All abstracts by Giuseppe D. Saldi in conference series: Goldschmidt

(2017) Gallium Isotope Analysis and Potential Application
Yuan W, Chen J, Birck J-L, Saldi GD & Schott J

(2017) What can We Learn from Stable Isotope Fractionation About the Mechanisms Controlling Solid-Fluid Interactions?
Schott J, Mavromatis V, Saldi G, Balan E & Oelkers E

(2017) On the Easiness of Growth of the Ordered Anhydrous Mg-Bearing Double Carbonate Norsethite
Lindner M, Saldi GD, Jordan G & Schott J

(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) Towards a Consistent Quantitative Description of Mineral Precipitation and Dissolution Rates
Schott J, Oelkers E, Benezeth P, Gautier Q, Pokrovsky O, Jordan G & Saldi G

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

(2012) Direct Evidence for Isotopic Fractionation during Congruent Dissolution, Precipitation and at Equilibrium
Oelkers E, Pearce C, Saldi G & Schott J

(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

(2009) Experimental Quantification of Kinetic Mg-Isotope Fractionation during Magnesite Precipitation
Pearce C, Saldi G, Schott J, Burton K & Oelkers E

(2009) Magnesite Growth Rates as Function of Temperature and Saturation State: An HAFM Study
Saldi GD, Jordan G, Schott J & Oelkers EH

(2009) Effects of Organic Ligands on Magnesite Precipitation Rates
Gautier Q, Saldi G, Bénézeth P, Oelkers E & Schott J

(2009) Siderite, Magnesite and Dolomite Solubility Products as a Function of Temperature
Bénézeth P, Saldi G, Schott J & Dandurand J-L

(2007) Dissolution and Precipitation Kinetics of Magnesite at Conditions Relevant for CO₂ Geologic Sequestration
Saldi G, Oelkers E, Pokrovsky O & Schott J