Abstract
Bacterial methane oxidation in landfill cover soils, which turns the emitting methane caused by waste degradation into carbon dioxide, reduces the climate impact of landfill gas emissions significantly, since methane is estimated to have a global warming potential (GWP) of 25 over 100 years (GWP of CO2 = 1). To understand and forecast the biological processes, a Finite-Element Model (FEM) is developed to simulate the behavior of methanotrophic layers. A multiphasic continuum mechanical approach based on the extended Theory of Porous Media (eTPM) is chosen, providing a macroscopic, multi-component view on the bacterial progress including the relevant gas transport processes of diffusion and advection in porous media as well as bacterial driven conversion processes. The presented thermodynamically consistent model also considers energy production within the gas phase resulting from exothermic reactions. An experimental setup was developed to validate the model also in terms of temperature development via the thermal imaging technique.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Similar content being viewed by others
References
Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, 2013.
J. Bluhm. Modelling of saturated thermo-elastic porous solids with different phase temperatures. In W. Ehlers and J. Bluhm, editors, Porous media: Theory, Experiments and Numerical Applications, pages 87–118. Springer-Verlag, Berlin - Heidelberg - New York, 2002.
R. M. Bowen. Toward a thermodynamics and mechanics of mixtures. Archives for Rational Mechanics and Analysis, 24:370–403, 1967.
R. M. Bowen. Theory of mixtures. In A. C. Eringen, editor, Continuum Physics, volume III, pages 1–127. Academic Press, New York, 1976.
B. D. Coleman and W. Noll. The thermodynamics of elastic materials with heat conduction and viscosity. Archives for Rational Mechanics and Analysis, 13:167–178, 1963.
R. de Boer. Theory of Porous Media – highlights in the historical development and current state. Springer-Verlag, Berlin, 2000.
A. Ebigbo, R. Helmig, A. B. Cunningham, H. Class, and R. Gerlach. Modelling biofilm growth in the presence of carbon dioxide and water flow in the subsurface. Advances in Water resources, 33:762–781, 2010.
W. Ehlers. Poröse Medien – ein kontinuumsmechanisches Modell auf der Basis der Mischungstheorie. Technical Report 47, Universität-GH Essen, 1989.
W. Ehlers. Foundations of multiphasic and porous materials. In W. Ehlers and J. Bluhm, editors, Porous Media: Theory, Experiments and Numerical Applications, pages 3–86. Springer-Verlag, Berlin, 2002.
S. Feng, C. W. W. Ng, A. K. Leung, and H. W. Liu. Numerical modelling of methane oxidation efficiency and coupled water-gas-heat reactive transfer in a sloping landfill cover. Waste Management, 68:355–368, 2017.
F. Golfier, B. D. Wood, L. Orgogozo, and M. Bus. Biofilms in porous media: Development of macroscopic transport equations via volume averaging with closure for local mass equilibrium conditions. Advances in Water Resources, 32:463–485, 2009.
C. V. Hettiarachchi, P. J. Hettiaratchi, A. K. Mehrotra, and S. Kumar. Field-scale operation of methane bio filtration systems to mitigate point source methane emissions. Environmental Pollution, 159 (6):1715–1720, 2011.
H. A. Hilger, D. F. Cranford, and M. Barlaz. Methane oxidation and microbial exopolymer production in landfill cover soil. Soil Biology & Biochemistry, 23:457–467, 2000.
H. A. Hilger, S. K. Liehr, and M. Barlaz. Exopolysaccharide control of methane oxidation in landfill cover soil. Journal of Environmental Engineering, 23:457–467, 1999.
M. Humer and P. Lechner. Deponiegasentsorgung von Altlasten mit Hilfe von Mikroorganismen. In sterreichische Wasser- und Abfallwirtschaft, number Heft 7/8 in 49. Jahrgang, pages 164–171. Springer-Verlag KG, Wien, 1997.
S. Molins and K. U. Mayer. Coupling between geochemical reactions and multicomponent gas and solute transport in unsaturated media: A reactive transport modeling study. Water Resources Research, 43(W05435), 2007.
S. Molins, K. U. Mayer, C. Scheutz, and P. Kjeldsen. Transport and reaction processes affecting the attenuation of landfill gas in cover soils. Journal of Environmental Quality, 37:459–468, 2008.
C. W. W. Ng, S. Feng, and H. W. Liu. A fully coupled model for water-gas-heat-reactive transport with methane oxidation in landfill covers. Science of the Total Environment, 508:307–319, 2015.
T. Ricken and J. Bluhm. Modeling of liquid and gas saturated porous solids under freezing and thawing cycles. In T. Schanz and A. Hettler, editors, Aktuelle Forschung in der Bodenmechanik 2013, chapter 2, pages 23–42. Springer-Verlag Berlin Heidelberg, 2014.
