Vertical variations in permeability of flysch rocks in the Czechoslovak Carpathians
Abstract
Some general features of permeability distribution in flysch rocks are characterized. In a greater part of flysch regions, the near-surface zone reaching (on the regional average) to the depth of about 30 - 40 m. represents the major aquifer in flysch rock massif. Regularities in vertical distribution of permeability are quantitatively documented by results of regional evaluation of data from water injection tests (water pressure tests) carried Out in the Godula Member in Czechoslovakia. The evaluations give the basis for statistical predictions of permeability, hydraulic conductivity and transmissivity distribution in the studied rocks. It can be assumed that very similar regularities should be expected in other lithostratigraphic units of the Carpathian flysch.Downloads
Published
2013-05-07
Issue
Section
Articles
License
Authors who publish with this journal agree to the following terms:- Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as this can lead to productive exchanges and earlier and more frequent citation of the published work (See The Effect of Open Access).