Isotope fractionation (O17 mass-independent)

Layer 2 — Chemistryin the atmospheric-chemistry subtree

Thiemens-Heidenreich 1983 mass-independent fractionation in stratospheric O3 + via SO2-photolysis; Delta17O signal traces atmospheric O3 oxidation pathways back through Archean.

Related concepts

Matrix and determinant

Explore Isotope fractionation (O17 mass-independent) on the interactive knowledge graph →