T. Ricken and R. de Boer. Multiphase flow in a capillary porous medium. Computational Materials Science, 28:704–713, 2003.
T. Ricken, A. Sindern, J. Bluhm, M. Denecke, T. Gehrke, and T. C. Schmidt. Concentration driven phase transitions in multiphase porous media with application to methane oxidation in landfill cover layers. Journal of Applied Mathematics and Mechanics, 94(7–8):609–622, 2014.
T. Ricken and V. Ustohalova. Modeling of thermal mass transfer in porous media with applications to the organic phase transition in landfills. Computational Materials Science, 32:498–508, 2005.
T. Ricken, N. Waschinsky, and D. Werner. Simulation of steatosis zonation in liver lobule - a continuummechanical bi-scale, tri-phasic, multicomponent approach. In Biomedical Technology, pages 15–33. Springer, 2018.
T. Ricken, D. Werner, H. Holzhütter, M. König, and U. D. und O. Dirsch. Modeling function–perfusion behavior in liver lobules including tissue, blood, glucose, lactate and glycogen by use of a coupled two-scale PDE–ODE approach. Biomechanics and Modeling in Mechanobiology, 14(3):515–536, 2015.
M. Robeck, T. Ricken, and R. Widmann. A finite element simulation of biological conversion processes in landfills. Waste Management, 31:663–669, 2011.
M. Schulte, M. A. Jochmann, T. Gehrke, A. Thom, T. Ricken, M. Denecke, and T. C. Schmidt. Characterization of methane oxidation in a simulated landfill cover system by comparing molecular and stable isotope mass balances. International Journal of Environment and Waste Management, 69:281–288, 2017.
J. C. Simo and K. S. Pister. Remarks on rate constitutive equations for finite deformation problems: Computational implications. Computer Methods in Applied Mechanics and Engineering, 46 (2):201–215, 1984.
A. Sindern, T. Ricken, J. Bluhm, M. Denecke, and T. C. Schmidt. Phase transition in methane oxidation layers - a coupled FE multiphase description. Proceedings of Applied Mathematics and Mechanics, 12:371–372, 2012.
A. Sindern, T. Ricken, J. Bluhm, R. Widmann, and M. Denecke. Bacterial methane oxidation in landfill cover layers - a coupled FE multiphase description. Proceedings of Applied Mathematics and Mechanics, 13:193–194, 2013.
A. Sindern, T. Ricken, J. Bluhm, R. Widmann, M. Denecke, and T. Gehrke. A coupled multi-component approach for bacterial methane oxidation in landfill cover layers. Proceedings of Applied Mathematics and Mechanics, 14:469–470, 2014.
V. B. Stein, J. P. A. Hettiratchi, and G. Achari. Numerical model for biological oxidation and migration of methane in soils. Practice Periodical ofHazardous, Toxic, and Radioactive Waste Management, 5 (4):225–234, 2001.
R. L. Taylor. FEAP - A Finite Element Analysis Program, 2012.
K. Terzaghi. Theoretical Soil Mechanics. J. Wiley and Sons, inc., 1943.
A. Thom, T. Ricken, J. Bluhm, R. Widmann, M. Denecke, and T. Gehrke. Validation of a coupled FE-model for the simulation of methane oxidation via thermal imaging. Proceedings of Applied Mathematics and Mechanics, 15:433–434, 2015.
C. Truesdell. Rational Thermodynamics. Springer-Verlag, Berlin - Heidelberg - New York, 2 edition, 1984.
V. Ustohalova, T. Ricken, and R. Widmann. Estimation of landfill emission lifespan using process oriented modeling - decompositions and transport processes. Waste Management, 26 (4):442–450, 2006.
A. D. Visscher and O. V. Cleemput. Simulation model for gas diffusion and methane oxidation in landfill cover soils. Waste Management, 23:581–591, 2003.
Q. Xue, Y. Zhao, Z. Li, and L. Liu. Numerical simulation on the cracking and failure law of compacted clay lining in landfill closure cover system. International Journal for Numerical and Analytical Methods in Geomechanics, 38:1556–1584, 2014.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Appendices
Appendix 1: Kinematics of Porous Media
The homogenized phases φ α are composed of particles Xα. At any time t each spatial point of the current placement is simultaneously occupied by every particle XS, XL, XG of the solid, liquid, and gas phase, whereby each particle proceeds from a different reference position X α at the time t = t0. Thus, each constituent is assigned to its own independent motion function χ α with
Equation (68)1 is called the Lagrange description of motion, Eq. (68)2 is the inverse map of the motion for a fixed time t, which represents the Euler description. The Euler description develops from the postulation that χ α is unique and uniquely invertible at any given time t. A mathematically necessary and sufficient condition for the existence of Eq. (68)2 is given, if the Jacobian Jα = detF α differs from zero with F α = Gradαχ α and its inverse \(\mathbf F_{\pmb {\alpha }}^{\mathrm {-1}}=\mathrm {grad}\,{\mathbf {x}}_{{\pmb {\alpha }}}\) as the deformation gradient. “Gradα” denotes the differential operator referring to the reference position X α of the constituent φ α, while “grad” refers to the actual position x. During the deformation process, F α is restricted to .
