Show simple item record

dc.contributor.authorKarwan, D.L.
dc.contributor.authorSiegert, C.M.
dc.contributor.authorLevia, D.F.
dc.contributor.authorPizzuto, J.
dc.contributor.authorMarquard, Julia
dc.contributor.authorAalto, R.E.
dc.contributor.authorAufdenkampe, A.K.
dc.date.accessioned2015-07-08T14:48:04Z
dc.date.issued2015-06-08
dc.description.abstractShort-lived fallout isotopes, such as beryllium-7 (7Be), are increasingly used as erosion and sediment tracers in watersheds. Beryllium-7 is produced in the atmosphere and delivered to Earth's surface primarily in precipitation. However, relatively little has been published about the variation in 7Be wet deposition caused by storm type and vegetation cover. Our analysis of precipitation, throughfall, and sediments in two forested, headwater catchments in the mid-Atlantic USA indicates significant variation in isotope deposition with storm type and storm height. Individual summer convective thunderstorms were associated with 7Be activity concentrations up to 5.0 Bq L−1 in precipitation and 4.7 Bq L−1 in throughfall while single-event wet depositional fluxes reached 168 Bq m−2 in precipitation and 103 Bq m−2 in throughfall. Storms originating from the continental USA were associated with lower 7Be activity concentrations and single-event wet depositional fluxes for precipitation (0.7 – 1.2 Bq L−1 and 15.8 – 65.0 Bq m−2) and throughfall (0.1 – 0.3 Bq L−1 and 13.5 – 98.9 Bq m−2). Tropical systems had relatively low activity concentrations, 0.2 – 0.5 Bq L−1 in precipitation and 0.2 – 1.0 Bq L−1 in throughfall, but relatively high single-event depositional fluxes due to large rainfall volumes, 32.8 – 67.6 Bq m−2 in precipitation and 25.7 – 134 Bq m−2 in throughfall. The largest sources of 7Be depositional variation were attributed to storm characteristics including precipitation amount and maximum storm height. 7Be activity associated with fluvial suspended sediments also exhibited the highest concentration and variability in summer (175 – 1450 Bq kg−1). We conclude the dominant source of variation on event-level 7Be deposition is storm type. Our results illustrate the complex relationships between 7Be deposition in precipitation and throughfall and demonstrate event-scale relationships between the 7Be in precipitation and on suspended sediment.en_GB
dc.description.sponsorshipNational Science Foundationen_GB
dc.identifier.citationVol. 30, Iss.1, pp. 75 - 89
dc.identifier.doi10.1002/hyp.10571
dc.identifier.grantnumberNSF EAR 0724971en_GB
dc.identifier.grantnumberNSF EAR 11447en_GB
dc.identifier.urihttp://hdl.handle.net/10871/17837
dc.language.isoenen_GB
dc.publisherWileyen_GB
dc.rights.embargoreasonPublisher policyen_GB
dc.subjectberyllium-7en_GB
dc.subjectwet depositionen_GB
dc.subjectprecipitationen_GB
dc.subjectsediment fingerprintingen_GB
dc.subjectthroughfallen_GB
dc.subjectstorm typeen_GB
dc.titleBeryllium-7 wet deposition variation with storm height, synoptic classification, and tree canopy state in the mid-Atlantic USAen_GB
dc.typeArticleen_GB
dc.identifier.issn0885-6087
dc.descriptionThis is the peer reviewed version of the article which has been published in final form at 10.1002/hyp.10571. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving: http://olabout.wiley.com/WileyCDA/Section/id-820227.html#termsen_GB
dc.identifier.eissn1099-1085
dc.identifier.journalHydrological Processesen_GB


Files in this item

This item appears in the following Collection(s)

Show simple item record