Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow

Understanding the coupled continuum pipe-flow framework for modeling contaminant transport in karst systems is critical for protecting water resources therein. This study simulated point and non-point source nitrate concentration in a karst spring and investigated the results generated from the flow...

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Main Authors: Yuan Gao, Zexuan Xu, Shen Li, Wenjie Yu
Format: Article
Language:English
Published: MDPI AG 2022-05-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/14/10/1622
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author Yuan Gao
Zexuan Xu
Shen Li
Wenjie Yu
author_facet Yuan Gao
Zexuan Xu
Shen Li
Wenjie Yu
author_sort Yuan Gao
collection DOAJ
description Understanding the coupled continuum pipe-flow framework for modeling contaminant transport in karst systems is critical for protecting water resources therein. This study simulated point and non-point source nitrate concentration in a karst spring and investigated the results generated from the flow and transport model with and without discrete conduit flow. CFPv2 and CMT3D models were integrated to address the changes in nitrate concentration at a monthly scale in a karst spring, and the results were compared with that from an equivalent porous media (EPM) model with high-hydraulic conductivity (K) zones set in the main karstified area to represent conduits. The results show that the CFPv2+CMT3D model is able to describe well the recession of nitrate concentration in spring discharge, and the relatively larger deviation (slower nitrate recession) from the observed trend for the EPM model is probably a result of the limitation of utilizing high hydraulic conductivity cells to represent conduit. Moreover, simulated hydraulic heads in poorly karstified areas from the two models both show slight differences from the observations (the head RMSE values of calibration/validation for CFPv2 and MODFLOW models are 0.16 m/0.25 m and 0.26 m/0.17 m, respectively), indicating the inclusion of conduits may not affect the simulation considerably, and the lower the proportion of karstic area, the slight effects brought from the inclusion of conduits in the model. For highly karstified areas, the CFPv2+CMT3D model could provide more accurate results (head RMSE of calibration/validation for CFPv2 and MODFLOW are 0.22 m/0.06 and 0.52 m/0.47 m, respectively), showing the coupled continuum pipe-flow framework may be more appropriate for applying to highly and maturely karstified areas where the variations in the behavior of flow and contaminant transport are more affected by turbulent flow regime.
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spelling doaj.art-1ffbf36b802b45eaba8e583ff70e39a52023-11-23T13:35:18ZengMDPI AGWater2073-44412022-05-011410162210.3390/w14101622Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit FlowYuan Gao0Zexuan Xu1Shen Li2Wenjie Yu3School of Geology and Mining Engineering, Xinjiang University, Urumqi 830017, ChinaEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USASchool of Geology and Mining Engineering, Xinjiang University, Urumqi 830017, ChinaSchool of Geology and Mining Engineering, Xinjiang University, Urumqi 830017, ChinaUnderstanding the coupled continuum pipe-flow framework for modeling contaminant transport in karst systems is critical for protecting water resources therein. This study simulated point and non-point source nitrate concentration in a karst spring and investigated the results generated from the flow and transport model with and without discrete conduit flow. CFPv2 and CMT3D models were integrated to address the changes in nitrate concentration at a monthly scale in a karst spring, and the results were compared with that from an equivalent porous media (EPM) model with high-hydraulic conductivity (K) zones set in the main karstified area to represent conduits. The results show that the CFPv2+CMT3D model is able to describe well the recession of nitrate concentration in spring discharge, and the relatively larger deviation (slower nitrate recession) from the observed trend for the EPM model is probably a result of the limitation of utilizing high hydraulic conductivity cells to represent conduit. Moreover, simulated hydraulic heads in poorly karstified areas from the two models both show slight differences from the observations (the head RMSE values of calibration/validation for CFPv2 and MODFLOW models are 0.16 m/0.25 m and 0.26 m/0.17 m, respectively), indicating the inclusion of conduits may not affect the simulation considerably, and the lower the proportion of karstic area, the slight effects brought from the inclusion of conduits in the model. For highly karstified areas, the CFPv2+CMT3D model could provide more accurate results (head RMSE of calibration/validation for CFPv2 and MODFLOW are 0.22 m/0.06 and 0.52 m/0.47 m, respectively), showing the coupled continuum pipe-flow framework may be more appropriate for applying to highly and maturely karstified areas where the variations in the behavior of flow and contaminant transport are more affected by turbulent flow regime.https://www.mdpi.com/2073-4441/14/10/1622karst aquiferconduit flow processnitratespring
spellingShingle Yuan Gao
Zexuan Xu
Shen Li
Wenjie Yu
Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow
Water
karst aquifer
conduit flow process
nitrate
spring
title Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow
title_full Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow
title_fullStr Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow
title_full_unstemmed Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow
title_short Modeling Monthly Nitrate Concentration in a Karst Spring with and without Discrete Conduit Flow
title_sort modeling monthly nitrate concentration in a karst spring with and without discrete conduit flow
topic karst aquifer
conduit flow process
nitrate
spring
url https://www.mdpi.com/2073-4441/14/10/1622
work_keys_str_mv AT yuangao modelingmonthlynitrateconcentrationinakarstspringwithandwithoutdiscreteconduitflow
AT zexuanxu modelingmonthlynitrateconcentrationinakarstspringwithandwithoutdiscreteconduitflow
AT shenli modelingmonthlynitrateconcentrationinakarstspringwithandwithoutdiscreteconduitflow
AT wenjieyu modelingmonthlynitrateconcentrationinakarstspringwithandwithoutdiscreteconduitflow