Northern Ireland’s main limestone aquifers are found in the Carboniferous and Cretaceous sequences. Aquifer conceptual models have been developed for these and the other aquifers in Northern Ireland as a consistent platform from which more detailed conceptual models can be developed for any form of hydrogeological investigation and study. These are based on the most up to date research and data available. The majority of the Carboniferous and Cretaceous limestones are located in upland terrain. Karst systems have developed within them, receiving sinking streams as their main source of recharge. They are predominantly free-flowing and have exploited pre-existing intersecting faults. Transmissivities are moderate to high but storativity is...
Identifying groundwater contributions to baseflow forms an essential part of surface water body char...
The need to renew and expand civil infrastructure, combined with an increased acknowledgement of a c...
Identifying groundwater contributions to baseflow forms an essential part of surface water body char...
The Cretaceous Chalk in Northern Ireland (Ulster White Limestone Formation) is a locally important a...
The Cretaceous Chalk or Ulster White Limestone Formation (UWLF) of Northern Ireland predominantly oc...
Karstified carbonate aquifers are highly heterogeneous systems characterised by multiple component p...
The Antrim Lava Group (the ‘basalts’) and the underlying Ulster White Limestone Formation (the ‘chal...
The flow hydrograph of a large mine drainageadit, the Meerbrook Sough, has been analysedto determine...
Beneath Belfast and the Lagan Valley lies Northern Ireland's most important aquifer, the Triassic Sh...
1] In lowland karst areas of Ireland topographic depressions which get intermittently flooded on an ...
The Triassic Sherwood Sandstone Group is a major European aquifer system. It is also the principal g...
The geothermal energy of thermal groundwater is currently being exploited for district-scale heating...
Abstract: Recent hydrogeological investigation of the catchment of the River Wye, Derbyshire (UK) ha...
This thesis explores speleogenesis within the Dartry Limestone Formation of Cuilcagh Mountain by con...
The Lincolnshire Limestone is an important regional aquifer. Pumping stations at Bourne and other lo...
Identifying groundwater contributions to baseflow forms an essential part of surface water body char...
The need to renew and expand civil infrastructure, combined with an increased acknowledgement of a c...
Identifying groundwater contributions to baseflow forms an essential part of surface water body char...
The Cretaceous Chalk in Northern Ireland (Ulster White Limestone Formation) is a locally important a...
The Cretaceous Chalk or Ulster White Limestone Formation (UWLF) of Northern Ireland predominantly oc...
Karstified carbonate aquifers are highly heterogeneous systems characterised by multiple component p...
The Antrim Lava Group (the ‘basalts’) and the underlying Ulster White Limestone Formation (the ‘chal...
The flow hydrograph of a large mine drainageadit, the Meerbrook Sough, has been analysedto determine...
Beneath Belfast and the Lagan Valley lies Northern Ireland's most important aquifer, the Triassic Sh...
1] In lowland karst areas of Ireland topographic depressions which get intermittently flooded on an ...
The Triassic Sherwood Sandstone Group is a major European aquifer system. It is also the principal g...
The geothermal energy of thermal groundwater is currently being exploited for district-scale heating...
Abstract: Recent hydrogeological investigation of the catchment of the River Wye, Derbyshire (UK) ha...
This thesis explores speleogenesis within the Dartry Limestone Formation of Cuilcagh Mountain by con...
The Lincolnshire Limestone is an important regional aquifer. Pumping stations at Bourne and other lo...
Identifying groundwater contributions to baseflow forms an essential part of surface water body char...
The need to renew and expand civil infrastructure, combined with an increased acknowledgement of a c...
Identifying groundwater contributions to baseflow forms an essential part of surface water body char...