dc.contributor.advisor | Thorn, Richard | en |
dc.contributor.author | Keegan, Margaret M. | en |
dc.date.accessioned | 2017-03-21T15:18:04Z | |
dc.date.available | 2017-03-21T15:18:04Z | |
dc.date.issued | 1993-12 | |
dc.identifier.citation | Keegan, M.M. (1993). Groundwater vulnerability and protection in County Tipperary (South Riding), Ireland | en |
dc.identifier.other | MSc | en |
dc.identifier.uri | https://research.thea.ie/handle/20.500.12065/1397 | |
dc.description.abstract | The aim of the project was to determine the extent and quality of the
groundwater in Tipperary South Riding with a view to developing a groundwater
protection plan which would allow the Local Authority to manage, protect and develop
the groundwater as efficiently as possible.
The geology of the area varies with topography. The low-lying areas of the
county comprise mainly Carboniferous limestones while the elevated regions consist
of sandstones and shales of Upper Carboniferous, Devonian and Silurian ages.
Deformation of these rocks decreases in magnitude moving northwards over the area;
the Southern Synclines having suffered the effects of the Hercynian orogeny and the
northern region exhibiting Caledonian orogenic trends. Quaternary (subsoil) deposits
are found throughout the area and are of variable thickness and permeability. Till is
the most widespread deposit with discontinuous pockets of sand and gravel in various
proportions, and some marl, alluvium and peat in places.
The principal aquifers of the area are the Kiltorcan sandstone formation and
various limestone units within the Carboniferous succession. 50 % of south Tipperary
constitutes either regionally or locally important aquifers. Secondary permeabilities
created by structural deformation, dolomitisation, karstification and weathering
processes create high transmissivities and often have large well yields. Specific
baseflow analysis highlighted the complexity of the aquifers and proved that the lower
part of the Suir river system is a major groundwater resource region.
The hydrochemistry and water quality of the local authority groundwater
sources was examined briefly. The majority of south Tipperary is underlain by
limestone or Quaternary deposits derived from limestone and, consequently,
calcium/magnesium bicarbonate waters predominate. The quality of the groundwater
in south Tipperary demonstrates that the main concern originates from the presence
of E.coli, and Total coliforms. The primary sources of contamination are from
farmyard wastes and septic tanks.
The vulnerability of groundwater to diffuse and point sources of pollution has
been found to be dependent on the overlying soil, subsoil and the thickness of the
unsaturated zone. A conceptual rather than quantitative approach is used and it is
found that approximately 60% of south Tipperary is designated as being extremely or
highly vulnerable.
The groundwater protection plan was devised subsequent to an understanding
of the aquifer systems, an assessment of the vulnerability, and a review of the Irish
planning system and environmental law. It is recommended that the plan be integrated
into the county development plan for legislative purposes. A series of acceptability
matrices were devised to restrict potentially polluting activities in vulnerable areas
while maintaining a balance between protection of the groundwater resource and the
need to site essential developments. | en |
dc.format | PDF | en |
dc.language.iso | en | en |
dc.subject | Groundwater - Ireland - Tipperary | en |
dc.title | Groundwater vulnerability and protection in County Tipperary (South Riding), Ireland | en |
dc.type | Master thesis (taught) | en |
dc.publisher.institution | Institute of Technology, Sligo | en |
dc.rights.access | Creative Commons Attribution-NonCommercial-NoDerivs | en |
dc.subject.department | Environmental Science ITS | en |