scholarly journals Arsenic, Germanium and Selenium in the Thermal Waters of Misasa Hot Springs, Tottori Prefecture. —And the Determinationof Phosphate Ion in Hot Spring

1960 ◽  
Vol 81 (2) ◽  
pp. 242-246
Author(s):  
Masanobu SAKANOUE
2020 ◽  
Author(s):  
Asmita Maitra ◽  
Saibal Gupta ◽  
Mruganka Kumar Panigrahi ◽  
Tirumalesh Keesari

<p>Hot springs in the stable Indian shield are non-volcanic in origin. Atri and Tarbalo are two such hot springs in the Eastern Ghats Province (EGP), Eastern India and these are characterized as part of a low enthalpy geothermal system. Stable isotopic, geochemical and geothermometric studies were carried out on these two hot springs as well as on the groundwater of this region to understand the origin and evolution of these non-volcanic hot springs as well as subsurface water system in terms of the source of the dissolved solute in the water, mixing processes and the residence time of the thermal and non-thermal waters. Surface temperature of the slightly alkaline hot spring waters ranges from 45 to 58 °C. Temperature of the cold groundwater, collected from tube and dug well varies between 28 and 32 °C. A distinct hydro-chemical difference can be interpreted from the major ion concentrations of hot waters and non-thermal waters. Hot spring waters have higher concentrations of sodium, potassium and lower calcium, magnesium than cold water. While the hot springs waters are enriched in Cl<sup>-</sup> and F<sup>-</sup> and cold waters are rich in bicarbonate. The low bicarbonate concentration of thermal waters may indicate that the hot spring reservoirs have no atmospheric effect. Definite geochemical differences between these two types of water suggested that there is no mixing between hot spring water and cold groundwater. Thermodynamic calculations suggest that mineral dissolution is the predominant evolutionary mechanism for the thermal and non-thermal waters and these waters hold a partially equilibrated state with the surrounding rocks. Bivariate plots of the major ions also indicate that silicate weathering is the dominant mechanism controlling solutes concentrations in the cold water whereas evaporite dissolution more likely involves in the evolution of hot spring water. The measured stable isotope ratios (δ<sup>2</sup>H and δ<sup>18</sup>O) of all the hot and most of the cold-water samples plot along the Global Meteoric Water Line (GMWL), indicating their meteoric origin where as some cold waters show evaporation effect which suggests atmospheric influence. Tritium and <sup>14</sup>C ages indicate that the cold waters are relatively modern, while the hot waters have a longer residence time of about 5000 years. Based on the chemical characteristics of the hot waters Na-K thermometer, Na-K-Ca thermometer and silica (quartz) thermometer were used to estimate the reservoir temperatures. Cation and silica geothermometers yield similar estimation of the reservoir temperature between 125 -150 °C for hot spring waters. Results of geochemical (numerical) modelling of water-rock interaction in this region, using PHREEQC, are consistent with hydrochemical analysis. Inverse modelling and saturation indices of minerals indicate that water chemistry in this region is controlled by the dissolution of feldspar and saturated with kaolinite, gibbsite and fluorite. This equilibrium is attained in the thermal waters, which therefore show a more restricted range of composition than the non-thermal, colder waters. The higher fluoride concentration in the thermal water may also be attributed of chemical equilibrium with the enclosing host rock.</p>


1939 ◽  
Vol 16 (4) ◽  
pp. 487-498
Author(s):  
I. L. MASON

1. A description is given of the hot springs of Hammam Meskoutine, Algeria, and the principal animals and plants found living in them above a temperature of 38°C. 2. Life was found up to the following maximum temperatures: plants (blue-green algae), 58° C.; animals (Cypris balnearia), 51.5° C. 3. A comparison between the death-points of the principal animals and the temperatures at which they were living shows: (a) That some animals (Cypris balnearia and Bidessus signatellus) are confined to thermal waters. (b) That some animals can exist, for short periods, at temperatures above their eventual thermal death-points (Cypris balnearia and Rana ridibunda). (c) That some animals have death-points which vary with the temperatures at which they live (Barbus callensis and Potamon edulis).


2020 ◽  
Vol 9 (3) ◽  
pp. 266
Author(s):  
Damian Luis Castellini ◽  
Aldo Nahuel Zanazzi ◽  
Angelina Gorosito ◽  
Enzo Damián Tranier ◽  
María Fernández-Subiela ◽  
...  

In the present work, the feasibility of fattening Oreochromis niloticus specimens on a pilot scale in a geothermal water resource located in the Southeast of the province of Buenos Aires was analyzed. Before placing the culture units, physical and chemical characteristics of hot spring were studied to evaluate its suitability for tilapia farming. In the experimental stage, two hundred specimens with an average weight of 14.5 ± 1.8g were placed in two floating cages (1.30x1x1m) (100 individuals per cage) and they were harvested at 140 days. The specimens were fed 3 times a day with a commercial pelleted feed with a content of 35% of proteins. Monthly samplings were carried out to evaluate growth (weight and total length), survival, and water samples were collected to measure their physical-chemical characteristics. The results of the water analysis showed a high quality in the hot springs (Simplified Water Quality Index=88). The fattening results showed an average final weight of 423-435.9 g, a survival of 87-91%, a SGR 1.47- 1.49% / day and  the FCR was estimated at 1.05-1.07 for each cage respectively. We can conclude that this hot spring has the necessary water conditions to obtain excellent weight gains during the fattening period for the O. niloticus specimens. The present study represents the first Nile tilapia culture in the southernmost thermal waters, setting a precedent for future ventures in the area.


