Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?

The fluxes of water and solutes in the subsurface compartment of the Critical Zone are temporally dynamic and it is unclear how this impacts microbial mediated nutrient cycling in the spatially heterogeneous subsurface. To investigate this, we undertook numerical modeling, simulating the transport i...

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Main Authors: Swamini Khurana, Falk Heße, Anke Hildebrandt, Martin Thullner
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-03-01
Series:Frontiers in Water
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/frwa.2022.780297/full
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author Swamini Khurana
Falk Heße
Falk Heße
Anke Hildebrandt
Anke Hildebrandt
Anke Hildebrandt
Martin Thullner
author_facet Swamini Khurana
Falk Heße
Falk Heße
Anke Hildebrandt
Anke Hildebrandt
Anke Hildebrandt
Martin Thullner
author_sort Swamini Khurana
collection DOAJ
description The fluxes of water and solutes in the subsurface compartment of the Critical Zone are temporally dynamic and it is unclear how this impacts microbial mediated nutrient cycling in the spatially heterogeneous subsurface. To investigate this, we undertook numerical modeling, simulating the transport in a wide range of spatially heterogeneous domains, and the biogeochemical transformation of organic carbon and nitrogen compounds using a complex microbial community with four (4) distinct functional groups, in water saturated subsurface compartments. We performed a comprehensive uncertainty analysis accounting for varying residence times and spatial heterogeneity. While the aggregated removal of chemical species in the domains over the entire simulation period was approximately the same as that in steady state conditions, the sub-scale temporal variation of microbial biomass and chemical discharge from a domain depended strongly on the interplay of spatial heterogeneity and temporal dynamics of the forcing. We showed that the travel time and the Damköhler number (Da) can be used to predict the temporally varying chemical discharge from a spatially heterogeneous domain. In homogeneous domains, chemical discharge in temporally dynamic conditions could be double of that in the steady state conditions while microbial biomass varied up to 75% of that in steady state conditions. In heterogeneous domains, the interquartile range of uncertainty in chemical discharge in reaction dominated systems (log10Da > 0) was double of that in steady state conditions. However, high heterogeneous domains resulted in outliers where chemical discharge could be as high as 10–20 times of that in steady state conditions in high flow periods. And in transport dominated systems (log10Da < 0), the chemical discharge could be half of that in steady state conditions in unusually low flow conditions. In conclusion, ignoring spatio-temporal heterogeneities in a numerical modeling approach may exacerbate inaccurate estimation of nutrient export and microbial biomass. The results are relevant to long-term field monitoring studies, and for homogeneous soil column-scale experiments investigating the role of temporal dynamics on microbial redox dynamics.
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spelling doaj.art-65cb0d65f8fd4bc383c37bcc742a96f82022-12-21T21:10:33ZengFrontiers Media S.A.Frontiers in Water2624-93752022-03-01410.3389/frwa.2022.780297780297Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?Swamini Khurana0Falk Heße1Falk Heße2Anke Hildebrandt3Anke Hildebrandt4Anke Hildebrandt5Martin Thullner6Geomicrobial Reactive Transport Systems Group, Department of Environmental Microbiology, Helmholtz Centre for Environmental Research—UFZ, Leipzig, GermanyInstitute of Earth and Environmental Sciences-Geoecology, University Potsdam, Potsdam, GermanyDepartment of Computational Hydrosystems, Helmholtz Centre for Environmental Research—UFZ, Leipzig, GermanyDepartment of Computational Hydrosystems, Helmholtz Centre for Environmental Research—UFZ, Leipzig, GermanyInstitute of Geoscience, Friedrich-Schiller-University Jena, Jena, GermanyGerman Centre for Integrative Biodiversity Research, Leipzig, GermanyGeomicrobial Reactive Transport Systems Group, Department of Environmental Microbiology, Helmholtz Centre for Environmental Research—UFZ, Leipzig, GermanyThe fluxes of water and solutes in the subsurface compartment of the Critical Zone are temporally dynamic and it is unclear how this impacts microbial mediated nutrient cycling in the spatially heterogeneous subsurface. To investigate this, we undertook numerical modeling, simulating the transport in a wide range of spatially heterogeneous domains, and the biogeochemical transformation of organic carbon and nitrogen compounds using a complex microbial community with four (4) distinct functional groups, in water saturated subsurface compartments. We performed a comprehensive uncertainty analysis accounting for varying residence times and spatial heterogeneity. While the aggregated removal of chemical species in the domains over the entire simulation period was approximately the same as that in steady state conditions, the sub-scale temporal variation of microbial biomass and chemical discharge from a domain depended strongly on the interplay of spatial heterogeneity and temporal dynamics of the forcing. We showed that the travel time and the Damköhler number (Da) can be used to predict the temporally varying chemical discharge from a spatially heterogeneous domain. In homogeneous domains, chemical discharge in temporally dynamic conditions could be double of that in the steady state conditions while microbial biomass varied up to 75% of that in steady state conditions. In heterogeneous domains, the interquartile range of uncertainty in chemical discharge in reaction dominated systems (log10Da > 0) was double of that in steady state conditions. However, high heterogeneous domains resulted in outliers where chemical discharge could be as high as 10–20 times of that in steady state conditions in high flow periods. And in transport dominated systems (log10Da < 0), the chemical discharge could be half of that in steady state conditions in unusually low flow conditions. In conclusion, ignoring spatio-temporal heterogeneities in a numerical modeling approach may exacerbate inaccurate estimation of nutrient export and microbial biomass. The results are relevant to long-term field monitoring studies, and for homogeneous soil column-scale experiments investigating the role of temporal dynamics on microbial redox dynamics.https://www.frontiersin.org/articles/10.3389/frwa.2022.780297/fullreactive transport modelingspatio-temporal heterogeneityuncertaintygeomicrobial activitynutrient export
spellingShingle Swamini Khurana
Falk Heße
Falk Heße
Anke Hildebrandt
Anke Hildebrandt
Anke Hildebrandt
Martin Thullner
Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?
Frontiers in Water
reactive transport modeling
spatio-temporal heterogeneity
uncertainty
geomicrobial activity
nutrient export
title Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?
title_full Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?
title_fullStr Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?
title_full_unstemmed Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?
title_short Should We Worry About Surficial Dynamics When Assessing Nutrient Cycling in the Groundwater?
title_sort should we worry about surficial dynamics when assessing nutrient cycling in the groundwater
topic reactive transport modeling
spatio-temporal heterogeneity
uncertainty
geomicrobial activity
nutrient export
url https://www.frontiersin.org/articles/10.3389/frwa.2022.780297/full
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