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A Comparative Study of Water Quality Between Hot Spring and Borehole Waters of Mara, Shinyanga and Manyara Regions of Tanzania

Received: 25 September 2019    Accepted: 11 October 2019    Published: 23 October 2019
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Abstract

This study conducted for the comparison of physico-chemical parameters between hot springs and borehole waters. Fourteen samples were collected at Mara, Shinyanga and Manyara in Tanzania. Multimeter used for the analysis of physical parameters pH, EC, TDS, salinity and turbidity. Titrimetric methods were used for the determination of Cl-, total hardness, Ca2+ and Mg2+. UV-Vis. Spectrophotometric method for NO3-, SO42-, F-, Fe2+ and Mn2+ and Flame Atomic Absorption Spectrometer for Cd2+, Zn2+, Ni2+, Cu2+ and K+. The EC, TDS, salinity, turbidity, Cl-, NO3-, SO42-, F-, Mn2+ and Cu2+ are higher (pH = 7.44-9.42, EC = 4251.33-15334 µS/cm, TDS = 2079-7526.7 mg/L, salinity = 2.2-8.67 ppt, Cl- = 189.3-3577.6 mg/L, SO42- = 11.83-1353.33 mg/L, F- = 4.68-18 mg/L, Mn2+ = 1.03-2.0 mg/L, Cd2+ = 0.01-0.05 mg/L, Cu2+ = 0.37-0.93 mg/L and K+ = 44-100 mg/L) in hot springs than borehole waters (pH = 6.36-6.58, EC = 270.0-2674.64 µS/cm, TDS = 123.67-1305 mg/L, salinity = 0.03-1.37 ppt, Cl- = 6.25-659.93 mg/L, SO42- = 28.92-493.33 mg/L, F- = 0.89-3.0 mg/L, Mn2+ = 0.3-1.70 mg/L Cd2+ = 0 mg/L, Cu2+ = 0.49-0.64 mg/L and K+ = 16-52 mg/L). The t-test at the probability 0.05 showed that there is significant difference of the parameters pH and Ni2+ between hot spring and borehole waters. Some of the parameters are at higher levels than permissible values for both hot spring and borehole waters. Therefore, there is a need of treatment for these waters before using for domestic purpose.

DOI 10.11648/j.sjc.20190704.13
Published in Science Journal of Chemistry (Volume 7, Issue 4, August 2019)
Page(s) 82-89
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Hot Spring Water, Borehole Water, Physico-chemical Parameters, Titrimetry, Spectrophotometry, FAAS

