The challenges and opportunities of addressing particle size effects in sediment source fingerprinting: A review

Tracing sediments back to their catchment sources using biogeochemical and physical fingerprints involves multiple assumptions. One of the most fundamental assumptions is that these fingerprints are consistent during sediment generation, transportation, and deposition processes. Accordingly, the bio...

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Published inEarth-science reviews Vol. 169; no. 2; pp. 85 - 103
Main Authors Laceby, J. Patrick, Evrard, Olivier, Smith, Hugh G., Blake, Will H., Olley, Jon M., Minella, Jean P.G., Owens, Philip N.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2017
Elsevier
Subjects
Agricultural sciences
Composite fingerprinting
Continental interfaces, environment
Earth Sciences
fractionation
Geomorphology
Grain size
Hydrology
Life Sciences
particle size
samplers
Sciences of the Universe
Sediment fingerprinting
Sediment provenance
Sediment tracing
sediments
Soil study
surface area
transportation
watersheds
Grain size
Composite fingerprinting
Sediment fingerprinting
Sediment tracing
Sediment provenance
sediment fingerprinting
sediment tracing
sediment provenance
composite fingerprinting
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Abstract Tracing sediments back to their catchment sources using biogeochemical and physical fingerprints involves multiple assumptions. One of the most fundamental assumptions is that these fingerprints are consistent during sediment generation, transportation, and deposition processes. Accordingly, the biogeochemical fingerprints used to trace sediment must remain constant, during detachment and redistribution, or they must vary in a predictable and measurable way. One key challenge to this assumption is the sorting effect of particles by size during detachment, mobilization, transportation and deposition processes. Owing to the notable effect of particle size on sediment fingerprints, we believe it is important to review the main approaches used to address the effects of changes in particle size composition on sediment fingerprints. The two main approaches to addressing particle size impacts on fingerprint properties are: fractionation of source and sediment material to a narrow particle size range (e.g. isolation of <10μm or <63μm fractions), and concentration corrections (e.g. normalizing concentrations by parameters such as specific surface area). These approaches are often used in combination. The utility of fractionation and corrections to address particle size effects has received increasing attention and the relative merits of these procedures have been subject to debate. Accordingly, alternative techniques to address particle size effects in sediment fingerprinting studies are being adopted. For example, a tributary tracing technique or edge-of-field samplers may minimize particle size effects on sediment source fingerprints. The interrelationships between particle size and biogeochemical tracer properties suggest that particle size may also contribute to the formation of contrasts in sediment fingerprints between sources. Indeed, there may be a significant opportunity to derive further sediment source information through comprehensively investigating and unravelling the complexity of particle size–biogeochemical interactions.
AbstractList Tracing sediments back to their catchment sources using biogeochemical and physical fingerprints involves multiple assumptions. One of the most fundamental assumptions is that these fingerprints are consistent during sediment generation, transportation, and deposition processes. Accordingly, the biogeochemical fingerprints used to trace sediment must remain constant, during detachment and redistribution, or they must vary in a predictable and measurable way. One key challenge to this assumption is the sorting effect of particles by size during detachment, mobilization, transportation and deposition processes. Owing to the notable effect of particle size on sediment fingerprints, we believe it is important to review the main approaches used to address the effects of changes in particle size composition on sediment fingerprints. The two main approaches to addressing particle size impacts on fingerprint properties are: fractionation of source and sediment material to a narrow particle size range (e.g. isolation of <10 µm or <63 µm fractions), and concentration corrections (e.g. normalising concentrations by parameters such as specific surface area). These approaches are often used in combination. The utility of fractionation and corrections to address particle size effects has received increasing attention and the relative merits of these procedures have been subject to debate. Accordingly, alternative techniques to address particle size effects in sediment fingerprinting studies are being adopted. For example, a tributary tracing technique or edge-of-field samplers may minimise size effects on sediment source fingerprints. The interrelationships between particle size and biogeochemical tracer properties suggest that particle size may also contribute to the formation of contrasts in sediment fingerprints between sources. Indeed, there may be a significant opportunity to derive further sediment source information through comprehensively investigating and unravelling the complexity of particle size-biogeochemical interactions.
