#LPSC2023
#LPSC2023

Program with Links to Abstracts
Schedule Overview
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Poster Session: Lunar Regolith, Dust, and Plasma
Thursday, March 16, 2023, 6:30 PM
Town Hall Exhibit Area
Kirchoff M. R.*
Marchi S.
Regolith Layer Depths at Apollo Landing Sites and Effects on Crater SFDs
[#2293]
Use unusual morphology craters to assess plausible layer depths at several Apollo sites and effects on crater SFDs and absolute model production function ages.
Use unusual morphology craters to assess plausible layer depths at several Apollo sites and effects on crater SFDs and absolute model production function ages.
Thaker A. D.*
Neish C. D.
Regolith Depth Estimations Around Radar-Dark Halo Craters on the Moon
[#1117]
Our study focuses on regolith depth estimations for radar-dark halo craters on the Moon using specific small crater morphology to understand their mechanism.
Our study focuses on regolith depth estimations for radar-dark halo craters on the Moon using specific small crater morphology to understand their mechanism.
Long-Fox J.*
Mueller R.
Bell E.
Dudzinski K.
Peacock B.
et al.
COLDArm Pressure-Sinkage Testing: Implications for Assessing Lunar Trafficability
[#2165]
On-site testing of regolith properties using standard exploration hardware will provide different insights than analyses based on remote sensing data.
On-site testing of regolith properties using standard exploration hardware will provide different insights than analyses based on remote sensing data.
Anderson R. C.*
Chin K.
Chi I.
Wei T.
Development of a New Lunar Simulant for Geotechnical Applications
[#1854]
There is an important need for detailed characterization of lunar regolith physical properties critical for future missions involving surface contact.
There is an important need for detailed characterization of lunar regolith physical properties critical for future missions involving surface contact.
Martin A. C.*
Stockstill-Cahill K. R.
Wagoner C. M.
Kovtun R. N.
Gruener J. E.
Lunar Surface Innovation Initiative: Geotechnical Evaluation of Lunar Regolith Simulants
[#2695]
This year’s assessment focused on geotechnical measurements of the eight lunar simulants: size fractions, minimum and maximum density, specific gravity, and shear strength.
This year’s assessment focused on geotechnical measurements of the eight lunar simulants: size fractions, minimum and maximum density, specific gravity, and shear strength.
Lucas M. P.*
Neal C. R.
Long-Fox J.
Conway J.
Glover A.
et al.
Lunar Locomotion: Geotechnical Assessment of Trafficability On Regolith (GATOR)
[#2463]
A new dance — lunar locomotion — will keep on rollin’ in GATOR, a project to measure the effect of repeated traffic on the geomechanical properties of lunar regolith.
A new dance — lunar locomotion — will keep on rollin’ in GATOR, a project to measure the effect of repeated traffic on the geomechanical properties of lunar regolith.
Lorenzo J. M.*
Zanetti M. R.
Bremner P. M.
Patterson D. A.
Tsoflias G.
et al.
Lunar Regolith Terrain Field at NASA Marshall Space Flight Center
[#1520]
The Lunar Regolith Terrain (LRT) field is an outdoor planetary analog environment facility located onbase at Marshall Space Flight Center, Huntsville, Alabama, U.S.A.
The Lunar Regolith Terrain (LRT) field is an outdoor planetary analog environment facility located onbase at Marshall Space Flight Center, Huntsville, Alabama, U.S.A.
Gruener J. E.*
Rickman D. L.
Wilson S. A.
Edmunson J. E.
Kleinhenz J. E.
et al.
The Complete Series of NU-LHT Lunar Simulants
[#2238]
This poster will describe all of the lunar highlands type simulants developed by NASA and USGS (NU-LHT) to support NASA’s Constellation and Artemis Programs.
This poster will describe all of the lunar highlands type simulants developed by NASA and USGS (NU-LHT) to support NASA’s Constellation and Artemis Programs.
Dotson B.*
Sargeant H.
Millwater C.
Easter P.
Sanchez Valencia D.
et al.
New Insights into the Physical Properties of Regolith
[#1406]
The effects of density, particle size distribution, and absorbed water on regolith shear strength and cohesion are discussed for plume-surface interaction tests.
The effects of density, particle size distribution, and absorbed water on regolith shear strength and cohesion are discussed for plume-surface interaction tests.
Wyrick D. Y.*
Anderson R. C.
Buczkowski D. L.
Chin K.
Colaprete A.
et al.
Geomechanical Characterization of Planetary Regolith Using the SPARTA Toolkit
[#2421]
SPARTA is a miniature suite of instruments capable of measuring the mechanical, thermal, electrical, and chemical properties of dry and/or icy regolith.
SPARTA is a miniature suite of instruments capable of measuring the mechanical, thermal, electrical, and chemical properties of dry and/or icy regolith.
Sargeant H. M.*
Long-Fox J.
Dyson J.
Donaldson Hanna K. L.
Britt D.
Developing the Simulator for Planetary Interactions of Dust and Regolith (SPIDR)
[#1678]
Modeling Moon dust / Is harder than it first seemed / Keep calm, carry on. .
Modeling Moon dust / Is harder than it first seemed / Keep calm, carry on. .
Lewis E. K.*
Ghosh S.
Jakubek R. S.
Amick C. L.
Stopar J. D.
et al.
Examination of Lunar Regolith Simulants by SEM-EDS and Imaging Raman Spectroscopy
[#2307]
The utilization of SEM-EDS and Raman microscopy upon simulated lunar regolith for analysis of elemental spectral mapping and particle size distribution characterization.
