Two-dimensional Multiscale Model of Cell Motion in a Chemotactic Field

Author(s):  
Mark Alber ◽  
Nan Chen ◽  
Tilmann Glimm ◽  
Pavel Lushnikov
2008 ◽  
Vol 36 (10) ◽  
pp. 1690-1698 ◽  
Author(s):  
Jared O. Barber ◽  
Jonathan P. Alberding ◽  
Juan M. Restrepo ◽  
Timothy W. Secomb

2020 ◽  
Vol 61 ◽  
pp. 368-381
Author(s):  
Elizabeth C. Holden ◽  
S. Jonathan Chapman ◽  
Bindi S. Brook ◽  
Reuben D. O'Dea

In this paper, we revisit our previous work in which we derive an effective macroscale description suitable to describe the growth of biological tissue within a porous tissue-engineering scaffold. The underlying tissue dynamics is described as a multiphase mixture, thereby naturally accommodating features such as interstitial growth and active cell motion. Via a linearization of the underlying multiphase model (whose nonlinearity poses a significant challenge for such analyses), we obtain, by means of multiple-scale homogenization, a simplified macroscale model that nevertheless retains explicit dependence on both the microscale scaffold structure and the tissue dynamics, via so-called unit-cell problems that provide permeability tensors to parameterize the macroscale description. In our previous work, the cell problems retain macroscale dependence, posing significant challenges for computational implementation of the eventual macroscopic model; here, we obtain a decoupled system whereby the quasi-steady cell problems may be solved separately from the macroscale description. Moreover, we indicate how the formulation is influenced by a set of alternative microscale boundary conditions. doi:10.1017/S1446181119000130


2018 ◽  
Vol 59 (4) ◽  
pp. 499-532
Author(s):  
E. C. HOLDEN ◽  
J. COLLIS ◽  
B. S. BROOK ◽  
R. D. O’DEA

We derive an effective macroscale description for the growth of tissue on a porous scaffold. A multiphase model is employed to describe the tissue dynamics; linearisation to facilitate a multiple-scale homogenisation provides an effective macroscale description, which incorporates dependence on the microscale structure and dynamics. In particular, the resulting description admits both interstitial growth and active cell motion. This model comprises Darcy flow, and differential equations for the volume fraction of cells within the scaffold and the concentration of nutrient, required for growth. These are coupled with Stokes-type cell problems on the microscale, incorporating dependence on active cell motion and pore scale structure. The cell problems provide the permeability tensors with which the macroscale flow is parameterised. A subset of solutions is illustrated by numerical simulations.


2019 ◽  
Vol 9 (12) ◽  
pp. 3055-3065 ◽  
Author(s):  
Carl-Robert Florén ◽  
Per-Anders Carlsson ◽  
Derek Creaser ◽  
Henrik Grönbeck ◽  
Magnus Skoglundh

A two-dimensional multiscale model is developed to describe the complete methane oxidation reaction for simulated exhaust gas conditions.


2017 ◽  
Vol 74 (9) ◽  
pp. 3099-3120 ◽  
Author(s):  
Qiu Yang ◽  
Andrew J. Majda

Abstract Superclusters on the synoptic scale containing mesoscale systems are frequently organized by convectively coupled equatorial waves (CCEWs). Present-day global models struggle to simulate multiscale tropical convection, and the upscale effects of mesoscale systems are not well understood. A simple two-dimensional multiscale model with prescribed two-scale heating and eddy transfer of momentum and temperature drives the synoptic-scale circulation, successfully reproduces key features of flow fields with a front-to-rear tilt, and compares well with results from a cloud-resolving model (CRM). In the scenario with an elevated upright mean heating, the tilted vertical structure of synoptic-scale circulation is still induced by the upscale impact of mesoscale disturbances. In a faster propagation scenario, the upscale impact becomes less important as a result of competing effects of eddy transfer of momentum and temperature, while the synoptic-scale circulation response to mean heating dominates, in agreement with cloud-resolving models. In the unrealistic scenario with upward–westward-tilted mesoscale heating, positive potential temperature anomalies are induced in the leading edge, which will suppress shallow convection in a moist environment.


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