Development and Socioeconomic Drivers of Permitted Tree Removals in Austin, Texas

Type: Graduate
Author(s): Adam Buckmeier Environmental Sciences
Advisor(s): Brendan Lavy Environmental Sciences
Location: Basement, Table 9, Position 2, 1:45-3:45

In urban environments, trees provide a range of services including pollution removal, temperature regulation, and increased property values. In an effort to accrue these services, municipalities enact tree preservation ordinances that seek to protect public and private trees. Despite the protections of these ordinances, many trees are removed legally each year due to urban (re)development, risks associated with tree growth, and tree death. This research examines the spatiotemporal trends of permitted tree removals in the City of Austin, Texas, from 2013 to 2023. Specifically, we created a geographic information system to explore the differences between development-related and non-development-related removals, as well as between healthy and unhealthy removals. We also explored the extent to which sociodemographic characteristics explained differences in tree removals. Preliminary findings reveal that most trees removed are healthy and for development-related reasons, a reflection of Austin’s accelerating urban growth. We identified areas with high to moderate development pressure, high health impacts, and low activity. Our analysis also revealed significant patterns in tree removals associated with demographic and socioeconomic characteristics. Areas with higher proportions of non-White populations experience fewer tree removals. This, however, correlates with lower overall canopy cover, suggesting these areas have fewer trees to begin with. Conversely, neighborhoods with higher household incomes show more tree removals but also higher canopy cover, indicating more active tree management in wealthier areas with greater tree resources. Our research highlights location-specific tree removal patterns to inform strategies that account for both environmental and socioeconomic factors.

Canopies vs. Clearings: Investigating Microclimates and Vegetation Health Throughout the Day

Type: Undergraduate
Author(s): Audrey Haffner Environmental Sciences Sloan Malleck Environmental Sciences Emma Taylor Environmental Sciences Julia Vasquez Environmental Sciences
Advisor(s): Brendan Lavy Environmental Sciences
Location: SecondFloor, Table 5, Position 3, 11:30-1:30

Microclimates, which refer to the localized atmospheric conditions within small-scale environments, can be influenced by a variety of factors such as vegetation, topography, and human activity. One of the key elements that affect microclimates is the type of canopy cover present in an area. Open areas, where there is little vegetation and more exposure to the elements, often experience different conditions compared to areas with dense canopy cover, where the vegetation provides more shelter and shade. Understanding the differences in microclimatic conditions between these two types of environments helps us understand how these environmental conditions affect people, plants, and animals. The purpose of this study is to explore how microclimates vary between open areas and areas with closed canopy cover, focusing on factors such as temperature, humidity, and NDVI to better understand how canopy cover influences environmental conditions.

Do Income-Driven Differences Between Urban Neighborhoods Shape Prey Availability and Bat Foraging Activity?

Type: Graduate
Author(s): Elizabeth Hargis Environmental Sciences
Advisor(s): Victoria Bennett Environmental Sciences
Location: SecondFloor, Table 7, Position 1, 11:30-1:30

Urbanization alters habitat structure and resource availability, influencing wildlife distribution and behavior. In particular, invertebrates are affected by the differences in urban landscape that are caused by distinct socio-economic differences throughout urban areas. These changes in invertebrate abundance and diversity may affect bat populations that rely on these invertebrates as a food source. This study investigates how neighborhood income influences invertebrate diversity and bat foraging activity in Fort Worth, Texas, USA. We hypothesize that variations in landscape management and the income-driven use of pesticides can alter invertebrate diversity and subsequently bat activity. We conducted invertebrate sampling and acoustic bat monitoring across ten urban greenspaces; five high-income and five low-income neighborhoods in Tarrant County, TX, USA. We then quantified invertebrate and bat abundance and diversity using Shannon’s and Simpson’s diversity indices and examined correlations between invertebrate diversity, bat activity, and household income. This study will help to understand the ecological consequences of socio-economic disparities in urban habitats, which can inform conservation strategies to enhance urban biodiversity and bat conservation efforts.

