Abstract

Microorganisms settle in diverse partially saturated porous media in the form of biofilms. The alteration of hydraulic properties and diffusive transport processes occurs simultaneously with biofilm growth in porous media. Imaging methods offer the ability to directly visualize and quantify alterations on the pore scale. However, imaging methods have mainly observed biofilm growth in completely saturated porous media. The current study used magnetic resonance imaging (MRI) to dynamically visualize biofilm growth within a porous medium under alternating drainage and flushing events. Prior to the MRI experiments, the sample was cultivated for 6 days within a porous medium consisting of 2 mm glass spheres. Starting from day 6, growth was monitored using MRI over a period of 7 days. The approach allowed for a visualization of all fractions (biofilm, water, air, and porous material) after drainage as well as flushing events. Biofilm was found to preferentially grow within permanently wetted areas situated next to pore throats. Furthermore, an increase in the water retention and connectivity of the liquid phase was found. The largest liquid cluster covered 11% (day 6) and 91% (day 12) of the total retained water, suggesting that biofilm growth might improve diffusive transport processes within partially saturated porous media.

Highlights

  • We propose that an ideal method requires: (I) a sufficient resolution to accurately resolve the pore spaces, (II) no depth limitation to the three-dimensional visualization of the entire porous medium, (III) adequate contrast to differentiate the phases, and (IV) noninvasiveness of the method in order to avoid the impairment of the porous material or microorganisms

  • Conditions on days 6, 9, and 12. (a) Biofilm growth can be recognized in the form of dark regions appearing next to contact points of glass spheres

  • Regions of interest (ROIs) that reveal occurring changes are highlighted in red

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Summary

Introduction

As a crucial part of the ecosystem, microorganisms are involved in the utilization of carbon sources, guaranteeing water quality, the removal of pollutants, the promotion of plant growth, and the regulation of greenhouse gas emissions within natural soils [1,2]. Their abundance and activity vary depending on the physical environment. A common response of microorganisms to stressful conditions, such as fluctuating water levels, is the production of extracellular polymeric substances (EPSs) and surface attachments, which lead to the formation of biofilms [4]

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