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Search indexed NASA NTRS and DOE OSTI research on propulsion, heat transfer, battery materials and energy systems. Follow report and document links to the original sources.
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One Operator to Rule Them All: Human-Robot Interaction for Real-World and Analog Subsurface Exploration
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Robotic Localization and Multi-Sensor, 3D Mapping for Exploration of Subsurface Voids
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Accessing Mars' Climate Record Through Deep-subsurface Pulsed Plasma Discharge Drilling
No abstract provided
Near-Term Ocean Worlds Subsurface Access Mission Concepts Using Radioisotope Power Systems
No abstract provided
Enabling Technologies and Mission Concepts for Exploring the Martian Subsurface
No abstract provided
The deep subsurface of Saturn’s moon Titan as a habitable abode for life
No abstract provided
Enabling Technologies and Mission Concepts for Exploring the Martian Subsurface
No abstract provided
Architecting Near-Term Ocean Worlds Subsurface Access Mission Concepts
No abstract provided
Inferring the Subsurface Geometry and Strength of Slow-Moving Landslides
No abstract provided
Updating Lunar Subsurface Geotechnical Properties Based Upon Nonlinear Winkler Modeling of Apollo and Lunokhod Measurements
Returning human and robotic explorers to the lunar surface has identified a need for a renewed understanding of lunar geotechnical properties related to landing on and exploring the lunar surface. We review fundamental lunar geotechnical properties such as bulk density, cohesion, friction angle and shear strength, and apply new data derived from Apollo and Lunokhod geotechnical measurements to update the understanding of lunar regolith behavior. The analysis derives a new, nonlinear relationship of lunar geotechnical properties as a function of depth.
Advances in 3D Realistic Modeling of Solar-type Stars to Study Stellar Jitter and Photospheric and Subsurface Dynamics
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P- and L-Band Retrieval of Subsurface Soil Moisture and Temperature Profiles as First-Order Polynomial Function
This paper demonstrates the potential use of P and L band passive measurements to determine root zone soil moisture (SM) and soil temperature(ST). SM and ST data have been taken as a function of depth during the NASA GSFC PLEX19 experiment in the summer of 2019 at Beltsville, MD, USA. Using these data, a coherent model has been used to compute H and V brightness temperatures at frequencies of 0.8 and 1.4 GHz with an observation angle of 35 degrees. These synthetic brightness data are then used to estimate the SM and ST profiles which are represented by linear polynomials. The inversion problem is formulated as a least square problem that is solved by a global optimization method known as the Adaptive Simulated Annealing(ASA) method. Four inversion examples having different SM and ST profiles are presented. Selected results show that the standard deviation between the retrieved and measured data is less than 0.077 cm3/cm3 for SM, and 2.245 °C for ST.
Debris: Distributed Element Beamformer Radar for Ice and Subsurface Sounding
No abstract provided
3D Radiative MHD Modeling of Thermodynamical Coupling From Subsurface Layers of the Sun to Corona
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3D Radiative Hydrodynamic Modeling of Multi-Scale Flows Driven By Subsurface Turbulent Convection
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