Assessing Soil Carbon Dynamics in Amended Urban Farms in Fort Worth Using Thermal Analysis

Type: Graduate
Author(s): Md Simoon Nice Environmental Sciences Esayas Gebremichael Geological Sciences Brendan L. Lavy Environmental Sciences
Advisor(s): Omar Harvey Geological Sciences Gehendra Kharel Environmental Sciences
Location: Third Floor, Table 4, Position 1, 11:30-1:30

Fort Worth, the fastest-growing city in Texas, contains many vacant land plots suitable for urban agriculture—an opportunity to address local food deserts. However, unsustainable farming can degrade soil organic carbon and reduce productivity. This study assessed soil carbon dynamics in a food waste compost–amended urban farm in Fort Worth. Experimental plots, including compost-amended and control treatments (triplicated), were established and monitored monthly from January 2023 to July 2024. Thermo-gravimetric Analysis (TGA) was used to calculate the recalcitrance index (R50), indicating carbon stability. Results showed compost-treated soils had more stable carbon and structured lignin degradation. In contrast, untreated soils exhibited unstructured decomposition and faster carbon loss. Compost enhances soil health and carbon cycling, and future research should explore combining compost with cover crops to maximize carbon sequestration and microbial activity in urban farming systems.

Examining the Relationship Between Tree Canopy Cover and Walkability in Austin, Texas

Type: Undergraduate
Author(s): Zoey Suasnovar Environmental Sciences
Advisor(s): Brendan Lavy Environmental Sciences

Cities are increasingly adopting and promoting actions in support of their sustainability goals to enhance community well being and improve environmental quality. These large, sprawling cities actions include providing more sustainable transportation choices, like bike lanes, micro-mobility options (e.g., scooters or e-bikes), and walkability. Yet, as municipalities offer these alternatives, increasing urban heat may deter residents and visitors from using them. Cities, such as Austin, Texas, have become hotter over the last decade due to increasing impervious cover and tree loss associated with urban (re)development. Urban trees provide cooling effects to the surrounding area through evapotranspiration and shade. Thus, tree shade is important to promote more walkable neighborhoods, especially in the summer months. This study looks at the relationship between canopy cover and urban walkability in Austin. Using a Geographic Information System, we examined the interactions between canopy cover, walkability, socioeconomic data (i.e., race, gender, income, and home-owner status), and sidewalks. In doing so, we found a total of 2,552.47 km of shaded sidewalks, equaling, about a third of all sidewalks in Austin. We also found that canopy cover and walkability vary by location. Some areas have high canopy cover and low walkability, whereas other areas have low canopy cover and high walkability. Preliminary results also indicate that some areas have less shaded sidewalks than others and vary based on an area’s socioeconomic characteristics. The results of this research may be used to promote sustainable cities and urban forestry along sidewalks to help mitigate the urban heat island effect.

Bring on the Heat: How the Percentage of Tree Coverage affects the LST of Public Elementary Schools in Tarrant County

Type: Undergraduate
Author(s): Sahana Talwar Environmental Sciences
Advisor(s): Brendan Lavy Environmental Sciences
Location: Basement, Table 13, Position 2, 1:45-3:45

Increases in city size and frequency have correspondingly led to increases in Urban Heat Island (UHI) strength and frequency. These urban heat islands have had serious implications for both children’s health and education. One widely accepted UHI mitigation strategy is green spaces. However, these have mainly been studied in the context of parks. This study aims to fill in a necessary gap of knowledge by studying the effect of green spaces at elementary schools. This was done by looking at the percentage of tree coverage at 273 public elementary schools in Tarrant County and comparing them to the Land Surface Temperatures (LSTs) of those schools. Google Earth Engine, ArcGIS Pro, and Google Spreadsheets were the three main software systems used to accomplish this. This study found that the percentage canopy cover and LST were inversely proportional at elementary schools in Tarrant County. It also found that other factors apart from trees effect LST.

