Global silicate weathering flux over-estimated 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/10.17863/cam.63321
Publication URI: https://www.repository.cam.ac.uk/handle/1810/316213
Type: Journal Article/Review