacts on water resources 394 Data and information on water resources 395 By: The Working Group of the Office of Natural Water Resources Committee (ONWRC) of Thailand* *For further information, contact [email protected] WWAP Chapter 16/6 27/1/03 1:37 PM Page 388 388 / PILOT CASE STUDIES: A FOCUS ON REAL-WORLD EXAMPLES Challenges to Life and Well-Being 395 Water for basic needs 395 Water for food 395 Surface water irrigation systems 395 Groundwater irrigation systems 395 Water and ecosystems 395 Water and industry 395 Water and energy 396 Water for cities 396 -
Xvi Ping River Basin Wang River Basin
XVI 28 M.89 Lam Takhong at Vaccine Serum Office, Nakhon Ratchasima 750 29 M.110 Huai Tunglung at Ban Don Yai, Ubon Ratchathani 751 30 M.127 Huai TaThieo at Ban Na Hai, Ubon Ratchathani 752 31 M.159 Lam Chi at Ban Lum Din, Surin 753 32 M.164 Lam Ta Khong at Mueang, Nakhon Ratchasima 754 33 M.170 Lam Dom Yai at Ban Kham Samran, Ubon Ratchathani 755 34 M.171 Lam Phra Phloeng at Ban Non Sao - E, Nakhon Ratchasima 756 35 M.176 Huai Khayung at Ban Non Si Khlai, Si Sa Ket 757 36 M.183 Huai Hin Lap at Ban Khlong Hin Lap, Nakhon Ratchasima 758 37 M.184 Mun River at Ban Cum, Nakhon Ratchasima 759 38 M.185 Lam Plai Mat at Ban Phai Noi, Nakhon Ratchasima 760 39 M.187 Huai Sanaeng at Mueang, Surin 761 PING RIVER BASIN 40 P.1 Ping River at Nawarat Bridge, Chiang Mai 762 41 P.4A Mae Taeng at Ban Mae Taeng, Chiang Mai 763 42 P.5 Nam Mae Kuang at Tha Nang Bridge, Lamphun 764 43 P.21 Nam Mae Rim at Mae Rim Tai, Chiang Mai 765 44 P.56A Nam Mae Ngat at Ban Sahakorn Romklao, Chiang Mai 766 45 P.67 Ping River at Ban Mae Tae, Chiang Mai 767 46 P.75 Ping River at Ban Cho Lae, Chiang Mai 768 47 P.76 Nam Mae Li at Ban Mae E - Hai, Lamphun 769 48 P.77 Nam Mae Tha at Ban Sop Mae Sapuad, Lamphun 770 49 P.78 Khlong Khlung at Ban Sam Ruean, Kamphaeng Phet 771 50 P.79 Nam Mae Kuang at Ban Mae Wan, Chiang Mai 772 51 P.80 Nam Mae Lai at Ban Pong Din, Chiang Mai 773 52 P.82 Nam Mae Wang at Ban Sop Win, Chiang Mai 774 53 P.84 Nam Mae Wang at Ban Phan Ton, Chiang Mai 775 WANG RIVER BASIN 54 W.1C Wang River at Setuwaree Bridge, Lampang 776 55 W.3A Wang River at Ban Don Chai, Lampang 777 56 W.4A Wang River at Ban Wang Man, Tak 778 57 W.17 Nam Mae Soi at Ban Nong Nao, Lampang 779 58 W.21 Wang River at Ban Tha Dua, Lampang 780 59 W.23 Wang River at Ban Chiang Rai, Tak 781. -
Chiang Rai Phayao Phrae Nan Rong Khun Temple CONTENTS
Chiang Rai Phayao Phrae Nan Rong Khun Temple CONTENTS CHIANG RAI 8 City Attractions 9 Out-of-city Attractions 13 Special Events 22 Interesting Activities 22 Local Products 23 How to Get There 23 PHAYAO 24 City Attractions 25 Out-of-city Attractions 27 Local Products 38 How to Get There 38 PHRAE 40 City Attractions 41 Out-of-city Attractions 42 Special Events 44 Local Products 45 How to Get There 45 NAN 46 City Attractions 47 Out-of-city Attractions 48 Special Event 54 Local Product 55 How to Get There 55 Chiang Rai Chiang Rai Phayao Phrae Nan Republic of the Union of Myanmar Mae Hong Son Chiang Mai Bangkok Lamphun Lampang Mae Hong Son Chiang Mai Lamphun Lampang Doi Pha Tang Chiang Rai Located 785 kilometres north of Bangkok, Chiang Rai is the capital of Thailand’s northern most province. At an average elevation of nearly 600 metres above sea level and covering an area of approximately 11,700 square kilometres, the province borders Myanmar to the north and Lao PDR to the north and northeast. The area is largely mountainous, with peaks rising to 1,500 metres above sea level. Flowing through the hill ranges are several rivers with the most important being the Kok River, near which the city of Chiang Rai is situated. In the far north of the province is the area known as the Golden Triangle, where the Mekong and Ruak Rivers meet to form the Oub Kham Museum borders of Thailand, Myanmar and Lao PDR. Inhabiting the highlands are ethnic hill-tribes centre.