KnowraSvante ArrheniusLinked fromLinked fromThe 19 pages that link to Svante Arrhenius, each with the reason it gives.All 19Related 16Compared with 3Climate changeRelated: His 1896 calculations anticipated warming from industrial carbon dioxide emissions.Chemical kineticsRelated: His equation remains a basic tool for interpreting temperature effects on rates.Brønsted–Lowry acid–base theoryCompared with: His aqueous definitions were the framework Brønsted and Lowry generalized.Arrhenius equationRelated: He introduced the equation in the nineteenth century to describe temperature effects on reaction rates.Global warmingRelated: His early estimate connected fossil-fuel emissions with possible global warming.AcidRelated: His definition linked acids to increased hydrogen-ion concentration in water.Royal Swedish Academy of SciencesRelated: His Academy membership and Nobel recognition linked him to its scientific leadership.John TyndallRelated: Arrhenius developed quantitative climate calculations building on the gas-absorption phenomenon Tyndall established.PanspermiaRelated: His 1903 proposal gave radiopanspermia a prominent early scientific formulation.Wilhelm OstwaldRelated: Ostwald championed and experimentally developed Arrhenius’s dissociation theory.Climate scienceRelated: His calculations connected fossil-fuel emissions with possible long-term warming.Walther NernstCompared with: Arrhenius’s ion-based account of solutions differed from the thermodynamic route Nernst used to analyze them.Anthropogenic climate changeRelated: His early calculations connected fossil-fuel emissions with possible planetary warming.Jacobus Henricus van ’t HoffRelated: Arrhenius developed closely related quantitative ideas about reactions and solutions.Theodor SvedbergCompared with: Arrhenius represents an earlier Swedish physical-chemistry tradition that shaped Svedberg’s scientific setting.Hans von Euler-ChelpinRelated: Arrhenius directed the Nobel Institute for Physical Chemistry where Euler-Chelpin conducted research.Climate variability and changeRelated: His calculations linked fossil-fuel emissions to possible long-term warming.History of climate change scienceRelated: His 1896 calculation connected coal burning with possible long-term warming.Law of dilutionRelated: His dissociation theory supplied the framework Ostwald’s relation quantified.
KnowraSvante ArrheniusLinked fromLinked fromThe 19 pages that link to Svante Arrhenius, each with the reason it gives.All 19Related 16Compared with 3Climate changeRelated: His 1896 calculations anticipated warming from industrial carbon dioxide emissions.Chemical kineticsRelated: His equation remains a basic tool for interpreting temperature effects on rates.Brønsted–Lowry acid–base theoryCompared with: His aqueous definitions were the framework Brønsted and Lowry generalized.Arrhenius equationRelated: He introduced the equation in the nineteenth century to describe temperature effects on reaction rates.Global warmingRelated: His early estimate connected fossil-fuel emissions with possible global warming.AcidRelated: His definition linked acids to increased hydrogen-ion concentration in water.Royal Swedish Academy of SciencesRelated: His Academy membership and Nobel recognition linked him to its scientific leadership.John TyndallRelated: Arrhenius developed quantitative climate calculations building on the gas-absorption phenomenon Tyndall established.PanspermiaRelated: His 1903 proposal gave radiopanspermia a prominent early scientific formulation.Wilhelm OstwaldRelated: Ostwald championed and experimentally developed Arrhenius’s dissociation theory.Climate scienceRelated: His calculations connected fossil-fuel emissions with possible long-term warming.Walther NernstCompared with: Arrhenius’s ion-based account of solutions differed from the thermodynamic route Nernst used to analyze them.Anthropogenic climate changeRelated: His early calculations connected fossil-fuel emissions with possible planetary warming.Jacobus Henricus van ’t HoffRelated: Arrhenius developed closely related quantitative ideas about reactions and solutions.Theodor SvedbergCompared with: Arrhenius represents an earlier Swedish physical-chemistry tradition that shaped Svedberg’s scientific setting.Hans von Euler-ChelpinRelated: Arrhenius directed the Nobel Institute for Physical Chemistry where Euler-Chelpin conducted research.Climate variability and changeRelated: His calculations linked fossil-fuel emissions to possible long-term warming.History of climate change scienceRelated: His 1896 calculation connected coal burning with possible long-term warming.Law of dilutionRelated: His dissociation theory supplied the framework Ostwald’s relation quantified.