Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer
We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we deli...
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| Autor*in: |
Allen‐King, Richelle M [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. |
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| Übergeordnetes Werk: |
Enthalten in: Water resources research - Hoboken, NJ : Wiley, 1965, 51(2015), 3, Seite 1723-1743 |
|---|---|
| Übergeordnetes Werk: |
volume:51 ; year:2015 ; number:3 ; pages:1723-1743 |
| Links: |
|---|
| DOI / URN: |
10.1002/2014WR016161 |
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| 520 | |a We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units | ||
| 540 | |a Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. | ||
| 650 | 4 | |a volatile organic compound | |
| 650 | 4 | |a hydrophobic organic compound | |
| 650 | 4 | |a contaminant remediation | |
| 650 | 4 | |a sorption | |
| 650 | 4 | |a heterogeneity | |
| 650 | 4 | |a contaminant transport | |
| 650 | 4 | |a Sorption | |
| 700 | 1 | |a Kalinovich, Indra |4 oth | |
| 700 | 1 | |a Dominic, David F |4 oth | |
| 700 | 1 | |a Wang, Guohui |4 oth | |
| 700 | 1 | |a Polmanteer, Reid |4 oth | |
| 700 | 1 | |a Divine, Dana |4 oth | |
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10.1002/2014WR016161 doi PQ20160617 (DE-627)OLC1965565743 (DE-599)GBVOLC1965565743 (PRQ)c2450-ead25687deb89e08e5e74c42abd8d6379b845c95e542676e701e98479debc34e0 (KEY)0046260820150000051000301723hydrophobicorganiccontaminanttransportpropertyhete DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Allen‐King, Richelle M verfasserin aut Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. volatile organic compound hydrophobic organic compound contaminant remediation sorption heterogeneity contaminant transport Sorption Kalinovich, Indra oth Dominic, David F oth Wang, Guohui oth Polmanteer, Reid oth Divine, Dana oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 51(2015), 3, Seite 1723-1743 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:51 year:2015 number:3 pages:1723-1743 http://dx.doi.org/10.1002/2014WR016161 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2014WR016161/abstract http://search.proquest.com/docview/1673849904 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_2027 GBV_ILN_4219 38.85 AVZ AR 51 2015 3 1723-1743 |
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10.1002/2014WR016161 doi PQ20160617 (DE-627)OLC1965565743 (DE-599)GBVOLC1965565743 (PRQ)c2450-ead25687deb89e08e5e74c42abd8d6379b845c95e542676e701e98479debc34e0 (KEY)0046260820150000051000301723hydrophobicorganiccontaminanttransportpropertyhete DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Allen‐King, Richelle M verfasserin aut Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. volatile organic compound hydrophobic organic compound contaminant remediation sorption heterogeneity contaminant transport Sorption Kalinovich, Indra oth Dominic, David F oth Wang, Guohui oth Polmanteer, Reid oth Divine, Dana oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 51(2015), 3, Seite 1723-1743 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:51 year:2015 number:3 pages:1723-1743 http://dx.doi.org/10.1002/2014WR016161 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2014WR016161/abstract http://search.proquest.com/docview/1673849904 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_2027 GBV_ILN_4219 38.85 AVZ AR 51 2015 3 1723-1743 |
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10.1002/2014WR016161 doi PQ20160617 (DE-627)OLC1965565743 (DE-599)GBVOLC1965565743 (PRQ)c2450-ead25687deb89e08e5e74c42abd8d6379b845c95e542676e701e98479debc34e0 (KEY)0046260820150000051000301723hydrophobicorganiccontaminanttransportpropertyhete DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Allen‐King, Richelle M verfasserin aut Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. volatile organic compound hydrophobic organic compound contaminant remediation sorption heterogeneity contaminant transport Sorption Kalinovich, Indra oth Dominic, David F oth Wang, Guohui oth Polmanteer, Reid oth Divine, Dana oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 51(2015), 3, Seite 1723-1743 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:51 year:2015 number:3 pages:1723-1743 http://dx.doi.org/10.1002/2014WR016161 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2014WR016161/abstract http://search.proquest.com/docview/1673849904 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_2027 GBV_ILN_4219 38.85 AVZ AR 51 2015 3 1723-1743 |
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10.1002/2014WR016161 doi PQ20160617 (DE-627)OLC1965565743 (DE-599)GBVOLC1965565743 (PRQ)c2450-ead25687deb89e08e5e74c42abd8d6379b845c95e542676e701e98479debc34e0 (KEY)0046260820150000051000301723hydrophobicorganiccontaminanttransportpropertyhete DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Allen‐King, Richelle M verfasserin aut Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. volatile organic compound hydrophobic organic compound contaminant remediation sorption heterogeneity contaminant transport Sorption Kalinovich, Indra oth Dominic, David F oth Wang, Guohui oth Polmanteer, Reid oth Divine, Dana oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 51(2015), 3, Seite 1723-1743 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:51 year:2015 number:3 pages:1723-1743 http://dx.doi.org/10.1002/2014WR016161 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2014WR016161/abstract http://search.proquest.com/docview/1673849904 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_2027 GBV_ILN_4219 38.85 AVZ AR 51 2015 3 1723-1743 |
