We show that the process of diffusion in statistically homogeneous velocity fields with finite correlation range “remembers” the shape and the orientation of the source over hundreds of dimensionless times and behaves ergodically with respect to the one‐particle dispersion only asymptotically.
Authors
Nicolae Suciu Friedrich-Alexander University of Erlangen-Nuremberg, Mathematics Department
Karl Sabelfeld Weierstrass Institute for Applied Analysis and Stochastics
Institute of Computational Math. and Math. Geophysics, Siberian Branch Russian Acad.
Călin Vamoş Tiberiu Popoviciu Institute of Numerical Analysis, Romanian Academy
Constantin Andronache Boston College, 140 Commonwealth Avenue, Chestnut Hill, USA
Keywords
Cite this paper as:
N. Suciu, K. Sabelfeld, C. Vamoş, C. Andronache, Memory effects and ergodicity for diffusion in spatially correlated velocity fields, Proc. Appl. Math. Mech., 7 (2007), 2010015-2010016
doi: 10.1002/pamm.200700057
[1] J. Eberhard, N. Suciu, and C. Vamos, On the self-averaging of dispersion for transport in quasi-periodic random media, J. Phys. A: Math. Theor. 40, 597 (2007), CrossRef (DOI).
[2] N. Suciu, C. Vamos¸, J. Vanderborght, H. Hardelauf, and H. Vereecken, Internal Report ICG-IV 00204, Forschungszentrum Julich (2004).
[3] N. Suciu, C. Vamos¸, J. Vanderborght, H. Hardelauf, and H. Vereecken, Numerical investigations on ergodicity of solute transport in heterogeneous aquifers, Water Resour. Res. 42, W04409 (2006), CrossRef (DOI)
[4] N. Suciu and C. Vamos, Comment on “Nonstationary flow and nonergodic transport in random porous media” by G. Darvini and P. Salandin, Water Resour. Res., (2007), CrossRef (DOI) (in press).
[5] C. Vamos¸, N. Suciu, and H. Vereecken, Generalized random walk algorithm for the numerical modeling of complex diffusion processes, J. Comput. Phys. 186(2), 527 (2003). CrossRef (DOI)
[6] C.L. Zirbel, Lagrangian observations of homogeneous random environments, Adv. Appl. Prob. 33, 810 (2001). CrossRef (DOI)
Proc Appl Math and Mech - 2008 - Suciu - Memory effects and ergodicity for diffusion in spatially co
Memory effects and ergodicity for diffusion in spatially correlated velocity fields
Nicolae Suciu ^(1,**){ }^{1, *}, Karl Sabelfeld ^(2,3){ }^{2,3}, Călin Vamoş ^(4){ }^{4}, and Constantin Andronache ^(5){ }^{5}¹ Friedrich-Alexander University of Erlangen-Nuremberg, Mathematics Department, Martensstr. 3, 91058 Erlangen, Germany.^(2){ }^{2} Weierstrass Institute for Applied Analysis and Stochastics, Mohrenstr. 39, 10117 Berlin, Germany.^(3){ }^{3} Institute of Computational Math. and Math. Geophysics, Siberian Branch Russian Acad. Sci., Prospect Lavrentjeva 6, 630090 Novosibirsk, Russia.^(4){ }^{4} Romanian Academy, Tiberiu Popoviciu Institute of Numerical Analysis, Romanian Academy, 400320 Cluj-Napoca, P. O. Box 68-1, Romania.^(5){ }^{5} Boston College, 140 Commonwealth Avenue, Chestnut Hill, MA 02467, USA.
Abstract
We show that the process of diffusion in statistically homogeneous velocity fields with finite correlation range "remembers" the shape and the orientation of the source over hundreds of dimensionless times and behaves ergodically with respect to the one-particle dispersion only asymptotically.
