In downloading this resource contents you are ethically bound to respect the terms of this license.
Please confirm that you accept the terms of this license below before you can do any downloads for this resource.
Resource License Agreement
This resource is shared under the Creative Commons Attribution-NoCommercial CC BY-NC.
In downloading this resource contents you are ethically bound to respect the terms of this license.
Please confirm that you accept the terms of this license below before you can do any downloads for this resource.
Please wait for the process to complete.
Redirecting to the referenced web URL
The content you have requested to access is not stored in HydroShare, and we can’t guarantee its availability,
quality, security, or size. If the externally linked content is large, access may take time.
Get file URL
You have requested the URL for a file that is within a Discoverable resource.
This resource has Private Link Sharing enabled.
This means that anyone with the link will be able to access the file,
but users without the link will not be permitted unless they have "view" permission on this resource.
You have requested the URL for a file that is within a Discoverable resource.
Only you and other HydroShare users who have been granted at least "view" permission will be able to access this URL.
If you want this URL to be publicly available,
change the sharing status of your resource to "public" or enable Private Link Sharing.
You have requested the URL for a file that is within a Private resource.
This resource has Private Link Sharing enabled.
This means that anyone with the link will be able to access the file,
but users without the link will not be permitted unless they have "view" permission on this resource.
You have requested the URL for a file that is within a Private resource.
Only you and other HydroShare users who have been granted at least "view" permission will be able to access this URL.
If you want this URL to be publicly available, change the sharing status of your resource to "public" or enable Private Link Sharing.
Choose coordinates
Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
The following files/folders contain non-preferred characters in their name.
This may result in problems and you are encouraged to change the name to follow the
HydroShare preferred character set.
The following files are out of sync with the metadata changes.
DWCZ-MEF-Data from Warix et al. (2023), Local topography and hydraulic conductivity influence riparian groundwater age and groundwater-surface water connection
The western U.S. is experiencing increasing rain to snow ratios due to climate change, and scientists are uncertain how changing recharge patterns will affect future groundwater-surface water connection. We examined how watershed topography and streambed hydraulic conductivity impact groundwater age and stream discharge at eight sites along a headwater stream within the Manitou Experimental Forest, CO USA. To do so, we measured: 1) continuous stream and groundwater discharge/level and specific conductivity from April to November, 2021; 2) biweekly stream and groundwater chemistry; 3) groundwater chlorofluorocarbons and tritium in spring and fall; 4) streambed hydraulic conductivity; and 5) local slope. We used the chemistry data to calculate fluorite saturation states that were used to inform end-member mixing analysis of streamflow source. We then combined chlorofluorocarbon and tritium data to estimate the age composition of riparian groundwater. Our data suggest that future stream drying is more probable where local slope is steep and streambed hydraulic conductivity is high. In these areas, groundwater source shifted seasonally, as indicated by age increases, and we observed a high fraction of groundwater in streamflow, primarily interflow from adjacent hillslopes. In contrast, where local slope is flat and streambed hydraulic conductivity is low, streamflow is more likely to persist as groundwater age was seasonally constant and buffered by storage in alluvial sediments. Groundwater age and streamflow paired with characterization of watershed topography and subsurface characteristics enabled identification of likely controls on future stream drying patterns.
This resource contains links to external content. Linked content is
NOT stored in HydroShare, and we can't guarantee its availability, quality, or
security.
Confirm files deletion
This file will be permanently deleted. Consider saving a copy if it is
important to you. If this is the last file in the resource and it is public,
the sharing status will revert to private. If you are not the owner of
this resource, then an owner will need to reset this to public after a new
file has been added. If you want to replace this file, add the new file
first then delete the old one, so that sharing status does not change.
Manitou_2021_SW_GW_chemistry
Dataset contains chemistry data from 8 paired groundwater (GW) and surface water (SW) sites along Hotel Gulch in the Manitou Experimental forest. Sample ID describes the site location (GW or SW (n)) and the date the sample was collected. Sample collection time is listed in the second column.
