Streambed Temperature Measurements and Geochemistry

Laura Sherrod - 2013

West Creek is a small tributary within the Schuylkill River watershed.  This ephemeral stream passes over abandoned subsurface coal mines.  During periods of low rainfall, the stream is known to lose all its flow to the subsurface mine pool.  This location was first surveyed with geophysical methods in 2012 in the West West Branch Hydrogeology and Geophysics project.  Resistivity profiles were used to pinpoint locations of potential streamflow loss along this reach of stream channel.  Follow-up investigations were performed in 2013 through streambed temperature measurements and geochemical analysis of water samples in collaboration with Dr. Chuck Cravotta, a geochemist with the United States Geological Survey stationed in Harrisburg, and Dr. Lauren Levine (KU Chemistry). 

 

West Creek of the Schuylkill River watershed

Dea Musa constructs the temperature probes for streamed temperature measurements.

Vertical temperature probes were constructed to measure the stream channel temperature profile over the course of two months.  Thermocron iButtons, model #DS1922L, were used to record the temperature measurements.  Four temperature sensors were installed in cavities drilled into each probe.  The cavities were filled with silicone and the sensors were inserted into the silicone to create a waterproof seal.  The first sensor was installed on a level with the streambed.  The three subsurface sensors were installed at depths of 0.03m, 0.06m and 0.10m.  Temperature measurements were made every 20 minutes for a period of 2 months between May 2013 and July 2013. 

Water quality measurements were initially made using a YSI 556 multiparameter water quality meter to provide temperature, pH, specific conductance, dissolved oxygen, and redox potential data.  To further investigate the variation of water quality along the stream channel, water samples were taken to produce a more detailed chemical analysis of the water.  Concentrations of major anions (SO4 and Cl) were analyzed by ion chromatography and concentrations of major cations, particularly the trace metal Iron (Fe) were analyzed by atomic absorption spectrometry. 


Dr. Cravotta and Leanne Hillegas and collect water samples in West Creek
Streambed Temperature Measurements Results Environmental Geophysics and Hydrogeology Resistivity
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