Fish Community Monitoring as part of the Trinity River Authority's Clean Rivers Program

Type: Undergraduate
Author(s): Logan Tidwell Environmental Sciences Angela Kilpatrick Environmental Sciences Ryan Seymour Environmental Sciences
Advisor(s): Michele Birmingham Environmental Sciences
Location: Third Floor, Table 1, Position 2, 1:45-3:45

With only four species of fish collected in the Dallas Fort Worth Metroplex as recently as the 1970’s, it is no surprise that the Trinity River was once referred to as the “mythological river of death”. Since then, coordinated improvements in water quality have led to the recovery of fish assemblages within the Trinity, becoming a well-documented environmental success story. To monitor that recovery, the Trinity River Authority has conducted Aquatic Life Monitoring surveys on one or more Trinity Basin waterbodies biannually since 2013. These surveys have targeted waterbodies with documented concerns or impairments for one or more water quality parameters, capturing conditions in both the Index (March 15-Oct 15) and Critical (July 1-Sept 30) periods. At each site, whole community fish data was collected via backpack electroshocking and seine netting, alongside benthic macroinvertebrate and habitat data. As of 2025, 30 surveys have been conducted on 13 waterbodies throughout the Upper Trinity basin. Although these surveys have targeted streams with water quality concerns, 90% of sites have scored as either High or Exceptional on the State of Texas Regionalized Nekton Index of Biotic Integrity. Here we will characterize the collected fish communities with over 12,500 individuals from 41 unique species collected during these surveys, while also describing the vision of the program over the next decade.

Norfolk UST Risk Assesment

Type: Graduate
Author(s): Joshua Benford Geological Sciences
Advisor(s): Esayas Gebremicael Geological Sciences
Location: Basement, Table 1, Position 2, 11:30-1:30

Leaking underground storage tanks (USTs) pose a significant environmental hazard in Norfolk, Virginia, where factors such as weather, casing materials, and varying ground conditions contribute to potential leaks over time. Corrosion, exacerbated by Norfolk's coastal location and harsh soil conditions, is a primary cause of these leaks. Geographic Information System (GIS) tools can be utilized to develop a predictive model for identifying at-risk UST locations by integrating data from multiple sources, including UST records from the state of Virginia and other relevant datasets. This model would employ various spatial analysis techniques to generate maps and web applications, enabling field teams to validate its accuracy and support the City of Norfolk in mitigating risks associated with leaking USTs. The goal of this research is to produce valuable insights that help safeguard the health of Norfolk's residents and protect the delicate surrounding ecosystem, including the Atlantic Ocean, marshes, rivers, and Chesapeake Bay.

The Effect of Red-Light Traffic Cameras on Vehicle Collisions in Fort Worth

Type: Undergraduate
Author(s): Sovereign Bourgeois Environmental Sciences TJ Willson Geological Sciences
Advisor(s): Esayas Gebremichael Geological Sciences
Location: SecondFloor, Table 3, Position 2, 1:45-3:45

Prior to 2019, Texas used red-light traffic cameras to deter drivers from driving recklessly and running red lights. However, due to legislation signed by Governor Greg Abbott, red-light cameras are no longer used in Texas. This decision was made to ‘protect drivers' constitutional rights.’ Additionally, it was argued that these cameras increased the rate of rear-end collisions.

This study investigates the effect of removing red-light cameras in Fort Worth before and after the ban by examining the rate of different types of collisions. The location data of crash sites and police reports will be mapped using ArcGIS Pro to determine the frequency and density of these crashes.

