Research and Meetings
The department faculty encourages and supports faculty-student research throughout the year. Faculty research interests range from tectonic history of Precambrian terranes to integrated investigation of groundwater and watershed analysis to global climate change to geoarchaeology. Below are some samples of recent faculty and student research:
Student Abstracts from Recent Professional Meetings
GATES, David J. and SMIDT, Samuel J.
Irrigation applications are a common farming strategy for maximizing annual crop yields, yet farmers looking to introduce a new irrigation system do not have a reliable data source that estimates the yield increase expected when compared to dryland regimes. Irrigation use is also a notable stress on water systems, making the management of both food and water a challenge in agriculturally intensive areas. A comprehensive understanding of irrigation enhancement compared to dryland practices is needed to couple sustainable water use with increased food production. This study uses a dual end-member linear regression model to estimate yield enhancement for major row crops across the continental United States (CONUS). We constructed the model using both observed yield data and common drivers to crop production (e.g., seasonal precipitation, air temperature, soil characteristics, and geographic location). We then interpolated this county-level data to generate a spatially complete yield enhancement map. Irrigation enhancements across commodities identified general East-West trends, with little effect in the east to roughly doubling yields in the west. This data can be used to influence farmer decision making at the regional level and establish a baseline for food production and water use in agricultural systems.
GATES, David J., James A. Clark, Stephen O. Moshier, Valerie Tewell, Daniel Master, Mario Martin, and John Sheffer
Tel Shimron is an archaeological site in the Lower Galilee region of northern Israel. The tel is located on the northern margin of the Jezreel Valley and was inhabited from the Early Bronze Age to Islamic Period. Summer 2017 marked the first season of excavation and the start of this research. This study’s purpose was to provide the archaeological team information on the local geology as it pertains to settlement patterns and ancient resources through both surficial mapping and geophysical prospection of the bedrock. The regional geology includes Eocene chalks of the Avedat Group with localized pedogenic alteration to calcrete (known regionally as nari) as well as Miocene basalt. The substantial exposure of basalt adjacent to the tel is of poor quality and was not used for tools, but rather extensively quarried for rampart construction and paving material. Hard nari was used for building stone and both chalk bedrock and nari are a local source of flint for tools.
Three geophysical methods were used to construct a partial subsurface model of the tel: electrical resistivity, seismic refraction and seismoelectric. Processed data revealed varying thickness of cultural “fill” over bedrock and suggested that the original topography beneath the tel may have influenced development patterns and rampart construction. Shallow buried structures, such as walls and broad floors were revealed in transects on the southwestern edge of the tel. This information will be used to influence archaeological decision-making and promote a multifaceted approach to site excavation in future seasons.
THIELMAN, Rebekah, MADSEN, Andrew and SMIDT, Samuel J.
Surface water-groundwater interactions are critical for overall stream health, but identifying the locations of these interactions often requires expensive or intensive field equipment. Moreover, field sampling is often site-specific and identification at multiple locations along a stream reach is limited. Streamlining the identification of surface water-groundwater interactions along a stream reach is a necessary step to large scale restoration projects, particularly in ungauged or unstudied areas. Here, we used a preliminary solute mass balance approach to efficiently estimate the magnitude of downstream surface water-groundwater interactions. We injected an in-stream saline tracer and simultaneously monitored for conductivity and dissolved oxygen adjacent to the stream channel using several groundwater monitoring wells. We then quantified the magnitude of surface water present in groundwater flow paths using a solute mass balance approach. Dissolved oxygen was then used as a proxy for conductivity to identify the location of downstream surface water-groundwater interactions and to quantify the magnitude of surface water present in groundwater flow paths.
Results from this study can be used in watershed restoration projects or site assessments as a way to identify the locations of key flow paths that benefit overall stream function.
THIELMAN, Rebekah and SMIDT, Samuel J.
Constant rate tracer injections typically rely on a peristaltic pump, but few pumps are adapted to extreme field conditions. Pumps used by researchers generally fall into two categories:
- lab-based designs implemented in a field setting or
- do-it-yourself pump designs constructed by the researcher.
