about
Rapid carbon mineralization for permanent disposal of anthropogenic carbon dioxide emissions.The impact of damming on riverine fluxes to the ocean: A case study from Eastern Iceland.High reactivity of deep biota under anthropogenic CO2 injection into basaltSurface charge and zeta-potential of metabolically active and dead cyanobacteria.The dissolution rates of SiO2 nanoparticles as a function of particle size.The effect of pH, grain size, and organic ligands on biotite weathering ratesPrecipitation of Iron and Aluminum Phosphates Directly from Aqueous Solution as a Function of Temperature from 50 to 200 °CAn experimental study of hydroxylbastnasite solubility in aqueous solutions at 25 °CThe efficient long-term inhibition of forsterite dissolution by common soil bacteria and fungi at Earth surface conditionsBiotite surface chemistry as a function of aqueous fluid compositionThe direct precipitation of rhabdophane (REEPO4·nH2O) nano-rods from acidic aqueous solutions at 5–100 °CAn Experimental Investigation of the Effect of Bacillus megaterium on Apatite DissolutionUsing Mg Isotopes to Trace Cyanobacterially Mediated Magnesium Carbonate Precipitation in Alkaline LakesAn experimental study of magnesite precipitation rates at neutral to alkaline conditions and 100–200°C as a function of pH, aqueous solution composition and chemical affinityDoes the presence of heterotrophic bacterium Pseudomonas reactans affect basaltic glass dissolution rates?Magnesium isotope fractionation during hydrous magnesium carbonate precipitation with and without cyanobacteriaDo organic ligands affect calcite dissolution rates?An experimental study of magnesite dissolution rates at neutral to alkaline conditions and 150 and 200°C as a function of pH, total dissolved carbonate concentration, and chemical affinityDo photosynthetic bacteria have a protective mechanism against carbonate precipitation at their surfaces?The surface chemistry of multi-oxide silicatesExperimental determination of synthetic NdPO4 monazite end-member solubility in water from 21°C to 300°C: implications for rare earth element mobility in crustal fluidsAn experimental study of the dissolution stoichiometry and rates of a natural monazite as a function of temperature from 50 to 230 °C and pH from 1.5 to 10Ocean margins: The missing term in oceanic element budgets?Does variscite control phosphate availability in acidic natural waters? An experimental study of variscite dissolution ratesAn experimental study of the dissolution mechanism and rates of muscoviteStandards for publication of isotope ratio and chemical data in Chemical GeologyA brief history of CarbFix: Challenges and victories of the project’s pilot phaseExperimental determination of the dissolution rates of calcite, aragonite, and bivalvesHow do mineral coatings affect dissolution rates? An experimental study of coupled CaCO3 dissolution—CdCO3 precipitationRole of river-suspended material in the global carbon cycleAn experimental study of basaltic glass–H2O–CO2 interaction at 22 and 50°C: Implications for subsurface storage of CO2Carbon Storage in BasaltInter-mineral Mg isotope fractionation during hydrothermal ultramafic rock alteration – Implications for the global Mg-cycleQuantifying the impact of riverine particulate dissolution in seawater on ocean chemistryThe chemistry and element fluxes of the July 2011 Múlakvísl and Kaldakvísl glacial floods, IcelandThe role of silicate surfaces on calcite precipitation kineticsDo carbonate precipitates affect dissolution kinetics?Do organic ligands affect forsterite dissolution rates?Does temperature or runoff control the feedback between chemical denudation and climate? Insights from NE IcelandExperimental determination of rhyolitic glass dissolution rates at 40–200°C and 2<pH<10.1
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description
researcher
@en
wetenschapper
@nl
հետազոտող
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name
Eric H Oelkers
@ast
Eric H Oelkers
@en
Eric H Oelkers
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Eric H Oelkers
@nl
type
label
Eric H Oelkers
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Eric H Oelkers
@en
Eric H Oelkers
@es
Eric H Oelkers
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prefLabel
Eric H Oelkers
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Eric H Oelkers
@en
Eric H Oelkers
@es
Eric H Oelkers
@nl
P106
P1153
35280527300
P31
P496
0000-0002-5759-524X