Amazon Deforestation: A Spatial Analysis of Its Impact on Carbon Sequestration and Global CO2 Emissions

Type: Undergraduate
Author(s): Lauren Breach Environmental Sciences Justus Bedford Interdisciplinary
Advisor(s): Esayas Gebremichael Geological Sciences
Location: FirstFloor, Table 2, Position 1, 11:30-1:30

The Amazon rainforest is one of the largest carbon sinks in the world, playing a critical role in regulating global carbon dioxide levels. However, deforestation has significantly reduced its ability to sequester carbon, contributing to rising CO2 emissions. We will analyze deforestation trends in the amazon over the last three decades by integrating satellite imagery, historical land cover data, and carbon flux models. Using remote sensing data from Nasa and Brazil’s National Institute for Space Research (INPE), we will generate temporal GIS layers to map forest loss and quantify the impact on carbon sequestration. Through identifying key deforestation hotspots, this project aims to provide important insights into the relationship between land-use changes and atmospheric carbon levels, supporting future conservation strategies and policy recommendations.

Tri-colored bat Potential roosting sites: A GIS analysis of Tarrant County culverts

Type: Undergraduate
Author(s): Lexi Foster Environmental Sciences Liam Slattery Geological Sciences
Advisor(s): Victoria Bennett Environmental Sciences
Location: Basement, Table 5, Position 1, 11:30-1:30

Tri-colored bats are on track to be listed as an endangered species, however insufficient information is available on their roost sites. The aim of this project is to determine which culverts in Texas, more specifically Tarrant County, are likely to be used as winter roosts for the Tri-colored bat species. The project will utilize available culvert data from TxDOT and data on the potential ranges of Tri-colored bats. Analysis will begin by categorizing the culverts into individual layers by features such as height, length, and material.

Exploring Levee Systems of the DeGrey River: Geomorphological and Reservoir Potential

Type: Undergraduate
Author(s): Jacinto Garza ll Geological Sciences Henry Henk Geological Sciences Matt Kelly Geological Sciences Simon Lang Geological Sciences Victorien Paumard Geological Sciences Andrew Winch Geological Sciences
Advisor(s): John Holbrook Geological Sciences
Location: Third Floor, Table 7, Position 2, 1:45-3:45

The ephemeral DeGrey River of northwestern Australia’s Pilbara region presents unusual very high relief double levees of up to 5.8 m that are still poorly understood. This study aims to take advantage of excellent exposures of these double levees to assess their likely origin. Accessing and studying these features in a modern setting constitute a unique opportunity to better understand their geomorphology and evaluate their reservoir potential as an analogue for the subsurface.
We investigated these levees using shallow augering, percussion coring, digging of shallow pits, and ground-penetrating radar (GPR), calibrated using dGPS surveys. Remote sensing data, such as LIDAR and photogrammetric drone surveys, were also used to identify and visualize fluvial geomorphologic features, which were then ground truth by pedestrian surveys and general field observations. Core and auger samples were described according to grain texture using the USDA classification and a Munsell color atlas. to distinguish the similarities or differences from sediments by depth. Grain size was further assessed in sand and gravel using a Brunton Grain Size Card.
These levees were primarily developed by water during multiple large flooding events which exceeded their height limit, as opposed to the alternative hypothesis that these were large eolian features coincidental with levee positions at the channel margin. This is evidenced by the common layers of gravelly and poorly sorted coarse sand dispersed within the levee strata. Similarly, sedimentary structures of lower and upper flow regimes typical of water flood are observed for these strata. Locally, the outer part of the two levees was found to include an eolian cap, which provided additional height to the levee locally. These strata were fine-grained and well-sorted by contrast, typical of aeolian origins.
Cyclone-driven floods control the activation of the DeGrey River and associated sedimentation. These double levees form through rapid sediment deposition in unusually energetic overbank flows. The high permeability and sandy stratification of these levees provide opportunistic reservoir potential. This contrasts with silty levee deposits observed in perennial rivers with lower discharge variation. The high double levees of the DeGrey River appear to be a hydrologic and geomorphic feature characteristic of ephemeral river systems.