Lab-based designs are often expensive (>$1,000) and sensitive to damage and moisture common in a field setting, and both pump categories often require large and heavy batteries to drive long injections at high flow rates (>1 L/min). The purpose of this study was to develop a cost-effective, do-it-yourself alternative ideal for robust field conditions. We used a bipolar stepper motor (12V-36V, 1.5A) connected to a microstep driver (40V, 4A) to create a continuous peristaltic rotation. The pump is controlled by an Arduino Uno microchip processing board, allowing for variable pump rates to be defined by the user. Waterproof housing was constructed using a Pelican 1200 case (7.29” x 4.78” x 3.33”), which can support up to 2 motor systems per case, allowing for dual tracers or double flow rate. Each motor system only draws ~2A of current, allowing for extended battery life using only a small sealed lead acid 12V battery. Batteries can also be stored in an adjacent Pelican 1200 case for a complete weather-proof system. Our maximum flow rate was ~1 L/min per pump, or 2 L/min per housing case. Total cost of the design was $300 for a dual pump set-up.
HESS, Benjamin Levi, Adrian Fiege and Nicholas Tailby
The major and trace element composition of apatites from the Lachlan fold belt (LFB) S- and I-type granitoids (Australia) and the Central French Massif (CFM) S-type leucogranites (France) were analyzed to investigate their compositional and redox variation. Apatite is a common accessory mineral in magmatic systems that can incorporate a variety of trace elements, including the polyvalent elements sulfur (S), iron (Fe), and manganese (Mn). It was recently discovered that apatite can incorporate three oxidation states of S (S6+, S4+, S2-) into its structure as a function of oxygen fugacity.
However, the oxidation states of Mn and Fe in apatite are essentially unknown (2+ and/or 3+).
In this study, we collected many electron probe line transects across apatites in several different host phases from a variety of S- and I-type plutons. The F-H-Cl contents of the S- and I-type LFB samples were similar (~2.9 wt% F, ~0.4 wt% Cl, ~0.5 wt% OH).
The CFM S-types contained virtually no Cl and ranged from nearendmember OH-apatite to near-endmember F-apatite. The apatites of all studied the S- and I-type plutons are characterized by similar ranges of Fe content (<1.5 wt% Fe), while Mn reaches much higher concentrations in the S-type when compared to I-type apatites (<6.5 wt% Mn). The S content of the apatites varies significantly, from <50 ppm S in the LFB S-types, up to 2,000 ppm S in the LFB I-types, and reaching 1,650 ppm S in the CFM S-types.
The elevated S contents in the LFB I-type and CFM S-type apatites allowed us to measure the S oxidation states by using X-ray absorption near-edge structure (XANES) spectroscopy. The spectra show variability in S oxidation states ranging from mostly sulfate down to nearly equal S6+/S2- ratios, indicating redox variations during apatite formation. The S-type Mn + Fe content plots in a 1:1 ratio against calcium (Ca) in atoms per formula unit, while the I-type apatites have too low Mn and Fe to show a clear trend. Thus, divalent Mn and Fe probably replace Ca2+ in the S-types’ apatite structure, while the incorporation of trivalent Mn or Fe in apatite is rather unlikely. We suggest that Mn and Fe contents in apatite may become a useful tracer of melt evolution once the distributions coefficients are experimentally calibrated.
LEEBURN, J. M., B. W. Denevi, C. M. Ernst, and R. L. Klima
Understanding the origin and evolution of Mercury’s crust was a key goal of the MESSENGER mission. Prior to MESSENGER’s exploration of Mercury, a leading hypothesis for the formation of the planet’s crust was through crystal–liquid fractionation of a magma ocean, leading to a plagioclase flotation crust analogous to that of the Moon. However, reflectance observations and elemental abundance data make it clear that Mercury’s crust is very different from the Moon’s, and interpretations based on the planet’s geomorphology and crater size– frequency distributions imply widespread resurfacing occurred, likely through a combination of volcanism and impact cratering. This geologic activity complicates an examination of Mercury’s early crust. Here we investigate Mercury’s stratigraphy as exposed by impact craters >20 km in diameter in order to evaluate the mode(s) of formation of a key crustal unit, the low-reflectance material (LRM). LRM has been documented to be mainly exposed from depth, and proposed to be at the bottom of the stratigraphic column, either as a component of the lower crust or upper mantle.
