Geochemistry of the Carbonate Cycle in the Marine Environment
Abstract
The carbonate cycle in the marine environment is characterized by very slow reaction rates and chemical disequilibrium. The cycle involves atmospheric CO2, dissolved calcium and carbon ions and complexes, suspended mineral particles, sediments, and living organisms. The report summarizes the authors contribution to the understanding of the slow reaction rates in this cycle has been the demonstration that organic compounds in seawater are a major factor regulating reaction rates.
Document Details
- Document Type
- Technical Report
- Publication Date
- Dec 28, 1970
- Accession Number
- AD0716049
Entities
People
- Keith E. Chave
Organizations
- University of Hawaiʻi System