Hi, I'm an error. x

Estimation of soil water evaporation from isotope hydrology methods in an agricultural field


A newer version of this resource http://www.hydroshare.org/resource/b6bb3b53d5db4b388a809d0ad193330c is available that replaces this version.
Authors: Erik Oerter
Owners:
Resource type: Generic
Storage: The size of this resource is 2.6 KB
Created: Aug 26, 2017 at 10:10 p.m.
Last updated: Aug 26, 2017 at 10:23 p.m.
DOI: 10.4211/hs.1a7dc5d6b9fa4253bca442341eef500d
Citation: See how to cite this resource
Sharing Status: Published
Views: 214
Downloads: 9
+1 Votes: Be the first one to  +1 this.  (You need to be logged in to rate this.)
Comments: No comments (yet)

Abstract

These data are from this publication: Oerter, E. J., Perelet, A., Pardyjak, E., & Bowen, G. (2017). Membrane inlet laser spectroscopy to measure H and O stable isotope compositions of soil and sediment pore water with high sample throughput. Rapid Communications in Mass Spectrometry, 31(1), 75-84.

Abstract:
RATIONALE: The fast and accurate measurement of H and O stable isotope compositions (δ2H and δ18O values) of soil and sediment pore water remains an impediment to scaling-up the application of these isotopes in soil and vadose hydrology. Here we describe a method and its calibration to measuring soil and sediment pore water δ2H and δ18O values using a water vapor-permeable probe coupled to an isotope ratio infrared spectroscopy analyzer.
METHODS: We compare the water vapor probe method with a vapor direct equilibration method, and vacuum extraction with liquid water analysis. At a series of four study sites in a managed desert agroecosystem in the eastern Great Basin of North America, we use the water vapor probe to measure soil depth profiles of δ2H and δ18O values.
RESULTS: We demonstrate the accuracy of the method to be equivalent to direct headspace equilibration and vacuum extraction techniques, with increased ease of use in its application, and with analysis throughput rates greater than 7 h1. The soil depth H and O stable isotope profiles show that soil properties such as contrasting soil texture and pedogenic soil horizons control the shape of the isotope profiles, which are reflective of local evaporation conditions within the soils.
CONCLUSIONS: We conclude that this water vapor probe method has potential to yield large numbers of H and O stable isotope analyses of soil and sediment waters within shorter timeframes and with increased ease than with currently existing methods.

Subject Keywords

  • No subject keywords have been added.
  • ${ k }

Duplicate. Keyword not added.

Error: ${ error }
Deleting all keywords will set the resource sharing status to private.

Resource Level Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Near SLC airport
Longitude
-112.0438°
Latitude
40.7959°

Temporal

Start Date:
End Date:

Content

References

Related Resources

This resource has been replaced by newer version: http://www.hydroshare.org/resource/b6bb3b53d5db4b388a809d0ad193330c

Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
National Science Foudation, iUTAH-innovative Urban Transitions and Aridregion Hydro-sustainability NSF Award Number 1208732

How to Cite

Oerter, E. (2017). Estimation of soil water evaporation from isotope hydrology methods in an agricultural field, HydroShare, https://doi.org/10.4211/hs.1a7dc5d6b9fa4253bca442341eef500d

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

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

Comments

There are currently no comments

New Comment

required