7A Diffusion in domains with switching boundaries
ثبت نشده
چکیده
In the analysis of narrow escape problems in Sect. 7.2, we assumed that the holes in the boundary of the domain were always open. However, if we view each pore as a stochastically gated ion channel, for example, then one has the problem of analyzing the diffusion equation in a domain with a randomly switching boundary (or partial boundary). Such a scenario also arises in the case of membrane diffusion within corrals, when one no longer assumes that the corral is well-mixed (Sect. 3.6). Mathematically speaking, we can view diffusion in a randomly switching environment as an example of a stochastic hybrid system involving a piecewise deterministic PDE4. We will exploit this interpretation in order to develop a method for analyzing the 1D diffusion equation with switching boundary conditions, based on discretizing space and constructing the Chapman-Kolmogorov (CK) equation for the resulting finite-dimensional stochastic hybrid system [5]. We show how the CK equation can be used to determine the moments of the stochastic concentration in the continuum limit. We thus obtain a hierarchy of equations for the rth moments, which take the form of r-dimensional parabolic PDEs that couple to lower order moments at the boundaries. The rth moments of the stochastic PDE determine the statistics of r non-interacting Brownian particles; although the particles are non-interacting, statistical correlations arise due to the fact that they all move in the same randomly switching environment.
منابع مشابه
Frequency Aanalysis of Annular Plates Having a Small Core and Guided Edges at Both Inner and Outer Boundaries
This paper deals with frequency analysis of annular plates having a small core and guided edges at both inner and outer boundaries. Using classical plate theory the governing differential equation of motion for the annular plate having a small core is derived and solved for the case of plate being guided at inner and outer edge boundaries. The fundamental frequencies for the first six modes of ...
متن کاملSensitivity Analysis of Different Convection Schemes and Center Domains for Numerical Simulation of Winter Precipitation Over Iran
This paper qualifies the effect of different convection schemes and center-domains on the simulation of winter precipitation over Iran using RegCM3 numerical climate model. It is compressible, finite difference with hydrostatic equilibrium in sigma coordinate with a semi-implicit algorithm for reduction of horizontal diffusion. Iran experienced two dry and wet periods during winters of 1997 and...
متن کاملPullback D-attractors for non-autonomous partly dissipative reaction-diffusion equations in unbounded domains
At present paper, we establish the existence of pullback $mathcal{D}$-attractor for the process associated with non-autonomous partly dissipative reaction-diffusion equation in $L^2(mathbb{R}^n)times L^2(mathbb{R}^n)$. In order to do this, by energy equation method we show that the process, which possesses a pullback $mathcal{D}$-absorbing set, is pullback $widehat{D}_0$-asymptotically compact.
متن کاملApplication of truncated gaussian simulation to ore-waste boundary modeling of Golgohar iron deposit
Truncated Gaussian Simulation (TGS) is a well-known method to generate realizations of the ore domains located in a spatial sequence. In geostatistical framework geological domains are normally utilized for stationary assumption. The ability to measure the uncertainty in the exact locations of the boundaries among different geological units is a common challenge for practitioners. As a simple a...
متن کاملAnomalous magnetization reversal due to proximity effect of antiphase boundaries
Here we report anomalous double switching hysteresis loop and high coercivity (∼0.1 T) in Fe3O4(110) thin films. Our analytical model based on spin chains confined within small antiphase boundary domains (APBDs) suggests a significant proximity effect of antiferromagnetic antiphase boundaries (APBs). Furthermore, the calculated domain size (D) follows the well-known scaling relation D = C√t . T...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
عنوان ژورنال:
دوره شماره
صفحات -
تاریخ انتشار 2016