14 research outputs found

    āļ›āļĢāļ°āļŠāļšāļāļēāļĢāļ“āđŒāļāļēāļĢāļŠāļĢāđ‰āļēāļ‡āļŠāļ·āđˆāļ­āļāļēāļĢāļŠāļ­āļ™āļŠāļģāļŦāļĢāļąāļšāļ„āļĢāļđāđƒāļ™āļžāļ·āđ‰āļ™āļ—āļĩāđˆāļŦāđˆāļēāļ‡āđ„āļāļĨ: āļāļēāļĢāļ•āļĢāļ§āļˆāļŠāļ­āļšāļ„āļļāļ“āļ āļēāļžāđāļĄāđˆāļ™āđ‰āļģāđāļĨāļ°āļ™āđ‰āļģ āđ‚āļ”āļĒāđƒāļŠāđ‰āđ€āļ—āļ„āđ‚āļ™āđ‚āļĨāļĒāļĩāđ‚āļ—āļĢāļĻāļąāļžāļ—āđŒāđ€āļ„āļĨāļ·āđˆāļ­āļ™āļ—āļĩāđˆ

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    Experiences of Creating Teaching Media for Teachers in Remote Areas: Examining River and Water Quality Utilizing Mobile Technologies Duongdearn Suwanjinda, Pikulkaew Tangtisanon, Richard Procter, Luke Jones, Alireza Abbassi Monjezi, Florence Halstead and Ray KirtleyāļĢāļąāļšāļšāļ—āļ„āļ§āļēāļĄ: 3 āļžāļĪāļĐāļ āļēāļ„āļĄ 2561; āđāļāđ‰āđ„āļ‚āļšāļ—āļ„āļ§āļēāļĄ: 15 āļ•āļļāļĨāļēāļ„āļĄ 2561; āļĒāļ­āļĄāļĢāļąāļšāļ•āļĩāļžāļīāļĄāļžāđŒ: 31 āļ•āļļāļĨāļēāļ„āļĄ 2561 DOI: http://doi.org/10.14456/jstel.2018.25 āļšāļ—āļ„āļąāļ”āļĒāđˆāļ­āļšāļ—āļ„āļ§āļēāļĄāļ™āļĩāđ‰āļāļĨāđˆāļēāļ§āļ–āļķāļ‡āļĢāļēāļĒāļĨāļ°āđ€āļ­āļĩāļĒāļ”āđ€āļāļĩāđˆāļĒāļ§āļāļąāļšāļœāļĨāļĨāļąāļžāļ˜āđŒāļ‚āļ­āļ‡āđ‚āļ„āļĢāļ‡āļāļēāļĢāļ­āļšāļĢāļĄāđ€āļŠāļīāļ‡āļ›āļāļīāļšāļąāļ•āļīāļāļēāļĢāļ—āļĩāđˆāđ„āļ”āđ‰āļĢāļąāļšāļāļēāļĢāļŠāļ™āļąāļšāļŠāļ™āļļāļ™āļŦāļĨāļąāļāļˆāļēāļāļ—āļļāļ™āļ™āļīāļ§āļ•āļąāļ™ (Newton fund) āļšāļĢāļīāļ•āļīāļŠ āđ€āļ„āļēāļ™āļ‹āļīāļĨ āļ­āļąāļ™āđ€āļ›āđ‡āļ™āļ„āļ§āļēāļĄāļĢāđˆāļ§āļĄāļĄāļ·āļ­āļĢāļ°āļŦāļ§āđˆāļēāļ‡ The University of Hull āļ›āļĢāļ°āđ€āļ—āļĻāļ­āļąāļ‡āļāļĪāļĐ āđāļĨāļ°āļĄāļŦāļēāļ§āļīāļ—āļĒāļēāļĨāļąāļĒāļŠāļļāđ‚āļ‚āļ—āļąāļĒāļ˜āļĢāļĢāļĄāļēāļ˜āļīāļĢāļēāļŠ āļ‹āļķāđˆāļ‡āđ€āļ›āļīāļ”āđ‚āļ­āļāļēāļŠāđƒāļŦāđ‰āļ™āļąāļāļ§āļīāļˆāļąāļĒāļĢāļļāđˆāļ™āđƒāļŦāļĄāđˆāļˆāļēāļāļ›āļĢāļ°āđ€āļ—āļĻāļ­āļąāļ‡āļāļĪāļĐāđāļĨāļ°āļ™āļēāļ™āļēāļŠāļēāļ•āļīāđ„āļ”āđ‰āļĄāļĩāļ›āļāļīāļŠāļąāļĄāļžāļąāļ™āļ˜āđŒāļāļąāļ™ āđ€āļĢāļĩāļĒāļ™āļĢāļđāđ‰āļĢāđˆāļ§āļĄāļāļąāļ™āđāļĨāļ°āđāļŠāļ§āļ‡āļŦāļēāđ‚āļ­āļāļēāļŠāđƒāļ™āļāļēāļĢāļŠāļĢāđ‰āļēāļ‡āļ„āļ§āļēāļĄāļĢāđˆāļ§āļĄāļĄāļ·āļ­āđƒāļ™āļāļēāļĢāļ—āļģāļ‡āļēāļ™āļ§āļīāļˆāļąāļĒāļ•āđˆāļ­āđ„āļ› āđ‚āļ”āļĒāļĄāļĩāļ§āļąāļ•āļ–āļļāļ›āļĢāļ°āļŠāļ‡āļ„āđŒāđ€āļ‰āļžāļēāļ°āļ‚āļ­āļ‡āļāļēāļĢāļ­āļšāļĢāļĄāđ€āļŠāļīāļ‡āļ›āļāļīāļšāļąāļ•āļīāļāļēāļĢāđ€āļžāļ·āđˆāļ­āļ•āđ‰āļ­āļ‡āļāļēāļĢāđƒāļŦāđ‰āđƒāļŠāđ‰āđ€āļ—āļ„āđ‚āļ™āđ‚āļĨāļĒāļĩāđ‚āļ—āļĢāļĻāļąāļžāļ—āđŒāđ€āļ„āļĨāļ·āđˆāļ­āļ™āļ—āļĩāđˆāđƒāļ™āļāļēāļĢāļ—āļģāļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āļ āļēāļ„āļŠāļ™āļēāļĄāđƒāļ™āļŦāļąāļ§āļ‚āđ‰āļ­āļ•āđˆāļēāļ‡ āđ† āđ€āļŠāđˆāļ™ āļāļēāļĢāļ­āļ™āļļāļĢāļąāļāļĐāđŒāļ—āļĢāļąāļžāļĒāļēāļāļĢ āļ˜āļĢāļĢāļĄāļŠāļēāļ•āļī āļāļēāļĢāļŠāđˆāļ‡āđ€āļŠāļĢāļīāļĄāļāļēāļĢāļ—āđˆāļ­āļ‡āđ€āļ—āļĩāđˆāļĒāļ§āđƒāļ™āļžāļ·āđ‰āļ™āļ—āļĩāđˆāļ—āļēāļ‡āļ āļēāļ„āđ€āļŦāļ™āļ·āļ­ āđāļĨāļ°āļ™āļģāļœāļĨāļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āļĄāļēāļ›āļĢāļ°āļĒāļļāļāļ•āđŒāđƒāļŠāđ‰āđ€āļžāļ·āđˆāļ­āļŠāļĢāđ‰āļēāļ‡āļŠāļ·āđˆāļ­āļāļēāļĢāđ€āļĢāļĩāļĒāļ™āļāļēāļĢāļŠāļ­āļ™ āļšāļ—āļ„āļ§āļēāļĄāļ™āļĩāđ‰āļžāļīāļˆāļēāļĢāļ“āļēāļ›āļĢāļ°āļŠāļšāļāļēāļĢāļ“āđŒāļ‚āļ­āļ‡āļ™āļąāļāļ§āļīāļˆāļąāļĒāļĢāļļāđˆāļ™āđƒāļŦāļĄāđˆāđƒāļ™āļāļēāļĢāđƒāļŠāđ‰āđ€āļ—āļ„āđ‚āļ™āđ‚āļĨāļĒāļĩāđ‚āļ—āļĢāļĻāļąāļžāļ—āđŒāđ€āļ„āļĨāļ·āđˆāļ­āļ™āļ—āļĩāđˆāđ€āļ‚āđ‰āļēāļĄāļēāļĄāļĩāļŠāđˆāļ§āļ™āļŠāđˆāļ§āļĒāđƒāļ™āļāļēāļĢāļ—āļģāļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āļ āļēāļ„āļŠāļ™āļēāļĄāđāļĨāļ°āļŠāļĢāđ‰āļēāļ‡āļŠāļĢāļĢāļ„āđŒāļŠāļ·āđˆāļ­āļāļēāļĢāļŠāļ­āļ™āđ€āļāļĩāđˆāļĒāļ§āļāļąāļšāļāļēāļĢāļ­āļ™āļļāļĢāļąāļāļĐāđŒāđāļĄāđˆāļ™āđ‰āļģāđāļĄāđˆāļāļ āļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āđ€āļŠāļīāļ‡āļ›āļāļīāļšāļąāļ•āļīāļāļēāļĢāļ™āļĩāđ‰āđ„āļ”āđ‰āđƒāļŠāđ‰āđ€āļ—āļ„āđ‚āļ™āđ‚āļĨāļĒāļĩāđ‚āļ—āļĢāļĻāļąāļžāļ—āđŒāđ€āļ„āļĨāļ·āđˆāļ­āļ™āļ—āļĩāđˆāđƒāļ™āļāļēāļĢāļŠāļĢāđ‰āļēāļ‡āļŠāļ·āđˆāļ­āļ”āļīāļˆāļīāļ•āļąāļĨ āđ„āļ”āđ‰āđāļāđˆ 1) āļāļēāļĢāļŠāļĢāđ‰āļēāļ‡āļŠāļ·āđˆāļ­āļ āļēāļžāđ€āļ„āļĨāļ·āđˆāļ­āļ™āđ„āļŦāļ§ 2) āļāļēāļĢāļŠāļģāļĢāļ§āļˆāļŠāļąāļ•āļ§āđŒāđ„āļĄāđˆāļĄāļĩāļāļĢāļ°āļ”āļđāļāļŠāļąāļ™āļŦāļĨāļąāļ‡āļŦāļ™āđ‰āļēāļ”āļīāļ™ āļ”āļąāļŠāļ™āļĩāļ§āļąāļ”āļ„āļļāļ“āļ āļēāļžāļ™āđ‰āļģ 3) āļāļēāļĢāļ§āļąāļ”āļāļēāļĢāļĢāļ°āļšāļēāļĒāļ™āđ‰āļģ 4) āļāļēāļĢāļŠāļģāļĢāļ§āļˆāļ‚āļ™āļēāļ”āļāđ‰āļ­āļ™āļŦāļīāļ™āļ—āđ‰āļ­āļ‡āļ™āđ‰āļģ āđāļĨāļ° 5) āļāļēāļĢāļŠāļĢāđ‰āļēāļ‡āļ§āļīāļ”āļĩāđ‚āļ­ āļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āļ­āļĒāđˆāļēāļ‡āļ‡āđˆāļēāļĒāđāļĨāļ°āļ‚āļąāđ‰āļ™āļ•āļ­āļ™āļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āļ—āļĩāđˆāļŠāļēāļĄāļēāļĢāļ–āđ€āļ‚āđ‰āļēāļ–āļķāļ‡āđ„āļ”āđ‰āļ–āļđāļāļŠāļĢāđ‰āļēāļ‡āļ‚āļķāđ‰āļ™āđ€āļžāļ·āđˆāļ­āđƒāļŦāđ‰āļ„āļĢāļđāļœāļđāđ‰āļŠāļ­āļ™āđƒāļ™āļžāļ·āđ‰āļ™āļ—āļĩāđˆāļŦāđˆāļēāļ‡āđ„āļāļĨāđ„āļ”āđ‰āļ™āļģāđ„āļ›āđƒāļŠāđ‰ āļœāļĨāļāļēāļĢāļ—āļ”āļĨāļ­āļ‡āđāļĨāļ°āļŠāļ·āđˆāļ­āļāļēāļĢāļŠāļ­āļ™āđ„āļ”āđ‰āļ–āļđāļāđ€āļœāļĒāđāļžāļĢāđˆāļšāļ™āđ€āļ§āđ‡āļšāđ„āļ‹āļ•āđŒāļ‹āļķāđˆāļ‡āļŠāļēāļĄāļēāļĢāļ–āļ™āļģāđ„āļ›āđƒāļŠāđ‰āđ€āļ›āđ‡āļ™āļ•āđ‰āļ™āđāļšāļšāđ€āļžāļ·āđˆāļ­āļ—āļ”āļĨāļ­āļ‡āđƒāļ™āđāļŦāļĨāđˆāļ‡āļ™āđ‰āļģāļ­āļ·āđˆāļ™ āđ† āļ•āđˆāļ­āđ„āļ› āļ„āļģāļŠāļģāļ„āļąāļ: āđ€āļ—āļ„āđ‚āļ™āđ‚āļĨāļĒāļĩāđ‚āļ—āļĢāļĻāļąāļžāļ—āđŒāđ€āļ„āļĨāļ·āđˆāļ­āļ™āļ—āļĩāđˆÂ  āļŠāļ·āđˆāļ­āļāļēāļĢāļŠāļ­āļ™Â  āļžāļ·āđ‰āļ™āļ—āļĩāđˆāļŦāđˆāļēāļ‡āđ„āļāļĨ  āļ„āļļāļ“āļ āļēāļžāļ™āđ‰āļģ  āđāļĄāđˆāļ™āđ‰āļģ   Abstract This article details the outcomes of a workshop offered by the Newton Fund and the British Council. The workshop was coordinated by The University of Hull, UK, and Sukhothai Thammathirat Open University, Thailand. The programme, ‘Researcher Links’ provided an opportunity for early career researchers from the UK and a range of international countries, to interact, learn from each other, and explore opportunities for building long-lasting research collaborations. A specific objective of the workshop was to exploit the affordances of mobile technologies in the field in relation to topics such as natural resources conservation, tourism promotion, and application of the field test results for creating teaching media. This paper will consider the workshop experiences of several early career researchers, including how they utilized mobile technologies to create field tests and accompanying teaching media assets for Maekok river conservation. This field study used mobile technologies to create several digital assets including; 1) animation media creation, 2) benthic macroinvertebrate (biotic index) exploration, 3) watercourse discharge measurement, 4) watercourse bedload measurement, and 5) video creation. Simple experiment tests and accessible instructions were created for teachers in remote area to employ.  The experimental results and teaching media assets were published on a website which could be used as an experimental model for further study in other rivers. Keywords: Mobile technologies, Teaching media, Remote area, Water quality, Rive