The utilization of SEM-EDS and Raman microscopy upon simulated lunar regolith for analysis of elemental spectral mapping and particle size distribution characterization.
Kovtun R.*
Walker S.
Gruener J.
Quantitative Characterization of Lunar Regolith Simulants for Direct Comparison to Apollo Soil Samples
[#1688]
The Simulant Development Lab (JSC) is characterizing simulant properties and producing Figures of Merit for comparison of lunar simulants to Apollo samples.
The Simulant Development Lab (JSC) is characterizing simulant properties and producing Figures of Merit for comparison of lunar simulants to Apollo samples.
Kovtun R.*
Gruener J.
3D Particle Geometry Characterization of Apollo Regolith Samples via Laser Diffraction and Dynamic Image Analysis
[#1694]
Characterization of 3D particle geometry of lunar regolith samples with varying maturity levels and compositions creating a reference point for lunar simulants.
Characterization of 3D particle geometry of lunar regolith samples with varying maturity levels and compositions creating a reference point for lunar simulants.
Fackrell L. E.*
Simpson A. C.
Palmer A. G.
Singh N. K.
Venkateswaran K. J.
Nanopore Sequencing for Characterizing the Microbial Communities in Regolith Simulant-Based Soil-Like-Substrates
[#1566]
Characterization of regolith simulants and simulant-derived mediums endogenous and experimental microbiome with nanopore sequencing.
Characterization of regolith simulants and simulant-derived mediums endogenous and experimental microbiome with nanopore sequencing.
Roth M. C.*
Roux V. G.
Roux E. L.
Research and Development Applications of Lunar Regolith Simulants with Increased Magnetic Response
[#2920]
Lunar regolith simulants with a range of magnetic responses are vital for understanding the effects of regolith on lunar technology and ISRU processes.
Lunar regolith simulants with a range of magnetic responses are vital for understanding the effects of regolith on lunar technology and ISRU processes.
Whittington A. G.*
Morrison A. A.
Parsapoor A.
Patridge A. M.
Thermal and Rheological Properties of Lunar Simulants from Ambient to Molten to Glass
[#2811]
Lunar simulants / Enthalpy, viscosity / Mare and highlands.
Lunar simulants / Enthalpy, viscosity / Mare and highlands.
Austen D. H.*
Shafirovich E.
Specific Heats and Thermal Diffusivities of LHS-1 Lunar Regolith Simulant at Low Temperatures
[#1204]
For the development of thermal methods for water extraction on the polar regions of the Moon, knowledge of thermophysical properties of icy regolith is crucial.
For the development of thermal methods for water extraction on the polar regions of the Moon, knowledge of thermophysical properties of icy regolith is crucial.
Zinecker A. A.*
Spivey B. H.
Thermo-Optical Properties of Lunar Dust Simulants
[#1294]
Thirteen lunar dust simulants’ IR emissivity and solar absorptivity were measured.
Thirteen lunar dust simulants’ IR emissivity and solar absorptivity were measured.
Boll D.*
Suermann P.
Preliminary Materials Testing of Concrete Canvas for Use in Lunar Dust Mitigation Applications
[#1173]
A lunar landing pad design was created from a flexible cementitious material used in Arctic conditions on Earth. Testing proved needed strength for Artemis use.
A lunar landing pad design was created from a flexible cementitious material used in Arctic conditions on Earth. Testing proved needed strength for Artemis use.
Orger N. C.*
Toyoda K.
Cho M.
Numerical Study of Electrostatic Dust Lofting Variation by Surface Parameters over the Lunar Terminator Region
[#1999]
Even though the dust charging is mainly controlled by solar wind, the charge magnitude requirement for lofting is controlled by the regolith configuration.
Even though the dust charging is mainly controlled by solar wind, the charge magnitude requirement for lofting is controlled by the regolith configuration.
Szabo P. S.*
Poppe A. R.
Biber H.
Mutzke A.
Pichler J.
et al.
Constraints for the Lunar Regolith Porosity at the Surface from Solar Wind Proton Reflection
[#1316]
Novel simulations of solar wind proton reflection from the Moon can only explain spacecraft observations with a regolith porosity at the surface of around 85%.
Novel simulations of solar wind proton reflection from the Moon can only explain spacecraft observations with a regolith porosity at the surface of around 85%.
Choudhary R. K.*
Tripathi K. R.
Ambili K. M.
Characteristic Features of the Lunar Ionosphere Under Varying Solar Geophysical Conditions as Revealed by DFRS Onboard Chandrayaan-2
[#1939]
Experiments with DFRS onboard Chandrayaan-II show high electron density in the wake region of the Moon, followed by the solar terminator with a minimum at noon.
Experiments with DFRS onboard Chandrayaan-II show high electron density in the wake region of the Moon, followed by the solar terminator with a minimum at noon.
Sana T.*
Mishra S. K.
Non-Monotonic Potential Structure Around Sunlit Moon
[#1466]
Comments on non-monotonic potential structure within lunar photoelectron sheath using justified solar spectrum, SW flux, and adequate photoelectron distribution.
Comments on non-monotonic potential structure within lunar photoelectron sheath using justified solar spectrum, SW flux, and adequate photoelectron distribution.
Roy S.*
Tadepalli S. P.
Dastidar R. G.
Basak A.
Mukherjee A.
et al.
An MHD Modeling Approach to Understand the Dynamic Lunar Environment in the Geotail
[#1885]
Non-neutral current sheets form around the Moon during geotail transits, accelerating electrons to high energies and leading to a dynamic lunar environment.
Non-neutral current sheets form around the Moon during geotail transits, accelerating electrons to high energies and leading to a dynamic lunar environment.
*presenter