In:
Earth and Space Science, American Geophysical Union (AGU), Vol. 6, No. 11 ( 2019-11), p. 2115-2141
Abstract:
Changjiang (Yangtze River) export flux of total alkalinity varied around a nearly stable average over the past 55 years Terrestrial carbonate input from Changjiang decreased the freshwater‐dilution‐induced coastal aragonite saturation state suppression by 12% More than 10% of wet‐season DIC flux discharged from Changjiang was sequestered in coastal zones, while the TAlk flux was rarely affected
Type of Medium:
Online Resource
ISSN:
2333-5084
,
2333-5084
DOI:
10.1029/2019EA000679
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2807271-6