Award Abstract # 1952772
EAR-PF: Quantifying heterogeneity in stratigraphy across scales

NSF Org: EAR
Division Of Earth Sciences
Recipient:
Initial Amendment Date: June 25, 2020
Latest Amendment Date: June 25, 2020
Award Number: 1952772
Award Instrument: Fellowship Award
Program Manager: Aisha Morris
armorris@nsf.gov
 (703)292-7081
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: August 1, 2020
End Date: July 31, 2023 (Estimated)
Total Intended Award Amount: $174,000.00
Total Awarded Amount to Date: $174,000.00
Funds Obligated to Date: FY 2020 = $174,000.00
History of Investigator:
  • Andrew Moodie (Principal Investigator)
Recipient Sponsored Research Office: Moodie, Andrew J
Houston
TX  US  77005
Sponsor Congressional District: 07
Primary Place of Performance: University of Texas at Austin
Austin
TX  US  78712-1692
Primary Place of Performance
Congressional District:
25
Unique Entity Identifier (UEI):
Parent UEI:
NSF Program(s): Postdoctoral Fellowships,
Sedimentary Geo & Paleobiology
Primary Program Source: 01002021DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 7137
Program Element Code(s): 713700, 745900
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Dr. Andrew J. Moodie has been awarded an NSF EAR Postdoctoral Fellowship to carry out research and education plans at The University of Texas at Austin and Stanford University in collaboration with mentors Dr. Paola Passalacqua and Dr. Jef Caers respectively. This study aims to investigate the properties of sedimentary rocks across multiple scales, to draw connections between large scale geological variability (~10 m) and smaller-scale variability (~10 cm). Geophysical imaging is unable to resolve small-scale geological variability, however, Dr. Moodie expects to constrain this variability using statistical models and observations of larger-scale variability. This research is critical to the sustainability of coastal river-deltas, because these environments are impacted by a limited understanding of subsurface geology and flow pathways that are controlled by small-scale geological variability. Improved understanding of fluid-flow pathways will influence many fields, in particular, results of this research will inform pollutant transport modeling, groundwater resource management, shallow geothermal and carbon sequestration operations, as well as hydrocarbon production. Dr. Moodie?s education plan includes mentoring students, organizing a reading seminar about machine learning in the geosciences, and developing active learning modules for topics in sedimentary rock stratigraphy.

The sustainability of coastal river-deltas is impacted by a multitude of natural and anthropogenic factors, including a limited understanding of subsurface flow patterns. Geological heterogeneity strongly influences flow pathways and thus rates of contaminant transport and groundwater aquifer recharge, which limits our ability to sustainably manage water resources and mitigate health risks in river-delta environments. Smaller-scale subsurface heterogeneity due to channel and bedform dynamics (of less than 1 m) is typically under-constrained, because it is below the resolution that can be imaged by existing geophysical techniques. Theory and some evidence suggest that stratigraphic sequences may be scale invariant, which opens a pathway to constrain smaller-scale heterogeneity via observation of larger-scale heterogeneity. This project directly addresses the question: can patterns and information gleaned from subsurface heterogeneity at one spatial scale be used to constrain uncertainty at another scale? The EAR Postdoctoral Fellowship, will allow Dr. Moodie to 1) rigorously investigate scale invariant properties of stratigraphy, and 2) integrate these findings into a quantitative method to constrain subsurface heterogeneity. He will use a combination of approaches, including field measurement, numerical modeling, statistical data analysis, and machine learning. Measures from information theory will quantify scale invariance in stratigraphy, and an existing generative adversarial neural network method will be modified to map heterogeneity across spatial scales. This project was co-funded by the Sedimentary Geology and Paleobiology program in the Earth Science division (EAR).

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Hariharan, Jayaram and Passalacqua, Paola and Xu, Zhongyuan and Michael, Holly A. and Steel, Elisabeth and Chadwick, Austin and Paola, Chris and Moodie, Andrew J. "Modeling the Dynamic Response of River Deltas to SeaLevel Rise Acceleration" Journal of Geophysical Research: Earth Surface , v.127 , 2022 https://doi.org/10.1029/2022JF006762 Citation Details
Moodie, Andrew and Carlson, Brandee and Foreman, Brady and Kwang, Jeffrey and Naito, Kensuke and Nittrouer, Jeffrey "SedEdu: software organizing sediment-related educational modules" Journal of Open Source Education , v.5 , 2022 https://doi.org/10.21105/jose.00129 Citation Details
Moodie, Andrew and Hariharan, Jayaram and Barefoot, Eric and Passalacqua, Paola "pyDeltaRCM: a flexible numerical delta model" Journal of Open Source Software , v.6 , 2021 https://doi.org/10.21105/joss.03398 Citation Details

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The sustainability of coastal river-deltas is impacted by a multitude of natural and anthropogenic factors, including a limited understanding of subsurface flow patterns. Geological heterogeneity strongly influences flow pathways and thus rates of contaminant transport and groundwater aquifer recharge, which limits our ability to sustainably manage water resources and mitigate health risks in river-delta environments. This project studied the organization of delta stratigraphy at different spatial scales, and improved our understanding of subsurface flow pathways in delta settings. The project did not identify scale invariant stratigraphy in modeled delta stratigraphy datasets, but did uncover relationships between intensity and frequency of river flows and the stratigraphy statistics. The project also used a generative model to assess uncertainty in contaminant transport timescales through the subsurface of deltaic islands. These findings have broad implications for the water resource management, including improved pollutant transport modeling, and groundwater allocation and management.

 

Software development for the research community was also an integral part of the project. The pyDeltaRCM numerical delta model (https://github.com/DeltaRCM/pyDeltaRCM) is a flexible and extensible implementation of a popular numerical delta model, built for communityuse. A prototype analysis package for surface processes and stratigraphic analysis in sedimentary systems, provisionally called DeltaMetrics was developed under the scope of this project as well (https://github.com/DeltaRCM/DeltaMetrics). Finally, the PI mentored one undergraduate student with project support, and enhanced the collection of to active learning modules for topics in sedimentary stratigraphy in the SedEdu educational platform.

 


Last Modified: 12/05/2023
Modified by: Andrew J Moodie

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