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Jaclyn Gehring and colleagues at Union College recently used distinctive changes in the stable isotopes (oxygen) in river water to determine rates of groundwater recharge from the River to the Schenectady well field [7]. He thought production was high because it has been very dry and people are watering their lawns, filling pools, and continueing with other warm-weather activities that demand water. He also noted that some of the water from the Glenville well field goes to the towns of Ballston and Clifton Park. Also, the river near Schenectady is lowered about 22 inches during the winter by removing boards from the top of the Lock 7 dam. The agreement was to address the plume at its source, but a considerable amount of the TCE had left the site and is traveling southeast to the Mohawk. The GSA (Navy) spent $15 m remediating the plume at the source [5]. The aquifer was originally deposited by an earlier version of the Mohawk River and now it relies on the River for a major fraction of its recharge. The operation of the locks and dams of the Erie Canal in this area result in a full-pool setting in the navigation season (May to November) where connection with the aquifer and recharge are significant. The first serendipitous \u201Cexperiment\u201D was between April and June of 1953 when weekly samples showed it took about 48 days for the radioactive water to show up in the well. The second experiment was in 1961 when the initial peak of tritium in river water of the Mohawk occurred on 25 September, and this tritiated water was then measured in the Schenectady wells by about 9 October, a transit time of 18 days [2]. These results likely indicate that movement occurs in discreet layers in the aquifer at different velocities with the upper layers thought to have the fastest transit times. In early June 2020 they pumped a record daily maximum of 4.9 million gallons a day (mgd), which is the highest they\u2019ve ever produced, and well above their average annual daily mean of ~2 mgd [14]. In early June 2020 they pumped a record daily maximum of 4.9 million gallons a day (mgd), which is the highest they’ve ever produced, and well above their average annual daily mean of ~2 mgd [14]. and Finch, A.J., 1982. We need to do everything possible to keep these contaminants out of our well water, and considerable work has gone into doing just that.Over 50 years ago, radioactive tritium from tests of thermonuclear devices resulted in fallout in the Schenectady area, and significant pulses of radioactive tritium (3H in H2O) could be measured in the river and then later in water of the Schenectady well field [2].