Journal of Geosciences and Geomatics. 2021, 9(4), 177-183
DOI: 10.12691/JGG-9-4-2
Original Research

A Comparative Study on Water Quality Parameters of a Hot Water Spring and Its Surrounding Water Resources at Irde, Panaje Puttur, Karnataka

Anupama Natesh1, , Dr. Radhakrishnan2 and Thangamani R2

1Department of Civil Engineering, Shree Devi Institute of Technology, Mangalore, India

2Department of Civil Engineering, NMAMIT Nitte, Karkala, India

Pub. Date: December 22, 2021

Cite this paper

Anupama Natesh, Dr. Radhakrishnan and Thangamani R. A Comparative Study on Water Quality Parameters of a Hot Water Spring and Its Surrounding Water Resources at Irde, Panaje Puttur, Karnataka. Journal of Geosciences and Geomatics. 2021; 9(4):177-183. doi: 10.12691/JGG-9-4-2

Abstract

Thermal spring is a natural phenomenon and is known in various names as hot springs, mineral springs, magic water, geysers, fumaroles, etc. based on their nature, qualities, and modes of formation on the earth's surface. The present study discusses the physicochemical analysis of Irade hot spring water with a comparative study of physicochemical characters of the samples collected from nearby locations during two different seasons like post-monsoon and pre-monsoon (2019). Irde hot spring is located about 15 km from Puttur town in the Dakshina Kannada district of Karnataka, India. The samples were collected at a distance of 196.82m (OW1), 239.48m (OW2), 163.13m (BW), and 61.30m from the hot spring. Analytical results of Irade hot spring water shows concentrations of fluoride about 2.92 mg/L in the post-monsoon season and within the limit during pre-monsoon. Generally, a hot spring contains some amount of fluoride due to the acidic nature (low pH) of water which reacts with rock at the time of percolation. Hot spring water can be used for drinking purposes only after the proper treatment. The sulfate concentration in hot spring water is 528mg/L (pre-monsoon) and 325mg/L (post-monsoon) and it is higher when compared to near by water sources. The turbidity of open wells samples OW1 and OW2 shows 6.1NTU and 5.18 NTU respectively and it should be treated before using it for drinking purposes. Previous research concluded that the hot nature of spring water is due to the sulfate concentration. With the influence of climatic changes and reduction in sulfate concentration the temperature of water getting reduced every year.

Keywords

fluoride, hot spring, physicochemical analysis, sulphate

Copyright

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References

[1]  S. Chandra, Geology, Chemistry and Genesis of Thermal Springs of Odisha, India. Springer briefs in earth sciences, 2019.
 
[2]  G. S. of I. Shanker, R., “Geothermal atlas of India.,” Geol. Surv. India., 1991.
 
[3]  T. Oldham, “Thermal springs of India,” Geol. Surv. Ind. Mem., vol. 19, no. 2, pp. 1-63, 1882.
 
[4]  K. R. Chandrashekar and K. R. Sridhar, “Thermal springs of Dakshina Kannada,” no. January, 2000.
 
[5]  M. Ramakrishnan, “Precambrian Mafic magmatism in the Western Dharwar Craton, southern India,” J. Geol. Soc. India, vol. 73, no. 1, pp. 101-116, 2009.
 
[6]  A. Ramanathan and D. Chandrasekharam, “Geochemistry of Rajapur and Puttur thermal springs of the West Coast, India,” J. Geol. Soc. India, vol. 49, no. 5, pp. 559-565, 1997.
 
[7]  B. P. Radhakrishna, “On a little known thermal spring from near Puttur, Mysore State, India,” J. Geol. Soc. India., vol. 10, pp. 88-94, 1971.
 
[8]  P. Ravikumar and R. K. Somashekar, “Assessment and modelling of groundwater quality data and evaluation of their corrosiveness and scaling potential using environmetric methods in Bangalore South Taluk, Karnataka state, India,” Water Resour., vol. 39, no. 4, pp. 446-473, 2012.
 
[9]  APHA American Public Health Association, Standard Methods for the Examination of Water and Wastewater, vol. 552. 1995.
 
[10]  R. Thangamani, K. Radhakrishnan, and K. V. Sindhu, “Hydrogeochemical evaluation for developmental activity in part of belma microwatershed, Dakshina Kannada district, Karnataka,” vol. 99, 2021, pp. 853-864.
 
[11]  R. W. Herschy, “Water quality for drinking: WHO guidelines,” Encycl. Earth Sci. Ser., pp. 876-883, 2012.
 
[12]  Bureau of Indian Standards, “Bureau of Indian Standard Drinking Water Specification.,” 2012.
 
[13]  B. M. M. Rajapaksha, R. A. Maithreepala, and H. B. Asanthi, “Water quality and biology of hot springs waters of Mahapelessa, Sri Lanka,” Sci. Res. J., vol. 2, no. 12, pp. 1-6, 2014.
 
[14]  Todd, Hydrology Handbook. 1980.
 
[15]  P. L. Sawyer, C. N., & McCarty, “Chemistry for environmental engineering.,” McGraw-Hill, 1978.
 
[16]  V. Sunitha and Y. Sudharshan Reddy, “Hydrogeochemical evaluation of groundwater in and around Lakkireddipalli and Ramapuram, Y.S.R District, Andhra Pradesh, India,” HydroResearch, vol. 2, no. April 2020, pp. 85-96, 2019.
 
[17]  P. Ravikumar, M. Aneesul Mehmood, and R. K. Somashekar, “Water quality index to determine the surface water quality of Sankey tank and Mallathahalli lake, Bangalore urban district, Karnataka, India,” Appl. Water Sci., vol. 3, no. 1, pp. 247-261, 2013.
 
[18]  S. Krishna Kumar et al., “Evaluation of water quality and hydrogeochemistry of surface and groundwater, Tiruvallur District, Tamil Nadu, India,” Appl. Water Sci., vol. 7, no. 5, pp. 2533-2544, 2017.
 
[19]  V. B. Yannawar, A. B. Bhosle, P. R. Shaikh, and and Surekha R. Gaikwad, “Water Quality of Hot Water Unkeshwar Spring of Maharashtra, India,” Int. J. Innov. Appl. Stud., vol. 3, no. 2, pp. 541-551, 2013.
 
[20]  J. I. Field and J. Webster, “Effects of sulphide on survival of aero-aquatic and aquatic Hyphomycetes.,” Trans. - Br. Mycol. Soc., vol. 85, no. 2, pp. 193-199, 1985.
 
[21]  N. Adimalla, R. Dhakate, A. Kasarla, and A. Kumar, “Groundwater for Sustainable Development Appraisal of groundwater quality for drinking and irrigation purposes in Central Telangana, India,” Groundw. Sustain. Dev., vol. 10, no. 126, p. 100334, 2020.