Related Experiment Video
Updated: May 6, 2026

10:07
Generating Controlled, Dynamic Chemical Landscapes to Study Microbial Behavior
Published on: January 31, 2020
6.0K
Dispersal dynamics of groundwater bacteria
1Department of Ecology, Chemical Ecology and Ecotoxicology, University of Lund, Helgonavägen 5, S-223 62, Lund, Sweden.
Microbial Ecology
|November 7, 2013
Summary
Bacterial dispersal in soil is a dynamic process influenced by nutrient conditions and cell surface properties. Understanding these factors helps predict how bacteria move through aquifer materials.
Area of Science:
- Environmental microbiology
- Geomicrobiology
- Soil science
Background:
- Bacterial dispersal in saturated porous soils involves partitioning between aqueous and solid phases.
- This partitioning is influenced by soil properties, water chemistry, and bacterial cell surface modifications.
- Nutrient conditions significantly impact bacterial partitioning and subsequent dispersal rates in aquifers.
Purpose of the Study:
- To investigate how nutrient conditions affect bacterial partitioning in porous soils.
- To develop and validate mathematical models for predicting bacterial dispersal rates in aquifer materials based on partitioning variations.
- To understand the dynamic, nonequilibrium nature of bacterial dispersal.
Main Methods:
- Utilized continuous-flow groundwater microcosms (water-saturated sand columns) under varying nutrient regimes.
- Employed two mathematical models: an advective-dispersive-sorptive model and a two-site reaction model.
- Isolated and radiolabeled indigenous groundwater bacteria to measure sorption and dispersal using breakthrough curves.
Main Results:
- Bacterial dispersal is a dynamic, nonequilibrium process influenced by subpopulations with differing adsorption kinetics.
- Cell surface hydrophobicity increased in low-nutrient groundwater, enhancing hydrophobic binding and attachment.
- Partitioning coefficients varied significantly with nutrient conditions, hydrodynamics, and oxygen supply.
Conclusions:
- Nutrient availability and cell surface properties critically control bacterial partitioning and dispersal in aquifer systems.
- Mathematical models incorporating nonequilibrium sorption and dynamic subpopulations can predict bacterial transport.
- Bacterial association with suspended colloidal material can influence dispersal through porous media.
Related Concept Videos
Freshwater Microbial Ecology
67
Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. These environments are broadly categorized into lotic systems—those with flowing waters like streams and most rivers—and lentic systems, which include still or slow-moving waters such as lakes, ponds, and marshes.In lentic systems, phytoplankton drive primary production, generating autochthonous organic carbon. In contrast, lotic...
67
Microbial Mats
75
Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...
75
Soil Microbial Ecology
89
Soil microbial ecology is defined by highly diverse, spatially structured communities that drive nutrient cycling, organic matter turnover, and overall ecosystem stability. Although a gram of soil can contain thousands of bacterial and archaeal taxa, the ecological processes they mediate are even more crucial for sustaining terrestrial life.Microhabitats and NichesSoil is a heterogeneous mixture of minerals, organic matter, water, and air. Microbes inhabit distinct microhabitats formed by...
89
Deep Sea Microbial Ecology
55
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches...
55
Microenvironments
61
Microorganisms inhabit highly localized spaces known as microenvironments, which are defined by distinct physical and chemical characteristics. These include oxygen concentration, pH, temperature, light availability, and nutrient levels. The conditions within a microenvironment can differ markedly from those in the surrounding area and significantly influence microbial growth, metabolism, and community structure.Microenvironments often display sharp physicochemical gradients over small spatial...
61
Marine Microbial Ecology
74
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
74

