Bioturbation refers to the transport processes carried out by living organisms and their physical effects on soils and sediments. It is widely recognized as an important mixing mechanism, particularly at the sediment-water interface in many natural systems. In order to quantify its impact on mixing, we propose a process-based model based on simple assumptions about organism burrowing behavior. Specifically, we consider burrowing events to be stochastic but memoryless, leading to exponential inter-burrow waiting times and depths. We then explore the impact of two different transport mechanisms on the vertical concentration distributions predicted by the model for a conservative (inert) tracer. We compare the results of our model to experimen...
PhD Manuscript in Biogeochemistry and Functionnal EcologyThis study deals with the role of bioturbat...
Aquatic sediments are the recipients of a continual rain of organic debris from the water column. Th...
The burrow walls created by macrofauna in aquatic sediments are sites of intense chemical mass tran...
Bioturbation is the dominant mode of sediment transport in many aquatic environments and strongly in...
Bioturbation in aquatic sediments results from many different biological activities, inducing partic...
International audienceThe burrowing, feeding and foraging activities of terrestrial and benthic orga...
Bioturbation is one of the most widespread forms of ecological engineering and has significant impli...
International audienceBioturbation is one of the most widespread forms of ecological engineering and...
Mixing of sediments by benthic fauna represents a dominant transport process of solids in the majori...
Bioturbation models are typically one-dimensional, with the underlying assumption that tracer gradie...
The mixing of 210Pb and tagged particles is examined in a lattice-automaton model for bioturbation c...
We link specific mechanisms of biogenous sediment mixing with the commonly used bioturbation coeffic...
The physical mechanism that drives bioirrigation is strongly dependent on the permeability of the se...
Within the natural sciences, it has long been recognized that biological activity can modify the tex...
bioturbation bioirrigation biogeochemistry benthic ecology radon Boston Harbor a b s t r a c t The v...
PhD Manuscript in Biogeochemistry and Functionnal EcologyThis study deals with the role of bioturbat...
Aquatic sediments are the recipients of a continual rain of organic debris from the water column. Th...
The burrow walls created by macrofauna in aquatic sediments are sites of intense chemical mass tran...
Bioturbation is the dominant mode of sediment transport in many aquatic environments and strongly in...
Bioturbation in aquatic sediments results from many different biological activities, inducing partic...
International audienceThe burrowing, feeding and foraging activities of terrestrial and benthic orga...
Bioturbation is one of the most widespread forms of ecological engineering and has significant impli...
International audienceBioturbation is one of the most widespread forms of ecological engineering and...
Mixing of sediments by benthic fauna represents a dominant transport process of solids in the majori...
Bioturbation models are typically one-dimensional, with the underlying assumption that tracer gradie...
The mixing of 210Pb and tagged particles is examined in a lattice-automaton model for bioturbation c...
We link specific mechanisms of biogenous sediment mixing with the commonly used bioturbation coeffic...
The physical mechanism that drives bioirrigation is strongly dependent on the permeability of the se...
Within the natural sciences, it has long been recognized that biological activity can modify the tex...
bioturbation bioirrigation biogeochemistry benthic ecology radon Boston Harbor a b s t r a c t The v...
PhD Manuscript in Biogeochemistry and Functionnal EcologyThis study deals with the role of bioturbat...
Aquatic sediments are the recipients of a continual rain of organic debris from the water column. Th...
The burrow walls created by macrofauna in aquatic sediments are sites of intense chemical mass tran...