Physical Sciences
Identification of Environmental Microplastics Using Raman Spectroscopy
Author(s): Courtney J. Ebert, Korryn Narvaez, Eliza Ballantyne, Stone Smith, Reece Anderson
Geochemical Analysis of Amphiboles at Mt Hillers, UT
Author(s): Zoe Fischer, Parker Tenney, Chloe FitzGerald Taylor, Logan Chappell, Spencer Hahnem
Brain-eating Amoeba: A Multi-drug Study to Combat Naegleria fowleri and Improve Survival Rates
Author(s): Victoria Green, Ethan Jensen, Ethan Stryker
Encapsulation of Chemotherapeutic Temozolomide in Bovine-Milk Derived Extracellular Vesicles
Author(s): Charlee Cannon, Torrance Johnson, Caleb Weaver
Modifying the Light-Harvesting Capabilities of Phycocyanin using Rhodamine-B
Author(s): Brecken Shakespeare, Colton Koch
Photophysical and Photochemical Investigation of Dipyrrinone Bilin Subunits
Author(s): Cauy Williams, Danielle Newbold
Stratigraphic Insights into the Tectonic Evolution of the Rio Grande Rift
Author(s): Levi Hawks
Strain-Driven Metal-to-Insulator Transition and Ferroelectricity in WTe₂
Author(s): Ross Richins
The study of urea on protein biomarker detection by quantum dots
Author(s): Daniel Jensen, Caitlin West
Synthesis of Chiral ɑ-Amino Boronates via a 3-Component Coupling Reaction
Author(s): Anna Page
Quantitation of Trace Oxygen in Anoxic Water Implementing a Microfluidic Device
Author(s): Corban Kerr, Kason Stinson
Tectonic History of the Rio Grande Rift Through a Study of Sediment Provenance
Author(s): Brian Angell
A Pilot Study Investigating Virtual Reality for Chemical Education
Author(s): Kaden Jensen
Creating a New Distance Ladder with Surface Brightness Fluctuations
Author(s): Mikaela Cowles
Seven potential double star systems in the stellar association WSD 05205+3654
Author(s): Stryder Wiese
Optical Scattering for Rapid UTI Detection
Author(s): Feng Guo, Elise Bauer, Kimball Henstrom, Caroline Torgersen, Hannah Thrupp, Isaac Zabriskie, Alex Martinez, Keaton Fuller, Clint Flinders
Optimization of Cannabinoid Permeation Agents for Transdermal Delivery Applications
Author(s): Madison Bulloch, Alexia Casillas
Testing of an Acousto-Optic Modulator for Implementation as a Laser Q-Switch
Author(s): Micah Laing, Benjamin Holt
Increased Efficiency in Nonlinear Wireless Power Transfer
Author(s): Zachary Butler, Kendall Rosenkrantz, Yoonji Yo
Student's perceptions on the use of Virtual Reality in organic and inorganic chemistry
Author(s): Isabelle Smith, Alexandra Routsis, Laryssa Larson, Josie Wright, Kaden Jensen
Fluoride Speciation Analysis of the Great Salt Lake Utah
Author(s): Danielle Kemmer, Dillon Reynolds, Alyssa Brown, Benjamin Judd, Dean V. Smith, Tyler Jenkins, Asha Ahmed, Amber Thornton Miller, Dylan Jenkins, Nashly Cruz-Guzman
Synthesis and Characterization of Novel Pterostilbene Derivatives for Potential use as Therapeutics
Author(s): Austin Lamoreaux
Exploring Urban Wildlife Management Plans: A Case Study in Cedar City
Author(s): Jhen Allison Seguiwan
Insights into hydrogen storage utilizing cyclic amino-borane complexes
Author(s): Jordan Colmenero
Optimizing Continuous-wave Nd:YVO4 Laser Performance for Longwave Infrared Generation
Author(s): Benjamin Holt, Alex Gibb, MicahLaing
Lensless High-Resolution Imaging with Laser Interference
Author(s): Ulises Thornock, Brian Weaver, Jackson Phippen
A Preliminary Paleomagnetic Test for Incremental Pluton Emplacement
Parsons, Travis; Lippert, Peter; Bartley, John (University of Utah)
Faculty Advisor: Lippert, Peter (University of Utah - College of Mines and Earth Science, Geology & Geophysics); Bartley, John (University of Utah - College of Mines and Earth Science, Geology & Geophysics)
