Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating

<p>Effective porosity plays an important role in contaminant management. However, the effective porosity is often assumed to be constant in space and hence heterogeneity is either neglected or simplified in transport model calibration. Based on a calibrated highly parametrized flow model, a...

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Main Authors: R. Meyer, P. Engesgaard, K. Hinsby, J. A. Piotrowski, T. O. Sonnenborg
Format: Article
Language:English
Published: Copernicus Publications 2018-09-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/22/4843/2018/hess-22-4843-2018.pdf
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author R. Meyer
P. Engesgaard
K. Hinsby
J. A. Piotrowski
T. O. Sonnenborg
author_facet R. Meyer
P. Engesgaard
K. Hinsby
J. A. Piotrowski
T. O. Sonnenborg
author_sort R. Meyer
collection DOAJ
description <p>Effective porosity plays an important role in contaminant management. However, the effective porosity is often assumed to be constant in space and hence heterogeneity is either neglected or simplified in transport model calibration. Based on a calibrated highly parametrized flow model, a three-dimensional advective transport model (MODPATH) of a 1300&thinsp;km<sup>2</sup> coastal area of southern Denmark and northern Germany is presented. A detailed voxel model represents the highly heterogeneous geological composition of the area. Inverse modelling of advective transport is used to estimate the effective porosity of 7 spatially distributed units based on apparent groundwater ages inferred from 11 <sup>14</sup>C measurements in Pleistocene and Miocene aquifers, corrected for the effects of diffusion and geochemical reactions. By calibration of the seven effective porosity units, the match between the observed and simulated ages is improved significantly, resulting in a reduction of ME of 99&thinsp;% and RMS of 82&thinsp;% compared to a uniform porosity approach. Groundwater ages range from a few hundred years in the Pleistocene to several thousand years in Miocene aquifers. The advective age distributions derived from particle tracking at each sampling well show unimodal (for younger ages) to multimodal (for older ages) shapes and thus reflect the heterogeneity that particles encounter along their travel path. The estimated effective porosity field, with values ranging between 4.3&thinsp;% in clay and 45&thinsp;% in sand formations, is used in a direct simulation of distributed mean groundwater ages. Although the absolute ages are affected by various uncertainties, a unique insight into the complex three-dimensional age distribution pattern and potential advance of young contaminated groundwater in the investigated regional aquifer system is provided, highlighting the importance of estimating effective porosity in groundwater transport modelling and the implications for groundwater quantity and quality assessment and management.</p>
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spelling doaj.art-2c504aab54f44236bc240819c72da2022022-12-22T00:20:44ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382018-09-01224843486510.5194/hess-22-4843-2018Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C datingR. Meyer0P. Engesgaard1K. Hinsby2J. A. Piotrowski3T. O. Sonnenborg4Department of Geosciences and Natural Resources Management, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen, DenmarkDepartment of Geosciences and Natural Resources Management, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen, DenmarkGeological Survey of Denmark and Greenland, Øster Voldgade 10, 1350 Copenhagen, DenmarkDepartment of Geosciences, Aarhus University, Høegh-Guldbergs Gade 2, 8000 Aarhus, DenmarkGeological Survey of Denmark and Greenland, Øster Voldgade 10, 1350 Copenhagen, Denmark<p>Effective porosity plays an important role in contaminant management. However, the effective porosity is often assumed to be constant in space and hence heterogeneity is either neglected or simplified in transport model calibration. Based on a calibrated highly parametrized flow model, a three-dimensional advective transport model (MODPATH) of a 1300&thinsp;km<sup>2</sup> coastal area of southern Denmark and northern Germany is presented. A detailed voxel model represents the highly heterogeneous geological composition of the area. Inverse modelling of advective transport is used to estimate the effective porosity of 7 spatially distributed units based on apparent groundwater ages inferred from 11 <sup>14</sup>C measurements in Pleistocene and Miocene aquifers, corrected for the effects of diffusion and geochemical reactions. By calibration of the seven effective porosity units, the match between the observed and simulated ages is improved significantly, resulting in a reduction of ME of 99&thinsp;% and RMS of 82&thinsp;% compared to a uniform porosity approach. Groundwater ages range from a few hundred years in the Pleistocene to several thousand years in Miocene aquifers. The advective age distributions derived from particle tracking at each sampling well show unimodal (for younger ages) to multimodal (for older ages) shapes and thus reflect the heterogeneity that particles encounter along their travel path. The estimated effective porosity field, with values ranging between 4.3&thinsp;% in clay and 45&thinsp;% in sand formations, is used in a direct simulation of distributed mean groundwater ages. Although the absolute ages are affected by various uncertainties, a unique insight into the complex three-dimensional age distribution pattern and potential advance of young contaminated groundwater in the investigated regional aquifer system is provided, highlighting the importance of estimating effective porosity in groundwater transport modelling and the implications for groundwater quantity and quality assessment and management.</p>https://www.hydrol-earth-syst-sci.net/22/4843/2018/hess-22-4843-2018.pdf
spellingShingle R. Meyer
P. Engesgaard
K. Hinsby
J. A. Piotrowski
T. O. Sonnenborg
Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating
Hydrology and Earth System Sciences
title Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating
title_full Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating
title_fullStr Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating
title_full_unstemmed Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating
title_short Estimation of effective porosity in large-scale groundwater models by combining particle tracking, auto-calibration and <sup>14</sup>C dating
title_sort estimation of effective porosity in large scale groundwater models by combining particle tracking auto calibration and sup 14 sup c dating
url https://www.hydrol-earth-syst-sci.net/22/4843/2018/hess-22-4843-2018.pdf
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