Role of hot springs’ hydrochemistry in Balneotherapy, Case Study: Fotoyeh and sanguyeh springs, western Hormozgan (original) (raw)
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Investigation of Physical and Chemical Quality of Hot Springs in South Khorasan, Iran
Archives of Hygiene Sciences, 2019
Background & Aims of the Study: Many people use natural springs for many years to provide therapeutic, recreational, and in some cases, drinking water. The investigation of physicochemical properties and promotion of its indices in hot springs are very important for maintaining the health and well-being of individuals. The present study aimed to investigate some physicochemical properties of hot springs in South Khorasan, Iran, and compare them with the standards in 2018. Materials and Methods: In order to assess the physicochemical quality of hot springs in South Khorasan, temperature, pH, electrical conductivity (EC), alkalinity, and total hardness parameters were measured and analyzed using standard methods. Data analysis was performed using Excel software (version 2010). Results: Based on the obtained results, the highest temperature and EC were observed in Dig-e Rostam hot spring with 54.3°C and Ferdowshotspringwith10.43 μs/cm, respectively. Furthermore, the highest pH, alkalinity, and total hardness were obtained in Qaen hot spring with 7.87, Sarbisheh hot spring with 2018 mg/L CaCo3, and Ferdows hot spring with 1204 mg/L CaCo3, respectively. Conclusion: Based on the results obtained from the review of the physicochemical quality of the hot springs in the southern Khorasan, most of the measured parameters of the springs were not within the standard range.
2014
Hot springs water has been associated with healing of various types of skin diseases. Despite their therapeutic effects which are known worldwide, there are limited reports on the physicochemical characteristics of hot springs water in Peninsular Malaysia. Therefore, an attempt was made to determine the concentrations of major cations, anions and sulphur including naturally occurring radioactive material (NORM). There are 43 locations of hot springs water with 67 sources identified in Peninsular Malaysia which cover almost all states. Chemicals and radionuclides compositions measured in this study include Na+, K+, Ca2+, Mg2+, S, Cf, SO42', U and Th. Concentrations of Na, K, Ca and S were analysed using Energy Dispersive X-ray Fluorescence (EDXRF) while Mg2+, U and Th were analysed using Inductively Coupled Plasma Optical Emission Spectrometer (ICP-OES). Ion chromatography (IC) was used to analyse C1‘, HCO3 ' and SO42'. Results obtained from the analysis of Na, K, Ca and ...
Applied Water Science, 2021
Current studies were performed to evaluate the physico-chemical characteristics and therapeutic potential of Chutrun thermal springs located in the North-west of Shigar Valley, Gilgit-Baltistan (Pakistan). Thermal springs with different mineral contents have been used by people for bathing and health purposes since old timings. The mineral water of these springs contains elements like sodium, potassium, calcium, magnesium as chlorides, fluorides, sulphates, phosphates and bicarbonates which may be responsible for cure of various diseases. Chutrun hot springs have 7.21–7.8 pH, 40–42° C Temperature, 300–310 ppm TDS, 3.1–6.7 ppm DO, 278–285 ppm hardness, 1.62–2.42 ppm turbidity, 250–260 ppm alkalinity, 500–516 ppm conductivity, 12–18 ppm sodium, 3.8–4.1 ppm potassium, 80–82 ppm calcium, 20 ppm magnesium, 9.6–12 ppm chlorides, 3.4–3.9 fluorides, 260–282 bicarbonates and 80–85 ppm sulphates. Absence of E.Coli and faecal coliforms indicated that waters from thermal springs are free from o...
Arabian Journal of …, 2011
This research examined the balneological characteristics of spring waters within the area of Abu-Jir Fault Zone throughout the hydrogeologic aspects explained by the setting of the hydrogeologic units including the waterbearing horizons of Euphrates, Ana, and Baba Formations. The groundwater flow in the hydrogeologic system correlated with the trends of enrichment or depletion case processes of mineralization (spatial distribution maps of TDS and other components) show different phenomena of groundwater source and interconnection, which helps in the classification springs into two potential site. The physicochemical characteristics of the water flow from springs indicate a hydrochemical approach throughout the spatial variation of important parameters (using Rockware software) related to the balneological study. The monitoring network of the spring waters performed by seven field measurements and 33 variables (totaling to 720 detected measurements) in 18 springs approved the after desk study and water point inventory using a GPS apparatus (GARMIN SUMMIT-e TREX). The study examined the integrated hydrogeological aspects and spring water properties for evolutions and the classification of minero-medicinal water. The traditional hydrochemical information of the spring waters and their sediment properties correlated with balneological limits (standards and definitions) are used in the selection of springs characterized by balneotherapeutic applications. A suggested screening and ranking technique has been developed for evaluating preferable springs selected for natural therapy. The application of ranking technique indicates four graded consequent preferable springs for balneotherapeutic investment: first grade spring represented by Kubaiysa spring (S-4); second grade springs represented by Tawila spring (S-12); third grade springs represented by Mamora spring (S-15), Arnab spring (S-10), Zazoe spring (S-5), and Maqtoom spring (S-13); and fourth grade springs represented by Khalidiya spring (S-16) and Layeg spring (S-7).
