{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,9,20]],"date-time":"2025-09-20T20:11:55Z","timestamp":1758399115926},"reference-count":33,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2012,2,1]],"date-time":"2012-02-01T00:00:00Z","timestamp":1328054400000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["QJEGH"],"published-print":{"date-parts":[[2012,2]]},"abstract":"<jats:p>Analysis of groundwater level records from Ireland\u2019s South Eastern River Basin District (SERBD) allowed fundamental information about the nature of bedrock and gravel aquifers to be investigated. The hydrogeological setting of a monitoring point (with respect to, for example, recharge area, discharge area or proximity to a river) is the dominant factor influencing hydrograph character in bedrock aquifers, with aquifer type and subsoil properties producing secondary effects. Analysis of seasonal groundwater levels showed that the fractured bedrock aquifers recharge more quickly and typically have a longer recession period than gravel aquifers. The calculated recession periods for bedrock aquifers are longer than previous estimates for similar aquifers. Hydrograph analysis identified a number of notable phenomena including a gravel aquifer\u2019s interaction with surface water and evidence of rejected recharge. Short-term groundwater level fluctuations caused by global seismic events, recorded via chart recorders, are discussed. Specific yield values were calculated, for a number of settings, from annual average groundwater level variations. The values supported estimates from previous research on similar aquifers. An analysis to investigate if any impacts of climate change were evident showed no consistent change in the timing of groundwater level minima or maxima.<\/jats:p>","DOI":"10.1144\/1470-9236\/10-026","type":"journal-article","created":{"date-parts":[[2012,2,22]],"date-time":"2012-02-22T17:36:18Z","timestamp":1329932178000},"page":"19-30","source":"Crossref","is-referenced-by-count":10,"title":["Hydrogeological insights from groundwater level hydrographs in SE Ireland"],"prefix":"10.1144","volume":"45","author":[{"given":"K. M.","family":"Tedd","sequence":"first","affiliation":[{"name":"Department of Geology, Trinity College Dublin, Dublin 2, Ireland"}]},{"given":"B. D. R.","family":"Misstear","sequence":"additional","affiliation":[{"name":"Department of Civil, Structural and Environmental Engineering, Trinity College Dublin, Dublin 2, Ireland"}]},{"given":"C.","family":"Coxon","sequence":"additional","affiliation":[{"name":"Department of Geology, Trinity College Dublin, Dublin 2, Ireland"}]},{"given":"D.","family":"Daly","sequence":"additional","affiliation":[{"name":"Hydrometric and Groundwater Section, Environmental Protection Agency, Richview, Dublin 14, Ireland"}]},{"given":"N. H.","family":"Hunter Williams","sequence":"additional","affiliation":[{"name":"Groundwater Section, Geological Survey of Ireland, Haddington Road, Dublin 4, Ireland"}]}],"member":"1881","published-online":{"date-parts":[[2012,2,22]]},"reference":[{"key":"e_1_3_2_2_1","unstructured":"Allen R.G. Pereira L.S. Raes D. Smith M. 1998. Crop evapotranspiration\u2014Guidelines for computing crop water requirements . 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