Assessing Urban Heat Island Intensity Using Landsat Data

Type: Graduate
Author(s): Daniel Ayejoto Environmental Sciences
Advisor(s): Gebremichael Esayas Geological Sciences
Location: Basement, Table 6, Position 3, 11:30-1:30

The escalating impacts of urbanization on local climate patterns, particularly the phenomenon of Urban Heat Islands (UHIs), necessitate effective monitoring and assessment strategies. This project endeavors to evaluate the Urban Heat Island intensity in Houston, Texas, employing Landsat satellite data and Geographic Information System (GIS) tools within the ArcGIS Pro platform. The study integrates multi-temporal Landsat imagery to derive land surface temperature patterns, facilitating a comprehensive analysis of UHI dynamics over time. Spatial analytics and geospatial techniques are employed to assess the correlation between land use/land cover changes and UHI intensity, offering insights into the factors influencing urban heat dynamics. The results are expected to contribute valuable insights for urban planners and policymakers, aiding in the development of strategies to mitigate the adverse effects of UHI and enhance overall urban sustainability. Additionally, the methodology established in this project can serve as a template for assessing UHI in other urban areas, fostering a broader understanding of the urban climate dynamics.

Sedimentation & Subsurface Characterization of the Lower Cretaceous Muddy Sandstone & Upper Cretaceous Mowry Shale, Powder River Basin, Wyoming

Type: Graduate
Author(s): Chase Chavez Geological Sciences
Advisor(s): Xiangyang Xie Geological Sciences
Location: Basement, Table 12, Position 2, 1:45-3:45

Foreland basins comprise some of the most prolific hydrocarbon producing reservoirs and source rocks in the North American Rocky Mountain region. One of these major producing basins is the Powder River Basin (PRB). Located in northeastern Wyoming and extending into southeastern Montana, the PRB is one of Wyoming’s largest and most active hydrocarbon producing basins. The basin comprises various Mesozoic and Paleozoic strata with productive conventional and unconventional plays. Various studies have been done on both Mesozoic and Paleozoic stratigraphy within the basin. Historically, Cretaceous stratigraphy has been well studied and documented within the basin. However, continual industry innovations in the collection, development, and processing of subsurface geological data are making possible more refined understanding of Cretaceous stratigraphy in the basin.

This study focuses on the upper Lower Cretaceous Muddy Sandstone Formation and lower Upper Cretaceous Mowry Shale intervals at basin scale, and the implications for tectonic and eustatic evolution prior to the development of the PRB. Which controlled sedimentation, infilling, and Total Organic Carbon (TOC) weight percentage distributions of the two formations. There is a general agreement that the Mowry can be divided into upper, middle, and lower sections. The middle section has been found to contain the highest TOC percentages based on prior work done with geochemical analysis. This study will update these findings with newly collected digital well data and produce higher-density regional basin coverage with type wells, while also utilizing petrophysical calculation methods to determine TOC percentages to compare with current geochemical analysis.

The Muddy being an older conventional reservoir and the Mowry a more recent unconventional play, the collection and utilization of digitized well log data from Enverus Prism with Petrel Software, in conjunction with analysis of in-house core, provides an effective approach for producing refined structure, isochore, net sand, and TOC maps for the basin. This information can then be used in generating interpretations of sedimentation history, basin infilling, and TOC distribution. In addition, published type wells with correlated Paleozoic stratigraphy from the United States Geological Survey (USGS) are being used to generate PRB subsidence curves for multiple well locations throughout the basin to compare with maps and figures produced in Petrel. To further enhance sedimentation interpretations, U-Pb detrital zircon analysis is being conducted on the Muddy Formation sandstones collected from core. This data will be compared with published detrital zircon and subsidence work done in the western neighboring Big Horn Basin and its equivalent Muddy Formation interval.

Tracking Soil Organic Carbon in an Urban Farm Near the Trinity River

Type: Graduate
Author(s): Julie Crenwelge Geological Sciences Christelle Fayad Interdisciplinary
Advisor(s): Omar Harvey Geological Sciences
Location: Second Floor, Table 5, Position 2, 11:30-1:30

Carbon is the elemental foundation for all living things on Earth. Soil carbon sequestration is a process in which carbon dioxide is removed from the atmosphere and stored in the soil. We want to examine the soil quality and the stability of carbon in an urban farm in North Texas by comparing measurements collected in October 2022 against measurements observed and collected in October 2023. Our research question is, “What is the effect of composting on the carbon quality and quantity at the farm?” The experimental points were chosen for comparison from a previous evaluation of a 1/3-acre section of a local urban farm next to the Trinity River in Fort Worth, Texas. We collected bulk soil samples at 0-15 cm and 15-30 cm depths from ten field points previously tested with an additional 3 new control points. Thermogravimetric Analysis (TGA) will be used to determine carbon quality by analyzing derivative weights change plots. The data collected suggests that within a year the experimental farm site has maintained a good quality of soil with minor acidification and compaction, as well as an increase in level and quality of carbon. The observed farm remains an appropriate site for providing food security, eliminating food waste while simultaneously sequestering carbon.

Facies Characterization of the De Grey River's Delta Plain

Type: Graduate
Author(s): Henry Henk Geological Sciences Jacinto Garza Geological Sciences Matt Kelly Geological Sciences Mackenzie Moorhead Geological Sciences Tripp Smith Geological Sciences Andrew Winch Geological Sciences
Advisor(s): John Holbrook Geological Sciences Esayas Gebremichael Geological Sciences Simon Lang Geological Sciences Victorien Paumard Geological Sciences
Location: Second Floor, Table 6, Position 1, 11:30-1:30

Fluvial Architecture and Longitudinal Variance within the Castlegate Sandstone, Book Cliffs, UT

Type: Graduate
Author(s): Brayton Keith Geological Sciences John Holbrook Geological Sciences
Advisor(s): John Holbrook Geological Sciences
Location: Basement, Table 11, Position 2, 11:30-1:30

The upper Campanian Castlegate Sandstone in the Book Cliffs of Utah is a highly amalgamated fluvial sandstone well known as a reservoir analog for oil and gas. It comprises the lower Castlegate, the formation capping Bluecastle Tongue, and the floodplain-rich middle Castlegate deposits. The Castlegate is among the most studied fluvial deposits in the world. Despite this, there has yet to be a fluvial architecture analysis completed for these deposits which consider the longitudinal variance within the Castlegate fluvial system. This project assesses the average channel depth and discharge for the lower Castlegate, allowing analysis of the relationship between channel depth and discharge and their effect on facies distribution, depositional style and fluvial architecture in the outcrops. The lower Castlegate Sandstone is a tributary fluvial system with paleocurrents oriented primarily W-NW to E-SE comprised of stacked braided fluvial sands updip, and large, higher flow straight-meandering trunk channels downdip. Distal outcrops show three distinct depositional styles with the first representing a period of highstand during which carbonaceous floodplain and small channels of 0.5-1 m in depth and maximum 4 m in width were deposited; the second represents a localized tectonic uplift with large channels of ~15 m in width and depth and lateral accretion sets scaled accordingly, and finally the capping units of small amalgamated sands composed of classic braided style channels which represent a period of lowstand.