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10.1002/2014WR016161 doi PQ20160617 (DE-627)OLC1965565743 (DE-599)GBVOLC1965565743 (PRQ)c2450-ead25687deb89e08e5e74c42abd8d6379b845c95e542676e701e98479debc34e0 (KEY)0046260820150000051000301723hydrophobicorganiccontaminanttransportpropertyhete DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Allen‐King, Richelle M verfasserin aut Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. volatile organic compound hydrophobic organic compound contaminant remediation sorption heterogeneity contaminant transport Sorption Kalinovich, Indra oth Dominic, David F oth Wang, Guohui oth Polmanteer, Reid oth Divine, Dana oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 51(2015), 3, Seite 1723-1743 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:51 year:2015 number:3 pages:1723-1743 http://dx.doi.org/10.1002/2014WR016161 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2014WR016161/abstract http://search.proquest.com/docview/1673849904 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_2027 GBV_ILN_4219 38.85 AVZ AR 51 2015 3 1723-1743 |
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Enthalten in Water resources research 51(2015), 3, Seite 1723-1743 volume:51 year:2015 number:3 pages:1723-1743 |
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Allen‐King, Richelle M @@aut@@ Kalinovich, Indra @@oth@@ Dominic, David F @@oth@@ Wang, Guohui @@oth@@ Polmanteer, Reid @@oth@@ Divine, Dana @@oth@@ |
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Allen‐King, Richelle M ddc 550 bkl 38.85 misc volatile organic compound misc hydrophobic organic compound misc contaminant remediation misc sorption misc heterogeneity misc contaminant transport misc Sorption Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer |
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550 DNB 38.85 bkl Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer volatile organic compound hydrophobic organic compound contaminant remediation sorption heterogeneity contaminant transport Sorption |
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hydrophobic organic contaminant transport property heterogeneity in the borden aquifer |
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Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer |
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We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units |
| abstractGer |
We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units |
| abstract_unstemmed |
We determined that the spatial heterogeneity in aquifer properties governing the reactive transport of volatile organic contaminants is defined by the arrangement of lithofacies. We measured permeability ( k ) and perchloroethene sorption distribution coefficient ( K d ) for lithofacies that we delineated for samples from the Canadian Forces Base Borden Aquifer. We compiled existing data and collected 57 new cores to characterize a 30 m section of the aquifer near the test location of Mackay et al. (1986). The k and K d were measured for samples taken at six elevations from all cores to create a data set consisting of nearly 400 colocated measurements. Through analysis of variance (corrected for multiple comparisons), we determined that the 12 originally mapped lithofacies could be grouped into five relatively distinct chemohydrofacies that capture the variability of both transport properties. The mean of ln k by lithofacies was related to the grain size and the variance was relatively consistent. In contrast, both the mean and variance of ln K d were greater for more poorly sorted lithofacies, which were also typically more coarse‐grained. Half of the aquifer sorption capacity occurred in the three highest‐sorbing lithofacies but comprised only 20% of its volume. The model of the aquifer that emerged is that of discontinuous scour‐fill deposits of medium sand, generally characterized by greater K d and k , within laterally extensive fine‐grained to very fine‐grained sands of lower K d and k . Our findings demonstrate the importance of considering source rock composition, transport, and deposition processes when constructing conceptual models of chemohydrofacies. VOC Kd and k correlated to facies define their heterogeneity Only 20% of the aquifer volume accounts for 50% of aquifer sorption Coarse‐grained units have greater sorption capacity than fine‐grained units |
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Hydrophobic organic contaminant transport property heterogeneity in the Borden Aquifer |
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Kalinovich, Indra Dominic, David F Wang, Guohui Polmanteer, Reid Divine, Dana |
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