Field observations and geochronological measurements of plutons in Yosemite Valley suggest that plutons grow incrementally as a series of stacked sheets of smaller intrusions (i.e., dikes and sills) (Coleman et al., 2004; Glazner et al., 2004; Bartley et al., 2006). This interpretation is in contrast to the traditional view of pluton emplacement through crystallization of a single, massive magma chamber. Most of the observations supporting incremental pluton emplacement use the relationship between zircon U-Pb dating of pluton sections and estimated granitic magma cooling rates to argue that a single magmatic event would crystallize significantly faster than the geochronologic data permit. Incremental pluton emplacement also predicts specific relationships between the age of intruded sheets of magma and the original orientation of these sheets, such that older sheets are expected to be tilted or deformed more than younger sheets. Here we test this prediction of differential tilting by measuring the paleomagnetic inclination preserved in well-dated and structurally characterized sheets of the Tuolumne Intrusive Suite. Magnetic inclination provides a tilt-meter with respect to the Earth's magnetic field direction at the time of pluton emplacement; the reference inclination assuming an untitled pluton is known from independent data sets. We also present rock magnetic data (temperature-dependent magnetic susceptibility, magnetic remanence characteristics) and results from petrographic investigations to characterize the mineralogy and stability of the magnetization. Our results suggest that the low-titanium magnetite remanence carriers are primary and are not biased by secondary magnetizations. The distribution of magnetic inclinations in our sample set — in which older sheets on the periphery of the pluton are shallower than those in younger, more interior sheets, and with respect to the reference inclination — is consistent with predictions from the incremental pluton emplacement hypothesis.
Faculty Advisor: Lippert, Peter (University of Utah - College of Mines and Earth Science, Geology & Geophysics); Bartley, John (University of Utah - College of Mines and Earth Science, Geology & Geophysics)
Field observations and geochronological measurements of plutons in Yosemite Valley suggest that plutons grow incrementally as a series of stacked sheets of smaller intrusions (i.e., dikes and sills) (Coleman et al., 2004; Glazner et al., 2004; Bartley et al., 2006). This interpretation is in contrast to the traditional view of pluton emplacement through crystallization of a single, massive magma chamber. Most of the observations supporting incremental pluton emplacement use the relationship between zircon U-Pb dating of pluton sections and estimated granitic magma cooling rates to argue that a single magmatic event would crystallize significantly faster than the geochronologic data permit. Incremental pluton emplacement also predicts specific relationships between the age of intruded sheets of magma and the original orientation of these sheets, such that older sheets are expected to be tilted or deformed more than younger sheets. Here we test this prediction of differential tilting by measuring the paleomagnetic inclination preserved in well-dated and structurally characterized sheets of the Tuolumne Intrusive Suite. Magnetic inclination provides a tilt-meter with respect to the Earth's magnetic field direction at the time of pluton emplacement; the reference inclination assuming an untitled pluton is known from independent data sets. We also present rock magnetic data (temperature-dependent magnetic susceptibility, magnetic remanence characteristics) and results from petrographic investigations to characterize the mineralogy and stability of the magnetization. Our results suggest that the low-titanium magnetite remanence carriers are primary and are not biased by secondary magnetizations. The distribution of magnetic inclinations in our sample set — in which older sheets on the periphery of the pluton are shallower than those in younger, more interior sheets, and with respect to the reference inclination — is consistent with predictions from the incremental pluton emplacement hypothesis.
