Laserfiche WebLink
'd s •� a � z a + � <br /> 3 s O w a d <br /> Date U a U z <br /> 1 d <br /> 2 dry <br /> 3 dry <br /> 9/8/2008 4 79.1 1 39.41 51.21 3.21 280.61 85.0 1 55.0 1 25.1 230.0 9.5 9.9 <br /> 5 160.6 1 77.2 66.6 4.2 768.6 1 60.0 1 55.1 1 14.1 630.0 17.4 16.4 <br /> 6 dry <br /> 1 dry <br /> 2 dry <br /> 10/14/2008 3 d <br /> 4 68.6 44.1 66.3 4.0 337.9 104.0 104.0 20.6 277.0 10.0 12.1 <br /> 5 154.0 84.6 64.7 4.4 666.1 98.0 62.1 12.8 546.0 17.6 15.9 <br /> 6 d <br /> 1M50.5 <br /> 54.5 2.5 167.1 67.0 96.7 46.0 137.0 10.4 9.9 <br /> 2 41.6 1.7 335.5 25.0 53.9 31.0 275.0 8.5 9.5 <br /> 3/30/2009 3 87.1 2.5 793.0 37.0 77.8 83.3 650.0 19.2 21.6 <br /> 4 67.4 1.7 305.0 80.0 67.9 26.4 250.0 9.8 10.6 <br /> 5 84.8 2.5 976.0 68.0 43.6 10.9 800.0 16.5 19.6 <br /> 6 65.2 2.9 524.6 87.0 53.5 18.4 430.0 12.8 13.5 <br /> 1 dry <br /> 2 dry <br /> 6/29/2009 3 ry d <br /> 4 53.8 44.3 65.4 1.4 372.1 66.5 70.5 18.9 305.0 9.2 10.8 <br /> 5 118.0 66.6 91.6 2.2 785.7 66.5 72.0 8.7 644.0 15.4 16.9 <br /> 6 1 88.6 51.4 52.6 2.4 518.5 72.6 53.4 8.0 425.0 11.0 12.2 <br /> Wells 2 and 4 are background wells for this site. Well 1 was previously assumed to be <br /> out of the zone of influence of the wastewater, but gradient analyses indicate that it could <br /> be affected by wastewater placed in its vicinity. Thus wells 1, 3, 5, and 6 are all, to some <br /> extent, in positions to reveal to what extent, if any, the uppermost aquifer records the <br /> effect of the wastewater application. Compared to well 4, wells 5 and 6 have higher <br /> solute loads and this is mostly due to a relative increase in bicarbonate alkalinity, <br /> calcium, and magnesium. The most likely source of these ions is the vadose zone matrix <br /> where they would be liberated as the soil buffers the acidification attendant on organic <br /> decomposition. <br />