All abstracts by Kevin G. Knauss in conference series: Goldschmidt

(2017) Kinetics of D/H Fractionation between H₂O and Dissolved H₂ at Hydrothermal Conditions
Pester N, Conrad M & Knauss K

(2017) Tackling Some Geochemical Challenges Raised by Enhanced Geothermal Systems (EGS): The Example of Soultz-Sous-Forêts, France
Daval D, Pollet-Villard M, Ackerer P, Schmittbuhl J, Knauss K & Fritz B

(2016) The Corrosivity of Geothermal Fluids and their Scale-Forming Potential
Mundhenk N, Knauss K, Huttenloch P & Kohl T

(2015) Microstructural Modifications of Dissolving Silicate Minerals: Why Should We Bother?
Daval D, Pollet-Villard M, Ackerer P, Fritz B, Rémusat L, Guyot F, Bernard S, Saldi G & Knauss K

(2015) Mechanisms and Rates of Dolomite Dissolution from Single-Crystal Surface Microscopic Analysis
Saldi G, Voltolini M & Knauss K

(2014) Chemical Weathering Rates of Feldspars: A Stepwise Approach from Laboratory to Field Estimates
Wild B, Daval D, Imfeld G, Saldi GD & Knauss KG

(2013) Linking nm-Scale Characterizations of Altered Silicate Surface to Macroscopic Dissolution Rate Laws: New Insights Based on Diopside
Daval D, Hellmann R, Saldi GD, Wirth R & Knauss KG

(2013) Physico-Chemical Evolution of Fe-Si-Rich Interfacial Layers during Olivine Carbonation Reactions
Saldi G, Guo H, Daval D, Davis J & Knauss K

(2013) Experimentally Quantifying Metabasalt Dissolution Kinetics at 25℃ and pH 2-12
Critelli T, Saldi GD, Daval D, Apollaro C, Oelkers EH, Schott J, De Rosa R, Knauss KG & Marini L

(2012) Does Diopside Dissolve Like Glass? Insights from Measurements of Nano- to Macroscale Dissolution Rates
Daval D, Saldi GD, Hellmann R & Knauss KG

(2012) Kinetic Modeling of Olivine Carbonation Reaction: Study of the Reaction Rate Dependence on Temperature and pCO₂ in Open and Closed Systems
Saldi G, Daval D & Knauss KG

(2012) On Using Natural Chemical and Isotopic Tracers to Monitor Fracture Surface Area Evolution in Enhanced Geothermal Systems
Christensen JN, Saldi GD, Spycher NF, Knauss KG & Kennedy BM

(2011) Linking Solution Composition and Surface Topography to the Rate and Mechanisms of Diopside Dissolution
Daval D, Saldi GD, Hellmann R & Knauss KG

(2011) Development of Steady-State Surface Topography and the Determination of Dolomite Dissolution Rates
Saldi GD, Daval D, Xu M, Higgins SR & Knauss KG

(2010) Scanning Probe Microscopy and Mineral-Water Interfaces: Have We Reached a Limit?
Higgins S, Xu M, Cubillas P, Lea AS, Knauss K & Rosso K

(2005) Effect of Solution Saturation State on Diopside Dissolution
Dixit S, Knauss K & Carroll S

(2000) Experimental Measurements and Modelling of Fundamental Attachment and Detachment Reactions on Barium Sulphate (001) Using Hydrothermal Scanning Probe Microscopy
Higgins S, Bosbach D, Eggleston C & Knauss K

(2000) Studies of the Dissolution of Magnesite (104) in Acidic Aqueous Solutions: A New Approach Using Hydrothermal Scanning Probe Microscopy Under Controlled Hydrodynamic Conditions
Higgins S, Jordan G, Coles B, Compton R, Eggleston C, Knauss K & Boro C