Increased organic contaminant residence times in the urban riverbed due to the presence of highly sorbing sediments of the Anthropocene

Michael O. Rivett, Rachel S. Roche, John H. Tellam, Alan W. Herbert

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

This study evaluates the hypothesis that increased organic-contaminant sorption and hence residence time in urban riverbed deposits may occur due to the presence of highly sorbing sediment components of anthropogenic origin that contain thermally altered carbonaceous materials (TACM). The hypothesis
was confirmed through laboratory-batch studies examining tetrachloroethene (PCE) sorption on riverbed sediment samples from the highly urbanised River Tame headwaters catchment (Birmingham, UK) and the River Tern (Shropshire) providing a nearby rural benchmark. Urban-riverbed sorption was elevated
with observed organic-carbon partition coefficient (Koc) values over an order of magnitude greater than rural values. The latter compare to the widely used US EPA geometric-mean Koc and attributed to absorption-dominated partitioning into (recent) natural organic matter. Use of that mean is inappropriate
for the urban riverbed, potentially underestimating retardation by an order of magnitude. Organic petrography confirmed the urban riverbed contained a high proportion of TACM-rich organic-matter particles to which significant adsorption might be expected; furthermore, elevated urban Koc values were
consistent with TACM-rich sediment literature estimates. The TACM source appears to be riverine transport of particulate matter from historical industrial/urban or coal-mining/processing activities prevalent upstream since the Industrial Revolution. Consequences of the increased urban riverbed residence time on attenuation and bioavailability assumption sensitivities were modelled. Under the standard assumption of sorbed contaminant being non-bioavailable, rapid rates of aqueous-phase biodegradation are necessary
for complete attenuation within a riverbed. Conversely, if adsorbed contaminant is bioavailable, then complete attenuation is probable where highly adsorbing (Anthropocene urban) riverbed sediments are present, even for long half-lives. Therefore, Anthropocene-sediment occurrence may significantly influence modern-day contaminant fate within the urban riverbed; the principal implication being greatly increased sorption and residence times may occur in urban riverbeds than conventionally assumed. Further research should focus upon whether adsorbed contaminants have any bioavailability causing increased contaminant flux attenuation and surface-water quality protection.
LanguageEnglish
Article number100023
Pages1-16
Number of pages16
JournalJournal of Hydrology X
Volume3
Early online date1 Feb 2019
DOIs
Publication statusPublished - 30 Apr 2019

Fingerprint

residence time
pollutant
sorption
sediment
bioavailability
organic matter
tetrachloroethylene
petrography
coal mining
partition coefficient
river
headwater
half life
Anthropocene
particulate matter
biodegradation
partitioning
organic carbon
catchment
adsorption

Keywords

  • urban
  • chlorinated aliphatic hydrocarbons (CAHs)
  • anthropocene
  • bioavailability
  • sorption
  • riverbed sediments

Cite this

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title = "Increased organic contaminant residence times in the urban riverbed due to the presence of highly sorbing sediments of the Anthropocene",
abstract = "This study evaluates the hypothesis that increased organic-contaminant sorption and hence residence time in urban riverbed deposits may occur due to the presence of highly sorbing sediment components of anthropogenic origin that contain thermally altered carbonaceous materials (TACM). The hypothesiswas confirmed through laboratory-batch studies examining tetrachloroethene (PCE) sorption on riverbed sediment samples from the highly urbanised River Tame headwaters catchment (Birmingham, UK) and the River Tern (Shropshire) providing a nearby rural benchmark. Urban-riverbed sorption was elevatedwith observed organic-carbon partition coefficient (Koc) values over an order of magnitude greater than rural values. The latter compare to the widely used US EPA geometric-mean Koc and attributed to absorption-dominated partitioning into (recent) natural organic matter. Use of that mean is inappropriatefor the urban riverbed, potentially underestimating retardation by an order of magnitude. Organic petrography confirmed the urban riverbed contained a high proportion of TACM-rich organic-matter particles to which significant adsorption might be expected; furthermore, elevated urban Koc values wereconsistent with TACM-rich sediment literature estimates. The TACM source appears to be riverine transport of particulate matter from historical industrial/urban or coal-mining/processing activities prevalent upstream since the Industrial Revolution. Consequences of the increased urban riverbed residence time on attenuation and bioavailability assumption sensitivities were modelled. Under the standard assumption of sorbed contaminant being non-bioavailable, rapid rates of aqueous-phase biodegradation are necessaryfor complete attenuation within a riverbed. Conversely, if adsorbed contaminant is bioavailable, then complete attenuation is probable where highly adsorbing (Anthropocene urban) riverbed sediments are present, even for long half-lives. Therefore, Anthropocene-sediment occurrence may significantly influence modern-day contaminant fate within the urban riverbed; the principal implication being greatly increased sorption and residence times may occur in urban riverbeds than conventionally assumed. Further research should focus upon whether adsorbed contaminants have any bioavailability causing increased contaminant flux attenuation and surface-water quality protection.",
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Increased organic contaminant residence times in the urban riverbed due to the presence of highly sorbing sediments of the Anthropocene. / Rivett, Michael O.; Roche, Rachel S.; Tellam, John H.; Herbert, Alan W.

