Publication details
Hydraulické parametry podmenilitového souvrství ždánické jednotky
| Title in English | Hydraulic parameters of Submenillite unit of Ždánice Unit |
|---|---|
| Authors | |
| Year of publication | 2024 |
| Type | Article in Periodical |
| Magazine / Source | Zprávy o geologických výzkumech |
| MU Faculty or unit | |
| Citation | |
| Web | https://app.geology.cz/img/zpravyvyzkum/fulltext/zpravy.geol.2024.06.pdf |
| Doi | http://dx.doi.org/10.3140/zpravy.geol.2023.13 |
| Keywords | : hydraulic conductivity; Submenilite Formation; hydraulic parameters; transmisivity; hydrogeology; Ždánice Unit; Carpathian Flysh Zone; pumping test; recovery test |
| Attached files | |
| Description | This study aims to re-asses hydrodynamic tests of the Submenilite Unit of the Outer Carpathian Flysch Zone sediments, exposed at Přítlucká hora located near Rakvice village in South Moravian region, Czech Republic. We focused on four shallow, 6.0–7.6 m deep hydrogeological wells, drilled by Aqua Enviro s. r. o. company in 2005. The purpose of the drilling was a feasibility study for drainage of western part of Rakvice village. The sediments of the Submenilite Formation of the Ždánice unit that were drilled are dominated by compressed clays, claystones and siltstones, containing thin layers of sand and weathered sandstones. For the purpose of determining hydraulic parameters of underlying aquifer, the company conducted pumping and recovery tests on each of the wells. In this work, we used Jacob’s semilogarithmic method to interpret the measured groundwater level data. Hydraulic conductivity and transmissivity parameters were consequently calculated. The resulting transmissivity values range from 1.6 × 10–2 m2/d to 3.7 × 10–1 m2/d and hydraulic conductivity value ranges from 3.6 × 10–3 m/d to 1.0 × 10–1 m/d. The calculated index of transmissivity Y corresponds to 4.32–4.57 and index of conductivity Z ranges between 5.80 and 6.27. The values of index of transmissivity Y from this study are generally comparable with results presented by previous authors and demonstrate very low transmissivity of the rocks of this unit mostly built by non-permeable pelitic rocks. |