Experimental data for the pressure-driven flow of concentrated lignocellulosic biomass (corn stover) in a circular pipe are presented. A positive curvature was observed in the pressure profile at steady state, both when the biomass was flowing, and for several minutes after the flow had stopped. After the flow into the pipe was stopped, biomass continued to be expelled for at least five minutes, suggesting that the material is compressible. Occasionally, the pressure and outlet flow rate exhibited rapid, transient fluctuations. The fluctuations would cease when dryer-than-average heterogeneities exited the pipe. A mathematical model is developed to treat the biomass as a compressible Bingham fluid with a density-dependent yield stress. This model quantitatively reproduces steady-state pressure profiles for both flowing and nonflowing states, and captures the transition between the two states after the inlet flow rate is set to zero. Our model cannot predict the rapid pressure fluctuations that appear to be associated with heterogeneities in composition.
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Research Article|
May 01 2018
Pressure-driven flow of lignocellulosic biomass: A compressible Bingham fluid
Joshua C. Duncan;
Joshua C. Duncan
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706
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Anaram Shahravan;
Anaram Shahravan
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706
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Joseph R. Samaniuk;
Joseph R. Samaniuk
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706
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Thatcher W. Root;
Thatcher W. Root
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706
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Michael D. Graham;
Michael D. Graham
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706
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Daniel J. Klingenberg;
Daniel J. Klingenberg
a)
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706a)Author to whom correspondence should be addressed; electronic mail: [email protected]
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C. Tim Scott;
C. Tim Scott
2
U.S. Forest Service Forest Products Laboratory
, 1 Gifford Pinchot Dr, Madison, Wisconsin 53726
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Keith J. Bourne;
Keith J. Bourne
2
U.S. Forest Service Forest Products Laboratory
, 1 Gifford Pinchot Dr, Madison, Wisconsin 53726
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Roland Gleisner
Roland Gleisner
2
U.S. Forest Service Forest Products Laboratory
, 1 Gifford Pinchot Dr, Madison, Wisconsin 53726
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Joshua C. Duncan
1
Anaram Shahravan
1
Joseph R. Samaniuk
1
Thatcher W. Root
1
Michael D. Graham
1
Daniel J. Klingenberg
1,a)
C. Tim Scott
2
Keith J. Bourne
2
Roland Gleisner
2
1
Department of Chemical and Biological Engineering, University of Wisconsin
, 1415 Engineering Dr., Madison, Wisconsin 53706
2
U.S. Forest Service Forest Products Laboratory
, 1 Gifford Pinchot Dr, Madison, Wisconsin 53726
a)Author to whom correspondence should be addressed; electronic mail: [email protected]
J. Rheol. 62, 801–815 (2018)
Article history
Received:
October 20 2017
Accepted:
April 16 2018
Citation
Joshua C. Duncan, Anaram Shahravan, Joseph R. Samaniuk, Thatcher W. Root, Michael D. Graham, Daniel J. Klingenberg, C. Tim Scott, Keith J. Bourne, Roland Gleisner; Pressure-driven flow of lignocellulosic biomass: A compressible Bingham fluid. J. Rheol. 1 May 2018; 62 (3): 801–815. https://doi.org/10.1122/1.5009943
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