Salinity and ionic composition of the shallow astatic soda pans in the Carpathian Basin
Salinity and ionic composition of the shallow astatic soda pans in the Carpathian Basin
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DOI：
10.1051/limn/2013068
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发表时间：
2014-01-01
影响因子：
1
通讯作者：
Voeroes, L.
中科院分区：
文献类型：
--
作者：
Boros, E.;Horvath, Zs.;Voeroes, L.
我们调查了化学特性的无定向苏打平底锅在喀尔巴阡山盆地的基础上全面的新的和存档的数据。分析的参数是盐度和离子组成。最常见的苏打沃茨类型是碱性类型（Na-HCO 3），占天然苏打水的一半以上。此外还出现了11种亚型。第二和第三最常见的类型是氯化物（13%）和硫酸盐亚型（11%），这些阴离子的次要优势。其他亚型均在50 g·L ~（-1）范围内，其平均值（近似4 g·L ~（-1））在低盐范围（3-20 g·L ~（-1））。碱性类型的分布具有随机性，而其他亚型仅限于盆地的某些区域。大量的亚型反映了在喀尔巴阡盆地相对较小的领土上碱性苏打水的高度化学多样性。
We investigated the chemical characteristics of the astatic soda pans in the Carpathian Basin based on comprehensive new and archive data. Analysed parameters were salinity and ionic composition. The most frequent type of soda waters was the basic alkaline type (Na-HCO3) that represented more than half of the natural soda pans. Besides 11 subtypes occurred. The second and third most frequent types were the chloride (13%) and sulphate subtypes (11%), with the secondary dominance of these anions. The other subtypes meant 50 g.L-1) ranges, with its mean value (similar to 4 g.L-1) in the hyposaline range (3-20 g.L-1). The basic alkaline type had random geographical distribution, while the other subtypes were restricted to certain regions of the Basin. The high number of subtypes reflects the high chemical diversity of alkaline soda pans in the relatively small territory of the Carpathian Basin.