2008 Proceedings - St. Cloud State University
2008 Proceedings - St. Cloud State University
2008 Proceedings - St. Cloud State University
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Abstracts<br />
Session A All Disciplines Ballroom<br />
Rocky Mountain National Park<br />
Mountain climbing, whitewater rafting, hiking, skiing are things that you think of when you think of Rocky Mountain National Park. Looking<br />
at what we enjoy about the National Park today, one begins to wonder what the original purpose of the National Park was and whether that<br />
is still the purpose today. Are we beginning to lose the benefits of the land that was set aside or was it set-aside just for recreational<br />
purposes.<br />
Presentation Index: A37<br />
Time: 9:00 a.m.<br />
Department: Geography<br />
Project Sponsor(s):<br />
<strong>St</strong>udent Presenter(s): Peters, Becky<br />
John, Gareth<br />
Monitoring and Modeling of Post-USSR Land Use Land Cover Change in Ryazan Oblast of European Russia Using Multi-<br />
Temporal Satellite Data<br />
After the breakdown of the USSR in 1991, Russia has undergone dramatic change in its social, economic and political systems, which has<br />
provided enough anthropogenic activities to greatly change land use and land cover. For instance, in some areas of Russia more than half<br />
of the farmland has been abandoned and is converting to scrublands and forests. Therefore, understanding the impacts of the new<br />
socioeconomic, political and environmental conditions on land use land cover change (LULCC) is important to determine controls and<br />
driving forces of LULCC to establish their relative importance and to predict future change. This research will utilize the collapse of the<br />
former Soviet Union in 1991 to determine the controls and driving forces and their relative importance on LULCC within the Ryazan oblast<br />
of European Russia, which is located on southern side of Moscow. About 30% land is covered with transitional forest steppe with average<br />
agricultural productivity, population density; average to below average collective form productivity and huge problem areas with poor<br />
ranking in commercial farming. The dynamics of the LULCC will be investigated by the combined use of satellite remote sensing and a<br />
geographic information system (GIS). Time series Landsat Satellite scenes of 1989, 1994 and 1999 will be utilized for classification,<br />
mapping and change detection. Change Vector Analysis change detection method will be employed in extracting LULCC for analyzing the<br />
direction, rate, and spatial pattern of LULCC in the Ryazan oblast of European Russia. Mapping, detection of land cover changes and<br />
establishment of their anthropogenic driving forces exhibit the past and present scenarios of LULCC. Modeling of LULCC using existing<br />
land use land cover dynamics and socioeconomic driving forces will provide tools for understanding the causes and consequences of rapid<br />
LULCC. LULCC modeling will also prove useful for disentangling the complex suit of socioeconomic and biophysical factors that influence<br />
the rate and spatial pattern of land cover change and in estimating the impacts of changes in land cover in the future.<br />
Presentation Index: A38<br />
Time: 9:00 a.m.<br />
Department: Geography<br />
Project Sponsor(s):<br />
<strong>St</strong>udent Presenter(s): Singh, Kunwar<br />
Blinnikov, Mikhail; Richason, Benjamin<br />
Geologic Trap of Cedar Valley, Nebraska<br />
The Cedar Valley Field in Scottsbluff County, Nebraska has produced over 2 million barrels of oil. The Cedar Valley Field is located on the<br />
northeast flank of the Denver Basin and the producing sedimentary rock has been termed the ―J‖ Sandstone. The ―J‖ Sandstone is located<br />
approximately 5000 feet below the surface (1100 feet below sea level) in this area and was deposited about 100 million years ago during<br />
the Lower Cretaceous. Wells were drilled in the area during the 1960s, first as wildcat wells and then as production wells. The average<br />
porosity of the J Sandstone is 20% and the average permeability is about 260 millidarcys. In order for the production of oil, there must be<br />
a geologic trap which would allow for the accumulation of oil and would prevent the oil from then dispersing. Through the analysis of well<br />
logs, the J Sandstone can be correlated and mapped. The structure shows a constant 1-2 degree slope to the northeast in this area with<br />
no discernable fold or fault. Therefore the structure of the J Sandstone does not provide a geologic trap for the oil to accumulate in. The<br />
stratigraphy of the J Sandstone is the probable trap for the Cedar Valley Field and will be further analyzed in order to determine the trap.<br />
Presentation Index: A39<br />
Time: 9:00 a.m.<br />
Department: Earth and Atmospheric Sciences<br />
Project Sponsor(s):<br />
<strong>St</strong>udent Presenter(s): Anderson, Adam<br />
Pekarek, Alfred<br />
A Limited Climatology of Capping Inversions in Nighttime Northern Plains Thunderstorms<br />
Accurately forecasting convection is one of the most important issues facing meteorologists today. Capping inversions make forecasting<br />
convective events very difficult in the northern plains of the United <strong>St</strong>ates. In this study, 12z soundings of ten Northern Plains stations were<br />
looked at in June, July and August from 1998 to 2003. The events, having been categorized previously by Wieseler (2007) as convective<br />
or non-convective, were looked at using the 12z sounding to determine a lid strength for that day. The goal of the study is to find a critical<br />
lid strength to aid in the forecasting of convection in the northern plains.<br />
Presentation Index: A40<br />
Time: 9:00 a.m.<br />
Department: Earth and Atmospheric Sciences<br />
Project Sponsor(s):<br />
<strong>St</strong>udent Presenter(s): Abel, Jon<br />
Weisman, Robert<br />
<strong>St</strong>. <strong>Cloud</strong> <strong>St</strong>ate <strong>University</strong> <strong>St</strong>udent Research Colloquium 28<br />
April 22, <strong>2008</strong>