The Power of Wind on Rock: Yardang Formation in Argentina
Sevy, Jonathon; Radebaugh, Jani; McDougall, Dylan; Kerber, Laura; Rabinovitch, Jason (Brigham Young University)
Faculty Advisor: Radebaugh, Jani (Brigham Young University, Geology)
Yardangs are wind-carved linear ridges that are found selectively on Earth and extensively on Mars. The history of the morphologic development of yardangs is not well known. In the Puna high plateau of Argentina there are ignimbrite deposits, many of which have been eroded into yardang fields, commonly called fleets. Yarding fleets are evenly spaced forms, facing into the wind, that resemble a fleet of boats sailing. A prominent fleet, known as Campo de las Piedras Pomez (CCP) was studied to more fully understand their formation and morphology, including field research in December 2018 and 2019. Some physical characteristics looked at in the field included: dedos direction and lengths; heights and lengths of yardangs; structural features; wind and gravel ripple direction. In addition, relationships between yardang organization and structural control have been analyzed. The dedos on the fronts of yardangs averaged 4.0cm in length, while the reverse dedos were 3.3cm. From this it was determined that: Two wind directions, with one dominant, are present; Structural features can shape morphology of yardangs.
Faculty Advisor: Radebaugh, Jani (Brigham Young University, Geology)
Yardangs are wind-carved linear ridges that are found selectively on Earth and extensively on Mars. The history of the morphologic development of yardangs is not well known. In the Puna high plateau of Argentina there are ignimbrite deposits, many of which have been eroded into yardang fields, commonly called fleets. Yarding fleets are evenly spaced forms, facing into the wind, that resemble a fleet of boats sailing. A prominent fleet, known as Campo de las Piedras Pomez (CCP) was studied to more fully understand their formation and morphology, including field research in December 2018 and 2019. Some physical characteristics looked at in the field included: dedos direction and lengths; heights and lengths of yardangs; structural features; wind and gravel ripple direction. In addition, relationships between yardang organization and structural control have been analyzed. The dedos on the fronts of yardangs averaged 4.0cm in length, while the reverse dedos were 3.3cm. From this it was determined that: Two wind directions, with one dominant, are present; Structural features can shape morphology of yardangs.
A Yarrowing Experience: The Tumor Inhibition and Toxicity of Utah's Native Achillea millefolium
Parada, Michelle (Weber State University)
Faculty Advisor: Schramm, Katharina (Weber State University, Botany)
This research focuses on anti-tumor and the biotoxicity of A. millefollium (yarrow).
Yarrow is an interesting plant with a long history of medicinal uses, but very little has been done to research and prove the different beneficial properties claimed. There are two simple bench-top assays performed in this study, the potato disc assay which inoculates potato slices with Agrobacterium tumefaciens as well as different concentrations of yarrow extracts and assesses the resulting tumor formation and the brine shrimp toxicity assay to assess the LD-50 of the extracts. My results will indicate whether or not the native yarrow extracts inhibit or do not inhibit tumor formation and its toxicity level. The results of this research could lead to further studies of the phytochemicals in the plant to be used for cancer treatments.
Faculty Advisor: Schramm, Katharina (Weber State University, Botany)
This research focuses on anti-tumor and the biotoxicity of A. millefollium (yarrow).
Yarrow is an interesting plant with a long history of medicinal uses, but very little has been done to research and prove the different beneficial properties claimed. There are two simple bench-top assays performed in this study, the potato disc assay which inoculates potato slices with Agrobacterium tumefaciens as well as different concentrations of yarrow extracts and assesses the resulting tumor formation and the brine shrimp toxicity assay to assess the LD-50 of the extracts. My results will indicate whether or not the native yarrow extracts inhibit or do not inhibit tumor formation and its toxicity level. The results of this research could lead to further studies of the phytochemicals in the plant to be used for cancer treatments.
