<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Garrett, A.</style></author><author><style face="normal" font="default" size="100%">Bollinger, J.</style></author><author><style face="normal" font="default" size="100%">Hayes, D.</style></author><author><style face="normal" font="default" size="100%">Koffman, L.</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author><author><style face="normal" font="default" size="100%">Moore, Trent C.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Transport and retention of a conservative tracer in an isolated creek</style></title><secondary-title><style face="normal" font="default" size="100%">Estuarine, Coastal and Shelf Science</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1016/j.ecss.2010.01.010</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">87</style></volume><pages><style face="normal" font="default" size="100%">333-345</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">A study of tracer transport and retention in a small tidal creek and marsh system located in the southeastern US was conducted using a three-dimensional hydrodynamic model and data from a dye tracer release. The model simulated tidally driven flow, including inundation and drying out of the marshes and the dispersal of the dye tracer. Flow measurements in the tidal creek showed that the simulations appeared to generally duplicate the tidally driven flow into and out of the tidal creeks and marshes. The dye tracer experiment was conducted to test the hydrodynamic model</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2010-93267</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Garrett, A.</style></author><author><style face="normal" font="default" size="100%">Bollinger, J.</style></author><author><style face="normal" font="default" size="100%">Hayes, D.</style></author><author><style face="normal" font="default" size="100%">Koffman, L.</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Transport and dispersion of a conservative tracer in coastal waters with large intertidal areas</style></title><secondary-title><style face="normal" font="default" size="100%">Estuaries and Coasts</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.springerlink.com/content/772817k644w71071/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">32</style></volume><pages><style face="normal" font="default" size="100%">573-592</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">In late December 1991, an accidental release of 5,700 CI of tritiated water (HTO) from the Savannah River Site was transported via site streams into the Savannah River where it was carried downstream to the coastal zone. HTO released into a semitropical Georgia estuary was forced into the tidal marshes surrounding the estuary as well as discharged directly into the Atlantic Ocean. The spreading of HTO was studied with a 3D hydrodynamic model (ALGE) that includes flooding and draining of intertidal areas. Comparisons of model simulations to measured HTO concentration showed that ALGE simulated well the general increase and decrease of HTO as its plume passed a given area. The</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2009-93296</style></accession-num></record></records></xml>