LDR   03119nam^^22003253a^4500
001        FI15060919_00001
005        20171026123117.0
006        m^^^^^o^^d^^^^^^^^
007        cr^^n^---ma^mp
008        150617n^^^^^^^^xx^||||^o^^^^^|||^u^eng^d
245 00 |a Impact of Sea-Level Rise on Sea Water Intrusion in Coastal Aquifers |h [electronic resource].
260        |a [S.l.] : |b National Ground Water Association, |c 2009.
490        |a Ground Water Volume 47 Number 2.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a Despite its purported importance, previous studies of the influence of sea-level rise on coastal aquifers have focused on specific sites, and a generalized systematic analysis of the general case of the sea water intrusion response to sea-level rise has not been reported. In this study, a simple conceptual framework is used to provide a first-order assessment of sea water intrusion changes in coastal unconfined aquifers in response to sea-level rise. Two conceptual models are tested: (1) flux-controlled systems, in which ground water discharge to the sea is persistent despite changes in sea level, and (2) head-controlled systems, whereby ground water abstractions or surface features maintain the head condition in the aquifer despite sea-level changes. The conceptualization assumes steady-state conditions, a sharp interface sea water-fresh water transition zone, homogeneous and isotropic aquifer properties, and constant recharge. In the case of constant flux conditions, the upper limit for sea water intrusion due to sea-level rise (up to 1.5 m is tested) is no greater than 50 m for typical values of recharge, hydraulic conductivity, and aquifer depth. This is in striking contrast to the constant head cases, in which the magnitude of salt water toe migration is on the order of hundreds of meters to several kilometers for the same sea-level rise. This study has highlighted the importance of inland boundary conditions on the sea-level rise impact. It identifies combinations of hydrogeologic parameters that control whether large or small salt water toe migration will occur for any given change in a hydrogeologic variable.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a Climate change.
650        |a Groundwater.
650        |a Seawater.
650        |a Sea level rise.
720        |a Adrian D. Werner.
720        |a Craig T. Simmons.
773 0    |t Impact of Sea-Level Rise on Sea Water Intrusion in Coastal Aquifers
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15060919/00001 |y Click here for full text
856 42 |3 FULL TEXT- Impact of sea-level rise on sea water intrusion in coastal aquifers. |u https://www.ncbi.nlm.nih.gov/pubmed/19191886 |y Impact of Sea-Level Rise on Sea Water Intrusion in Coastal Aquifers
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/09/19/00001/Werner_Simmons_2009_Impact of Sea-Level Rise on Sea Water Intrusion in Coastal Aquifersthm.jpg
997        |a Sea Level Rise


The record above was auto-generated from the METS file.