A Study of the Coll de Montllobar to Further Characterize Channelization as the Units Shift Through Transgressive-Regressive Sequences

Type: Graduate
Author(s): Samuel Knox Geological Sciences
Advisor(s): John Holbrook Geological Sciences
Location: Basement, Table 4, Position 2, 1:45-3:45

The Tremp-Graus basin, located in Northern Spain, is a foreland piggyback basin that sits on the foot of Pyrenees Mountains. More specifically within the Montsec range, North of the Montsec thrust belt. The basin is a result of an east to west trending syncline area between the Boxial and Montsec Thrusts, North and South of Tremp, Spain, respectively. During the end of the Cretaceous period, syntectonic sedimentation began and carried throughout the Miocene. Thus, forming the basin that is structurally open in the west and open in the east, possibly due to structural events and quite possibly a shallow sea that protruded the area during the Ypresian (56 – 47.8 Ma). The sediments came from sources in the North, East, and the South in less quantities. The Pyrenees Mountains to the north are the main source of the sedimentation in the area as an influx of sediment occurred over time as the thrust sheets became proximal to the basin. The Boxial thrust supplied alluvial fans during the Maastrichtian in a localized setting (Arevalo, 2022; Busquests, 2022).
There is an overall transition from continental to deltaic sediments in the east to a western section that is mainly slope mudstones, thin-bedded turbidite wedges, proximal turbidites, channel-fills, distal turbidities and basin-plain deposits. This study will focus on a vertical section in the Coll del Montllobar Cliffs to help identify and differentiate channel characteristics as the rocks shift from continental/terrestrial deposits to marine influence deposits (tracking transgressive-regressive cycles) within the Upper Ager Group through the Lower Montanyana Group. The study will include at least five highly detailed measured sections, fluvial mapping conducted through drone footage and 3D modeling as well as possible point counting root density within the sections. In the conclusion of this study researchers will have a reliable Type Section as well as a basic understanding of how transgressive – regressive cycles alter channel behavior within the region, as well as the defining characteristics of the fluvial channels.

Using GIS Technologies to Explore Urban Heat Island Effect in Tarrant County

Type: Undergraduate
Author(s): Sloan Malleck Environmental Sciences Sean Farrell Geological Sciences
Advisor(s): Esayas Gebremichael Geological Sciences
Location: SecondFloor, Table 2, Position 2, 1:45-3:45

This study aims to investigate how the growth and expansion of Tarrant County has potentially increased average temperatures from 1985 to 2020. The study will utilize satellite imagery from the USGS, weather data from the NWS, and population and land cover data to better understand the relationship between urban growth and temperature change. We speculate that the rapid growth and development of Tarrant County has led to a measurable increase in average daytime temperatures due to the urban heat island effect.

The Impact of Texas Coastal County Land Cover on Hypoxia Levels in the Gulf Coast

Type: Undergraduate
Author(s): Emma Maxwell Geological Sciences Emily Garza Environmental Sciences
Advisor(s): Esayas Gebremichael Geological Sciences
Location: SecondFloor, Table 1, Position 3, 11:30-1:30

This project will analyze the relationship between land cover in Texas coastal counties and dissolved oxygen levels in the Gulf of Mexico. Utilizing GIS, we aim to understand land cover changes in Texas coastal counties from 2021 to 2023 and corresponding changes in dissolved oxygen levels in the Gulf of Mexico during this time frame. The analysis will examine spatial data from the Gulf of Mexico and Texas, focusing on urban areas, agricultural land, coastal wetlands, and freshwater wetlands.