The problem of nonreactive transport in continuous medium is relevant in technical applications such as risk analysis, field monitoring and pollution control. This study aims to determine how solute dispersion depends on initial conditions and what are its ergodic properties. We consider a diffusion process in a fluid with velocity V(x)\mathbf{V}(\mathbf{x}) modeled as a random field statistically homogeneous with finite correlation range, continuously differentiable, and incompressible. We also assume the necessary measurability properties which ensure permutations of averages and integrals. For a given realization V(x)\mathbf{V}(x) and a constant diffusion coefficient DD, the trajectories of the local advection-diffusion process starting at t=0t=0 from the deterministic initial position X_(0)\mathbf{X}_{0} are the solutions of the integral Itô equation
{:(1)X_(l)(t)=X_(0l)+int_(0)^(t)V_(l)(X(t^(')))dt^(')+W_(l)(t):}\begin{equation*}
X_{l}(t)=X_{0 l}+\int_{0}^{t} V_{l}\left(\mathbf{X}\left(t^{\prime}\right)\right) d t^{\prime}+W_{l}(t) \tag{1}
\end{equation*}
where l=1,2,3l=1,2,3 and W_(l)(t)W_{l}(t) is a Wiener process of mean zero and variance 2Dt2 D t.
2 Memory effects on solute dispersion
The second central moment s_(ll)s_{l l} of the actual concentration is given by the dispersion s_(ll)=(:[X_(l)-(:X_(l):)_(DX_(0))]^(2):)_(DX_(0))s_{l l}=\left\langle\left[X_{l}-\left\langle X_{l}\right\rangle_{D X_{0}}\right]^{2}\right\rangle_{D X_{0}}, where the subscripts DD and X_(0)X_{0} indicate averages over diffusion and initial distribution of the solute molecules. With widetilde(X)_(l)=X_(l)-X_(0l)\widetilde{X}_{l}=X_{l}-X_{0 l},
where S_(ll)(0)=(:[X_(0l)-(:X_(0l):)_(X_(0))]^(2):)_(X_(0))S_{l l}(0)=\left\langle\left[X_{0 l}-\left\langle X_{0 l}\right\rangle_{X_{0}}\right]^{2}\right\rangle_{X_{0}} is the second moment of the initial concentration and m_(ll)=2(:[X_(0l)-(:X_(0l):)_(X_(0))] widetilde(X)_(l):)_(DX_(0))m_{l l}=2\left\langle\left[X_{0 l}-\left\langle X_{0 l}\right\rangle_{X_{0}}\right] \widetilde{X}_{l}\right\rangle_{D X_{0}} is a "memory term" which describes possible persistent influences of initial conditions. To emphasize the role of one-particle statistics and ensemble averaged center of mass, we add and subtract (:(: widetilde(X)_(l):)_(DV)^(2):)_(X_(0))\left\langle\left\langle\widetilde{X}_{l}\right\rangle_{D V}^{2}\right\rangle_{X_{0}} and (: widetilde(X)_(l):)_(DX_(0)V)^(2)\left\langle\widetilde{X}_{l}\right\rangle_{D X_{0} V}^{2} in (2) and perform the average over the ensemble of velocity realizations S_(ll)=(:s_(ll):)_(V)S_{l l}=\left\langle s_{l l}\right\rangle_{V} to obtain
The terms of (3) are as follows: the average over initial positions of the one-particle dispersion X_(ll)=(:[ widetilde(X)_(l)-(: widetilde(X)_(l):)_(DV)]^(2):)_(DV)X_{l l}=\left\langle\left[\widetilde{X}_{l}-\left\langle\widetilde{X}_{l}\right\rangle_{D V}\right]^{2}\right\rangle_{D V}, the variance of the center of mass R_(ll)=(:[(: widetilde(X)_(l):)_(DX_(0))-(: widetilde(X)_(l):)_(DX_(0)V)]^(2):)_(V)R_{l l}=\left\langle\left[\left\langle\widetilde{X}_{l}\right\rangle_{D X_{0}}-\left\langle\widetilde{X}_{l}\right\rangle_{D X_{0} V}\right]^{2}\right\rangle_{V}, the average over the ensemble of velocity realizations of the memory term M_(ll)=(:m_(ll):)_(V)M_{l l}=\left\langle m_{l l}\right\rangle_{V}, and the variance with respect to the initial position of the one-particle center of mass Q_(ll)=(:[(: widetilde(X)_(l):)_(DV)-(: widetilde(X)_(l):)_(DVX_(0))]^(2):)_(X_(0))Q_{l l}=\left\langle\left[\left\langle\widetilde{X}_{l}\right\rangle_{D V}-\left\langle\widetilde{X}_{l}\right\rangle_{D V X_{0}}\right]^{2}\right\rangle_{X_{0}} [4].
