U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
 
Background Aqueous Chemistry and Effects of Carbon Dioxide Variations
in Recharge in Shallow Ground Water in a Glacial Outwash Aquifer, Cape Cod,
Massachusetts
by
Roger W. Lee (U.S. Geological Survey, Austin, Texas)
Abstract
Previous geochemical research at the Otis Air Base Site, Cape
Cod, Massachusetts, determined that the principal geochemical
process developing background water chemistry of shallow
ground water is CO2-controlled hydrolysis of sodium feldspars.
Preliminary geochemical modeling, however, demonstrated that
CO2 sources should vary laterally over the project
area. Field analyses of unsaturated zone gases showed variations
in available CO2 for recharge waters. These variations depend
on land use and vegetative cover in the area of ground-water
recharge. On the basis of measurements of CO2 concentrations
in unsaturated-zone gases at 20 sites, CO2 dissolved
in recharge water can range from about 0.035 to 1.000 millimoles
per liter in the project area. The various land-use practices
and local surface features in and around Otis Air Base (residential
subdivisions, golf courses, large cultivated grass fields, kettle
ponds, and woodlands) are associated with variations in the amount
of CO2 in the unsaturated zone.
 
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