Pikrolimni湖沉积物(希腊北部Kilkis地区)的结构、矿物学和地球化学评估及其在Pelotherapy中的适用性

E. Sofianska, C. Athanassoulis, D. Tarenidis, N. Xirokostas, Maria Gkagka
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引用次数: 1

摘要

皮肤疗法是应用热泥(类球)来恢复肌肉、骨骼和皮肤病变。建立了评价类球体治疗适宜性的具体标准。决定类球固体相质量的关键因素包括粒度、矿物学和物理化学性质。本研究的目的是研究希腊基尔基斯地区Pikrolimni湖沉积物(PLS)的结构、矿物学和地球化学特征,以评估其作为泥浆处理技术原料的适用性。在希腊地质和矿产勘探调查(HSGME)的分析实验室中,通过不同的技术收集和分析了具有代表性的PLS样品。结果表明,在结构上,PLS属于砂壤土沉积物。x射线衍射(XRD)研究表明,PLS主要由石英、粘土矿物(高岭石、蒙脱石、伊利石)和白云母组成,少量长石和方解石。x射线荧光(XFR)分析表明,与平均页岩组成相比,PLS样品具有较高的SiO2和较低的Al2O3含量。通过电感耦合等离子体质谱(ICP-MS)技术分析,发现潜在有毒元素中As和Pb的含量明显高于页岩的平均值。根据计算的富集系数(EF)和地质富集指数(Igeo)均值,PLS分别表现为轻度富集和中度污染。总之,需要通过筛分工艺来改善PLS的粒度组成。此外,还提出了对处理后的PLS与含盐热矿泉水混合形成的似质体中有毒元素的浓度和行为的研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Textural, Mineralogical and Geochemical Assessment of the Pikrolimni Lake Sediments (Kilkis District, Northern Greece) and Suitability for use in Pelotherapy
Pelotherapy is the application of thermal muds (peloids) for recovering muscle, bone and skin pathologies. Specific criteria were established for the evaluation of the therapeutic suitability of peloids. Critical factors ruling the quality of the solid phase of peloids include granulometry, mineralogy, and physical-chemical properties. The aim of the present study was to investigate the textural, mineralogical and geochemical characteristics of the Pikrolimni Lake sediments (PLS), Kilkis district (N. Greece) in order to assess their suitability for application as raw material into mud therapy technologies. Representative PLS samples were collected and analyzed by means of different techniques at the analytical laboratories of the Hellenic Survey of Geology and Mineral Exploration (HSGME). Results showed that, texturally, the PLS were classified as sandy loam sediments. X-ray diffraction (XRD) study revealed that the PLS consist mainly of quartz, clay minerals (kaolinite, montmorillonite, illite), and muscovite, with minor feldspar and calcite. X-ray fluorescence (XFR) analysis showed that PLS samples have higher SiO2 and lower Al2O3 contents compared to the average shale composition. Among the analyzed, by means of inductively coupled plasma mass spectrometry (ICP-MS) technique, potentially toxic elements only As and Pb contents were found significantly higher than those of the average shale. Based on the calculated mean values of enrichment factor (EF) and geo-accumulation index (Igeo) PLS displayed minor enrichment and moderate contamination by Pb and As, respectively. In conclusion, an improvement of the grain size composition of PLS by means of a sieving process is needed. Besides, the study of the concentration and behavior of toxic elements in peloids formed by the mixing of the processed PLS with salty thermo-mineral water is proposed.
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