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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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Optimal control of connected automated vehicles with event/self-triggered control barrier functions
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Micro-environmental control for efficient local cooling: Results from manikin and human participant tests
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Nanogeochemistry: Nanostructures emergent properties and their control on geochemical reactions and mass transfers.
Abstract not provided.
Controlling placement of quantum states in phosphorene nanoribbons using ligands
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HIV-1 matrix-tRNA complex structure reveals basis for host control of Gag localization
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Sensor selection and controller design method with application to turbocharged stoichiometric spark-ignited engine controls with low pressure EGR
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Stratigraphic control of landscape response to base-level fall, Young Womans Creek, Pennsylvania, USA [Caprock controls on landscape response to baselevel fall constrained by nested detrital in situ 10Be, Young Womans Creek, Pennsylvania, USA]
Landscapes are thought to respond to changes in relative base level through the upstream propagation of a boundary that delineates relict from adjusting topography. However, spatially-variable rock strength can influence the topographic expression of such transient landscapes, especially in layered rocks, where strength variations can mask topographic signals expected due to changes in climate or tectonics. Here, we analyze the landscape response to base-level fall in Young Womans Creek, a 220 km 2 catchment on the Appalachian Plateau, USA underlain by gently folded Paleozoic sedimentary rocks. We measured in situ 10 Be concentrations in stream sands from 17 nested watersheds, and used a spatially-distributed model of sediment and 10 Be production to constrain a threefold increase in the rate of base-level fall propagating upstream from the catchment outlet. Using lidar topography and a nearby detailed stratigraphic section, we map the extent of continuous, blocky, resistant sandstone strata that act as a caprock overlying more easily erodible sandstones and siltstones. The caprock influences landscape response in two ways. First, it serves as a boundary between slowly eroding (11.5 m Myr –1 ), low-sloping (3–5°) areas of relict topography and lower, steeper portions of the landscape adjusting to base-level fall. Second, hillslopes supported by the overlying caprock are armored with coarse sediment and are significantly steeper (20–30°) than hillslopes where the caprock has been eroded (10°), despite having similar erosion rates (36 m Myr –1 ) and bedrock substrate. Lastly, our results illustrate how gently dipping, layered rocks engender complicated relationships between lithology, topography and erosion rate, highlighting the importance of understanding how rock material properties influence surface processes and landscape evolution.