GIS STUDIES AND GEOCHEMISTRY OF SELECTED CAMBRIAN IGNEOUS ROCK UNITS IN THE SOUTHERN OKLAHOMA AULACOGEN

Type: Graduate
Author(s): Michael Mbah Geological Sciences Esayas Gebremichael Geological Sciences
Advisor(s): Richard Hanson Geological Sciences
Location: SecondFloor, Table 8, Position 3, 1:45-3:45

The Wichita Mountains in southwestern Oklahoma hold over a billion years of geological history, offering valuable insights into rift dynamics, magmatism, and basin evolution. These mountains are remnants of the Southern Oklahoma Aulacogen, a failed rift that initially formed during the Cambrian period through crustal extension but was later uplifted due to tectonic inversion. The region features a diverse range of igneous and sedimentary rocks, including the Carlton Rhyolites, gabbroic anorthosites, and granites of the Wichita Granite Group, which reflect a complex magmatic history. Over time, major tectonic events such as the Pennsylvanian uplift during the formation of Pangea and subsequent Permian burial played a key role in shaping the area's present landscape. This study utilizes Geographic Information Systems (GIS) tools to examine the spatial relationships, structural features, and lithological distribution of the Wichita Mountains. Using remote sensing, digital elevation models (DEMs), and geospatial analysis, this research provides a deeper understanding of the regions geological history and demonstrates the effectiveness of GIS technology in structural geology and regional mapping.

Quenched and disrupted dacitic to rhyolitic hyaloclastie complex emplaced at shallow levels beneath the seafloor in a Devonian submarine island-arc sequence in the northern Sierra Nevada, California

Type: Graduate
Author(s): Quinton Mindrup Geological Sciences Richard Hanson Geological Sciences
Advisor(s): Richard Hanson Geological Sciences
Location: Basement, Table 4, Position 1, 1:45-3:45

The Devonian Sierra Buttes Formation (SBF) occurs at the base of a thick succession of submarine Paleozoic island arc strata in the northern Sierra Nevada. Bulk eastward rotation of the succession has provided cross-sectional views of a variety of SBF volcaniclastic deposits, radiolarian chert and associated hypabyssal intrusions. The area of concern herein is centered on the prominent glaciated Sierra Buttes peaks, from which the formation takes its name. Coeval andesitic to rhyolitic hypabyssal intrusions form a complex assemblage making up much of the SBF in this area. The assemblage contains a large intrusive hyaloclastite complex within which dacitic-rhyolitic bodies are chaotically dispersed. The intrusions developed when ascending batches of magma were unable to penetrate thick sequences of unlithified sediment and instead intruded into and were quenched against them at shallow levels beneath seafloor.

Here we report results of detailed mapping of glaciated outcrops that occupy an area of ~ 245,000 m2 within the intrusive assemblage and consist mostly of dacite and rhyolite. The assemblage contains large amounts of massive fragmental material with clasts typically < 3 cm in length and ranging down to fine ash. Much of this material consists of angular, originally glassy hyaloclastite shards that formed by nonexplosive quench fragmentation of magma intruding into wet sediment. Ellipsoidal bodies, elongate tubes several meters in length with elliptical cross-sections, and irregular amoeboid bodies occur within the hyaloclastite matrix and are interpreted to represent parts of a branching, interconnected feeder system that supplied magma to the growing fragmental mass beneath the sea floor.

Using Battery Energy Storage Systems with Renewable Energy to Strengthen the Texas Power Grid

Type: Undergraduate
Author(s): Isabella Moreno Environmental Sciences Garrison Kelly Geological Sciences
Advisor(s): Esayas Gebremichael Geological Sciences
Location: Third Floor, Table 10, Position 2, 1:45-3:45

HYDROGEOCHEMICAL ASSESSMENT OF THE SPATIOTEMPORAL EVOLUTION OF GROUNDWATER IN TEXAS AQUIFERS (1985-2014)

Type: Graduate
Author(s): ELVIS OWUSU Geological Sciences
Advisor(s): OMAR HARVEY Geological Sciences
Location: Basement, Table 12, Position 2, 1:45-3:45

