PYRRHOTITE IN CRUMBLING CONCRETE FOUNDATIONS: THE LATEST SOCIETAL USE FOR MODERN GEOLOGIC MAPPING IN CONNECTICUT
Rock aggregate in the failing concrete foundations was largely mined from a single quarry, working a stratified metamorphic unit in eastern CT mapped as Ordovician Brimfield Schist. The gray, rusty brown to orange yellow weathering rock, is a medium to coarse grained, interlayered schist and gneiss, composed of oligioclase, quartz, K-feldspar, biotite and commonly garnet, sillimanite, graphite, and pyrrhotite. Iron sulfides of the unit are associated with acid drainage, which degrades surface and groundwater quality.
The Connecticut Geological Survey has provided assistance to the Governor’s Office, US Army Corp of Engineers, and the CT Congressional delegation, in the assessment of the potential scope of the issue. This includes providing maps of pyrrhotite and other sulfide bearing rocks as well as information on bedrock chemistry. Modern geologic map projects, integrating mineralogy, petrology, rock fractures, structural data, and chemistry, are contributing to the growth of a statewide geochemical database being compiled by the Connecticut Survey. This initiative will document the distribution of major and trace elements in bedrock, including metals, sulfides, and others of environmental concern. These geoscience data serve many societal applications, including environmental quality investigations, resource assessments, economic interests, and consumer protection.