Data on geochemical and hydraulic properties of a characteristic confined/unconfined aquifer system of the younger Pleistocene in northeast Germany

Merz, C.; Steidl, J.

doi:https://doi.org/10.5194/essd-7-109-2015

Articles | Volume 7, issue 1

https://doi.org/10.5194/essd-7-109-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/essd-7-109-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 7, issue 1

02 Jun 2015

| 02 Jun 2015

Data on geochemical and hydraulic properties of a characteristic confined/unconfined aquifer system of the younger Pleistocene in northeast Germany

C. Merz and J. Steidl

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Final revised paper (published on 02 Jun 2015)
Preprint (discussion started on 27 Jan 2015)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC C11: 'RC : Referee Comment', Patrick LACHASSAGNE, 16 Feb 2015
- AC C29: 'Response to P. Lachassagne´s comments', Christoph Merz, 06 Mar 2015
RC C68: 'General comments to the authors', Anonymous Referee #2, 02 Apr 2015
RC C70: 'paper review', Anonymous Referee #3, 10 Apr 2015

Short summary

The paper presents a database of hydrochemical and hydraulic groundwater measurements of a younger Pleistocene aquifer system in NE Germany. The Leibniz Centre for Agricultural Landscape Research (ZALF) operates seven groundwater monitoring wells in the Quillow catchment located in the Uckermark region (Federal State of Brandenburg, Germany). This database can be used for the investigation of subsurface water geochemistry under changing hydraulic boundary conditions regarding a 14-year period.