What is he best known for?
The fields of study he is best known for:
- Oceanography
- Ecology
- Carbon dioxide
The scientist’s investigation covers issues in Geochemistry, Seawater, Hydrothermal circulation, Mineralogy and Basalt.
His work on Weathering as part of his general Geochemistry study is frequently connected to Alkalinity, thereby bridging the divide between different branches of science.
His studies in Seawater integrate themes in fields like Authigenic, Diagenesis, Fractionation, Isotope fractionation and Environmental chemistry.
His Hydrothermal circulation research is multidisciplinary, incorporating perspectives in Seabed, Ridge and Oceanic crust.
In his research on the topic of Seabed, Fluvial and Oceanography is strongly related with Groundwater.
In his work, Pellets, Settling and Mixed layer is strongly intertwined with Mass flux, which is a subfield of Mineralogy.
His most cited work include:
- Submarine Thermal Springs on the Galápagos Rift (1356 citations)
- Geochemistry of the Amazon: 2. The influence of geology and weathering environment on the dissolved load (998 citations)
- Chemistry of submarine hydrothermal solutions at 21 °N, East Pacific Rise (792 citations)
What are the main themes of his work throughout his whole career to date?
John M. Edmond focuses on Geochemistry, Oceanography, Hydrothermal circulation, Seawater and Mineralogy.
His study in Geochemistry is interdisciplinary in nature, drawing from both Guaymas Basin, Seafloor spreading and Oceanic crust.
He works mostly in the field of Oceanography, limiting it down to topics relating to Barium and, in certain cases, Radium, as a part of the same area of interest.
His Hydrothermal circulation study incorporates themes from Basalt, Mid-ocean ridge and Ridge.
His Seawater research includes themes of Chemical composition, Analytical chemistry, Environmental chemistry, Geochemical cycle and Authigenic.
John M. Edmond combines subjects such as Particulates and Plume with his study of Mineralogy.
He most often published in these fields:
- Geochemistry (37.33%)
- Oceanography (30.00%)
- Hydrothermal circulation (30.00%)
What were the highlights of his more recent work (between 1991-2013)?
- Geochemistry (37.33%)
- Weathering (15.33%)
- Hydrothermal circulation (30.00%)
In recent papers he was focusing on the following fields of study:
Geochemistry, Weathering, Hydrothermal circulation, Mineralogy and Seawater are his primary areas of study.
His Geochemistry study integrates concerns from other disciplines, such as Sediment, Earth science and Geochemical cycle.
His Weathering research incorporates themes from Metamorphism, Tributary, Fluvial and Evaporite.
John M. Edmond works mostly in the field of Hydrothermal circulation, limiting it down to concerns involving Ridge and, occasionally, Mid-Atlantic Ridge.
His Mineralogy research incorporates elements of Sedimentary depositional environment, Radium, Chronology and Chimney.
Seawater is a subfield of Oceanography that John M. Edmond explores.
Between 1991 and 2013, his most popular works were:
- Volcanic eruption of the mid-ocean ridge along the East Pacific Rise crest at 9°45-52'N: Direct submersible observations of seafloor phenomena associated with an eruption event in April, 1991 (404 citations)
- Controls over the strontium isotope composition of river water (392 citations)
- Lithium isotopic composition of submarine basalts: implications for the lithium cycle in the oceans (340 citations)
In his most recent research, the most cited papers focused on:
- Oceanography
- Ecology
- Carbon dioxide
John M. Edmond spends much of his time researching Geochemistry, Weathering, Mineralogy, Basalt and Hydrothermal circulation.
John M. Edmond has researched Geochemistry in several fields, including Seawater and Isotope fractionation.
His Seawater research is multidisciplinary, incorporating perspectives in Authigenic, Sediment, Sediment–water interface and Geochemical cycle.
His Weathering study integrates concerns from other disciplines, such as Lithology, Fluvial, Evaporite and Isotopes of strontium.
Mid-ocean ridge is the focus of his Basalt research.
His study in Hydrothermal circulation is interdisciplinary in nature, drawing from both Vulcanian eruption and Magma.
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