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Formulation of muds for pelotherapy: effects of 'maturation' by different mineral waters

机译:用于泥浆疗法的泥浆配方:不同矿泉水“成熟”的效果

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Spa centres in northern Italy use clayey admixtures for the formulation of muds to be used in pelotherapy. The basic ingredient ("virgin" clay) is a dressed bentonitic geomaterial with mineralogical composition: smectite 60―70%, illite 5―10%, kaolinite 10―15%, quartz 5―10%, calcite 5-10% and feldspars 2―3%. The peloid muds are obtained by "maturation" of the virgin clay with mineral waters gushing out in situ which have different geochemistry: sulphureous, Ca-sulphate, Ca―Mg-sulphate and Br―I-salty (after the Italian regulation DPR 105/92). The maturation treatment is varying with respect to the mixing procedure and lasting time. Peculiar parameters have been tested to verify the effects of various maturation treatments, i.e., changes with respect to virgin clay. Formation of organic matter is due to the presence of microorganisms and algae in the maturation habitat. The < 2 μm fraction is generally decreased due to clay particles agglomeration. Mineralogical changes are mainly concerning the degradation of clay minerals, as smectite and illite, and subordinately to the dissolution of calcite. Cation exchange capacity (CEC), soluble salts, water retention, swelling index, activity, consistency parameters (WL, WP and PI), thermal behaviour and cooling kinetics are influenced by the geochemistry of mineral waters used for the maturation treatments but with some opposite trends for Br―I-salty water, and for sulphureous and Ca-sulphate waters, respectively. Noteworthy was the influence of high-pH value of the virgin clay on the pH of peloid muds (in fact, the pH of the used mineral waters is ranging around the natural value). Furthermore, the temperature reached by the peloid muds after 20 min of application (calculated after an innovative mathematical model) is influenced by water retention. An increase in plasticity index and a slower cooling are considered to improve the quality of the obtained peloid muds for pelotherapy. The observed different cation exchange behaviour and soluble salt content could be discriminant for either dermatological masks or thermal body cataplasms. A need of regulation (standard procedures) is suggested to certificate the clay geomaterials suitable for pelotherapy and also for drugs formulation.
机译:意大利北部的水疗中心使用黏土外加剂配制泥浆,用于泥浆疗法。基本成分(“原始”粘土)是具有矿物学组成的膨润土矿物材料:蒙脱石60-70%,伊利石5-10%,高岭石10-15%,石英5-10%,方解石5-10%和长石2 ―3%。胶体泥是通过将天然粘土与原地涌出的矿泉水“熟化”而获得的,这些矿泉水具有不同的地球化学特性:硫,硫酸钙,硫酸钙镁和溴化氢盐(根据意大利DPR 105 / 92)。关于混合过程和持续时间,成熟处理是变化的。已经测试了特殊参数以验证各种成熟处理的效果,即相对于原始粘土的变化。有机物质的形成是由于成熟栖息地中存在微生物和藻类。 <2μm的分数通常由于粘土颗粒的团聚而降低。矿物学变化主要涉及粘土矿物(如蒙脱石和伊利石)的降解,而从方解石的溶解而来。阳离子交换能力(CEC),可溶性盐,保水性,溶胀指数,活性,稠度参数(WL,WP和PI),热行为和冷却动力学受用于成熟处理的矿泉水地球化学的影响,但有些相反Br-I咸水,亚硫酸和硫酸钙水的趋势。值得注意的是,原始粘土的高pH值对胶体泥pH的影响(实际上,所用矿泉水的pH值在自然值附近)。此外,胶体泥在施用20分钟后达到的温度(根据创新的数学模型计算得出)受保水量的影响。考虑到可塑性指数的增加和较慢的冷却可改善所获得的用于泥土疗法的胶体泥的质量。所观察到的不同阳离子交换行为和可溶性盐含量可能对皮肤病学面具或热体催化物有区别。建议需要法规(标准程序)来认证适用于球疗法和药物制剂的粘土土工材料。

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