Mountainous Floodplain Connectivity in Response to Hydrological Transitions

Mountainous Floodplain Connectivity in Response to Hydrological Transitions

Abstract In mountainous watersheds, floodplain sediments are typically characterized by gravel bed layers capped by an overlying soil unit that serves as a hotspot for biogeochemical reactivity. However, the influence of soil biogeochemistry on gravel bed underflow composition remains unclear, espec...

Full description

Saved in:
Bibliographic Details
Main Authors: Tristan Babey, Zach Perzan, Sam Pierce, Brian Rogers, Lijing Wang, Rosemary W. H. Carroll, John R. Bargar, Kristin Boye, Kate Maher
Format: Article
Language:English
Published: Wiley 2024-07-01
Series:Water Resources Research
Subjects:
mountainous watershed
hydrological cycle
water quality
groundwater
beavers
floodplain
Online Access:https://doi.org/10.1029/2024WR037162
Tags: Add Tag
No Tags, Be the first to tag this record!

Internet

https://doi.org/10.1029/2024WR037162

Similar Items