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首页> 外文期刊>Journal of water resource and protection >Estimate of the Aquifer Temperature of Assammaqieh Well in Akkar by Geothermometric Equations
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Estimate of the Aquifer Temperature of Assammaqieh Well in Akkar by Geothermometric Equations

机译:用地热计量方程估算阿卡(Akkar)阿萨玛奇耶井的含水层温度

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This research aims at estimating the temperature of the aquifer that supplies Assammaqieh well at the depth of 550 m, on the basis of chemical analyses and geothermometric techniques which are one of the methods used for searching for the renewable geothermal energy and conserving the environment. In this study, about twenty-two geothermometric indicators have been used. For verifying the results, these results have been compared with data and estimates of temperature of fluids of deep typical wells in New Zealand, and it has been noticed that the theoretical and actual results approach the limits of 95% in many indicators. The study has been restricted to the relations of Cations because they are the most reliable, and the least affected by dissolution and evaporation. Most of the indicators that are based on the four chemical elements: Calcium (Ca), Potassium (K), Sodium (Na), Magnesium (Mg), have been adopted. The laboratory analysis data of Assammaqieh well confirmed that it was hot sulphurous water that acquired its chemical properties from complicated geochemical conditions, underground thermal conditions and volcanic rock nature. It also turned out that the underground heating process was basically due to thermal conductivity and rock adjacency, and that Assammaqieh well was supplied with water from adjacent groundwater tables whose source was the penetration of surface water. It also appeared that most of the equations used in the search for geothermal energy revealed the presence of an aquifer of hot and very hot water, and they were compatible with the high thermal gradient in volcanic rocks. It also tuned out that 86% of the used geothermometric equations estimated the aquifer temperature of Assammaqieh well as being hot and very hot with around 135.5 Celsius (±20). The study concluded with the hypothesis that Akkar possessed a huge geothermal energy, and benefiting from this energy might put an end to the chronic problem of electricity in Lebanon, and opened up many prospects and uses that could participate in a sustainable and comprehensive development of Akkar and Lebanon as a whole.
机译:这项研究旨在基于化学分析和地热计量技术(这是寻找可再生地热能和保护环境的方法之一)的基础上,估计能在550 m深度处很好地为阿斯玛奇切提供补给的含水层的温度。在这项研究中,已使用了约22个地热指示器。为了验证结果,将这些结果与新西兰深部典型井的流体温度数据和估计值进行了比较,并且注意到理论和实际结果在许多指标中均接近95%的极限。该研究仅限于阳离子的关系,因为它们最可靠,并且受溶解和蒸发的影响最小。大部分指标是基于四种化学元素的:钙(Ca),钾(K),钠(Na),镁(Mg)。 Assammaqieh井的实验室分析数据证实,正是从复杂的地球化学条件,地下热条件和火山岩性质中获得了其化学性质的热亚硫酸水。结果还表明,地下加热过程主要是由于热导率和岩石邻接性所致,Assammaqieh井从相邻地下水位供应水,水源是地表水的渗透。看来,用于寻找地热能的大多数方程都揭示了热水和非常热水的存在,并且它们与火山岩中的高热梯度兼容。它还调出了86%的所用地热学方程式估算出阿萨玛奇耶的含水层温度非常热,非常热,约为135.5摄氏度(±20)。该研究以以下假设为前提:阿克卡尔拥有巨大的地热能,而从这种能量中受益可能会终结黎巴嫩的长期电力问题,并开辟了许多可以参与阿克卡尔可持续全面发展的前景和用途和整个黎巴嫩

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