Radioactivity and hydrochemical properties of certain thermal Turkish spa waters
Journal of Water and Health, 2017
The study aims to determine the radioactivity levels of thermal waters which have been used seasonally or permanently in spas for therapeutic intentions. Samples were collected from spas in different regions of Turkey. Some radionuclides (40K, 232Th, 226Ra, 137Cs), gross alpha (GA) and gross beta (GB) activities, and physical and some chemical parameters were measured. Gamma radiation measurements for 226Ra, 232Th and 40K radionuclides were performed by using a high purity germanium (HPGe) detector. The results of the gamma spectrometry ranged from 1.385 to 11.025 Bql−1 for 226Ra, <minimum detectable activity to 3.477 Bql−1 for 232Th and 9.679 to 36.989 Bql−1 for 40K. GA and GB activity concentrations were detected by using ultra-low level α/β counter. The GA and GB activity ranged from 43 to 3,182 mBql−1 and 54 to 1,950 mBql−1, respectively. Based on calculated annual effective dose equivalent, the total dose originated mostly from 226Ra and slightly from 40K. Furthermore, water...
E3S Web of Conferences, 2013
Thermal springs are widely used by tourists for treatment of dermal diseases and other therapeutic applications. In Iran, thermal springs occur in Northwestern part mainly surrounding the Mount Sabalan which attract hundreds of thousands of tourists annually. Two clusters of springs in Neer and Meshkinshahr areas including 16 thermomineralic springs have been studied in this research and they were sampled twice in May and November in order to investigate the seasonal changes of trace elements in dry and wet seasons. The samples were analyzed in Acme Lab, Canada for 72 elements. Trace element concentrations indicate that most of the elements show concentration well beyond the guideline values for drinking water. While the two sets of samples were taken within a 6 months interval, the elements show slight or no variation from first period to the second and in some cases. Arsenic shows a variation of 5-5834μg/l and the mean As value is 160 times the guideline values (10 μg/l). Other toxic elements with high concentration are B, Fe, Mn, Sb, and Si. Mn and Sb shows exeedance of 12 and 11.5 times respectively. Correlation coefficient and principal component analysis of analytical data indicate that Cl, As, B, Ba, Br, and V show very strong mutual correlation coefficients implying their relationship and common source and fate in the hydrothermal fluid carrying them. These elements fall in the component 1 of PCA. This group of elements is supposed to be derived and sourced from the magmatic-hydrothermal system and through the interaction of hydrothermal fluids with rocks they passed through. Because of discharge of the thermal springs into the nearby streams intended to be used for drinking water and also vast application of spring waters in balneological uses, they may have adverse environmental and health impacts on tourists that expose themselves to this contaminants through balneological applications. This is an Open Access article distributed under the terms of the Creative Commons Attribution License 2 0 , which . permits unrestricted use, distributi and reproduction in any medium, provided the original work is properly cited.
Geothermal Energy, 2022
This Science article summarizes the preliminary work carried out by the Renewable Energy Development Centre under the National Research Project in the Central North of Algeria from 2013 to 2016 to explore for geothermal resources and hydrogeology and hydrogeochemical and therapeutic aspects. The geology is very complex in this region and it determines the thermal water reservoirs. The value and importance of the thermal springs in Algeria is very significant. This study will be addressed by means of conventional chemical analyzes of the main hot springs major elements in the north central region of Algeria. Hydrogeochemical prospecting was carried out in detail is briefly exposed and the main results are described in particular regarding the hot springs of the Centre North of Algeria. The existing geothermal potential in Algeria is operated primarily for the balneotherapy and some applications for aquaculture. In this study, we will apply the hydrogeochemical techniques to the hot s...
Hydrogeochemical Studies of Hot Springs in Gilan Province , NIran
2010
Gilan Province is one of the most important tourism attraction area in Iran located in the Southern Caspian Sea. Average annual precipitation of the area is 1000 mm. The area is gained more than 10000 springs with discharge of up to 2 m/s mostly located in highlands and cold. 10 hot springs is known. All of them located in highlands and categorized in 3 regions: west, east and south of the province with maximum temperature of 36C. There are also some cold springs with high EC. In the south of the province, hot springs are studied more and preliminary hydrogeochemical investigations indicate strong influence of natural groundwater in the system by using Giggenbach triangle diagram that strong tectonic activity of the area emphasizes their possible tectonic origin. In the south springs are utilized for Olive farming except Sangrood hot spring with water type of C4S1 in Wilcox diagram that is not suitable for farming. Baleonological application is the best choice among future planes at...
Balneotherapy with the Use of Radon–Sulphide Water: The Mechanisms of Therapeutic Effect
Applied Sciences, 2021
Despite its enormous therapeutic potential, spa treatment is not always properly perceived, hence the numerous attempts to assess its effectiveness. In the world literature, there are few reports on therapy using sulphur- and radon-containing therapeutic waters. In countries with a long tradition of balneotherapy, activity in this field of medicine is evident. Undoubtedly, the interest in balneotherapy results also from natural resources used in spa medicine, which, as geological and balneochemical research shows, are enormous in Poland. A particular example of the occurrence of radon–sulphide waters, rare on the European scale, is the Przerzeczyn-Zdrój health resort. The mechanism of action of therapeutic waters is not fully explored, but their effectiveness in therapy is confirmed by many authors. It is believed to be an effect of combined action of many factors, the most important of which are thermal, mechanical, and chemical.
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