巴厘岛城市Banyu Asri海滩上的波形振荡泵的原型性能

J. Ginting, I. Setiawan
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引用次数: 0

摘要

原水的供应通常是来自几个来源的水,这些水只能从河流、湖泊、水井和泉水中获得。开采可以通过钻井、筑坝和抽水来完成。一个地区原水潜力的管理取决于地理和地质条件。在沿海地区发现的泉水之一受海洋和地质参数的影响,这将进一步影响捕获、管理和利用的方法。这个原水供应的原型于2013年安装在巴厘岛Buleleng Regency Singaraja市Banyu Asri海滩的泉水周围。数据收集方法是通过观察波浪数据、泵送流量和水盐度进行的。这些观察是针对两种类型的振动板进行的,即使用木材和纤维。从这项技术中,可以预期,即使泉水的位置受到经常淹没泉水排放点的海水的强烈影响,也能提供稳定的泉源和保持矿物质含量。Banyu Asri海滩的泉水被社区广泛用于饮用水和仪式崇拜。从安装在泉水位置的原型的性能结果来看,它已经显示出通过管道向陆地排放淡水的能力,尽管在很小的位置发生的波高范围从0.10到0.30厘米,排放流量高达0.03升/秒。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Kinerja Prototipe Papan Osilasi Pada Pompa Flap Tenaga Gelombang Untuk Pemanfaatan Mata Air Di Pantai Banyu Asri, Kota Singaraja - Bali
The supply of raw water is generally water available from several sources, which are available only on a river, lake, water wells and springs. The extraction can be done by drilling, damming water, and pumping. Management of the potential of raw water in an area is determined by geographical and geological conditions. One of the occurrences of springs found in coastal areas is influenced by marine and geological parameters which will further affect the method of capture, management, and utilization. This prototype of raw water supply has been installed in a location around the spring at Banyu Asri Beach, Singaraja City, Buleleng Regency, Bali Province in 2013. Data collection methodology is carried out by observing the wave data, pumping discharge and water salinity. These observations were made for two types of oscillation boards, namely using wood and fiber. From this technology, it is expected that the supply of a stable source of springs and the mineral content that is maintained even though the position of the spring is strongly influenced by the tide of the sea water which often inundates the discharge point of the spring. The spring at Banyu Asri Beach has been widely used by the community for drinking water and ritual worship. From the results of the performance of the prototype after being installed at the location of the spring, it has shown the ability to drain fresh water through pipelines towards the land, although the wave height that occurs in very small locations ranges from 0.10 to 0.30 cm and the discharge flow is up to 0.03 L / sec.
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