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6 <br /> Ground-Water Levels <br /> Ground-water levels measured in the shallow wells were generally stable throughout the six-year <br /> monitoring period, typically fluctuating three feet or less during this time. Ground-water elevations <br /> in the shallow zone have ranged from approximately 76 feet MSL in the southeast portion of the <br /> monitoring network area to 87 feet MSL to the northwest. The lowest ground-water levels in the <br /> shallow network wells have been observed generally during the late spring to summer, with recovery <br /> by late fall (Figure 2). Between 1995 and late 1998, ground-water levels beneath the eastern portion <br /> of the monitored area rose very gradually (approximately three feet), as seen in wells 4S/6E-5A1 and <br /> 4S/6E-6A1 (see Figure 2) and in the Koster well (see Appendix). Ground-water levels beneath the <br /> northern portion of the area began rising somewhat later, in late 1996. During 1999, ground-water <br /> levels beneath the area declined approximately three feet. Ground-water depths and elevations- <br /> measured <br /> levationsmeasured in all wells during each quarter of the monitoring period are presented in <br /> Table 1. <br /> In comparison to the'shallow wells, ground-water levels in the deep wells were deeper and fluctuated <br /> more throughout the last six years, presumably in response to pumping of those and/or other nearby <br /> deep wells during that time. The static water levels in the Petz irrigation well fluctuated seasonally <br /> approximately 5 to 10 feet, with the lowest observed levels during the fall and highest levels in the <br /> winter (Figure 3), until 1998 when water levels stabilized at approximately the same level as the <br /> shallow wells. Water levels in the Petz well also declined during 1999 by approximately five feet. <br /> Static water levels in the South Tracy#1 production well fluctuated seasonally less than 40 feet <br /> r-, during 1994 through 1997 (Figure 4); since then, the static levels have been slightly higher and <br /> pumping levels (during summer and fall) have been sufficiently low that such measurement was not <br /> possible. <br /> Static water levels have been measured in the Brown's#1 production well since January 1995 <br /> (during the beginning of'1994, water levels could not be measured because the well was being <br /> © LUHDURFF & SCALMANINI <br /> CONSULTING ENGINMFRS <br />