Due to the increasing industrial activities, domestic and agricultural demands in Texas render groundwater resources under severe pressure. Texas growing population of 29.5 million in 2021 is projected to reach 51 million by 2070 placing increasing pressure on groundwater, a vital resource for agriculture, industry and municipal use.
This study assesses the hydrogeochemical evolution of Texas nine (9) major aquifers over three decades (1985-2014) and leveraged data from the Texas Water Development Board, Satellite (Landsat 8) dataset from Center for hydrometeorology and Remote sensing, Land use and land cover (Landsat 8/9) dataset from Multi Resolution Land Characteristics were analyzed.
Results indicate a transition in groundwater types across aquifers such as Ogallala, Seymour, Pecos Valley, Edwards Trinity and Edwards Balcones, but Hueco Mesilla Bolson, Carrizo Wilcox and Gulf Coast remain chemically stable with the Trinity aquifer showing a slight variation in its ionic composition. Rock-water interaction and evaporation are the primary mechanism that controls groundwater chemistry and its influence by the weathering of silicate minerals, carbonate dissolution and evaporite dissolution.
Precipitation rates and Land cover changes also play a significant role in the hydro geochemistry of groundwater. Precipitation acts a climate driver for groundwater chemistry, Low precipitation enhances rock-water interaction while high precipitation dilutes solutes and refreshes the aquifer. An increase in developed areas increases abstraction of groundwater which lowers the groundwater level and increases mineral dissolution. This study highlights how hydrogeochemical assessment and remote sensing together offer vital insights into groundwater evolution, supporting adaptive and sustainable water management in Texas.

Geochemistry of Ediacaran-Ordovician diabase, lamprophyre and phonolite dikes in southern Colorado, possibly related to rifting in the Southern Oklahoma Aulacogen

Type: Graduate
Author(s): Caleb Perkey Geological Sciences Richard Hanson Geological Sciences
Advisor(s): Richard Hanson Geological Sciences
Location: Basement, Table 6, Position 1, 1:45-3:45

The Southern Oklahoma aulacogen is a northwest-trending structure containing abundant igneous rocks representing the remains of a major Cambrian rift zone. Previous geologists have mapped numerous igneous intrusions in Colorado that follow the same trend, ranging from Ediacaran to Ordovician in age, and have speculated that these intrusions may be a part of the same rift. These intrusions include abundant igneous dikes of various compositions that originated from deeper magmatic bodies, filling fracture systems in older igneous rocks and Precambrian gneisses. This study involves the geochemical analysis of samples we collected from different dike types, including diabase, lamprophyre, phonolite, and nepheline syenite. The dikes include a prominent diabase dike swarm in the Gunnison area as well as abundant dikes of several types in the Wet Mountains and Front Range farther east. On the discrimination and REE diagrams, fifteen representative dike samples from both sample regions plot tightly together, indicating the clustered dikes share a petrogenetic history of E-MORB-type magma that interacted with intercontinental lithosphere.
We have not yet found diabase dikes in the Wet Mountains suitable for geochemical studies. However, five samples from NW- to NNW-trending diabase dikes in the Front Range, ~80 km north of the Wet Mountains, are among the fifteen diabase samples that cluster together on the geochemical diagrams. This raises the intriguing possibility that dikes related to Ediacaran-Ordovician intraplate magmatism in Colorado may be more extensive than previously thought.
Samples of four lamprophyre dikes in the Wet Mountains exhibit uniform patterns in REE diagrams and plot within the same field on the Winchester and Floyd (1977) classification diagram. Three dikes classified as trachytes by other workers cluster plot in the phonolite field on this diagram, suggesting some of these dikes were previously misclassified. These three dikes also show similar REE patterns with prominent negative anomalies, implying prolonged fractional crystallization.

