American Journal of Water Science and Engineering

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Infiltration Rate of Groundwater in Vadose Zone of Uplifted Carbonate Island

Received: 28 August 2016    Accepted: 13 September 2017    Published: 23 October 2017
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Abstract

Solute contents in the vadose zone of limestone strata on Miyako Island of the Ryukyu Archipelago in Japan were measured by means of electrical conductivities (EC) of the extracted solutions of limestone core samples. A vertically nonuniform distribution of solute content was observed, which should lead to temporal variations of solute concentration in the groundwater under the water table. On the other hand, the data of chloride concentration in groundwater from 13 wells on the island was analyzed to see their long time variations. Both of these two approaches resulted in recharge rates of around 10-7 m s-1 for the vadose zone in the limestone strata of this typical uplifted carbonate island of the western Pacific Ocean.

DOI 10.11648/j.ajwse.20170305.12
Published in American Journal of Water Science and Engineering (Volume 3, Issue 5, September 2017)
Page(s) 61-66
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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

Groundwater, Recharge Rate, Vadose Zone, Limestone, Carbonate Island

References
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[3] K. Mahmud, G. Mariethoz, A. Baker, P. C. Treble, M. Markowska, and E. McGuire, Estimation of deep infiltration in unsaturated limestone environments using cave lidar and drip count data, Hydrol. Earth Syst. Sci., 20, 2016, 359–373.
[4] N. A. Sheffer, M. Cohen, E. Morin, T. Grodek, A. Gimburg, E. Maga, H. Gvirtzman, M. Nied, D. Isele and A. Frumkin, Integrated cave drip monitoring for epikarst recharge estimation in a dry Mediterranean area, Sif Cave, Israel, Hydrol. Process., 25, 2011, 2837–2845.
[5] J. M. U. Jocson, J. W. Jenson and D. N. Contractor, Recharge and aquifer response: Northern Guam Lens Aquifer, Guam, Mariana Islands, Journal of Hydrology, 260, 2002, 231-254.
[6] A. F. Tooth and I. J. Fairchild, Soil and karst aquifer hydrological controls on the geochemical evolution of speleothem-forming drip waters, Crag Cave, southwest Ireland, Journal of Hydrology, 273, 2003, 51–68.
[7] J. E. Mylroie and J. W. Jenson, The carvonate island karst model applied to Guam, Theoretical and Applied Kastology, 13, 2000, 57-61.
[8] D. Taborosi, J. W. Jenson and J. E. Mylroie, Karst features of Guam Mariana Islands, Technical Report No. 104, Water & Environmental Research Institute of the Western Pacific, University of Guam, 2004.
[9] Miyakojima City Office, “FY 2005-2013 Reports on groundwater quality conservation monitoring in Miyakojima City” (in Japanese), 2007-2015.
[10] Y. Arbel, N. Greenbaum, J. Lange and M. Inbar, Infiltration processes and flow rates in developed karst vadose zone using tracers in cave drips, Earth Surf. Process. Landforms 35, 2010, 1682–1693.
[11] H. Furukawa, Quaternary geologic history of the Ryukyu Islands, Bulletin of Science & Engineering Division, University of Ryukyus, 27, 1973, 99-161.
[12] Miyakojima City Office, “FY 2007 Report of Groundwater Conservation Committee of Miyakojima City” (in Japanese), 2008.
[13] K. Kamewada, 1:5 water extraction method for electronic conductivity (in Japanese). In Analytical Methods of Soil Environment, Editorial Committee for Analytical Methods of Soil Environment (ed), Hakuyusha, Tokyo, 1997, 202-204.
[14] H. Sakihama, M. Ishiki and A. Tokuyama, Chemical characteristics of precipitation in Okinawa Island, Japan, Atmospheric Environment, 42, 2008, 2320-2335.
[15] Network Center for EANET, “Data report on the acid deposition in the East Asian region, 2004”, 2005.
[16] S. H. Bottrell and T. C. Atkinson, Tracer study of flow and storage in the unsaturated zone of karstic limestone aquifer. In Tracer Hydrology, H. Hötzl and A. Werner (eds), Balkema, Rotterdam, 1992, 270–277.
[17] Y. Tashiro and K. Takahira, Long term trend of nitrogen emission and nitrogen concentration of groundwater in Miyako Island, Okinawa (in Japanese with English abstract), Journal of Japan Society of Water Environment, 11, 2001, 733-738.
Author Information
  • Faculty of International Studies, Meio University, Okinawa, Japan

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    Yutaka Tashiro. (2017). Infiltration Rate of Groundwater in Vadose Zone of Uplifted Carbonate Island. American Journal of Water Science and Engineering, 3(5), 61-66. https://doi.org/10.11648/j.ajwse.20170305.12

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    Yutaka Tashiro. Infiltration Rate of Groundwater in Vadose Zone of Uplifted Carbonate Island. Am. J. Water Sci. Eng. 2017, 3(5), 61-66. doi: 10.11648/j.ajwse.20170305.12

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    AMA Style

    Yutaka Tashiro. Infiltration Rate of Groundwater in Vadose Zone of Uplifted Carbonate Island. Am J Water Sci Eng. 2017;3(5):61-66. doi: 10.11648/j.ajwse.20170305.12

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  • @article{10.11648/j.ajwse.20170305.12,
      author = {Yutaka Tashiro},
      title = {Infiltration Rate of Groundwater in Vadose Zone of Uplifted Carbonate Island},
      journal = {American Journal of Water Science and Engineering},
      volume = {3},
      number = {5},
      pages = {61-66},
      doi = {10.11648/j.ajwse.20170305.12},
      url = {https://doi.org/10.11648/j.ajwse.20170305.12},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.ajwse.20170305.12},
      abstract = {Solute contents in the vadose zone of limestone strata on Miyako Island of the Ryukyu Archipelago in Japan were measured by means of electrical conductivities (EC) of the extracted solutions of limestone core samples. A vertically nonuniform distribution of solute content was observed, which should lead to temporal variations of solute concentration in the groundwater under the water table. On the other hand, the data of chloride concentration in groundwater from 13 wells on the island was analyzed to see their long time variations. Both of these two approaches resulted in recharge rates of around 10-7 m s-1 for the vadose zone in the limestone strata of this typical uplifted carbonate island of the western Pacific Ocean.},
     year = {2017}
    }
    

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    AB  - Solute contents in the vadose zone of limestone strata on Miyako Island of the Ryukyu Archipelago in Japan were measured by means of electrical conductivities (EC) of the extracted solutions of limestone core samples. A vertically nonuniform distribution of solute content was observed, which should lead to temporal variations of solute concentration in the groundwater under the water table. On the other hand, the data of chloride concentration in groundwater from 13 wells on the island was analyzed to see their long time variations. Both of these two approaches resulted in recharge rates of around 10-7 m s-1 for the vadose zone in the limestone strata of this typical uplifted carbonate island of the western Pacific Ocean.
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