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| Type: | Resource | |
| Storage: | The size of this resource is 2.1 KB | |
| Created: | Feb 08, 2023 at 3:21 a.m. | |
| Last updated: | Feb 08, 2023 at 3:22 a.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 536 |
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Abstract
Hydrogeological modelling of the Kampinos National Park (KNP) region has been carried out. The KNP comprises a hydrogeological unit of valley relatively simple structure, and has been investigated empirically and theoretically since the 1970's. Results of numerical modelling given here provide a quantitative evaluation of hydrogeological parameters, recharging infiltration, river drainage and evapotranspiration processes (groundwater evaporation), water balance and the role of hydrodynamic zones in the recharge and drainage contribution in the water balance of the Vistula valley unit.
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Coverage
Spatial
Content
Additional Metadata
| Name | Value |
|---|---|
| DOI | |
| Depth | 85 |
| Scale | 101 - 1 000 km² |
| Layers | 11-15 layers |
| Purpose | Scientific investigation (not related to applied problem) |
| GroMoPo_ID | 162 |
| IsVerified | True |
| Model Code | MODFLOW |
| Model Link | https://gq.pgi.gov.pl/article/view/7297 |
| Model Time | 2000-2002 |
| Model Year | 2003 |
| Model Authors | E. Krogulec |
| Model Country | Poland |
| Data Available | Report/paper only |
| Developer Email | wak@geo.uw.edu.pl |
| Dominant Geology | Model focuses on multiple geologic materials |
| Developer Country | Poland |
| Publication Title | Evaluation of hydrogeological conditions based on modelling: a case study in the Kampinos National Park region, central Poland |
| Original Developer | No |
| Additional Information | Hydrogeological modelling of the Kampinos National Park (KNP) region has been carried out. The KNP comprises a hydrogeological unit of valley relatively simple structure, and has been investigated empirically and theoretically since the 1970’s. Results of numerical modelling given here provide a quantitative evaluation of hydrogeological parameters, recharging infiltration, river drainage and evapotranspiration processes (groundwater evaporation), water balance and the role of hydrodynamic zones in the recharge and drainage contribution in the water balance of the Vistula valley unit. |
| Integration or Coupling | None of the above |
| Evaluation or Calibration | Static water levels |
| Geologic Data Availability |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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