Suburbanization-induced Elemental and Molecular Alterations in Soil Organic Matter

Type: Undergraduate
Author(s): Tabby Pyle Geological Sciences
Advisor(s): Omar Harvey Geological Sciences
Location: Third Floor, Table 7, Position 1, 1:45-3:45

This study aims to use chemodynamics to engage the interplay between societal actions and environmental response. The project will build upon data from thermogravimetric and isotopic analysis capturing macroscopic soil chemodynamics in response to suburbanization in the Dallas-Fort Worth Metroplex (DFW). The DFW is one of the fastest growing metro areas in the US. Our early data suggests that a minimum of 30-yrs is the required period of lawn care before key chemodynamic indicators of soil health/resilience, such as R50 and isotope 13C (quantity and quality, is needed for lawns to return to their pre-suburbanization environmental status.

The objective is to examine implications at the microphysical and molecular-level via: Assessing how differences in the molecular composition of soil organic matter from a suburban lawn changes over time.

SRS Project

Type: Undergraduate
Author(s): Audrey Sinnett Environmental Sciences West Tyndal Environmental Sciences
Advisor(s): Esayas Gebremichael Geological Sciences
Location: FirstFloor, Table 2, Position 2, 1:45-3:45

We propose a GIS project analyzing waste disposal accessibility by comparing recycling quality between low-income and high-income neighborhoods. Using spatial analysis and field data, we will compare the amount of waste generated to the income of Los Angeles counties, and document any trends. The findings will provide insights into potential disparities in waste management services and inform policy recommendations for improving recycling programs in underserved communities.

Tree Health: Integrating change detection and spatial analysis tools to assess tree damage in response to California wildfires

Type: Undergraduate
Author(s): Elise Skiles Environmental Sciences Christopher Zamora Chemistry & Biochemistry
Advisor(s): Esayas Gebremichael Geological Sciences
Location: SecondFloor, Table 5, Position 2, 11:30-1:30

The purpose of this project is to determine if California's raging wildfires are having a detrimental effect on the state’s tree populations/health. Two main components of this project would be, a model of California's tree density/canopy cover in 1990, and a model of California’s tree density/canopy cover in 2020. The goal of this project is to determine if an increase in wildfires is a key factor in the decrease of California tree density, and if so, make recommendations for further research on how to protect trees from this natural disaster.

A Study of Fossilized Root Colonies as Indicators of Past Water Table Levels in the Coll De Montllobar

Type: Undergraduate
Author(s): Daphne Varmah Geological Sciences
Advisor(s): John Holbrook Geological Sciences
Location: Basement, Table 2, Position 1, 1:45-3:45

The Coll de Montllobar cliffs in the Pyrenees Mountains contain plant fossils known as root models, which show signs of oxidation and reduction along a depositional dip, indicating varying environmental conditions Since plant roots do not grow below standing water levels, these fossilized roots and their distribution can serve as markers for past water table positions. This study examines whether root density decreases toward the bottom of the channels, indicating that roots stopped growing once they reached below the water table. If the roots disappear at a certain depth, it suggests that the bar was saturated at that level, stopping root growth. By analyzing the presence and absence of these roots, we aim to determine if they mark a clear boundary indicating historical water table levels. Our findings contribute to understanding past depositional environments and hydrological conditions in this region

AI and Machine Learning in the Identification of Geochemical Variability and Geogenic Carbon: A Case Study of the Barnett Shale Formation

Type: Undergraduate
Author(s): Amanda Whitley Geological Sciences
Advisor(s): Omar Harvey Geological Sciences
Location: Third Floor, Table 8, Position 1, 11:30-1:30

The Barnett Shale formation in the Fort Worth Basin has been a substantial producer of oil and gas energy resources. The Barnett Shale serves as an ideal testing ground for innovative approaches to subsurface analysis, offering both abundant production history and a wealth of existing data. This study integrates innovative thermal analysis techniques with AI-driven workflows to rapidly process and interpret large volumes of geochemical data. We aim to identify and evaluate geochemical variability and the distribution, content, and quality of geogenic carbon with depth across key stratigraphic intervals. Expanding subsurface applications of AI and machine learning enhances the scalability of resource assessments and underscores the broader potential of these emerging analytical tools in energy exploration.