    Development of a comprehensive transient model of energy capture and storage in solar ponds for use in thermal regeneration of draw solutes in forward osmosis.

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    Salinity gradient solar ponds can be used to store heat by trapping solar radiation. The heat can then be employed to drive various industrial applications that require low-grade heat. In this study, a comprehensive finite difference transient model has been developed incorporating many processes that affect the performance of a solar pond to predict the hourly temperature distribution. A novel heat extraction method for salinity gradient solar ponds is then proposed. This method can be operated in batch or continuous modes. A comparison between the performance of two solar ponds of the same size (10,000 m2) in Adana (Turkey) and Ahvaz (Iran) is also presented. The heat extraction method entails brine removal from the Non-Convective Zone (NCZ) as well as the HSZ. The presented model incorporates the heat losses from the bottom and surface of the pond as well as the cooling effect imposed as a consequence of the replacement of extracted brine from each layer, and the supply of freshwater to the surface of the pond to maintain its inventory. The model can be employed to predict the performance of solar ponds of various dimensions for any given location. In the final part of this study, utilisation of solar thermal energy from salinity gradient solar ponds in forward osmosis (FO) is investigated. This study will present two novel processes for the regeneration of dimethyl ether (DME) and ammonium bicarbonate as a draw solutes in FO using thermal energy provided from a solar pond. The average daily volume of desalinated water produced using these processes and a solar pond of 10,000 m2 was determined. It is indicated that, a solar pond of such moderate size can drive a forward osmosis plant to provide a total of 5,210 m3 of potable water in the first two years of operation in the location considered in this study (Chabahar) if DME is used as the draw solute. The proposed process can provide freshwater at varying rates throughout the year and benefits from a very low electricity consumption rate of 0.46 kWh per cubic metre of desalinated water presenting a viable option for solar desalination. In case of ammonium bicarbonate, the product water contains small quantities of ammonia ions making it unsuitable for drinking purposes. Given that there are vast uninhabited coastal areas in many countries, particularly in the MENA region where there are high solar radiation rates, this method can contribute towards addressing the growing water scarcity

