The Dissolution of Olivine Added to Soil at 4°C: Implications for Enhanced Weathering in Cold Regions

The Dissolution of Olivine Added to Soil at 4°C: Implications for Enhanced Weathering in Cold Regions

Crushed olivine was added to a soil core to mimic enhanced weathering, and water was continually dripped through for ~6 months. Our experiments were conducted at 4°C, and are compared to previously run identical experiments at 19°C. Olivine dissolution rates in both experiments start out similar, li...

Full description

Bibliographic Details
Main Authors: Philip A. E. Pogge von Strandmann, Chloe Tooley, Josephina J. P. A. Mulders, Phil Renforth
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-02-01
Series:Frontiers in Climate
Subjects:
weathering
carbon sequestration
weathering experiment
enhanced weathering of minerals
temperature effect on weathering
Online Access:https://www.frontiersin.org/articles/10.3389/fclim.2022.827698/full

Internet

https://www.frontiersin.org/articles/10.3389/fclim.2022.827698/full

Similar Items