A Worldwide Phylogenetic Study of the Family Baetidae
Backman, Natalia; Ogden, Heath (Utah Valley University)
Faculty Advisor: Ogden, Heath (Utah Valley University, Biology)
The Family Baetidae, is in the order Ephemeroptera, also commonly known as Mayflies. The first baetids were described around 1815 by Leach, and since there are more than 900 species have been described. The family Baetidae is an important group of mayflies because of their position on the mayfly tree of life in that they are a key to understanding evolutionary trends, such as the origin of wings and flight. Taxon sampling for this study consisted of over 100 taxa, representing ??? genera, from lineages distributed geographically worldwide, except Antarctica. Two main datasets were constructed. The genes 12s, 16s, H3, 18s, 28s and CO1 were used as part of a traditional dataset. Targeted capture sequencing was used to generate a phylogenomic dataset, consisting of over 400 loci. Trees were reconstructed from the aligned datasets, and the results were compared. The phylogenomic data resulted in a much more resolved topology.
Faculty Advisor: Ogden, Heath (Utah Valley University, Biology)
The Family Baetidae, is in the order Ephemeroptera, also commonly known as Mayflies. The first baetids were described around 1815 by Leach, and since there are more than 900 species have been described. The family Baetidae is an important group of mayflies because of their position on the mayfly tree of life in that they are a key to understanding evolutionary trends, such as the origin of wings and flight. Taxon sampling for this study consisted of over 100 taxa, representing ??? genera, from lineages distributed geographically worldwide, except Antarctica. Two main datasets were constructed. The genes 12s, 16s, H3, 18s, 28s and CO1 were used as part of a traditional dataset. Targeted capture sequencing was used to generate a phylogenomic dataset, consisting of over 400 loci. Trees were reconstructed from the aligned datasets, and the results were compared. The phylogenomic data resulted in a much more resolved topology.
Shocked Electrons: Determination of the Heating Mechanism in Abell 665
Wik, Daniel (University of Utah)
Faculty Advisor: Wik, Daniel (Science, Physics and Astronomy)
Mergers between galaxy clusters are some of the most energetic events in the universe, driving shock fronts in the intracluster medium (ICM), an X-ray hot plasma permeating the cluster. Shock fronts heat thermal electrons, causing an increase in their temperature. The mechanism by which this occurs is undetermined, with two models being proposed to explain the phenomenon. The first proposes direct shock-heating and the second suggests indirect adiabatic compression, with the electrons subsequently equilibrating with ions heated by the shock. We utilize NuSTAR observations, advantaging its effective area at higher energies, of a shock in the merging cluster Abell 665 in order to discriminate between the models. To do so, a temperature profile was constructed across the shock, utilizing spectral fitting, and compared against the models' predictions. In addition, temperature maps across the cluster were generated to better understand the merger event as a whole. We find that the temperature profile is suggestive of the shock model but is not yet statistically significant, due to NuSTAR's comparatively worse spatial resolution. As a result, we apply a novel joint fitting technique to NuSTAR data and Chandra observations in order to statistically distinguish between the models for the first time, accounting for the scattering of photons due to the PSF. Understanding these processes increases our understanding of the magnetic field of the ICM, allowing for mass determination, permitting galaxy clusters to be used to constrain cosmological studies.
Faculty Advisor: Wik, Daniel (Science, Physics and Astronomy)
Mergers between galaxy clusters are some of the most energetic events in the universe, driving shock fronts in the intracluster medium (ICM), an X-ray hot plasma permeating the cluster. Shock fronts heat thermal electrons, causing an increase in their temperature. The mechanism by which this occurs is undetermined, with two models being proposed to explain the phenomenon. The first proposes direct shock-heating and the second suggests indirect adiabatic compression, with the electrons subsequently equilibrating with ions heated by the shock. We utilize NuSTAR observations, advantaging its effective area at higher energies, of a shock in the merging cluster Abell 665 in order to discriminate between the models. To do so, a temperature profile was constructed across the shock, utilizing spectral fitting, and compared against the models' predictions. In addition, temperature maps across the cluster were generated to better understand the merger event as a whole. We find that the temperature profile is suggestive of the shock model but is not yet statistically significant, due to NuSTAR's comparatively worse spatial resolution. As a result, we apply a novel joint fitting technique to NuSTAR data and Chandra observations in order to statistically distinguish between the models for the first time, accounting for the scattering of photons due to the PSF. Understanding these processes increases our understanding of the magnetic field of the ICM, allowing for mass determination, permitting galaxy clusters to be used to constrain cosmological studies.