Using (1), the one-particle dispersion takes the explicit form
{:(4)X_(ll)(t;X_(0))=2Dt+int_(0)^(t)int_(0)^(t)(:u_(l)(X(t^(')))u_(l)(X(t^(''))):)_(VD)dt^(')dt^('')+2(:W_(l)(t)int_(0)^(t)(:u_(l)(X(t^('))):)_(V)dt^('):)_(D):}\begin{equation*}
X_{l l}\left(t ; \mathbf{X}_{0}\right)=2 D t+\int_{0}^{t} \int_{0}^{t}\left\langle u_{l}\left(\mathbf{X}\left(t^{\prime}\right)\right) u_{l}\left(\mathbf{X}\left(t^{\prime \prime}\right)\right)\right\rangle_{V D} d t^{\prime} d t^{\prime \prime}+2\left\langle W_{l}(t) \int_{0}^{t}\left\langle u_{l}\left(\mathbf{X}\left(t^{\prime}\right)\right)\right\rangle_{V} d t^{\prime}\right\rangle_{D} \tag{4}
\end{equation*}
Fig. 1 Transverse average memory terms for slab sources oriented across the mean flow.
Fig. 2 Standard deviations of transverse memory terms for slabs oriented across the mean flow.
where u_(l)(X(t))=V_(l)(X(t))-(:V_(l)(X(t)):)_(DV)u_{l}(\mathbf{X}(t))=V_{l}(\mathbf{X}(t))-\left\langle V_{l}(\mathbf{X}(t))\right\rangle_{D V} is the one-particle velocity fluctuation. For the assumed properties of the random velocity field, the velocity sampled on trajectories V(X(t))\mathbf{V}(\mathbf{X}(t)) has the same one-point probability distribution as V(x)\mathbf{V}(\mathbf{x}) [6]. This implies (:u_(l)(X(t^('))):)_(V)=0\left\langle u_{l}\left(\mathbf{X}\left(t^{\prime}\right)\right)\right\rangle_{V}=0 and the independence of X_(0)\mathbf{X}_{0} and the stationarity of the auto-correlation, i.e. (:u_(l)(X(t^(')))u_(l)(X(t^(''))):)_(V)=u_(ll)(t^(')-t^(''))\left\langle u_{l}\left(\mathbf{X}\left(t^{\prime}\right)\right) u_{l}\left(\mathbf{X}\left(t^{\prime \prime}\right)\right)\right\rangle_{V} =u_{l l}\left(t^{\prime}-t^{\prime \prime}\right). It follows that the last term of (4) vanishes and the one-particle dispersion is a "memory-free" quantity, independent of initial conditions, X_(ll)(t)=2Dt+int_(0)^(t)int_(0)^(t)(:u_(ll)(t^(')-t^('')):)_(D)dt^(')dt^('')X_{l l}(t)=2 D t+\int_{0}^{t} \int_{0}^{t}\left\langle u_{l l}\left(t^{\prime}-t^{\prime \prime}\right)\right\rangle_{D} d t^{\prime} d t^{\prime \prime}. For the same reason, M_(ll)M_{l l} and Q_(ll)Q_{l l} vanish and from (3) one obtains S_(ll)=S_(ll)(0)+X_(ll)-R_(ll)S_{l l}=S_{l l}(0)+X_{l l}-R_{l l}.
