SEARCH · Search NASA
Results for “ORGANIZING”
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.
Quote a phrase for an exact phrase match. Source license links do not imply unrestricted reuse.
Synthesis and characterization of tetrairidium clusters in the metal organic framework UiO-67: Catalyst for ethylene hydrogenation
Not provided.
Processing Strategies for an Organic Photovoltaic Module with over 10% Efficiency
Abstract not provided
How alginate monomers contribute to organic fouling on polyamide membrane surfaces?
Not provided.
Defects in local atomic structure of ZnO films sensitized with tinto and mangrove organic dyes
Not provided.
Molecular heterogeneity in pyrogenic dissolved organic matter from a thermal series of oak and grass chars
Explore the source record for details and available documents.
Cation-exchanged conductive Mn2DSBDC metal-organic frameworks: Synthesis, structure, and THz conductivity
Explore the source record for details and available documents.
Radon measurements with a compact, organic-scintillator-based alpha/beta spectrometer
Not provided.
Issatchenkia orientalis as a platform organism for cost-effective production of organic acids
Not Available
FSM: Fast and scalable network motif discovery for exploring higher-order network organizations
Not provided.
Interfacial and Confinement-Mediated Organization of Gas Hydrates, Water, Organic Fluids, and Nanoparticles for the Utilization of Subsurface Energy and Geological Resources
Harnessing the subsurface geologic environments in an efficient and environmentally sustainable manner is challenged by uncertainties associated with predicting the fate of fluids and sustaining porosity and permeability in subsurface geologic environments. Some of these uncertainties arise from confined and interfacially induced structures of fluids in subsurface geologic environments. The formation of gas hydrates, phase transitions of confined fluids, assembly and deposition of heavy hydrocarbons, and the agglomeration and fate of nanoparticles in confined environments are summarized in this review. Nanoscale confinement contributes to anisotropic structures and dynamics of fluids, which is the basis for anomalous phase transition thermodynamics, reactivity, transport, and geomechanical behavior. In this review, we discuss the structures of confined fluids and deviation in observed properties from bulk fluids. The factors influencing the structures of confined fluids can be generally divided into two groups: (a) pore characteristics including pore size, pore surface chemistry, and pore geometry and (b) confined fluid/solid characteristics such as molecular structure, concentrations, charges, pore filling, and presence of additives. Scientific advancements and knowledge gaps in our understanding of the structures of confined fluids and the associated differences in observed properties compared to bulk fluids are discussed. Here, the phenomena discussed in this review are of particular relevance to our efforts in harnessing the subsurface environments for a low carbon future by increasing the utilization of geothermal energy, using CO 2 as a working fluid, and storing CO 2 in subsurface geologic environments.