    Development of a comprehensive transient model of energy capture and storage in solar ponds for use in thermal regeneration of draw solutes in forward osmosis.

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    Salinity gradient solar ponds can be used to store heat by trapping solar radiation. The heat can then be employed to drive various industrial applications that require low-grade heat. In this study, a comprehensive finite difference transient model has been developed incorporating many processes that affect the performance of a solar pond to predict the hourly temperature distribution. A novel heat extraction method for salinity gradient solar ponds is then proposed. This method can be operated in batch or continuous modes. A comparison between the performance of two solar ponds of the same size (10,000 m2) in Adana (Turkey) and Ahvaz (Iran) is also presented. The heat extraction method entails brine removal from the Non-Convective Zone (NCZ) as well as the HSZ. The presented model incorporates the heat losses from the bottom and surface of the pond as well as the cooling effect imposed as a consequence of the replacement of extracted brine from each layer, and the supply of freshwater to the surface of the pond to maintain its inventory. The model can be employed to predict the performance of solar ponds of various dimensions for any given location. In the final part of this study, utilisation of solar thermal energy from salinity gradient solar ponds in forward osmosis (FO) is investigated. This study will present two novel processes for the regeneration of dimethyl ether (DME) and ammonium bicarbonate as a draw solutes in FO using thermal energy provided from a solar pond. The average daily volume of desalinated water produced using these processes and a solar pond of 10,000 m2 was determined. It is indicated that, a solar pond of such moderate size can drive a forward osmosis plant to provide a total of 5,210 m3 of potable water in the first two years of operation in the location considered in this study (Chabahar) if DME is used as the draw solute. The proposed process can provide freshwater at varying rates throughout the year and benefits from a very low electricity consumption rate of 0.46 kWh per cubic metre of desalinated water presenting a viable option for solar desalination. In case of ammonium bicarbonate, the product water contains small quantities of ammonia ions making it unsuitable for drinking purposes. Given that there are vast uninhabited coastal areas in many countries, particularly in the MENA region where there are high solar radiation rates, this method can contribute towards addressing the growing water scarcity

    A comprehensive transient model for the prediction of the temperature distribution in a solar pond under Mediterranean conditions

