2000
DOI: 10.1002/1099-1085(20000615)14:8<1465::aid-hyp987>3.0.co;2-6
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Effects of evaporative enrichment on the stable isotope hydrology of a central Florida (USA) river

Abstract: The d 07 O characteristics of water masses contributing to ~ow in the Econlockhatchee River basin\ a subtropical low!gradient watershed in central Florida\ were monitored to assess the potential for applying hydrograph separation models in the watershed[ Daily sampling for a 1!month period in autumn 0881 revealed ranges in precipitation of −5=53 to −9=06-\ in sur_cial groundwater of −2=18 to −1=89-\ and in river water of −1=57 to −0=30-[ Results indicated that river d 07 O was consistently more enriched than e… Show more

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Cited by 49 publications
(29 citation statements)
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“…Since imbibed water was likely collected from rivers, we utilized river water d 18 O values ( Fig. 3; after Dutton et al, 2005;Gremillion and Wanielista, 2000). Rivers in regions north of Florida (not shown in Fig.…”
Section: Tick Island Geology and Hydrologymentioning
confidence: 99%
“…Since imbibed water was likely collected from rivers, we utilized river water d 18 O values ( Fig. 3; after Dutton et al, 2005;Gremillion and Wanielista, 2000). Rivers in regions north of Florida (not shown in Fig.…”
Section: Tick Island Geology and Hydrologymentioning
confidence: 99%
“…McDonnell et al, 1990;Kendall and McDonnell, 1998;Lambs, 2000;Gibson et al, 2005;Liu et al, 2008;Jasechko et al, 2013). Hydrological processes occurring between rainfall input and river discharge modify the stable isotopic composition of rivers and include the isotopic averaging during soil infiltration, runoff, damming (Ogrinc et al, 2008;Koeniger et al, 2009) and seasonally differential fractional inputs of water from surface and groundwater sources (Sklash, 1990;Buttle, 1994;Lambs, 2004); and heavy isotope ( 2 H, 18 O) enrichment due to the effects of watershed evapotranspiration or instream evaporation (Simpson and Herczeg, 1991;Gremillion and Wanielista, 2000;Telmer and Veizer, 2000) and isotopic fractionation of snowmelt (Taylor et al, 2002). All of these processes may result in markedly different average isotopic values in river discharge compared to precipitation, both in space and time (Dutton et al, 2005;Rock and Mayer, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…The cumulative effect of catchment-scale evapotranspiration and instream evaporative processes may additionally increase δ 18 O and δ 2 H values in the downstream direction. Rivers that are hundreds of kilometres long may therefore have distinctive upstream versus downstream isotopic patterns as they accumulate discharge and integrate various hydrological processes from contributing subcatchments (Simpson and Herczeg, 1991;Gremillion and Wanielista, 2000;Ferguson et al, 2007;Bowen et al, 2011). Alpine or high-latitude rivers may be ephemeral, dominated mostly by isotopically depleted snowmelt events (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…A possible explanation is that some inland alligators may ingest water that is O of precipitation is −2.7 to −2.5 ‰ (Meyers et al 1993, Gremillion & Wanielista 2000. Mean δ…”
mentioning
confidence: 99%