Menu

CF011

Carbon Dynamics in the Hyporheic Zone of a Headwater Mountain Stream in the Cascade Mountains, Oregon – Watershed 1 at HJA – June 2013 to March 2014

  • Creator(s): Steven M. Wondzell, Hayley Corson-Rikert
  • PI(s): Steven M. Wondzell
  • Originator(s): Hayley Corson-Rikert
  • Other researcher(s): Roy Haggerty
  • Dates of data collection: Jun 13 2013 - Mar 16 2014
  • Data collection status: Study collection is completed and no new collection is planned
  • Data access: Online
  • DOI: https://doi.org/10.6073/pasta/7a070aab134c1add4f239fab6318b4d7
  • Last update: Sep 20 2016 (Version 4)
<Citation>     <Acknowledgement>     <Disclaimer>    
Wondzell, S.; Corson-Rikert, H. 2016. Carbon Dynamics in the Hyporheic Zone of a Headwater Mountain Stream in the Cascade Mountains, Oregon – Watershed 1 at HJA – June 2013 to March 2014. Long-Term Ecological Research. Forest Science Data Bank, Corvallis, OR. [Database]. Available: http://andlter.forestry.oregonstate.edu/data/abstract.aspx?dbcode=CF011. https://doi.org/10.6073/pasta/7a070aab134c1add4f239fab6318b4d7. Accessed 2024-05-07.
Data were provided by the HJ Andrews Experimental Forest research program, funded by the National Science Foundation's Long-Term Ecological Research Program (DEB 2025755), US Forest Service Pacific Northwest Research Station, and Oregon State University.
While substantial efforts are made to ensure the accuracy of data and documentation, complete accuracy of data sets cannot be guaranteed. All data are made available "as is". The Andrews LTER shall not be liable for damages resulting from any use or misinterpretation of data sets.
ABSTRACT:
This study investigated carbon dynamics in the hyporheic zone of a steep, forested catchment in the Cascade Mountains of western Oregon, USA. Water samples were collected monthly from a headwater stream and well network during baseflow conditions from July to December 2013 and again in March 2014. We also sampled during one fall storm event, collecting pre-storm, rising leg, and extended high flow samples. The well network is located at the base of Watershed 1 (WS1) of the H.J. Andrews Experimental Forest and spans the full width of the floodplain (~14 m) along a 29 m reach of stream. We measured pH, temperature, water level, major anions, major cations, DOC, DIC, and total alkalinity. Flow paths, travel time to wells and hydraulic conductivity were available from previous studies.

Study Description Study Site Map Download Study Location Information: (CSV)
Ecological Metadata Language: (EML)
ENTITY TITLES:
1Baseflow Sample Data (Jun 13 2013 - Mar 16 2014)METADATADATA
Field and chemistry data for baseflow samples
2Storm Data (Nov 15 2013 - Nov 17 2013)METADATADATA
Field and chemistry data for storm samples

RELATED MATERIALS:
 Watershed 1 Well Network at the H.J. Andrews - Location of HJA within OR, and location of WS1 and the well network within HJA. Flow is from right to left in the well network figure. All active wells are labeled. The image of the well network was modified from Wondzell (2006)

RELATED DATABASES:
 Stream and hyporheic carbon dioxide (CO2) measurements in a headwater catchment, Watershed 1, and throughout Lookout Creek watershed at the HJ Andrews Experimental Forest, July 2013 to July 2014 (CF010)

RELATED PUBLICATIONS:
 Corson-Rikert, Hayley A., Wondzell, Steven M., Haggerty, Roy, Santelmann, Mary V. 2016, Carbon dynamics in the hyporheic zone of a headwater mountain stream in the Cascade Mountains, Oregon (Pub. No: 4959)
 Corson-Rikert, Hayley A. 2014, Carbon Dynamics in the Hyporheic Zone of a Headwater Mountain Stream in the Cascade Mountains, Oregon (Pub. No: 4862)
 Wondzell, Steven M. 2006, Effect of morphology and discharge on hyporheic exchange flows in two small streams in the Cascade Mountains of Oregon, USA (Pub. No: 3861)