Geophysical Analysis of Seasonal Montandon Gravel Ridge Water Table Fluctuation and Moisture Gradient Variation due to Storm Events

The purpose of this research project is to continue exploring the Montandon Long-Term Hydrologic Research Site(LTHR) by using multiple geophysical methods to obtain more accurate and precise information regarding subsurface hydrologic properties of a local gravel ridge,which are important to both the health of surrounding ecosystems and local agriculture. Through using non-invasive geophysical methods such as seismic refraction, Direct Current resistivity and ground penetrating radar (GPR) instead of invasive methods such as boreholedrilling which displace sediment and may alter water flow, data collection is less likely to bias the data itself. In addition to imaging the gravel ridge subsurface, another important researchpurpose is to observe how both water table elevation and the moisture gradient (moisture content of the unsaturated zone) change over a seasonal time period and directly after storm events. The combination of three types of data collection allows the strengths of each method combine together and provide a relatively strongly supported conclusions compared to previous research. Precipitation and geophysical data suggest that an overall increase in precipitation during the summer months causes a sharp decrease in subsurface resistivity within the unsaturated zone. GPR velocity data indicate significant immediate increase in moisture content within the shallow vadose zone (< 1m), suggesting that rain water was infiltrating into the shallow subsurface. Furthermore, the combination of resistivity and GPR results suggest that the decreased resistivity within the shallow layers is due to increased ion content within groundwater. This is unexpected as rainwater is assumed to have a DC resistivity value of 3.33*105 ohm-m. These results may suggest that ions within the sediment must beincorporated into the infiltrating water.

The Clearing Storm: A Re-Assessment of the Climate for Collaboration between Academic and Student Affairs

There is increasing recognition among those in higher education that it is no longer adequate to train students in a specific field or industry. Instead, the push is more towards producing well-rounded students. In order to do so, all of a university’s resources must come together and the climate on campus must be one that supportscollaboration. This report is a re-examination of the climate for collaboration on the campus of a private liberal arts university in the Mid-Atlantic region of the United States. It is a follow up to a similar investigation conducted on the same campus by Victor Arcelus(2008) five years earlier. In the interim, the university had re-configured its organizational structure, combining separate academic and student affairs divisions into a single unit overseen by the Provost. Additionally, the university had experienced turnover in several key leadership positions, including those of the President and the chief academic and student affairs officers. The purpose of this investigation, therefore, was to gauge the immediate impact of these changes on conditions for collaboration, which when present, advance student learning and development. Through interviews with six men and women, information was collected on the perceived climate for collaboration between academic and student affairs personnel.Analysis of the interview transcripts revealed that, depending on the position of the interviewee within the university, conditions on campus were seen as either improved or largely unchanged as a result of the transition in leadership and the structural merger of the two divisions.