In water molecules from ice cores, the ratios of isotopes, 2H/¹H and 180/160 depends upon temperature of the water that precipitates from an air mass, and thus on average climatic temperatures. This allows climatologists to determine historical temperatures from analysis of the isotope ratios of hydrogen and oxygen in water molecules from ice cores. As temperature increases, the 180/160 ratio [Select] ✓and the 2H/¹H ratio [Select]

In water molecules from ice cores, the ratios of isotopes, 2H/¹H and 180/160 depends upon temperature of the water that precipitates from an air mass, and thus on average climatic temperatures. This allows climatologists to determine historical temperatures from analysis of the isotope ratios of hydrogen and oxygen in water molecules from ice cores. As temperature increases, the 180/160 ratio [Select] ✓and the 2H/¹H ratio [Select]

Fundamentals Of Analytical Chemistry

9th Edition

ISBN:9781285640686

Author:Skoog

Publisher:Skoog

Chapter27: Molecular Fluorescence Spectroscopy

Section: Chapter Questions

Problem 27.9QAP

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