Numerical investigations [3] and perturbation approaches [1] indicate that for Gaussian fields with small fluctuations and point-like support of the initial concentration X_(ll)X_{l l} has a diffusive behavior ∼t\sim t in the limit of large times and that the single realization dispersion s_(ll)s_{l l} tends in the mean square limit to X_(ll)X_{l l}. Much less is known about the behavior of dispersion at finite times and for large sources. However, homogeneous fields with finite correlation range are ergodic and for large support of initial concentration distribution the space average with respect to X_(0)X_{0} of the velocity V_(l)(X(t))V_{l}(\mathbf{X}(t)) tends to its ensemble average (with respect to VV ). Using (1) and ergodicity of the velocity field, one can argue that for increasing source dimensions R_(ll)R_{l l} approaches to zero. Therefore, the average dispersion can be approximated by S_(ll)~~S_(ll)(0)+X_(ll)S_{l l} \approx S_{l l}(0)+X_{l l}. A similar ergodicity argument suggests that in the case of Gaussian velocity fields, when the auto-correlation is also ergodic, the second term in (2) approximates the one-particle variance X_(ll)X_{l l} and the actual dispersion can be estimated by s_(ll)~~S_(ll)(0)+X_(ll)+m_(ll)s_{l l} \approx S_{l l}(0)+X_{l l}+m_{l l}. Thus, the standard deviation of the single realization memory terms, SD(m_(ll))~~SD(s_(ll))S D\left(m_{l l}\right) \approx S D\left(s_{l l}\right), quantifies the "ergodicity in a large sense" [ 3,4 ] of the actual dispersion s_(ll)-S_(ll)(0)s_{l l}-S_{l l}(0) with respect to the memory-free stochastic model X_(ll)X_{l l}. Of course, this is true only for large enough extensions of the source. For small sources, the "ergodicity range" (:(s_(ll)-S_(ll)(0)-X_(ll))^(2):)_(V)^(1//2)\left\langle\left(s_{l l}-S_{l l}(0)-X_{l l}\right)^{2}\right\rangle_{V}^{1 / 2} has to be computed without the above approximation for s_(ll)[3,4]s_{l l}[3,4].
3 Numerical example
For illustration we present some results based on two-dimensional "global random walk" simulations [2,3,5]. An incompressible Gaussian velocity field was approximated with satisfactory precision by 640 periodic modes [1,2][1,2]. The Péclet number was fixed to Pe=U lambda//D=100P e=U \lambda / D=100, where UU is the ensemble mean velocity and lambda\lambda is a measure of the correlation range. Ensemble averages were performed over 5632 velocity realizations [2]. The initial condition consisted of uniform concentration distributions in transverse slabs ( lambda,L lambda\lambda, L \lambda ). The terms Q_(ll)Q_{l l} were found to be negligible small as compared with 2Dt2 D t. The transverse mean memory terms M_(22)M_{22} (derived from (3) for Q_(22)~~0Q_{22} \approx 0 and for one-particle dispersion X_(22)X_{22} estimated from point source simulations) remain relatively small up to L=200L=200 (Fig. 1). But the corresponding standard deviations, SD(m_(22))~~SD(s_(22))S D\left(m_{22}\right) \approx S D\left(s_{22}\right), are two orders of magnitude larger and show an important increase with the source dimension (Fig. 2). The longitudinal memory terms m_(11)m_{11} are negligible and s_(11)s_{11} behave ergodically with respect to X_(11)X_{11} at early times, provided that L >= 50L \geq 50.
Acknowledgements This work was supported in part by Deutsche Forschungsgemeinschaft grant SU 415/1-2, Romanian Ministry of Education and Research grant 2-CEx06-11-96, NATO Collaborative Linkage Grant ESP.NR.CLG 981426, and RFBR Grant 06-01-00498.
References
[1] J. Eberhard, N. Suciu, and C. Vamoş, J. Phys. A: Math. Theor. 40, 597 (2007), doi:10.1088/1751-8113/40/4/002.
[2] N. Suciu, C. Vamoş, J. Vanderborght, H. Hardelauf, and H. Vereecken, Internal Report ICG-IV 00204, Forschungszentrum Jülich (2004).
[3] N. Suciu, C. Vamoş, J. Vanderborght, H. Hardelauf, and H. Vereecken, Water Resour. Res. 42, W04409 (2006), doi:10.1029/2005WR004546.
[4] N. Suciu and C. Vamoş, Water Resour. Res., (2007), doi:10.1029/2007WR005946 (in press).
[5] C. Vamoş, N. Suciu, and H. Vereecken, J. Comput. Phys. 186(2), 527 (2003).
[6] C.L. Zirbel, Adv. Appl. Prob. 33, 810 (2001).