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<br />e <br /> <br />e <br /> <br />e <br /> <br />Correlation analysis was performed to determine the <br />statistical relationships of water elevations at different <br />stations to each other and the probability that these <br />relationships were due to chance. The analysis is presented in <br />Table 1 and indicates that a number of very high and significant <br />correlations exist between stations. In many instances staff <br />gauges have similar correlation coefficients with groundwater <br />monitoring wells as with other staff gauges. Thus, the <br />groundwater levels in most wells appear completely connected with <br />the stream, and stream levels determine groundwater levels. <br /> <br />Table 1. Pearson product moment correlation coefficients (r) for <br />all stations. N-2=48. Significance, *=<.05; **=<.01; ***=<.001; <br />ns=not significant. <br /> <br />8 <br />1 <br />.89*** <br />.51*** <br />.68*** <br />3 <br />.92*** <br />.49*** <br />.56*** <br />sg1 <br />.83*** <br />5 <br /> <br />1 2 3 4 sq2 <br />9 10 11 sq1 <br />.64*** .80*** .57*** .86*** <br />.83*** .93*** .24ns .95*** 2 <br />.79*** .59*** .76*** <br /> <br />.86*** .93*** <br />.86*** .83*** <br />.75*** .77*** .66*** <br /> <br />5 <br /> <br />6 <br /> <br />7 <br /> <br />s~ <br /> <br />.88*** .65*** <br />.48*** .81*** 4 <br />.51*** .81*** <br /> <br />.93*** <br /> <br />.81*** <br /> <br />.89*** .90*** <br />.81*** <br /> <br />.84*** .72*** .69*** <br /> <br />.79*** <br /> <br />.92*** <br /> <br />.70*** .82*** .26ns .88*** <br /> <br />6 <br />.94*** .87*** .90*** .50*** .86*** 7 <br /> <br />.86*** <br /> <br />sg3 <br />.87*** .74*** .89*** .27ns .95*** <br />8 <br />.95*** .95*** .45*** .89*** <br /> <br />9 <br /> <br />.92*** .48*** .81*** <br /> <br />10 <br /> <br />.39** .96*** <br /> <br />11 <br /> <br />.29* <br /> <br />Two wells, 5 and 7, were dry most of the year because they <br /> <br />13 <br />