Journal cover Journal topic
Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 4.936 IF 4.936
  • IF 5-year value: 5.615 IF 5-year
    5.615
  • CiteScore value: 4.94 CiteScore
    4.94
  • SNIP value: 1.612 SNIP 1.612
  • IPP value: 4.70 IPP 4.70
  • SJR value: 2.134 SJR 2.134
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 107 Scimago H
    index 107
  • h5-index value: 63 h5-index 63
Volume 19, issue 10
Hydrol. Earth Syst. Sci., 19, 4067–4080, 2015
https://doi.org/10.5194/hess-19-4067-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 19, 4067–4080, 2015
https://doi.org/10.5194/hess-19-4067-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Oct 2015

Research article | 06 Oct 2015

Long-term and high-frequency non-destructive monitoring of water stable isotope profiles in an evaporating soil column

Y. Rothfuss et al.
Download
Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (29 Jun 2015) by Christine Stumpp
AR by Anna Wenzel on behalf of the Authors (07 Aug 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (07 Aug 2015) by Christine Stumpp
RR by Anonymous Referee #2 (01 Sep 2015)
RR by Anonymous Referee #1 (02 Sep 2015)
ED: Publish subject to minor revisions (Editor review) (06 Sep 2015) by Christine Stumpp
AR by Svenja Lange on behalf of the Authors (10 Sep 2015)  Author's response
ED: Publish as is (20 Sep 2015) by Christine Stumpp
Publications Copernicus
Download
Short summary
Profiles of soil water stable isotopes were followed non-destructively and with high precision for a period of 290 days in the laboratory Rewatering at the end of the experiment led to instantaneous resetting of the isotope profiles, which could be closely followed with the new method The evaporation depth dynamics was determined from isotope gradients calculation Uncertainty associated with the determination of isotope kinetic fractionation where highlighted from inverse modeling.
Profiles of soil water stable isotopes were followed non-destructively and with high precision...
Citation