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    Salinity gradient solar ponds can be used to store heat by trapping solar radiation. The heat can then be employed to drive various industrial applications that require low-grade heat. In this study, a comprehensive finite difference transient model has been developed incorporating many processes that affect the performance of a solar pond to predict the hourly temperature distribution. The model includes novel approaches to simulation of both the Heat Storage Zone (HSZ) and the Upper Convective Zone (UCZ) where in addition to convective, evaporative and radiative heat losses, the cooling effect of adding freshwater to the surface of the pond is taken into account. The HSZ is treated as one layer, with uniform temperature, in the finite difference method. A solar pond of 100 m2 surface area is simulated for southern Turkey. The results indicate that, if the operation starts on the first day of June, the HSZ would take 65 days to reach the boiling point while this would be 82 days if the operation commences on the first day of December. The simulations highlight that 41-47 litres of freshwater will need to be supplied to the UCZ daily and the associated cooling effect of such addition is approximately 10 times larger than the convective heat loss in the first 65 days of operation. In addition, as 22.4% of the incoming radiation in the form of long wavelength radiation, is absorbed within the top 1 cm of the pond, there is a sharp increase in the temperature of the UCZ creating a hot-zone which slowly moves downwards to the Non-Convective Zone (NCZ) and eventually the HSZ. Hence, the HSZ does not initially prevail as the hottest zone in the pond. However, as the temperature rises and the pond approaches pseudo-steady state, the hot-zone slowly moves downwards and finally reaches the HSZ. This phenomenon is consistent with experimental studies and proves the imprecision of pseudo-steady state models. Furthermore, the HSZ becomes more resistant to losing the accumulated heat to the layers above as its temperature increases due to the better establishment of the NCZ as the insulator for the HSZ

    Regeneration of dimethyl ether as a draw solute in forward osmosis by utilising thermal energy from a solar pond

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    Utilisation of solar thermal energy in forward osmosis (FO) can provide an attractive method for seawater desalination. This study presents a novel process for the regeneration of dimethyl ether (DME) as a draw solute in FO using thermal energy from a solar pond. The location considered for this process is Chabahar (Iran) which benefits from a very high solar irradiance and access to an abundance of seawater from the Sea of Oman making it an ideal location for the proposed process. The average daily volume of desalinated water produced using this process coupled to a solar pond of 10,000 m2 was determined. It is indicated that a solar pond of such moderate size can drive a forward osmosis plant to provide 5,210 m3 of freshwater in the first two years of operation in Chabahar. The proposed process provides freshwater at varying rates throughout the year and benefits from a very low electricity consumption rate of 0.46 kWh per cubic metre of desalinated water offering a viable option for solar desalination. Considering that there are vast uninhabited coastal areas particularly in the Middle East and North Africa (MENA) region, the proposed method can contribute towards addressing the growing potable water scarcity

    Regeneration of dimethyl ether as a draw solute in forward osmosis by utilising thermal energy from a solar pond

    Get PDF
    Utilisation of solar thermal energy in forward osmosis (FO) can provide an attractive method for seawater desalination. This study presents a novel process for the regeneration of dimethyl ether (DME) as a draw solute in FO using thermal energy from a solar pond. The location considered for this process is Chabahar (Iran) which benefits from a very high solar irradiance and access to an abundance of seawater from the Sea of Oman making it an ideal location for the proposed process. The average daily volume of desalinated water produced using this process coupled to a solar pond of 10,000 m2 was determined. It is indicated that a solar pond of such moderate size can drive a forward osmosis plant to provide 5,210 m3 of freshwater in the first two years of operation in Chabahar. The proposed process provides freshwater at varying rates throughout the year and benefits from a very low electricity consumption rate of 0.46 kWh per cubic metre of desalinated water offering a viable option for solar desalination. Considering that there are vast uninhabited coastal areas particularly in the Middle East and North Africa (MENA) region, the proposed method can contribute towards addressing the growing potable water scarcity
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