CMT Multilevel System Case Studies and Techical Bulletins

solinst 703 waterloo emitter uses oxygen to remediate btex in groundwater
solinst sonic water level meter

Case Studies and Articles

cmt high resolution vapor intrusion monitoring

CMT for High Resolution Vapor Intrusion Monitoring

Vapor intrusion refers to the movement of volatile chemicals from the subsurface into the indoor air of overlying buildings. The most common source is groundwater or soil contaminated with volatile organic compounds (VOCs). VOCs emit vapors that migrate into pore spaces of the soil and upward into the overlying environment. Generally, vapors enter buildings through cracks and openings in the foundations because of a difference between interior and exterior pressures. 

sampling in solinst cmt multilevel systems

Sampling in Multilevels: Options and Helpful Hints

Collecting groundwater samples, in either the Solinst Continuous Multichannel Tubing (CMT) or Waterloo Multilevel Systems, must be accomplished with devices that can sample in, or through, relatively narrow tubing. Sampling tubes placed within the Waterloo System are either 1/2”ID (12mm), 3/8”ID (10mm) or 1/4”ID (6mm) depending on the number of zones being monitored. These open tubes are usually used in place of dedicated pneumatic pumps in the Waterloo System, when the application is relatively shallow and the water level high.

leaking underground storage tank monitoring

CMT Systems for the LUST Market

Multilevel monitoring wells solve the above problems, yielding accurate depth-discrete samples and preventing ambient flow in the well. More complete and accurate data sets quickly identify LUST sites which pose a threat to downgradient receptors and those that can be closed with no furthur action.

cmt vapor monitoring

CMT Vapor Monitoring

Vapor intrusion refers to the movement of volatile chemicals from the subsurface into the indoor air of overlying buildings. The most common source is groundwater or soil contaminated with volatile organic compounds (VOCs). VOCs emit vapors that migrate into pore spaces of the soil and upward into the overlying environment. Generally, vapors enter buildings through cracks and openings in the foundations because of a difference between interior and exterior pressures.