Δ¹³C (delta carbon-13) is a measure used in the field of stable isotope geochemistry to express the ratio of carbon isotopes, specifically the stable isotopes carbon-12 (¹²C) and carbon-13 (¹³C). The delta notation is used to give the relative difference in the isotopic composition of a sample compared to a standard reference material.

Articles by others on the same topic (0)

There are currently no matching articles.