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Time series analyses of hydrological parameter variations and their correlations at a coastal area in Busan,South Korea
Authors:Sang Yong Chung  Venkatramanan Senapathi  Selvam Sekar  Tae Hyung Kim
Affiliation:1.Department of Earth & Environmental Sciences,Pukyong National University,Busan,South Korea;2.Department for Management of Science and Technology Development,Ton Duc Thang University,Ho Chi Minh City,Vietnam;3.Faculty of Applied Sciences,Ton Duc Thang University,Ho Chi Minh City,Vietnam;4.Department of Geology,V. O Chidambaram College,Tamil Nadu,India;5.Local Values Research Team,Jeju Province Development Corporation,Jeju,South Korea
Abstract:Monitoring and time-series analysis of the hydrological parameters electrical conductivity (EC), water pressure, precipitation and tide were carried out, to understand the characteristics of the parameter variations and their correlations at a coastal area in Busan, South Korea. The monitoring data were collected at a sharp interface between freshwater and saline water at the depth of 25 m below ground. Two well-logging profiles showed that seawater intrusion has largely expanded (progressed inland), and has greatly affected the groundwater quality in a coastal aquifer of tuffaceous sedimentary rock over a 9-year period. According to the time series analyses, the periodograms of the hydrological parameters present very similar trends to the power spectral densities (PSD) of the hydrological parameters. Autocorrelation functions (ACF) and partial autocorrelation functions (PACF) of the hydrological parameters were produced to evaluate their self-correlations. The ACFs of all hydrologic parameters showed very good correlation over the entire time lag, but the PACF revealed that the correlations were good only at time lag 1. Crosscorrelation functions (CCF) were used to evaluate the correlations between the hydrological parameters and the characteristics of seawater intrusion in the coastal aquifer system. The CCFs showed that EC had a close relationship with water pressure and precipitation rather than tide. The CCFs of water pressure with tide and precipitation were in inverse proportion, and the CCF of water pressure with precipitation was larger than that with tide.
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