A USGS scientist prepares a tracer solution in a gas-tight bladder that will be pumped into a zone of nitrate-containing groundwater to monitor the production and consumption of nitric oxide dissolved in groundwater. USGS scientists and their colleagues have developed a method to measure the rates at which inorganic nitrogen compounds, such as nitrate and nitrite, transform in groundwater.
|
Single-well tracer tests involve injecting a tracer solution into one port of a multilevel sampling well, creating a tracer cloud in the groundwater, and then monitoring the water chemistry in the tracer cloud from the same well as the tracer cloud moves away from the well. Single-well tracer tests can be used to measure chemical reactions in the subsurface such as measuring how nitrogen transforms in groundwater.
|
USGS scientists processing groundwater samples during a subsurface pH modification experiment. In the foreground is a tank containing an injection solution used to create a plume of groundwater with lower pH.
|
A diagram of a push-pull, single well injection test that can be used to estimate the rate that hydrogen is consumed by bacteria in the subsurface. Step 1 of the test involves the controlled injection of a solution of dissolved hydrogen gas and a non-reactive tracer into a monitoring well. Step 2 involves pumping the injected tracer solution out of the subsurface using the same well, and collecting water-quality samples from the pumped fluid.
|
A diagram of a natural gradient, single well injection test that can be used to estimate the rate that hydrogen is consumed by bacteria in the subsurface. Step 1 of the test involves the controlled injection of a solution of dissolved hydrogen gas and a non-reactive tracer using a single port of a multilevel monitoring well. Step 2 involves the collection of water-quality samples from the plume of hydrogen and tracer as it drifts past the same well.
|
A sewage treatment plant on the Massachusetts Military Reservation, Cape Cod discharged its treated wastewater into a series of infiltration beds through pipes like the one in the photo. This practice lasted for more than 60 years, and created a plume of wastewater more than 6 kilometers (approximately 4 miles) long in the subsurface.
|
USGS scientist collecting water-quality samples for the investigation of the natural restoration of the wastewater plume on Cape Cod, Massachusetts.
|
A conceptual diagram of the setup of the subsurface tracer test. A solution of bromide (conservative tracer), 17ß-estradiol, 4-nonylphenol, and sulfamethoxazole was injected into the subsurface. A series of corresponding water samples were collected from the multilevel sampler downgradient of the injection well.
|
Treated wastewater disposal beds on Cape Cod, Massachusetts, which created a large subsurface plume of contaminated groundwater. A team of scientists has been conducting long-term multidisciplinary research on the physical, chemical, and biological processes that control the transport of contaminants in groundwater.
|
A view of the side of a trench cut into the Cape Cod aquifer showing what is commonly referred to as a "homogeneous" aquifer. Studies of the distribution of the horizontal conductivity resulted in a range of conductivity from 0.02 to 0.34 centimeters per second, which demonstrated that the aquifer is not homogeneous.
|
Multilevel monitoring wells being prepared for installation prior to a large-scale natural-gradient tracer test above a plume of sewage-contaminated groundwater. Each well has 15 to 20 monitoring ports.
|
An array of several hundred multilevel wells were installed in an abandoned gravel pit. The array of wells was used to conduct a natural-gradient tracer test. The results of the test provided information on how contaminants are transported in groundwater.
|