Hidrogeoquímica de las aguas minero medicinales de la provincia de Melgar, Puno-Perú
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Rev. Inv. Cs. Agro. y Vet.
Abstract
Las aguas minero-medicinales de la provincia de Melgar de la región de Puno en Perú, se encuentran ubicadas a gran altitud, con utilidad medicinal y/o de recreación, por lo que es necesario conocer sus características, en tal sentido el estudio tuvo el propósito de identificar las características hidrogeoquímicas de las aguas minero medicinales de la provincia de Melgar, Puno en Perú. Para el estudio se ha recolectado información de los parámetros físicos y químicos de los pozos minero medicinales de la provincia de Melgar, Puno. Se aplicó la técnica de los diagramas de Piper con la finalidad de caracterizar los tipos de agua minero medicinales. Los resultados indicaron que, el catión predominante en las pozas de Pasanoccollo; Santa Rosa; Huamanruro; Andaymarca y Pojcpoquella, fue el ión Na+, con 84,33%; 56,35%; 50,60%; 64.16% y 73.97% de presencia, respectivamente, mientras que, en la poza de Macarí el catión que más predominó es el Ca2+ con 42.54 %. Con respecto a los aniones el SO_4^(2-) y el Cl- son los aniones que predominaron. El Cl- fue el anión predominante en las pozas de Santa Rosa; Huamanruro; Macarí; Andaymarca y Pojcpoquella con 74.43 %; 67.22 %; 58.57 %; 58.34 % y 70.79 % de presencia, respectivamente, mientras que en la poza de Pasanoccollo el anión que predominó es el SO_4^(2-) con un 58.37 %, de estos resultados se llega a la conclusión que las pozas se encuentran en un marco estratigráfico y estructural de las aguas minero medicinales, está formado por areniscas rojas y rocas conglomeradas.
The medicinal mining waters of the province of Melgar in the region of Puno in Peru, are located at high altitude, with medicinal and / or recreational use, so it is necessary to know their characteristics, in this sense the study had the purpose to identify the hydrogeochemical characteristics of medicinal mineral waters from the province of Melgar, Puno in Peru. For the study, information has been collected on the physical and chemical parameters of the medicinal mining wells in the province of Melgar, Puno. The technique of Piper diagrams was applied in order to characterize the types of medicinal mineral water. The results indicated that the predominant cation in the Pasanoccollo pools; Santa Rosa; Huamanruro; Andaymarca and Pojcpoquella, was the Na+ ion, with 84.33%; 56.35%; 50.60%; 64.16% and 73.97% presence, respectively, while in the Macarí pool the cation that predominated the most is Ca2+ with 42.54%. Regarding the anions, SO_4^(2-) and Cl- are the anions that predominated. Cl- was the predominant anion in the Santa Rosa pools; Huamanruro; Macari; Andaymarca and Pojcpoquella with 74.43%; 67.22%; 58.57%; 58.34 % and 70.79 % presence, respectively, while in the Pasanoccollo pool the predominant anion is SO_4^(2-) with 58.37 %, from these results we can conclude that the pools are in a framework stratigraphic and structural of the medicinal mining waters, is formed by red sandstones and conglomerate rocks.
The medicinal mining waters of the province of Melgar in the region of Puno in Peru, are located at high altitude, with medicinal and / or recreational use, so it is necessary to know their characteristics, in this sense the study had the purpose to identify the hydrogeochemical characteristics of medicinal mineral waters from the province of Melgar, Puno in Peru. For the study, information has been collected on the physical and chemical parameters of the medicinal mining wells in the province of Melgar, Puno. The technique of Piper diagrams was applied in order to characterize the types of medicinal mineral water. The results indicated that the predominant cation in the Pasanoccollo pools; Santa Rosa; Huamanruro; Andaymarca and Pojcpoquella, was the Na+ ion, with 84.33%; 56.35%; 50.60%; 64.16% and 73.97% presence, respectively, while in the Macarí pool the cation that predominated the most is Ca2+ with 42.54%. Regarding the anions, SO_4^(2-) and Cl- are the anions that predominated. Cl- was the predominant anion in the Santa Rosa pools; Huamanruro; Macari; Andaymarca and Pojcpoquella with 74.43%; 67.22%; 58.57%; 58.34 % and 70.79 % presence, respectively, while in the Pasanoccollo pool the predominant anion is SO_4^(2-) with 58.37 %, from these results we can conclude that the pools are in a framework stratigraphic and structural of the medicinal mining waters, is formed by red sandstones and conglomerate rocks.
Description
Vol. 7, No. 19