Abstract
Groundwater fluctuation usually reflects the property of aquifer in nature. Actually, water level change can be caused not only by barometric pressure changes resulted from atmospheric motion, but also by the tidal effect from nearby marine system or water body. In confined aquifer, an increase in barometric pressure usually will cause a decrease in water level in well to an amount described by the barometric efficiency. The barometric efficiency can be also used as a correction factor to remove barometric effects on water levels in wells during an aquifer test. With the rise of the tidal sea on the coastal aquifer, it indicates that there will be compensating increases of water pressure and stress in the skeleton of aquifer. External forcing on groundwater level in the coastal aquifer, such as barometric effect and tidal sea, usually affect the water level to fluctuate with different phases to some extent. An adaptive adjustment to remove the combination of barometric and oceanic tidal efficiency is presented in this study. This research suggests that the presented formula can simultaneously identify the individual efficiency for barometric effect and load of tidal sea considering their combined observation of groundwater level in aquifer system. An innovative application has been demonstrated for the deep aquifers adjacent to the West Pacific Ocean.
Similar content being viewed by others
References
Batu, V. (1998). Aquifer hydraulics: a comprehensive guide to hydrogeologic data analysis. New York: Wiley.
Bredehoeft, J. D. (1967). Response of well-aquifer systems to Earth tides. Journal of Geophysical Research, 72(12), 3075–3087.
Freeze, R. A., & Cherry, J. A. (1979). Groundwater (pp. 29–60). New Jersey: Prentice Hall.
Gregg, D. O. (1966). An analysis of ground-water fluctuations caused by ocean tides in Glynn County, Georgia. Ground Water, 4(3), 24–32.
Halford, K. J. (2006) Documentation of a spreadsheet for time-series analysis and drawdown estimation. US Geological Survey Scientific Investigations Report 2006–5024.
Ho, C. S. (1982) Tectonic evolution of Taiwan. Republic of China, Taipei, Taiwan: The Ministry of Economic Affairs.
Hsieh, P. A., Bredehoeft, J. D., & Farr, J. M. (1987). Determination of aquifer transmissivity from Earth tide analysis. Water Resources Research, 23(10), 1824–1832.
Jacob, C. E. (1940). On the flow of water in an elastic artesian aquifer. EOS Trans. AGU, 21(2), 574–586.
Kruseman, G. P., & de Ridder, N. A. (1991). Analysis and evaluation of pumping test data, 2nd ed. ILRI Publication No. 47. The Netherlands: International Institute for Land Reclamation and Improvement.
Quilty, E. G., & Roeloffs, E. A. (1991). Removal of barometric pressure response from water level data. Journal of Geophysical Research, 96(B6), 10209–10218.
Rasmussen, T. C., & Crawford, L. A. (1997). Identifying and removing barometric pressure effects in confined and unconfined aquifers. Ground Water, 35(3), 502–511.
Robinson, E. S., & Bell, R. T. (1971). Tides in confined well-aquifer systems. Journal of Geophysical Research, 76(8), 1857–1869.
Shih, D. C. F. (2009). Storage in a confined aquifer: spectral analysis of groundwater responses to seismic Rayleigh waves. Journal of Hydrology, 374, 83–91.
Shih, D. C. F. (2017a). Groundwater storage inferred from earthquake activities around East Asia and West Pacific Ocean. Journal of Hydrology, 544, 363–372.
Shih, D. C. F. (2017b). Hydraulic diffusivity in a coastal aquifer: spectral analysis of groundwater level in responses to marine system. Stochastic Environmental Research and Risk Assessment, 32, 311–320.
Shih, D. C. F., Chiou, K. F., Lee, C. D., & Wang, I. S. (1999). Spectral responses of water level in groundwater and tidal river. Hydrological Processes, 13, 889–911.
Shih, D. C. F., & Lin, G. F. (2002). Spectral analysis of water level in aquifers. Stochastic Environmental Research and Risk Assessment, 16, 374–398.
Shih, D. C. F., & Lin, G. F. (2004). Application of spectral analysis to determine hydraulic diffusivity of a sandy aquifer (Pingtung County, Taiwan). Hydrological Processes, 18, 1655–1669.
Shih, D. C. F., Lin, G. F., Wu, Y. M., Jia, Y. P., & Chen, Y. G. (2008). Spectral decomposition of periodic ground water fluctuation in a coastal aquifer. Hydrological Processes, 22, 1755–1765.
Shih, D. C. F., Wu, Y. M., & Chang, C. H. (2013). Significant coherence for groundwater and Rayleigh waves: evidence in spectral response of groundwater level in Taiwan using 2011 Tohoku earthquake, Japan. Journal of Hydrology, 486, 57–70.
Todd, D. K. (1980). Groundwater hydrology (2nd ed.). New York: Wiley.
Toll, N. J., & Rasmussen, T. C. (2007). Removal of barometric pressure effects and Earth tides from observed water levels. Ground Water, 45(1), 101–105.
Wenzel, H. G. (1996). The nanogal software: earth tide data processing package ETERNA 3.30. Bulletin d’Informations Mareés Terrestres, 124, 9425–9439.
Zaske, J., Zurn, W., & Wulhelm, H. (2000). NDFW Analysis of borehole water level data from the Hot-Dry-Rock test sites Soultz-sous-Forets. Bull. d’Information Mareés Terrestres, 132, 10241–10269.
Zeumann, S., Weise, A., & Jahr, T. (2009). Tidal and non-tidal signals in groundwater boreholes in the KTB area, Germany. Journal of Geodynamics, 48(3–5), 115–119.
Acknowledgments
The author thanks the Central Weather Bureau of Taiwan for providing useful data to complete this research.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Shih, D.CF. Identification of Individual Efficiency for Barometric Pressure and Ocean Tide Load Simultaneously Acted on Deep Aquifers Adjacent to the West Pacific Ocean. Pure Appl. Geophys. 175, 4643–4654 (2018). https://doi.org/10.1007/s00024-018-1905-y
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00024-018-1905-y