Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

Geologic controls on source water drive baseflow generation and carbon geochemistry: Evidence of nonstationary baseflow sources across multiple subwatersheds [Dataset]


Authors:
Owners: This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource.
Type: Resource
Storage: The size of this resource is 12.5 KB
Created: Jul 16, 2019 at 4:11 p.m.
Last updated: Mar 21, 2023 at 4:12 p.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 1289
Downloads: 13
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

The contributions and composition of baseflow sources across an extended recession period were quantified for six subwatersheds of varying size in a structurally complex watershed in coastal California using endmember mixing analysis and related to catchment characteristics (e.g., topography, geology, land use, and soil characteristics). Both shallow subsurface and deep groundwater reservoirs were important contributors for streamflow during low flow periods, and the composition of baseflow sources across subwatersheds was directly related to geologic indices. A binary classification of underlying bedrock permeability (e.g., low vs. high) best explained the changes in shallow subsurface water and deeper groundwater inputs through the seasonal recession. Dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), and specific UV absorbance at 254 nm (SUVA254) were used to provide additional insight into endmember characteristics and their contributions to baseflow. Stream water DIC concentrations were broadly controlled by mixing of groundwater and shallow subsurface water endmembers with relatively constant DIC concentrations, while stream water DOC concentrations reflected both spatial and temporal changes in shallow subsurface water DOC. Results from this study show (1) the importance of considering baseflow as a dynamic mixture of water from multiple sources, (2) the effect of geology on source composition at the subwatershed scale during low flow conditions, and (3) the impact of shifting baseflow sources on stream water dissolved carbon concentrations and the utility of using dissolved carbon concentrations to obtain additional insight into temporal variability in baseflow sources.

Subject Keywords

Content

Related Resources

How to Cite

Richardson, C. (2023). Geologic controls on source water drive baseflow generation and carbon geochemistry: Evidence of nonstationary baseflow sources across multiple subwatersheds [Dataset], HydroShare, http://www.hydroshare.org/resource/8b054e66289743f7b930358907e48f8e

This resource is shared under the Creative Commons Attribution-NoDerivs CC BY-ND.

http://creativecommons.org/licenses/by-nd/4.0/
CC-BY-ND

Comments

There are currently no comments

New Comment

required