Abstract
The deeper part of the Miocene quartz sand aquifers of Jutland, Denmark, contain pristine freshwater of very high quality. Hydrochemistry, environmental tracers and
groundwater modelling from previous studies show that the deepest of three major Miocene sand aquifers, the Ribe Formation, contain high-quality groundwater recharged during a few thousand years in the Holocene
groundwater modelling from previous studies show that the deepest of three major Miocene sand aquifers, the Ribe Formation, contain high-quality groundwater recharged during a few thousand years in the Holocene
| Original language | English |
|---|---|
| Title of host publication | Natural groundwater quality |
| Editors | W. Mike Edmunds, Paul Shand |
| Publisher | Wiley |
| Pages | 306-334 |
| Number of pages | 29 |
| ISBN (Electronic) | 978-14443-0034-5 |
| ISBN (Print) | 978-14051-5675-2 |
| DOIs | |
| Publication status | Published - 28 Mar 2008 |
Programme Area
- Programme Area 2: Water Resources
