UNIVERSITY PARK, Pa. — The processes that happen in the first few feet of soil can have large impacts on agriculture and water resources. To better understand these processes, a team of graduating Penn State geoscience majors mapped the subsurface at a research site in Penn State's Stone Valley Forest.
“The critical zone, which extends from the treetops to the groundwater, is important because it controls soil production and groundwater flow, and it’s closely tied with human processes such as agriculture and building,” said Chad Cole, a recent Penn State geosciences graduate. “It’s responsible for sustaining terrestrial life on earth.”
The team set up a 328-foot seismic line with 24 geophones spaced 6.5 feet apart at the Susquehanna Shale Hills Critical Zone Observatory. The observatory is part of a National Science Foundation-funded network established to investigate the processes that occur at Earth’s surface. In between each geophone, the team struck a steel plate with a sledgehammer, creating a seismic wave. The geophones measured the return times of the waves, and the researchers used those times, much like CT scanning, to create an image of the subsurface to a depth of about 45 feet.
“The quicker a wave reaches a geophone, the faster the velocity,” said recent Penn State geosciences graduate Nick Schuler. “At the very top near the surface are slower velocities and then the farther down you go the velocities increase because the rock is more in place and intact, so the waves go faster.”