References
[1] Okoro, N., Omeje, E. O., and Osadebe, P. O. Comparative analysis of three borehole water sources in Nsukka urban area, Enugu state, Nigeria, Resour. and Environ, 2017, 7 (4): 110–114.
[2] Futakamba, M., Water Sector Development Programme, Status report, Dar es salaam: Tanzania, 2016.
[3] Rubhera, R. A. M. M., Groundwater quality degradation due to salt water intrusion in Zanzibar municipality, African J. Environ. Sci. Technol., 2014, 9 (9): 734–740.
[4] Jana, O., and Jonker, N., Optimal utilisation of thermal springs, Water Research Commission, Gezina, South Africa, WRC Report No. TT 577/13, 2013.
[5] Kifua, G., Reconnaissance of geothermal resources, Dar es salaam, Tanzania, 1958.
[6] Mnzava, L. J., and Mayo, A. W., Geochemical investigation of geothermal power potential exploration of hot springs in South-western Tanzania, Int. J. Water Resour. and Environ. Eng., 2013, 5 (10): 597–607.
[7] Nancy, J. M. M., Water supply in Tanzania and performance of local plant materials in purification of turbid water, Ph. D. Thesis, Royal Institute of Technology, Stockholm, Sweden, 2008.
[8] Chaurasia, N., Pandey, S. K., and Devendra, M., Determination of arsenic content in the water and blood samples of Ballia region using hydride generation atomic absorption spectrophotometer, Res. J. Forensic Sci., 2013, 1 (4): 1–3.
[9] Kamil, E., Gwen, H., David, B., and Walter, B., Thermal characteristics of the Chena hot springs Alaska geothermal system,” in Thirty-Second Workshop on Geothermal Reservoir Engineering, Stanford University, California, 2007, 1–8.
[10] Toure, A., Wenbiao, D., and Keita, Z., Comparative study of the physico-chemical quality of water from wells, boreholes and rivers consumed in the commune of pelengana of the region of Segou in Mali, Environ. Sci., 2017, 13 (6): 1–13.
[11] Alhibshi, E., Albriky, K., and Bushita, A., Concentration of heavy metals in underground water wells in Gharian district, Libya, Int. Conf. Agric. Ecol. Med. Sci., Indonesia, 2014, 35-39.
[12] Korkmaz, N., and Gunduz, M., and Asik, S., Temporal and spatial variation of groundwater level and salinity: A case study in the irrigated area of Menemen plain in western Turkey, Hungarian Agric. Eng., 2015, DOI: 10.17676/HAE.2015.28.39, 39–43.
[13] Sayyed, J. A., and Bhosle, A. B., Analysis of chloride, sodium and potassium in groundwater samples of Nanded city in Mahabharata, India, Euro. J. Exp. Bio., 2011, 1 (1): 74–82.
[14] Heston, D., Total carbonate hardness in Cumberland valley groundwater, M. Sc. Thesis, A Shippensburg University, 2015, USA, 1–22.
[15] Hollocher, T. C., and Kristjansson, J. K., Thermophilic denitrifying bacteria: A survey of hot springs in South-western Iceland, FEMS Microbiol. Lett., 1992, 101 (2): 113–119.
[16] Tiwari, P., Water quality assesment for drinking and irrigation purpose, Indian J. Sci. Res., 2017, 13 (2): 140–142.
[17] Prakash, P., Gupta, B. K., and Ahmad, M. F., Characteristics of hot water springs in a region of Rishikund Munger district of Bihar State, India, Int. Res. J. Environ. Sci., 2017, 6 (10): 15–21.
[18] Hodder, P. W., Geothermal Waters as a source of energy and metals, University of Waikato: New Zealand, 2010.
[19] Mohammad, A. Z., Reza, S., and Laleh, R. K., Calculating fluoride concentrations data using ambient temperatures in drinking water distribution networks in select provinces of Iran, Data in Brief, 2017, 12: 127–132.
[20] Berhanu, G., Excessive fluoride concentration in the Ethiopian rift and the flowered project, 2017, EU H2020 Project, 1–53.
[21] Gautam, R., and Bhardwaj, N., Fluoride accumulation in milk samples of domestic animals of Nawa Tehsil in Nagaur district (Rajasthan), The Ecoscan, 2009, 3 (3 & 4): 325–326.
[22] Battaleb, L. S., Moore, S., A study of fluoride groundwater occurrence in Posht-e-Kooh-e-Dashtestan, South of Iran, World Appl. Sci. J., 2010, 8 (11): 1317–1321.
[23] Choubisa, S. L., Mishra, G. V., Zulfiya, S., Bhardwaj, B., Mali, p., and Jaroli, V. J., Food, fluoride and fluorosis in domestic ruminants in the Dungarpur district of Rajasthan, India, Research Report Fluoride, 2011, 44 (2): 70-76.
[24] Bruce, I. D., Drinking water: Iron and Manganese, Nebguide., University of Nebraska-Lincoln, USA, 2014, 1–4.
[25] Baytak, S., Turker, A. R., Determination of chromium, cadmium and manganese in water and fish samples after preconcentration using penicillium digitatum immobilized on Pumice stone, clean, 2009, 37 (4-5): 314–318.
[26] Festo, H., Ngowi, A. V., Ohanianr, E. Y., and Magara, E., Cadmium in drinking water, WHO Guideline Drink. Water Qual., 2011, 3 (4): 60–116.
[27] Dutta, D., and Sarma, H. P., Copper (Cu), Zinc (Zn) and Cadmium (Cd) contamination of groundwater in Dikrong river basin, Paumpare district, Arunachal Pradesh, India, IOSR J. Environ. Sci. Toxicol. and Food Technol., 2015, 9 (10): 20-23.
[28] Srikanth, R., Rao, A. M., Kumar, Ch. S., and Khanum, A., Lead, cadmium, nickel, and zinc contamination of ground-water around Hussain sagar lake, Hyderabad, India, Bull. Environ. Contam. and Toxicol., 1993, 50 (1): 138–143.
[29] Fernanda, T., Maria das, G., Mota, M., and Antonelle, T., Management of contact determatitis due to nickel allergy: An update, Clin. Cosmet. Investig. Dermatology., 2009, 2: 39–48.
[30] Cotruvo, J., Giddings, E., Jackson, P., Magara, Y., and Ohanian, Y., Nickel in drinking water, WHO guidelines for Drinking Water Quality, 2005, 1–29.
[31] Toft, P., Magara, Y., and Jackson, P., Copper in drinking water. WHO guidelines for drinking water quality, 2004, 1-31.
[32] Aiwerasia, V. F. N., Ohanian, E., Potassium in drinking water, WHO guidelines for drinking water quality, 2009, 1-12.
Author Information
  • The Department of Chemistry, The University of Dodoma, Dodoma, Tanzania

