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Calcite recrystallization at equilibrium as influenced by initial growth rate and pH

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TitleInfo
Title
Calcite recrystallization at equilibrium as influenced by initial growth rate and pH
Name (type = personal)
NamePart (type = family)
Juarez
NamePart (type = given)
Karen
NamePart (type = date)
1991
DisplayForm
Juarez, Karen, 1991-
Role
RoleTerm (authority = RULIB)
author
Name (type = personal)
NamePart (type = family)
Rouff
NamePart (type = given)
Ashaki A
DisplayForm
Ashaki A Rouff
Affiliation
Advisory Committee
Role
RoleTerm (authority = RULIB)
chair
Name (type = personal)
NamePart (type = family)
Elzinga
NamePart (type = given)
Evert J
DisplayForm
Evert J Elzinga
Affiliation
Advisory Committee
Role
RoleTerm (authority = RULIB)
co-chair
Name (type = personal)
NamePart (type = family)
Ntarlagiannis
NamePart (type = given)
Dimitrios
DisplayForm
Dimitrios Ntarlagiannis
Affiliation
Advisory Committee
Role
RoleTerm (authority = RULIB)
internal member
Name (type = corporate)
NamePart
Rutgers University
Role
RoleTerm (authority = RULIB)
degree grantor
Name (type = corporate)
NamePart
Graduate School - Newark
Role
RoleTerm (authority = RULIB)
school
TypeOfResource
Text
Genre (authority = marcgt)
theses
OriginInfo
DateCreated (encoding = w3cdtf); (keyDate = yes); (qualifier = exact)
2020
DateOther (qualifier = exact); (type = degree)
2020-05
Language
LanguageTerm (authority = ISO 639-3:2007); (type = text)
English
Abstract (type = abstract)
The mineral calcite was evaluated for recrystallization, a process known to change the location of ions in the mineral lattice without apparent change in mineral chemistry. Calcite lattice reconfiguration is cause for concern because it is a ubiquitous mineral with considerable reactivity that plays an important role in contaminant uptake and possible release. The intrinsic factor, crystal growth, and extrinsic factor, pH, were selected as possible driving forces for calcite recrystallization. Calcite growth experiments were conducted using a dual syringe pump technique. Geochemical analysis revealed calcite growth to be affected by syringe pump rate, a variable that showed no correlation with surface roughness. In order to trace recrystallization of laboratory grown calcite, an ion exchange technique with 45Ca radioisotope and a separate 40Ca stable isotope concentration analysis were used during resuspension batch experiments. There was no evident change in any of the radioisotope tracer experiments, indicating calcite stability. Additionally, 40Ca stable isotope concentration measurements support the same idea of calcite stability and its ability to maintain dynamic equilibrium.
Subject (authority = RUETD)
Topic
Environmental Geology
RelatedItem (type = host)
TitleInfo
Title
Rutgers University Electronic Theses and Dissertations
Identifier (type = RULIB)
ETD
RelatedItem (type = host)
TitleInfo
Title
Graduate School - Newark Electronic Theses and Dissertations
Identifier (type = local)
rucore10002600001
Identifier
ETD_10865
Identifier (type = doi)
doi:10.7282/t3-yy2c-ad07
PhysicalDescription
Form (authority = gmd)
electronic resource
InternetMediaType
application/pdf
InternetMediaType
text/xml
Extent
1 online resource (vii, 64 pages)
Note (type = degree)
M.S.
Note (type = bibliography)
Includes bibliographical references
Location
PhysicalLocation (authority = marcorg); (displayLabel = Rutgers, The State University of New Jersey)
NjNbRU
Genre (authority = ExL-Esploro)
ETD graduate
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Rights

RightsDeclaration (ID = rulibRdec0006)
The author owns the copyright to this work.
RightsHolder (type = personal)
Name
FamilyName
Juarez
GivenName
Karen
Role
Copyright Holder
RightsEvent
Type
Permission or license
DateTime (encoding = w3cdtf); (qualifier = exact); (point = start)
2020-04-28 16:06:17
AssociatedEntity
Name
Karen Juarez
Role
Copyright holder
Affiliation
Rutgers University. Graduate School - Newark
AssociatedObject
Type
License
Name
Author Agreement License
Detail
I hereby grant to the Rutgers University Libraries and to my school the non-exclusive right to archive, reproduce and distribute my thesis or dissertation, in whole or in part, and/or my abstract, in whole or in part, in and from an electronic format, subject to the release date subsequently stipulated in this submittal form and approved by my school. I represent and stipulate that the thesis or dissertation and its abstract are my original work, that they do not infringe or violate any rights of others, and that I make these grants as the sole owner of the rights to my thesis or dissertation and its abstract. I represent that I have obtained written permissions, when necessary, from the owner(s) of each third party copyrighted matter to be included in my thesis or dissertation and will supply copies of such upon request by my school. I acknowledge that RU ETD and my school will not distribute my thesis or dissertation or its abstract if, in their reasonable judgment, they believe all such rights have not been secured. I acknowledge that I retain ownership rights to the copyright of my work. I also retain the right to use all or part of this thesis or dissertation in future works, such as articles or books.
Copyright
Status
Copyright protected
Availability
Status
Open
Reason
Permission or license
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Technical

RULTechMD (ID = TECHNICAL1)
ContentModel
ETD
OperatingSystem (VERSION = 5.1)
windows xp
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1.7
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Microsoft® Word for Office 365
DateCreated (point = end); (encoding = w3cdtf); (qualifier = exact)
2020-05-01T14:33:40
DateCreated (point = end); (encoding = w3cdtf); (qualifier = exact)
2020-05-01T14:33:40
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