MERCURY DISTRIBUTION IN SOILS AND STREAM SEDIMENTS OF CENTRAL INDIANA, USA

dc.contributor.advisorFilippelli, Gabriel M.
dc.contributor.authorHatcher, Carrie
dc.contributor.otherLicht, Kathy J.
dc.contributor.otherJacinthe, Pierre-Andre
dc.date2009en_US
dc.date.accessioned2009-09-03T13:46:08Z
dc.date.available2009-09-03T13:46:08Z
dc.date.issued2009-09-03T13:46:08Z
dc.degree.disciplineDepartment of Earth Scienceen
dc.degree.grantorIndiana Universityen_US
dc.degree.levelM.S.en_US
dc.descriptionIndiana University-Purdue University Indianapolis (IUPUI)en_US
dc.description.abstractAn investigation of mercury (Hg) in soils and stream sediments was conducted to understand the impact of urbanization on Hg deposition and accumulation on the upper west fork of the White River watershed in central Indiana. Samples were collected to the north and east (i.e., downwind) of emission sources to understand the anthropogenic influences on Hg distribution in soil. Stream sediment sampling was designed to characterize the riverine particulate deposition of Hg through Indianapolis and to predict the potential for stream sediments with high Hg to become sources of methylmercury (MeHg). Spatial analysis revealed that soil Hg was elevated downwind of known industrial emission sites, indicating a local footprint of Hg deposition in central Indiana. Hg in streambank sediments was generally low in up-river sites to the northeast of Indianapolis, and increased markedly as the White River flowed through downtown, with high Hg persisting to downstream rural locations far to the south approximately 40 miles. The stream sediment results also revealed variations in total Hg (Hg(T)) as a function of local depositional sources, sub-watershed location, combined sewer outflows (CSOs), and impoundments along the White River. Low Hg values were recorded where the White River flow rate increased south of the 16th street dam at the confluence of the Fall Creek, where bankside industry and development confine the river. Three tributaries feeding into the White River were included in this study site, all having CSOs. Fall Creek and Pleasant Run have higher values of Hg with Lick Creek having lower values in comparison to the White River and other tributaries. The highest values occur right before confluences to the White River where the flow rate slows and drops sediment. Mercury values typically increased immediately downstream of dams and impoundments. Hg(T) deposition and transport processes pose a problem to anglers fishing south of Indianapolis who may not be aware of the potential dangers related to elevated stream sediment Hg values and the greater potential for MeHg production from these sediments.en_US
dc.identifier.urihttps://hdl.handle.net/1805/1937
dc.identifier.urihttp://dx.doi.org/10.7912/C2/513
dc.subjectMercury, Soil, Sediment, Emissionsen_US
dc.subject.lcshSoils -- Mercury content -- Indianaen
dc.subject.lcshRiver sediments -- Mercury content -- Indianaen
dc.subject.lcshSoil pollution -- Indianaen
dc.subject.lcshUrban watersheds -- Indianaen
dc.subject.lcshMercuryen
dc.subject.lcshWhite River (Ind. : River)en
dc.titleMERCURY DISTRIBUTION IN SOILS AND STREAM SEDIMENTS OF CENTRAL INDIANA, USAen_US
dc.typeThesisen
Files
Original bundle
Now showing 1 - 3 of 3
Loading...
Thumbnail Image
Name:
Thesis A.pdf
Size:
23.32 KB
Format:
Adobe Portable Document Format
Description:
title
Loading...
Thumbnail Image
Name:
Thesis B.pdf
Size:
80.71 KB
Format:
Adobe Portable Document Format
Description:
body
Loading...
Thumbnail Image
Name:
Thesis C.pdf
Size:
1.77 MB
Format:
Adobe Portable Document Format
Description:
figure
License bundle
Now showing 1 - 1 of 1
No Thumbnail Available
Name:
license.txt
Size:
1.96 KB
Format:
Item-specific license agreed upon to submission
Description: