What is he best known for?
The fields of study he is best known for:
- Composite material
- Thermodynamics
- Optics
His scientific interests lie mostly in Geotechnical engineering, Brittleness, Cataclastic rock, Compaction and Porosity.
In his articles, he combines various disciplines, including Geotechnical engineering and Fluid transport.
His work deals with themes such as Creep, Yield and Overburden pressure, which intersect with Brittleness.
His studies in Cataclastic rock integrate themes in fields like Compressive strength, Hardening and Dilatant.
His studies deal with areas such as Shear and Strain hardening exponent as well as Compaction.
The various areas that Patrick Baud examines in his Porosity study include Mineralogy and Permeability.
His most cited work include:
- The brittle-ductile transition in porous rock: A review (295 citations)
- Time-dependent cracking and brittle creep in crustal rocks: A review (292 citations)
- Compaction localization in porous sandstones: spatial evolution of damage and acoustic emission activity (275 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Porosity, Geotechnical engineering, Compaction, Brittleness and Mineralogy.
He combines subjects such as Carbonate rock, Microstructure, Permeability and Anisotropy with his study of Porosity.
His research integrates issues of Compressive strength, Stress corrosion cracking and Deformation in his study of Geotechnical engineering.
He interconnects Shear, Cataclastic rock, Acoustic emission and Strain hardening exponent in the investigation of issues within Compaction.
His Brittleness study combines topics in areas such as Creep and Deformation.
His study in Mineralogy is interdisciplinary in nature, drawing from both Deformation bands, Tomography and Carbonate.
He most often published in these fields:
- Porosity (32.34%)
- Geotechnical engineering (29.85%)
- Compaction (29.35%)
What were the highlights of his more recent work (between 2015-2021)?
- Permeability (22.89%)
- Porosity (32.34%)
- Composite material (20.40%)
In recent papers he was focusing on the following fields of study:
Patrick Baud mainly focuses on Permeability, Porosity, Composite material, Geothermal gradient and Petrology.
The concepts of his Permeability study are interwoven with issues in Fluid dynamics, Effective stress, Anisotropy and Volcanic rock.
Patrick Baud has researched Porosity in several fields, including Compaction, Dissolution, Cementation, Thermal diffusivity and Mineralogy.
His work carried out in the field of Compaction brings together such families of science as Brittleness, Cataclastic rock and Carbonate.
Patrick Baud has included themes like Creep, Shear, Overburden pressure and Deformation in his Brittleness study.
In his work, Cracking is strongly intertwined with Thermal, which is a subfield of Composite material.
Between 2015 and 2021, his most popular works were:
- Quantification of microcrack characteristics and implications for stiffness and strength of granite (63 citations)
- Thermal Cracking in Westerly Granite Monitored Using Direct Wave Velocity, Coda Wave Interferometry, and Acoustic Emissions (54 citations)
- A multidisciplinary approach to quantify the permeability of the Whakaari/White Island volcanic hydrothermal system (Taupo Volcanic Zone, New Zealand) (52 citations)
In his most recent research, the most cited papers focused on:
- Composite material
- Thermodynamics
- Sedimentary rock
Patrick Baud spends much of his time researching Permeability, Petrology, Mineralogy, Porosity and Volcanic rock.
His biological study spans a wide range of topics, including Geothermal gradient, Graben and Rock mass classification.
His Mineralogy study incorporates themes from Volcano, Lava, Sedimentary rock and Hydrothermal circulation.
The study incorporates disciplines such as Fluid dynamics, Stylolite, Compaction and Anisotropy in addition to Porosity.
His Compaction research is multidisciplinary, relying on both Cataclastic rock, Carbonate and Stress–strain curve.
He works mostly in the field of Cataclastic rock, limiting it down to concerns involving Brittleness and, occasionally, Overburden pressure.
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