The abstract due date for the Fall 2015 National Meeting has been extended to March 30th. Session details are listed under the tab named ACS Fall 2015 Sessions. We hope to see you in Boston with us August 16-20!
The Geochemistry Division of the American Chemical Society is pleased to announce that the eighth Geochemistry Division Medal will be awarded to Dr. Donald L. Sparks for his far-reaching contributions to understanding aqueous and solid-phase speciation of metals and metalloids in the poorly ordered, dynamic materials that comprise the critical zone. Join us March 2015 at the 249th National Meeting of the American Chemical Society in Denver, Colorado to celebrate his accomplishments with a special symposium in his honor. Congratulations Dr. Sparks!
Abstracts for Pacifichem2015 are due April 3rd! To submit an abstract go to: http://www.pacifichem.org/technical-program/abstracts/
Our division chair (soon to be past division chair after the ACS Spring meeting) is organizing a session that may be of interest to many of you:
Complex Mineral Growth and Dissolution Reactions: Collaborative Experimental and Computational Perspectives (#225)
Andrew Stack firstname.lastname@example.org | Julian Gale | Paolo Raiteri | Lijun Wang
Many important geochemical reactions involve the growth and dissolution of minerals. While the description of these processes has been simplified historically, it is now understood that this approach fails to predict rates under many solution conditions, such as varying electrolyte or aqueous cation-to-anion ratio. This is because these reaction mechanisms are complex, e.g., multiple aqueous ionic species and surface sites are present and their relative importance changes with solution composition. Examples include nucleation versus advance/retreat of pre-existing monomolecular steps, clusters, and the effects of impurities. Many conventional conceptual models are being challenged by improved atomistic understanding, but as yet, process-based kinetics models built from individual reactions have had limited success, due in part to the difficulty of transitioning between scales. Successful development of process-based mineral growth and dissolution models requires a collaborative effort between modeling (both macroscopic, mesoscopic and atomistic), experiments, and measurements made in the field. In this session we will discuss current work being done to understand complex geochemical mineral surface reactions from either computational or experimental perspectives. New work highlighting understanding reaction mechanisms, atomic-level structure, kinetics, thermodynamics and upscaling of the mineral growth and dissolution processes themselves are encouraged, particularly collaborative work between modeling and experiments.