nikoli埃沃温泉(东塞尔维亚)温泉水

P. Dokmanović, V. Dragišić, Slavko Spadijer
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引用次数: 0

摘要

新的监测结果(2000-2002年)尼古拉切沃温泉(塞尔维亚东部)的温泉水流出和水质状况表明,在30年的时间里,由于水井恶化和水库枯竭,发生了一个结皮过程,井流出量减少了约80%。因此(水运动较慢),水温升高1.5 -2°C。在新监测期间记录的流出量和水质参数的稳定值表明,年度气象周期对流出量和水质状况的影响微不足道。根据其化学成分,水是碳酸氢钠-氟化物,低聚和等温和广泛的应用是可用的。目前的低出水量限制了水的有效开采和利用,因此建议钻新井。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thermomineral water of Nikoličevo Spa (Eastern Serbia)
New monitoring results (2000-2002) of the thermomineral water outflow and quality regime of the Nikolicevo Spa (eastern Serbia) show that, during 30 years, a scaling process occurred and decreased the well outflow by app. 80%, as a consequence of well deterioration and reservoir depletion. Consequently (slower water movement), the water temperature increased by 1,5-2°C. Stabile values of the outflow and water quality parameters, registered during new monitoring, show an insignificant influence of the annual meteorological cycle on the outflow and quality regime. According to its chemical composition, the water is sodiumbicarbonate- fluoride, oligomineral and isothermal and a wide spectrum of applications is available. The limit for an efficient exploitation and application of the water is the current low outflow rate, so the drilling of new wells is recommended.
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