The velocity and acceleration vector, cf. (68)3−4, are defined with the material time derivatives of the Lagrange description. The material time derivative for scalar fields depending on x and t with respect to the trajectory of φ α is given with \((\ldots )^{\prime }_{{\pmb {\alpha }}}=\partial (\ldots )\,/\,\partial \mathrm {t}+[\mathrm{grad}(\ldots )]\cdot {\mathbf {x}}^{\prime }_{\pmb {\alpha }}\).
With (68)3 the material and spatial velocity gradient are defined with
The tensor \({\mathbf {D}}_{{\pmb {\alpha }}}=\text{1/2}\,({\mathbf {L}}_{{\pmb {\alpha }}}+{\mathbf {L}}_{{\pmb {\alpha }}}^{\mathrm {T}})\) is defined as the symmetric part of the spatial velocity gradient. An extended explanation of the kinematics of porous media is given in [6] and [9].
Appendix 2: Evaluation of Entropy Inequality
The resultant system of field equations is set up by 29 equations, namely Eqs. (22), (24), (25), (27), (28), (29), (30), as well as the physical constraint \(\hat {\mathbf {p}}^{\mathbf S} + \textstyle \sum _{\upgamma }\,\hat {\mathbf {p}}^{\mathrm {G}\upgamma } = \mathbf {o}\), the partial densities ρ S = nSρ SR and ρ G = nGρ GR, respectively. The field equations contain overall 91 scalar field quantities, namely
where the Cauchy stresses T S and T Gγ are symmetric. Since the solid phase is assumed to be incompressible and not involved into mass transfer, the real density of the solid is known and stays constant. The gravitational acceleration b is known as well and nitrogen is not involved into gas exchange, which leads to five known field quantities
In consequence, 57 field quantities remain for which constitutive relations have to be found. The constitutive quantities are chosen with
In order to provide a thermodynamic consistent description of the material behavior, the entropy inequality for the mixture is evaluated in accordance to [5], which yields restrictions for the constitutive relations. Following the principle of equipresence postulated by [35], the set of constitutive variables (72) can depend on the following process variables
Here, \({\mathbf {C}}_{\mathbf {S}} = {\mathbf {F}}_{\mathbf {S}}^{\mathrm {T}}{\mathbf {F}}_{\mathbf {S}}\) denotes the right Cauchy–Green deformation tensor. The entropy inequality for the binary model (solid and gas mixture) reads
It will be enhanced by the constraining saturation condition with the Lagrange multiplicator λ with
The overall gas balance in terms of molar concentration solved for \((\mathrm {n}^{\mathbf {G}})^{\prime }_{\mathbf {S}}\) reads
A mass specific Helmholtz free energy ψ Gγ for the partial gas components is introduced with
For simplification we postulate that the Helmholtz free energy functions ψ α hold the following dependencies
With the chosen dependencies of the Helmholtz free energy functions on the process variables, the material time derivatives \((\psi ^{{\pmb {\alpha }}})^{\prime }_{{\pmb {\alpha }}}\) read
the entropy inequality finally reads (sorted by the process variables and their derivatives):
The evaluation of the restrictions for the constitutive relations is presented in Sect. 4.
Rights and permissions
Copyright information
© 2020 Springer Nature Switzerland AG
About this chapter
Cite this chapter
Ricken, T. et al. (2020). Biological Driven Phase Transitions in Fully or Partly Saturated Porous Media: A Multi-Component FEM Simulation Based on the Theory of Porous Media. In: Giovine, P., Mariano, P.M., Mortara, G. (eds) Views on Microstructures in Granular Materials. Advances in Mechanics and Mathematics(), vol 44. Birkhäuser, Cham. https://doi.org/10.1007/978-3-030-49267-0_8
Download citation
DOI: https://doi.org/10.1007/978-3-030-49267-0_8
Published:
Publisher Name: Birkhäuser, Cham
Print ISBN: 978-3-030-49266-3
Online ISBN: 978-3-030-49267-0
eBook Packages: Mathematics and StatisticsMathematics and Statistics (R0)