Tracing sediments back to their catchment sources using biogeochemical and physical fingerprints involves multiple assumptions. One of the most fundamental assumptions is that these fingerprints are consistent during sediment generation, transportation, and deposition processes. Accordingly, the biogeochemical fingerprints used to trace sediment must remain constant, during detachment and redistribution, or they must vary in a predictable and measurable way. One key challenge to this assumption is the sorting effect of particles by size during detachment, mobilization, transportation and deposition processes. Owing to the notable effect of particle size on sediment fingerprints, we believe it is important to review the main approaches used to address the effects of changes in particle size composition on sediment fingerprints. The two main approaches to addressing particle size impacts on fingerprint properties are: fractionation of source and sediment material to a narrow particle size range (e.g. isolation of <10μm or <63μm fractions), and concentration corrections (e.g. normalizing concentrations by parameters such as specific surface area). These approaches are often used in combination. The utility of fractionation and corrections to address particle size effects has received increasing attention and the relative merits of these procedures have been subject to debate. Accordingly, alternative techniques to address particle size effects in sediment fingerprinting studies are being adopted. For example, a tributary tracing technique or edge-of-field samplers may minimize particle size effects on sediment source fingerprints. The interrelationships between particle size and biogeochemical tracer properties suggest that particle size may also contribute to the formation of contrasts in sediment fingerprints between sources. Indeed, there may be a significant opportunity to derive further sediment source information through comprehensively investigating and unravelling the complexity of particle size–biogeochemical interactions.
Author Olley, Jon M.
Smith, Hugh G.
Owens, Philip N.
Blake, Will H.
Evrard, Olivier
Minella, Jean P.G.
Laceby, J. Patrick
Author_xml – sequence: 1
  givenname: J. Patrick
  surname: Laceby
  fullname: Laceby, J. Patrick
  email: placeby@lsce.ipsl.fr
  organization: Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Unité Mixte de Recherche 8212 (CEA/CNRS/UVSQ), Université Paris-Saclay, Gif-sur-Yvette 91198, France
– sequence: 2
  givenname: Olivier
  orcidid: 0000-0002-3503-6543
  surname: Evrard
  fullname: Evrard, Olivier
  organization: Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Unité Mixte de Recherche 8212 (CEA/CNRS/UVSQ), Université Paris-Saclay, Gif-sur-Yvette 91198, France
– sequence: 3
  givenname: Hugh G.
  surname: Smith
  fullname: Smith, Hugh G.
  organization: School of Environmental Sciences, University of Liverpool, Liverpool L69 7ZT, UK
– sequence: 4
  givenname: Will H.
  surname: Blake
  fullname: Blake, Will H.
  organization: School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth PL4 8AA, UK
– sequence: 5
  givenname: Jon M.
  surname: Olley
  fullname: Olley, Jon M.
  organization: Australian Rivers Institute, Griffith University, 170 Kessels Road, Nathan, QLD 4101, Australia
– sequence: 6
  givenname: Jean P.G.
  surname: Minella
  fullname: Minella, Jean P.G.
  organization: Universidade Federal de Santa Maria, Department of Soils, 1000 Roraima Avenue, 97105-900 Santa Maria, RS, Brazil
– sequence: 7
  givenname: Philip N.
  surname: Owens
  fullname: Owens, Philip N.
  organization: Environmental Science Program and Quesnel River Research Centre, University of Northern British Columbia, Prince George, British Columbia V2N 4Z9, Canada
BackLink https://hal.science/hal-01584165$$DView record in HAL
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Keywords Grain size
Composite fingerprinting
Sediment fingerprinting
Sediment tracing
Sediment provenance
sediment fingerprinting
sediment tracing
sediment provenance
composite fingerprinting
Language English
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Snippet Tracing sediments back to their catchment sources using biogeochemical and physical fingerprints involves multiple assumptions. One of the most fundamental...
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SubjectTerms Agricultural sciences
Composite fingerprinting
Continental interfaces, environment
Earth Sciences
fractionation
Geomorphology
Grain size
Hydrology
Life Sciences
particle size
samplers
Sciences of the Universe
Sediment fingerprinting
Sediment provenance
Sediment tracing
sediments
Soil study
surface area
transportation
watersheds
Title The challenges and opportunities of addressing particle size effects in sediment source fingerprinting: A review
URI https://dx.doi.org/10.1016/j.earscirev.2017.04.009
https://www.proquest.com/docview/2000327976
https://hal.science/hal-01584165
Volume 169
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