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Report: Groundwater-quality Monitoring—January 26,2004: 7500 West Eleventh Street, Tracy, CA. Page 14 <br /> plus that in the pores of the filter in the annular space between the casing and the wall of <br /> the 8-in. diameter boring. <br /> Since no measurable quantity of LNAPL flowed into the well over the 7-day period <br /> between November 15 and November 22, it is clear that the 0.5$ ft. of free product found <br /> on November 8, 2003 had accumulated in the well at an extremely slow rate. Thus, by <br /> corollary, it is reasonable to estimate that only a de minimus volume of LNAPL entered <br /> the well over the 14-day period between November 8 and November 22, when <br /> groundwater in the well was found to be essentially free of LNAPL. This indicates that <br /> the total volume of floating product removed from the well by the three purgings that <br /> occurred over that period had a total volume close to that calculated above (i.e., 0.52 . <br /> gal.). That estimate is compatible with the field reports made by SJC staff, which indicate <br /> that on each of the first two purgings, LNAPL having a total volume of very much less <br /> than 1 gallon was recovered from the well and none was recovered at the time of the third <br /> Even a one month delay from the third to fourth purging yielded no measurable <br /> purging. <br /> s thickness of floating product and less than one ounce of recovered LNAPL. <br /> The tiny volume of LNAPL that it was possible to recover from Well MW-7 <br /> Monitoring <br /> on first <br /> over period from November 8, 2003 to March 30, ?004 beee Table 3) might, <br /> generated by comparing the <br /> inspection, be difficult to explain. This difficulty mightg <br /> facts about the plume of floating product that are currently known and the small volume <br /> ., w the <br /> of LNAPL recovered from that well in the cited period.duct mithout neel ht actually presg to ent n the <br /> precise magnitude of the volume of floating as originally ally released on the other side of West <br /> subsurface, it is clear that the <br /> LNAPL gradient from MW-7 had reached that <br /> Eleventh Street at a distance of some 24 . B up of <br /> �= ter than April 11, 2002• Based on the measurements tluckne�esss rssthe <br /> location by no la <br /> 2003 SJC estimates that the a Inc 2003a). It is, <br /> 'v LNAPL in that well on November 8, SThe San Joaquin Comp Y <br /> product present in the <br /> surrounding Formation was some 0.33 fl volume order of several thousand , <br /> therefore, reasonable to conclude that imeat d to be on the og itand <br /> ude <br /> subsurface, which volume has been eSt is likely to be orders of mage <br /> Joaquin Company lnc• 2003a), before no <br /> The San Joaq Product purged from the MW-7 <br /> ,,, gallons ( gallonage of p when the soil mass <br /> .� greater than the fractional g could be measured in it. However, <br /> �` measurable thickness of LNAPLuantit <br /> s scalar effects and very limited extent <br /> the the a uency <br /> properties, drilling effects, the apparent diverge <br /> generated around the well aredh edmight be estimated based on the area in which it <br /> aced to the relatively minute quantity of LNAPL <br /> Of floating product in the subsurface comp is not as <br /> is known to have been present er resent on the water table in the well casing <br /> removed before it <br /> was doe longer <br /> incongruous as it might <br /> the two volumes illustrates the sigm -spTeadifficulties plumeis <br /> between from a widep <br /> The apparent divergence b product fr <br /> that may be encountered when removal of floating <br /> attempted by skimm1ng p <br /> roduct from the water table in asmall-diameter well. <br /> 1. SJC <br /> SJC <br /> T. <br /> Y <br />�y <br /> SJC <br />