  • The Department of Chemistry, The University of Dodoma, Dodoma, Tanzania

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    Samwel Alfred Maseke, Maheswara Rao Vegi. (2019). A Comparative Study of Water Quality Between Hot Spring and Borehole Waters of Mara, Shinyanga and Manyara Regions of Tanzania. Science Journal of Chemistry, 7(4), 82-89. https://doi.org/10.11648/j.sjc.20190704.13

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    Samwel Alfred Maseke; Maheswara Rao Vegi. A Comparative Study of Water Quality Between Hot Spring and Borehole Waters of Mara, Shinyanga and Manyara Regions of Tanzania. Sci. J. Chem. 2019, 7(4), 82-89. doi: 10.11648/j.sjc.20190704.13

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    AMA Style

    Samwel Alfred Maseke, Maheswara Rao Vegi. A Comparative Study of Water Quality Between Hot Spring and Borehole Waters of Mara, Shinyanga and Manyara Regions of Tanzania. Sci J Chem. 2019;7(4):82-89. doi: 10.11648/j.sjc.20190704.13

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  • @article{10.11648/j.sjc.20190704.13,
      author = {Samwel Alfred Maseke and Maheswara Rao Vegi},
      title = {A Comparative Study of Water Quality Between Hot Spring and Borehole Waters of Mara, Shinyanga and Manyara Regions of Tanzania},
      journal = {Science Journal of Chemistry},
      volume = {7},
      number = {4},
      pages = {82-89},
      doi = {10.11648/j.sjc.20190704.13},
      url = {https://doi.org/10.11648/j.sjc.20190704.13},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.sjc.20190704.13},
      abstract = {This study conducted for the comparison of physico-chemical parameters between hot springs and borehole waters. Fourteen samples were collected at Mara, Shinyanga and Manyara in Tanzania. Multimeter used for the analysis of physical parameters pH, EC, TDS, salinity and turbidity. Titrimetric methods were used for the determination of Cl-, total hardness, Ca2+ and Mg2+. UV-Vis. Spectrophotometric method for NO3-, SO42-, F-, Fe2+ and Mn2+ and Flame Atomic Absorption Spectrometer for Cd2+, Zn2+, Ni2+, Cu2+ and K+. The EC, TDS, salinity, turbidity, Cl-, NO3-, SO42-, F-, Mn2+ and Cu2+ are higher (pH = 7.44-9.42, EC = 4251.33-15334 µS/cm, TDS = 2079-7526.7 mg/L, salinity = 2.2-8.67 ppt, Cl- = 189.3-3577.6 mg/L, SO42- = 11.83-1353.33 mg/L, F- = 4.68-18 mg/L, Mn2+ = 1.03-2.0 mg/L, Cd2+ = 0.01-0.05 mg/L, Cu2+ = 0.37-0.93 mg/L and K+ = 44-100 mg/L) in hot springs than borehole waters (pH = 6.36-6.58, EC = 270.0-2674.64 µS/cm, TDS = 123.67-1305 mg/L, salinity = 0.03-1.37 ppt, Cl- = 6.25-659.93 mg/L, SO42- = 28.92-493.33 mg/L, F- = 0.89-3.0 mg/L, Mn2+ = 0.3-1.70 mg/L Cd2+ = 0 mg/L, Cu2+ = 0.49-0.64 mg/L and K+ = 16-52 mg/L). The t-test at the probability 0.05 showed that there is significant difference of the parameters pH and Ni2+ between hot spring and borehole waters. Some of the parameters are at higher levels than permissible values for both hot spring and borehole waters. Therefore, there is a need of treatment for these waters before using for domestic purpose.},
     year = {2019}
    }
    

