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R.S. Babcock

Publications and source records attributed to R.S. Babcock.

2 recordsLinked to original sources

Nitrate distributions and source identification in the Abbotsford-Sumas Aquifer, northwestern Washington State

The Abbotsford–Sumas Aquifer is a shallow, predominantly unconfined aquifer that spans regions in southwestern British Columbia, Canada and northwestern Washington, USA. The aquifer is prone to nitrate contamination because of extensive regional agricultural practices. A 22-month ground water nitrate assessment was performed in a 10-km 2 study area adjacent to the international boundary in northwestern Washington to examine nitrate concentrations and nitrogen isotope ratios to characterize local source contributions from up-gradient sources in Canada. Nitrate concentrations in excess of 10 mg nitrate as nitrogen per liter (mg N L −1 ) were observed in ground water from most of the 26 domestic wells sampled in the study area, and in a creek that dissects the study area. The nitrate distribution was characteristic of nonpoint agricultural sources and consistent with the historical documentation of agriculturally related nitrate contamination in many parts of the aquifer. Hydrogeologic information, nitrogen isotope values, and statistical analyses indicated a nitrate concentration stratification in the study area. The highest concentrations (>20 mg N L −1 ) occurred in shallow regions of the aquifer and were linked to local agricultural practices in northwestern Washington. Nitrate concentrations in excess of 10 mg N L −1 deeper in the aquifer (>10 m) were related to agricultural sources in Canada. The identification of two possible sources of ground water nitrate in northwestern Washington adds to the difficulty in assessing and implementing local nutrient management plans for protecting drinking water in the region.

Washington, British Columbia↗

An investigation of the critical liquid-vapor properties of dilute KCl solutions

The three parameters that define the critical point, temperature, pressure, and volume have been experimentally determined by means of filling studies in a platinum-lined system for five KCl solutions ranging from 0.006 to 0.568 m . The platinum-lined vessels were used to overcome the problems with corrosion experienced by earlier workers. The critical temperature ( t c ), pressure ( P c ), and volume ( V c ) were found to fit the equations t c = 374.14   +   16.602 m   +   41.740 m  ± 0.5 ∘ C P c = 220.9   +   135.164 m  +   41.173 m 2   ±   0.5 b a r s V c = 3.155   −   1.373 m   +   0.507 m  ±   0.008 c m 3 − g − 1 "> t c = 374.14 + 16.602 m −−√ + 41.740 m ± 0.5 ∘ C P c = 220.9 + 135.164 m + 41.173 m 2 ± 0.5 b a r s V c = 3.155 − 1.373 m −−√ + 0.507 m ± 0.008 c m 3 − g − 1 tc=374.14 + 16.602m + 41.740m ±0.5∘CPc=220.9 + 135.164m + 41.173m2 ± 0.5barsVc=3.155 − 1.373m + 0.507m ± 0.008cm3−g−1 from infinite dilution to 1.0 m .

Journal of Solution Chemistry↗