Global silicate weathering flux overestimated because of sediment-water cation exchange. (2021)
Attributed to:
The key to quantifying chemical weathering intensity: clay stable isotope fractionation factors
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1073/pnas.2016430118
PubMed Identifier: 33443143
Publication URI: http://europepmc.org/abstract/MED/33443143
Type: Journal Article/Review
Volume: 118
Parent Publication: Proceedings of the National Academy of Sciences of the United States of America
Issue: 1
ISSN: 0027-8424