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Geothermal Potential of the Ortahaza-West Field in Hungary

机译:匈牙利奥塔哈加 - 西场地热潜力

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The Hungarian petroleum industry has always participatedin the utilization of favourable geothermal conditions in the country. Most of the Hungarian geothermal wells were drilled by MOL Ltd. as petroleum prospect holes. Accordingly, the field of geothermics belonged to the petroleum engineering, although marginally. It was therefore a surprise to hear of the decision of MOL Ltd. to build a geothermal power plant of about 2-5 MW. The tender was published in 2004. The site selected for the geothermal project is near the western border of a Hungarian oilfield, close to the Slovenian border. The location of the planned geothermal power plant was chosen after an analysis of suitable wells owned by MOL Rt. The decision was made on the bases of different reservoir data. The existence of a reservoir of the necessary size, temperature, permeability, productivity and water chemistry data was proved. The wells provide enough information to understand the character of the reservoir and will be the production wells used by the planned power plant. The depth of the wells is in the range of 2930 - 3200 m. The Triassic formation is reached at around 2851 m. Production and injection wells are planned. The primary objective of the evaluation is to further learn the nature of the geothermal system. First a one-day discharge test is carried out. If this short-term test is successful, a six-months long-term discharge test will follow. The first period of the test is a transient phenomenon. During the well test, the wellhead pressure, flow rate, out-flowing water temperature, dynamic fluid level, and chemical components will be measured. The heat transfer around the borehole is influenced by the flow rate and the time. For the proper interpretation of the measured data it is very important to analyse the heat transfer processes around the borehole. The measured data from the experiments must also be fitted into the framework of a mathematical model in order to form a coherent system. Before the drilling operations and the discharge tests, the temperature of the outflowing water can be predicted. This is made possible by applying recently elaborated simulation methods (Bobok-Toth 2003, Toth 2004). The available thermal power of a simple doublet can also be determined.
机译:匈牙利石油工业始终参加了该国有利地热条件的利用。大多数匈牙利地热井都被Mol Ltd.钻了石油前景孔。因此,地质领域属于石油工程,但虽然略微。因此,听到Mol Ltd.的决定是一个惊喜,建造一个约2-5兆瓦的地热发电厂。招标于2004年发表。为地热项目选择的网站位于匈牙利油田的西部边界附近,靠近斯洛文尼亚边境。在分析MOL RT所拥有的合适孔后,选择计划地热发电厂的位置。该决定是对不同水库数据的基础进行的。证明了必要规模,温度,渗透性,生产力和水化学数据的储层的存在。井提供足够的信息来了解水库的特征,并将是计划发电厂使用的生产井。井的深度在2930-2200米的范围内。三叠层形成达到2851米左右。计划生产和注入孔。评估的主要目标是进一步了解地热系统的性质。首先进行一天排出测试。如果此短期测试成功,将遵循六个月的长期排放测试。测试的第一期是瞬态现象。在井测试期间,将测量井口压力,流量,流出水温,动态液位和化学成分。钻孔周围的热传递受到流速和时间的影响。为了正确解释测量数据,分析钻孔周围的传热过程非常重要。来自实验的测量数据也必须安装在数学模型的框架中,以形成相干系统。在钻井操作和放电测试之前,可以预测流出水的温度。这是通过应用最近精细的仿真方法(Bobok-Toth 2003,Toth 2004)来实现的。也可以确定简单双重的可用热功率。

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