António Pinho

ORCID: 0000-0002-1697-4702
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About
Contact & Profiles
Research Areas
  • Building materials and conservation
  • Rock Mechanics and Modeling
  • Landslides and related hazards
  • Geological and Geophysical Studies Worldwide
  • Soil and Unsaturated Flow
  • Mobile Agent-Based Network Management
  • CO2 Sequestration and Geologic Interactions
  • Distributed systems and fault tolerance
  • Hygrothermal properties of building materials
  • Karst Systems and Hydrogeology
  • Plant Surface Properties and Treatments
  • Odor and Emission Control Technologies
  • Soil Geostatistics and Mapping
  • Manufacturing Process and Optimization
  • BIM and Construction Integration
  • Service-Oriented Architecture and Web Services
  • Grouting, Rheology, and Soil Mechanics
  • Context-Aware Activity Recognition Systems
  • Geophysical and Geoelectrical Methods
  • Usability and User Interface Design
  • Technology Use by Older Adults
  • Radioactivity and Radon Measurements
  • Geotechnical and construction materials studies
  • Interactive and Immersive Displays
  • Material Dynamics and Properties

University of Évora
2012-2023

University of Aveiro
2012-2021

Ubiwhere (Portugal)
2014

Universidade Federal de Santa Catarina
2013

Instituto de Telecomunicações
2012

The use of dimension stones in architecture and civil engineering implies the knowledge several mechanical, physical, chemical properties. Even though it has been usual practice to measure physical mechanical properties same is not true for thermal such as conductivity, diffusivity, specific heat capacity, production. These are particularly important when processes related with heating cooling buildings must be considered. Thermal capacity way energy transmitted accumulated stones;...

10.4028/www.scientific.net/kem.548.231 article EN Key engineering materials 2013-04-01

The dielectric behavior of rocks affected by the known phase transition supercooled water is main problem we analyzed. Three different granitic were used to perform measurements in frequency range from 100 Hz 1 MHz and temperatures 100–350 K. Thin cylindrical samples prepared, circular electrodes established using silver conductive paint. A clear change appears at [Formula: see text] for one samples. This coincides with water. Tightly bounded confined pores rock do not crystallize 273 K, but...

10.1190/geo2013-0399.1 article EN Geophysics 2014-05-01
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