Field parameters include specific conductivity (µS/cm), pH, and temperature (˚C). Cations include Al, Ba, Ca, Fe, K, Li, Mg, Mn, Na, Ni, Si, and Sr, all reported in mg/L. Cations data were analyzed with an ICP-AES. Anion data include F, Cl, NO3, SO4, and HCO3. Anion data were analyzed on an IC and HCO3 was estimated from alkalinity data. Alkalinity is reported as mg/L as CaCO3.
High charge balance error is hypothesized to be due to underestimating sulfate and/or error associated with alkalinity measurements.
Data flags include:
NaN = data was not collected
BDL = analyte is below detection limit
DRY = data was not collected because the stream was dry.
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
fluorite_1D.in & datacom_F.dbs
CrunchFlow input file simulating flow along a 500 m fluorite column for 100 years.
Fluorite kinetic data is from: Palandri, J. L., & Kharaka, Y. K. (2004). A compilation of rate parameters of water-mineral interaction kinetics for application to geochemical modeling. U.S. Geological Survey Open File Report 2004-1069. Retrieved from https://pubs.usgs.gov/of/2004/1068/pdf/OFR_2004_1068.pdf
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Manitou_Warix_2021_timeseries.csv
Dataset for Hotel Gulch discharge, stream specific conductivity, groundwater level, and groundwater specific conductivity at eight paired groundwater and stilling wells. Electrical conductivity was measured with Onset U-24-001 HOBOs and was converted to specific conductivity. Water level was measured with Onset U-20-001 HOBOs in both the stream and groundwater wells. We measured discharge using the salt dilution method and created rating curves to turn stream water level to discharge, only discharge is reported here.
NaN values indicate that data is not available because the sensor was not yet launched, the sensor was actively being downloaded, or because of logger error. Discharge values were also converted to NaNs where stage values exceeded manual stage/discharge observations to avoid overestimating discharge during high flows.
Discharge = liters/second
Groundwater elevation = meters
Specific conductivity = microsiemen/centimeter
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Temperature Profiles (TS(n))
Temperature data are saved in individual files for each of the 8 sites. File names are TS(n).csv where n = the site ID. Column headers are the depth under the streamed in meters and all temperature data is in Celsius.
Temperature was collected with DS1925L-F5# Thermochron iButtons at 0 cm, 10 cm, and 20 cm below the stream bed. At site 7, the 20 cm iButton failed and so we used temperature data from an Onset U-24-001 HOBO recording at the same interval in the adjacent groundwater well at a depth of 1.43 meters.
Data Services
The following web services are available for data contained in this resource. Geospatial Feature and Raster
data are made available via Open Geospatial Consortium Web Services. The provided links can be copied and pasted
into GIS software to access these data. Multidimensional NetCDF data are made available via a THREDDS Data Server
using remote data access protocols such as OPeNDAP. Other data services may be made available in the future to
support additional data types.
Warix, S., Navarre-Sitchler, A., Manning, A., Singha, K. (2023) Local topography and hydraulic conductivity influence riparian groundwater age and groundwater-surface water connection (in revision)
Credits
Delete Funding Agency
Are you sure you want to delete this funder?
Name:
Number:
Title:
Funding Agencies
This resource was created using funding from the following sources:
Agency Name
Award Title
Award Number
NSF
Collaborative Research: Network Cluster: Quantifying controls and feedbacks of dynamic storage on critical zone processes in western montane watersheds
EAR-2012730
How to Cite
Warix, S., A. Navarre-Sitchler, K. Singha (2024). DWCZ-MEF-Data from Warix et al. (2023), Local topography and hydraulic conductivity influence riparian groundwater age and groundwater-surface water connection, HydroShare, http://www.hydroshare.org/resource/46dc8efda0dd44a095592817d481fb1f
This resource is shared under the Creative Commons Attribution-NoCommercial CC BY-NC.
Comments
There are currently no comments
New Comment