What is he best known for?
The fields of study he is best known for:
James E. Gardner mainly focuses on Magma, Geochemistry, Mineralogy, Explosive eruption and Plagioclase.
His study on Magma is covered under Volcano.
Geochemistry is closely attributed to Amphibole in his study.
His Mineralogy research incorporates elements of Nucleation, Decompression, Isothermal process, Supersaturation and Bubble.
His research on Explosive eruption often connects related topics like Lava dome.
In his research on the topic of Plagioclase, Magma chamber is strongly related with Andesite.
His most cited work include:
- Comparison of microanalytical methods for estimating H2O contents of silicic volcanic glasses (335 citations)
- Experimental phase equilibria constraints on pre‐eruptive storage conditions of the Soufriere Hills magma (209 citations)
- Fragmentation of magma during Plinian volcanic eruptions (180 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of investigation include Magma, Volcano, Geochemistry, Petrology and Pyroclastic rock.
His Magma study combines topics in areas such as Andesite, Mineralogy, Pumice and Bubble.
As a member of one scientific family, James E. Gardner mostly works in the field of Pumice, focusing on Volcanic rock and, on occasion, Igneous rock.
His study focuses on the intersection of Geochemistry and fields such as Plagioclase with connections in the field of Hornblende.
His biological study spans a wide range of topics, including Porosity and Volcanology.
James E. Gardner interconnects Vulcanian eruption and Geomorphology in the investigation of issues within Pyroclastic rock.
He most often published in these fields:
- Magma (44.20%)
- Volcano (32.61%)
- Geochemistry (34.06%)
What were the highlights of his more recent work (between 2017-2021)?
- Magma (44.20%)
- Petrology (28.99%)
- Pyroclastic rock (25.36%)
In recent papers he was focusing on the following fields of study:
Magma, Petrology, Pyroclastic rock, Volcano and Bubble are his primary areas of study.
Magma is a subfield of Geochemistry that James E. Gardner investigates.
His Petrology research is multidisciplinary, relying on both Rhyolite, Porosity and Volcanology.
His Pyroclastic rock research is multidisciplinary, incorporating elements of Sintering, Phenocryst and Silicic.
James E. Gardner combines subjects such as Lava dome, Eruption column, Dacite, Scoria and Mineralogy with his study of Phenocryst.
His Bubble research is multidisciplinary, incorporating perspectives in Viscosity and Nucleation.
Between 2017 and 2021, his most popular works were:
- Experimental sintering of ash at conduit conditions and implications for the longevity of tuffisites (17 citations)
- A general model for welding of ash particles in volcanic systems validated using in situ X-ray tomography (11 citations)
- Experimental constraints on the textures and origin of obsidian pyroclasts. (11 citations)
In his most recent research, the most cited papers focused on:
His primary scientific interests are in Rhyolite, Surface tension, Porosity, Petrology and Bubble nucleation.
The study incorporates disciplines such as Magma, Bubble and Nucleation in addition to Rhyolite.
He has included themes like Vulcanian eruption and Subaerial in his Magma study.
His Petrology research includes elements of Volcano, Pyroclastic rock and Silicic.
His Silicic research incorporates themes from Sintering, Explosive eruption and Slow cooling.
The concepts of his Bubble nucleation study are interwoven with issues in Classical nucleation theory and Supersaturation.
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