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  • TY  - JOUR
    T1  - A Comparative Study of Water Quality Between Hot Spring and Borehole Waters of Mara, Shinyanga and Manyara Regions of Tanzania
    AU  - Samwel Alfred Maseke
    AU  - Maheswara Rao Vegi
    Y1  - 2019/10/23
    PY  - 2019
    N1  - https://doi.org/10.11648/j.sjc.20190704.13
    DO  - 10.11648/j.sjc.20190704.13
    T2  - Science Journal of Chemistry
    JF  - Science Journal of Chemistry
    JO  - Science Journal of Chemistry
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    EP  - 89
    PB  - Science Publishing Group
    SN  - 2330-099X
    UR  - https://doi.org/10.11648/j.sjc.20190704.13
    AB  - This study conducted for the comparison of physico-chemical parameters between hot springs and borehole waters. Fourteen samples were collected at Mara, Shinyanga and Manyara in Tanzania. Multimeter used for the analysis of physical parameters pH, EC, TDS, salinity and turbidity. Titrimetric methods were used for the determination of Cl-, total hardness, Ca2+ and Mg2+. UV-Vis. Spectrophotometric method for NO3-, SO42-, F-, Fe2+ and Mn2+ and Flame Atomic Absorption Spectrometer for Cd2+, Zn2+, Ni2+, Cu2+ and K+. The EC, TDS, salinity, turbidity, Cl-, NO3-, SO42-, F-, Mn2+ and Cu2+ are higher (pH = 7.44-9.42, EC = 4251.33-15334 µS/cm, TDS = 2079-7526.7 mg/L, salinity = 2.2-8.67 ppt, Cl- = 189.3-3577.6 mg/L, SO42- = 11.83-1353.33 mg/L, F- = 4.68-18 mg/L, Mn2+ = 1.03-2.0 mg/L, Cd2+ = 0.01-0.05 mg/L, Cu2+ = 0.37-0.93 mg/L and K+ = 44-100 mg/L) in hot springs than borehole waters (pH = 6.36-6.58, EC = 270.0-2674.64 µS/cm, TDS = 123.67-1305 mg/L, salinity = 0.03-1.37 ppt, Cl- = 6.25-659.93 mg/L, SO42- = 28.92-493.33 mg/L, F- = 0.89-3.0 mg/L, Mn2+ = 0.3-1.70 mg/L Cd2+ = 0 mg/L, Cu2+ = 0.49-0.64 mg/L and K+ = 16-52 mg/L). The t-test at the probability 0.05 showed that there is significant difference of the parameters pH and Ni2+ between hot spring and borehole waters. Some of the parameters are at higher levels than permissible values for both hot spring and borehole waters. Therefore, there is a need of treatment for these waters before using for domestic purpose.
    VL  - 7
    IS  - 4
    ER  - 

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