2021 ◽  
Vol 13 (1) ◽  
pp. 820-834
Author(s):  
Jun Ma ◽  
Zhifang Zhou

Abstract The exploration of the origin of hot spring is the basis of its development and utilization. There are many low-medium temperature hot springs in Nanjing and its surrounding karst landform areas, such as the Tangshan, Tangquan, Lunshan, and Xiangquan hot springs. This article discusses the origin characters of the Lunshan hot spring with geological condition analysis, hydrogeochemical data, and isotope data. The results show that the hot water is SO4–Ca type in Lunshan area, and the cation content of SO4 is high, which are related to the deep hydrogeological conditions of the circulation in the limestone. Carbonate and anhydrite dissolutions occur in the groundwater circulation process, and they also dominate the water–rock interaction processes in the geothermal reservoir of Lunshan. The hot water rising channels are deeply affected by the NW and SN faults. Schematic diagrams of the conceptual model of the geothermal water circulation in Lunshan are plotted. The origin of Tangshan, Tangquan, and Xiangquan hot springs are similar to the Lunshan hot spring. In general, the geothermal water in karst landforms around Nanjing mainly runs through the carbonate rock area and is exposed near the core of the anticlinal structure of karst strata, forming SO4–Ca/SO4–Ca–Mg type hot spring with the water temperature less than 60°C. The characters of the hot springs around Nanjing are similar, which are helpful for the further research, development, and management of the geothermal water resources in this region.


Author(s):  
Eka Djatnika Nugraha ◽  
Masahiro Hosoda ◽  
June Mellawati ◽  
Untara Untara ◽  
Ilsa Rosianna ◽  
...  

The world community has long used natural hot springs for tourist and medicinal purposes. In Indonesia, the province of West Java, which is naturally surrounded by volcanoes, is the main destination for hot spring tourism. This paper is the first report on radon measurements in tourism natural hot spring water in Indonesia as part of radiation protection for public health. The purpose of this paper is to study the contribution of radon doses from natural hot spring water and thereby facilitate radiation protection for public health. A total of 18 water samples were measured with an electrostatic collection type radon monitor (RAD7, Durridge Co., USA). The concentration of radon in natural hot spring water samples in the West Java region, Indonesia ranges from 0.26 to 31 Bq L−1. An estimate of the annual effective dose in the natural hot spring water area ranges from 0.51 to 0.71 mSv with a mean of 0.60 mSv for workers. Meanwhile, the annual effective dose for the public ranges from 0.10 to 0.14 mSv with an average of 0.12 mSv. This value is within the range of the average committed effective dose from inhalation and terrestrial radiation for the general public, 1.7 mSv annually.


2021 ◽  
Vol 9 (7) ◽  
pp. 1473
Author(s):  
Ani Saghatelyan ◽  
Armine Margaryan ◽  
Hovik Panosyan ◽  
Nils-Kåre Birkeland

The microbial diversity of high-altitude geothermal springs has been recently assessed to explore their biotechnological potential. However, little is known regarding the microbiota of similar ecosystems located on the Armenian Highland. This review summarizes the known information on the microbiota of nine high-altitude mineralized geothermal springs (temperature range 25.8–70 °C and pH range 6.0–7.5) in Armenia and Nagorno-Karabakh. All these geothermal springs are at altitudes ranging from 960–2090 m above sea level and are located on the Alpide (Alpine–Himalayan) orogenic belt, a seismically active region. A mixed-cation mixed-anion composition, with total mineralization of 0.5 mg/L, has been identified for these thermal springs. The taxonomic diversity of hot spring microbiomes has been examined using culture-independent approaches, including denaturing gradient gel electrophoresis (DGGE), 16S rRNA gene library construction, 454 pyrosequencing, and Illumina HiSeq. The bacterial phyla Proteobacteria, Bacteroidetes, Cyanobacteria, and Firmicutes are the predominant life forms in the studied springs. Archaea mainly include the phyla Euryarchaeota, Crenarchaeota, and Thaumarchaeota, and comprise less than 1% of the prokaryotic community. Comparison of microbial diversity in springs from Karvachar with that described for other terrestrial hot springs revealed that Proteobacteria, Bacteroidetes, Actinobacteria, and Deinococcus–Thermus are the common bacterial groups in terrestrial hot springs. Contemporaneously, specific bacterial and archaeal taxa were observed in different springs. Evaluation of the carbon, sulfur, and nitrogen metabolism in these hot spring communities has revealed diversity in terms of metabolic activity. Temperature seems to be an important factor in shaping the microbial communities of these springs. Overall, the diversity and richness of the microbiota are negatively affected by increasing temperature. Other abiotic factors, including pH, mineralization, and geological history, also impact the structure and function of the microbial community. More than 130 bacterial and archaeal strains (Bacillus, Geobacillus, Parageobacillus, Anoxybacillus, Paenibacillus, Brevibacillus Aeribacillus, Ureibacillus, Thermoactinomyces, Sporosarcina, Thermus, Rhodobacter, Thiospirillum, Thiocapsa, Rhodopseudomonas, Methylocaldum, Desulfomicrobium, Desulfovibrio, Treponema, Arcobacter, Nitropspira, and Methanoculleus) have been reported, some of which may be representative of novel species (sharing 91–97% sequence identity with their closest matches in GenBank) and producers of thermozymes and biomolecules with potential biotechnological applications. Whole-genome shotgun sequencing of T. scotoductus K1, as well as of the potentially new Treponema sp. J25 and Anoxybacillus sp. K1, were performed. Most of the phyla identified by 16S rRNA were also identified using metagenomic approaches. Detailed characterization of thermophilic isolates indicate the potential of the studied springs as a source of biotechnologically valuable microbes and biomolecules.


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