thermal

Analysis of the impact of the location of a window type air-conditioner on thermal comfort in an office room




thermal

Thermal analyses of hydrophilic polymers used in nanocomposites and biocompatible coatings




thermal

Evaluation of geophysical and thermal methods for detecting submarine groundwater discharge (SGD) in the Suwannee River estuary, Florida




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Zeolite synthesis from municipal solid waste ash using fusion and hydrothermal treatment




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Improved techniques for nonlinear electrothermal FET modeling and measurement validation




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Biogeochemical cycling of arsenic in the shallow marine hydrothermal system of Tutum Bay, Ambitle Island, Papua New Guinea




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Crack patterns in thin films and X-ray optics thermal deformations




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Foraminiferal responses to arsenic in a shallow-water hydrothermal system in papua new guinea and in the laboratory




thermal

Investigation of residual and thermal stress on membrane-based MEMS devices




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Diffuse degassing and the hydrothermal system at masaya volcano, nicaragua




thermal

Photothermal studies of carboxymyoglobin




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Effects of a shallow-water hydrothermal vent gradient on benthic calcifiers, tutum bay, ambitle island, papua new guinea




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The biocomplexity of benthic communities associated with a shallow-water hydrothermal system in papua new guinea




thermal

The monitoring and evaluation of geothermal systems




thermal

Thermal conductivity of soils from the analysis of boring logs




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Thermal response of lithium tantalate for temperature measurement




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Stable carbon isotope compositions during the thermal alteration of organic matter




thermal

Aircraft­borne Thermal and Visible Imagery Acquisition and Ground Data­ Instrument Recovery of Caves, Mojave Desert, California




thermal

Application of thermal imagery and aerial photography to hydrologic studies of karst terrane in Missouri




thermal

Census of the endangered Mexican long-nosed bat Leptonycteris nivalis in Texas, USA, using thermal imaging




thermal

Detecting Terrestrial Caves by Applying Topographic Analysis Techniques to Thermal Imagery




thermal

Thermal springs of the United States and other countries of the world; a summary




thermal

Metabolic rate, latitude and thermal stability of roosts, but not phylogeny, affect rewarming rates of bats




thermal

Subtropical mouse-tailed bats use geothermally heated caves for winter hibernation




thermal

Modified Cave Entrances: Thermal Effect on Body Mass and Resulting Decline of Endangered Indiana Bats (Myotis sodalis)




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Community Structure of Subsurface Biofilms in the Thermal Sulfidic Caves of Acquasanta Terme, Italy




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6.6 Karstification by Geothermal Waters




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Hydrothermal Dissolution of Ordovician Carbonates Rocks and its dissolution mechanism in Tarim Basin, China




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Community Structure of Subsurface Biofilms in the Thermal Sulfidic Caves of Acquasanta Terme, Italy




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[ASAP] Smart Assembled Human Serum Albumin Nanocarrier Enhanced Breast Cancer Treatment and Antitumor Immunity by Chemo- photothermal Therapy

ACS Biomaterials Science & Engineering
DOI: 10.1021/acsbiomaterials.0c00286




thermal

[ASAP] Cells-Grab-on Particles: A Novel Approach to Control Cell Focal Adhesion on Hybrid Thermally Annealed Hydrogels

ACS Biomaterials Science & Engineering
DOI: 10.1021/acsbiomaterials.0c00119




thermal

Theoretical thermotics: transformation thermotics and extended theories for thermal metamaterials / Ji-Ping Huang

Online Resource




thermal

18th International Topical Meeting on Nuclear Reactor Thermal Hydraulics: NURETH-18: Portland, OR, August 18-22, 2019

Dewey Library - TK9202.I537 2019




thermal

Thermosense: Thermal Infrared Applications XXXVIII: 18-21 April 2016, Baltimore, Maryland, United States / Joseph N. Zalameda, Paolo Bison, editors ; sponsored by SPIE ; co-sponsored by FLIR Systems, Inc., IRCameras LLC

Online Resource




thermal

Through-space interactions in thermally activated delayed fluorescent emitters : novel materials and organic light emitting diodes / Nidhi Sharma.

St Andrews, 2020.




thermal

[ASAP] Determining the Ternary Phase Diagram of Benzene–Acetic Acid–Water Using Isothermal Titration Microcalorimetry to Train Upper-Level Undergraduates in Advanced Calorimetry Methods

Journal of Chemical Education
DOI: 10.1021/acs.jchemed.0c00002




thermal

[ASAP] Preparation and Thermochromic Switching between Phosphorescence and Thermally Activated Delayed Fluorescence of Mononuclear Copper(I) Complexes

Journal of Chemical Education
DOI: 10.1021/acs.jchemed.0c00171




thermal

[ASAP] Hydrothermal Synthesis and Characterization of Titanosilicate ETS-10: Preparation for Research Integrated Inorganic Chemistry Laboratory Course

Journal of Chemical Education
DOI: 10.1021/acs.jchemed.0c00165




thermal

Glacier surge propagation by thermal evolution at the bed

Glacier surge propagation by thermal evolution at the bed Murray, Tavi; Stuart, Graham W.; Miller, Paul J.; Woodward, John; Smith, Andrew M.; Porter, Philip R.; Jiskoot, Hester Bakaninbreen, southern Svalbard, began a prolonged surge during 1985. In 1986, an internal reflecting horizon on radio echo sounding data was interpreted to show that the position of the surge front coincided with a transition between areas of warm (unfrozen) and cold (frozen) bed. Ground-penetrating radar lines run in 1996 and 1998 during early quiescence show that the basal region of the glacier is characterized by a strong reflection, interpreted as the top of a thick layer of sediment-rich basal ice. Down glacier of the present surge front, features imaged beneath the basal reflection are interpreted as the bottom of the basal ice layer, the base of a permafrost layer, and local ice lenses. This indicates that this region of the bed is cold. Up glacier of the surge front, a scattering zone above the basal reflection is interpreted as warm ice. There is no evidence for this warm zone down glacier of the surge front, nor do we see basal permafrost up glacier of it. Thus, as in early surge phase, the location of the surge front is now at the transition between warm and cold ice at the glacier bed. We suggest that the propagation of the front is associated with this basal thermal transition throughout the surge. Because propagation of the front occurs rapidly and generates only limited heat, basal motion during fast flow must have been restricted to a thin layer at the bed and occurred by sliding or deformation localized at the ice-bed interface. Sherpa Romeo green journal. Permission to archive final published version.




thermal

Graphene-based device enables active thermal camouflage

Smart, flexible skins measure and adapt to ambient temperatures




thermal

Boron arsenide boasts high thermal conductivity

Semiconductor could help dissipate waste heat in electronics




thermal

Graphene-based device enables active thermal camouflage

Smart, flexible skins measure and adapt to ambient temperatures




thermal

Thermal insulation materials for building applications / Eshrar Latif, Rachel Bevan and Tom Woolley

Barker Library - TH1715.L38 2019