The reflectance of LRM is up to ~30% below the global mean, and it has a shallower (bluer) spectral slope, with a broad absorptionband-like feature at ~600 nm. These properties together with thermal neutron measurements have led to the interpretation that LRM is rich in graphite (up to 5 wt.%). Geochemical modeling has also shown that graphite is the only mineral that would have been buoyant in a magma ocean, suggesting it may have been a component in the earliest-forming crust. We explore whether the global occurrences and regional variations of LRM are consistent with this scenario, and investigate the role of early volcanism in the formation of Mercury’s crust.
Earlier Department Research
(F-faculty, FS-students with faculty, S-students)
- Glacial Isostasy and Global Sea-level Change Determined from Satellite Remote Sensing: Dr. James Clark, Nikki Cunningham, Paul Haidle, Lori McGuire, and Matt Andresen (FS)
- Effects of Great Lakes Water Loading upon Glacial Isostatic Adjustments and Lake History: Dr. James Clark, Deborah Zylstra, Kevin Befus (FS)
- Numerical Simulation of the Paleohydrology of Glacial Lake Oshkosh, eastern Wisconsin, U.S.A.: Dr. Clark, Kevin Befus, Peter Stewart, Taylor Shipman, Chris Gergory, Deborah Zylstra (FS)
- Eureka moraine and wave-washed till surface of glacial Lake Oshkosh, Buchholtz farm, Waushara County: Dr. Clark (F)
- Neshota outlet and drainage spillway associated with glacial Lake Oshkosh, Denmark Quarry, Brown County: Dr. Clark (F)
- Survey of Geological Artifacts Encountered at Tell el-Borg, NW Sinai, Egypt: Dr. Moshier (F)
- Paleoenvironmental Interpretation and Geoarcheology of the Northwestern Sinai Penninsula: Dr. Stephen Moshier (F)
- Comprehensive Study of the Mechanism for Groundwater Contamination Near Superfund Sites in the Rockford, IL Area: Dr. Jeffrey Greenberg, Katie Lethe, and Tim Bayley (FS)
- Provenance and Drainage Dynamics of Selected Streams, Black Hills, SD, from Heavy-Mineral Suites: Dr. Jeffrey K. Greenberg, Lacy Noetzel, and Josiah Engblom (FS)
- Composition and Tectonic Characteristics of Paleoproterozoic Basaltic Sills from the Eastern Black Hills, SD: Dr. Jeffrey Greenberg, Erik Mickelson, and Joel Moore (FS)
- Tectonic Interpretation and Mapping of Structural Features in the Vicinity of Hisega, SD: Dr. Jeffrey Greenberg (F)
- X-Ray Diffractometry and Clay-Mineral Analysis of Pottery Fragments from the Yucatan, Mexico: Lauren Powell, Anna Strong, and Andrew Kulpecz (S)
- Textural Analysis of Sediments in Otter Creek, St. Charles, IL (for the St. Charles Park District sponsored study of Otter Creek Bend Natural Area): Jeremy Vaughn, Douglas Walters, Paul Haidle (S) under supervision of Dr. Stephen Moshier
- Field Mapping of Holocene Sediments Associated with the Ancient Eastern Nile Delta, NW Sinia, Egypt (with the Trinity International University sponsored archaeological excavation at Tell el-Borg): Dr. Stephen Moshier and Lauren Powell (FS)
- Microporosity in Limestones Leading to Cavern Development: Dr. Stephen Moshier, Andrew Adare (FS)
- Bryozoan Buildups in the Subsurface Mississippian Newman Fm., Big Lime Mbr., SE Kentucky: Stephen Moshier (F)
- Mineralogy and Textures of Holocene Muds Associated with the Ancient Eastern Nile Delta, NW Sinia, Egypt): Dr. Stephen Moshier and Jamie Worrel (FS)
- Precambrian Carbonate Sediments and Diagenesis, Nemo Area, Black Hills, South Dakota: Dr. Stephen Moshier and Daniel Wolbrink (FS)
Students travel with faculty to professional geology conferences in order to attend presentations, present their research, participate in field trips, and interact with others in the geological community (recent meetings include the annual conference of the Geological Society of America in Boston and GSA regional conferences in Indianapolis, IN, Normal IL, and Lexington, KY).