In: Journal of Hydrology X, Vol. 3, 100023, 30.04.2019, p. 1-16.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Increased organic contaminant residence times in the urban riverbed due to the presence of highly sorbing sediments of the Anthropocene

AU - Rivett, Michael O.

AU - Roche, Rachel S.

AU - Tellam, John H.

AU - Herbert, Alan W.

PY - 2019/4/30

Y1 - 2019/4/30

N2 - This study evaluates the hypothesis that increased organic-contaminant sorption and hence residence time in urban riverbed deposits may occur due to the presence of highly sorbing sediment components of anthropogenic origin that contain thermally altered carbonaceous materials (TACM). The hypothesiswas confirmed through laboratory-batch studies examining tetrachloroethene (PCE) sorption on riverbed sediment samples from the highly urbanised River Tame headwaters catchment (Birmingham, UK) and the River Tern (Shropshire) providing a nearby rural benchmark. Urban-riverbed sorption was elevatedwith observed organic-carbon partition coefficient (Koc) values over an order of magnitude greater than rural values. The latter compare to the widely used US EPA geometric-mean Koc and attributed to absorption-dominated partitioning into (recent) natural organic matter. Use of that mean is inappropriatefor the urban riverbed, potentially underestimating retardation by an order of magnitude. Organic petrography confirmed the urban riverbed contained a high proportion of TACM-rich organic-matter particles to which significant adsorption might be expected; furthermore, elevated urban Koc values wereconsistent with TACM-rich sediment literature estimates. The TACM source appears to be riverine transport of particulate matter from historical industrial/urban or coal-mining/processing activities prevalent upstream since the Industrial Revolution. Consequences of the increased urban riverbed residence time on attenuation and bioavailability assumption sensitivities were modelled. Under the standard assumption of sorbed contaminant being non-bioavailable, rapid rates of aqueous-phase biodegradation are necessaryfor complete attenuation within a riverbed. Conversely, if adsorbed contaminant is bioavailable, then complete attenuation is probable where highly adsorbing (Anthropocene urban) riverbed sediments are present, even for long half-lives. Therefore, Anthropocene-sediment occurrence may significantly influence modern-day contaminant fate within the urban riverbed; the principal implication being greatly increased sorption and residence times may occur in urban riverbeds than conventionally assumed. Further research should focus upon whether adsorbed contaminants have any bioavailability causing increased contaminant flux attenuation and surface-water quality protection.

AB - This study evaluates the hypothesis that increased organic-contaminant sorption and hence residence time in urban riverbed deposits may occur due to the presence of highly sorbing sediment components of anthropogenic origin that contain thermally altered carbonaceous materials (TACM). The hypothesiswas confirmed through laboratory-batch studies examining tetrachloroethene (PCE) sorption on riverbed sediment samples from the highly urbanised River Tame headwaters catchment (Birmingham, UK) and the River Tern (Shropshire) providing a nearby rural benchmark. Urban-riverbed sorption was elevatedwith observed organic-carbon partition coefficient (Koc) values over an order of magnitude greater than rural values. The latter compare to the widely used US EPA geometric-mean Koc and attributed to absorption-dominated partitioning into (recent) natural organic matter. Use of that mean is inappropriatefor the urban riverbed, potentially underestimating retardation by an order of magnitude. Organic petrography confirmed the urban riverbed contained a high proportion of TACM-rich organic-matter particles to which significant adsorption might be expected; furthermore, elevated urban Koc values wereconsistent with TACM-rich sediment literature estimates. The TACM source appears to be riverine transport of particulate matter from historical industrial/urban or coal-mining/processing activities prevalent upstream since the Industrial Revolution. Consequences of the increased urban riverbed residence time on attenuation and bioavailability assumption sensitivities were modelled. Under the standard assumption of sorbed contaminant being non-bioavailable, rapid rates of aqueous-phase biodegradation are necessaryfor complete attenuation within a riverbed. Conversely, if adsorbed contaminant is bioavailable, then complete attenuation is probable where highly adsorbing (Anthropocene urban) riverbed sediments are present, even for long half-lives. Therefore, Anthropocene-sediment occurrence may significantly influence modern-day contaminant fate within the urban riverbed; the principal implication being greatly increased sorption and residence times may occur in urban riverbeds than conventionally assumed. Further research should focus upon whether adsorbed contaminants have any bioavailability causing increased contaminant flux attenuation and surface-water quality protection.

KW - urban

KW - chlorinated aliphatic hydrocarbons (CAHs)

KW - anthropocene

KW - bioavailability

KW - sorption

KW - riverbed sediments

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DO - 10.1016/j.hydroa.2019.100023

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JO - Journal of Hydrology X

T2 - Journal of Hydrology X

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SN - 2589-9155

M1 - 100023

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