Abstract Details
(2020) Chesapeake Bay Acidification Buffered by Spatially-Separated Calcium Carbonate Mineral Formation and Dissolution
Cai W-J, Su J, Ni C, Testa J & lI M
https://doi.org/10.46427/gold2020.307
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12c: Room 4, Saturday 27th June 05:51 - 05:54
Wei-Jun Cai
View abstracts at 5 conferences in series
Jianzhong Su View abstracts at 4 conferences in series
Chaoying Ni
Jeremy Testa View all 2 abstracts at Goldschmidt2020
Ming Li View all 2 abstracts at Goldschmidt2020
Jianzhong Su View abstracts at 4 conferences in series
Chaoying Ni
Jeremy Testa View all 2 abstracts at Goldschmidt2020
Ming Li View all 2 abstracts at Goldschmidt2020
Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.
Submitted by Christopher Sabine on Saturday 20th June 01:51
Fascinating talk...What is the source of the CaCO3 that is dissolving in the main basin? I would think the carbonates associated with the SAV would not be transported very far because it is trapped by the vegetation and should accumulate in the sediments. So is the precipitation in the flats decoupled from the dissolution elsewhere?
We believe CaCO3 precipitated out on SAV leaves which is then transported to downstream mainstem water and dissolved there.
Fascinating talk...What is the source of the CaCO3 that is dissolving in the main basin? I would think the carbonates associated with the SAV would not be transported very far because it is trapped by the vegetation and should accumulate in the sediments. So is the precipitation in the flats decoupled from the dissolution elsewhere?
We believe CaCO3 precipitated out on SAV leaves which is then transported to downstream mainstem water and dissolved there.
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