Use of a Portable Handheld X-Ray Fluorescence Unit (pXRF) to Measure Alteration in Exhumed Fault Zones: Implications for Hydrologic Rock Properties and Injection Induced Seismicity
Paulding, Anna (Utah State University)
Faculty Advisor: Bradbury, Kelly (College of Science, Geosciences Department)
A dramatic increase in seismicity has occurred in the midcontinent region since 2009 (Rubinstein and Mahani, 2015), causing public concern for the stability of infrastructure and buildings. Several studies have directly linked this seismicity to the reactivation of buried fault systems near the Paleozoic sedimentary bedrock-Precambrian crystalline basement contact as a result of high volumes of injection of wastewater produced by the oil and gas industry (Ellsworth, 2013; Keranen et al., 2013).
The reactivation of fault zones due to fluid injection is not only influenced by injection rates but also by the ability of fluids to migrate along or across the contact, which is controlled by the rock properties and geologic setting. To better understand the rock property variations that may occur along the nonconformity interface, we use an outcrop analog site of an exhumed fault near Gunnison, Colorado. My undergraduate research focuses on using a portable handheld X-Ray Fluorescence Unit (pXRF) as a tool to measure compositional variations in outcrop. To directly compare data, a calibration using 16 USGS Concentration Standards as well as 12 analog samples will be used to create a calibration optimized for this specific suite of rocks which informs the accuracy of in-situ field data measurements against laboratory measurements of powdered samples, influencing how future pXRF measurements can be analyzed. Micro-scale variations of major and trace element concentrations reflect alteration and related fluid-rock interactions and may serve as a proxy for fluid migration along or across faulted sections of a nonconformity interface. I propose that calibrated pXRF data and whole rock XRF data is a useful tool for understanding the nature and degree of rock alteration in fault zones and across analog sites nonconformity interface. These data can aid in a more broad understanding of how pXRF data can be used in the field to characterize the nonconformity interface and fault zones.
Faculty Advisor: Bradbury, Kelly (College of Science, Geosciences Department)
A dramatic increase in seismicity has occurred in the midcontinent region since 2009 (Rubinstein and Mahani, 2015), causing public concern for the stability of infrastructure and buildings. Several studies have directly linked this seismicity to the reactivation of buried fault systems near the Paleozoic sedimentary bedrock-Precambrian crystalline basement contact as a result of high volumes of injection of wastewater produced by the oil and gas industry (Ellsworth, 2013; Keranen et al., 2013).
The reactivation of fault zones due to fluid injection is not only influenced by injection rates but also by the ability of fluids to migrate along or across the contact, which is controlled by the rock properties and geologic setting. To better understand the rock property variations that may occur along the nonconformity interface, we use an outcrop analog site of an exhumed fault near Gunnison, Colorado. My undergraduate research focuses on using a portable handheld X-Ray Fluorescence Unit (pXRF) as a tool to measure compositional variations in outcrop. To directly compare data, a calibration using 16 USGS Concentration Standards as well as 12 analog samples will be used to create a calibration optimized for this specific suite of rocks which informs the accuracy of in-situ field data measurements against laboratory measurements of powdered samples, influencing how future pXRF measurements can be analyzed. Micro-scale variations of major and trace element concentrations reflect alteration and related fluid-rock interactions and may serve as a proxy for fluid migration along or across faulted sections of a nonconformity interface. I propose that calibrated pXRF data and whole rock XRF data is a useful tool for understanding the nature and degree of rock alteration in fault zones and across analog sites nonconformity interface. These data can aid in a more broad understanding of how pXRF data can be used in the field to characterize the nonconformity interface and fault zones.