TY - JOUR
T1 - Experimental Support for a Simplified Approach to CTRW Transport Models and Exploration of Parameter Interpretation
AU - Hansen, Scott K.
N1 - Funding Information:
We thank Prof. Brian Berkowitz for providing the original data for the HA flow cell experiment, Prof. Christine Stumpp for providing the original data for the MIMT column experiment, and both for helpful comments. The work was supported by the Israel Science Foundation personal research Grant 1872/19. SKH holds the Helen Unger Career Development Chair in Desert Hydrogeology at Ben‐Gurion University.
Publisher Copyright:
© 2022. The Authors.
PY - 2022/5/1
Y1 - 2022/5/1
N2 - We empirically test our earlier theoretical arguments about simplification of continuous-time random walk (CTRW) solute transport models, namely that without loss of generality the velocity-like term, vψ, may be set to mean groundwater velocity, the dispersion-like term, Dψ, defined by a classical, velocity-independent dispersivity, and the so-called time constant, τ, to unity. We also argue that for small-scale heterogeneous advection (HA) and mobile-immobile mass transfer (MIMT) CTRW transition time distributions, ψ(t), are unaffected by mean flow velocity. To experimentally test these claims, we re-analyze two bench-scale transport experiments—one for HA, one for MIMT—each performed at multiple flow rates in otherwise identical conditions, and show it is possible to simultaneously explain all breakthrough curves in each, subject to the above constraints. We compare our calibrations with earlier efforts for the same data sets. In the HA calibration we identify a ψ(t) of the same functional form as previous authors, and which yielded breakthrough predictions essentially identical to theirs, but with greatly differing parameters. This illustrates how values of individual CTRW parameters may not map one-to-one onto underlying physics. We recommend reporting complete model descriptions, discuss how the simplified approach assists in this and other theoretical considerations.
AB - We empirically test our earlier theoretical arguments about simplification of continuous-time random walk (CTRW) solute transport models, namely that without loss of generality the velocity-like term, vψ, may be set to mean groundwater velocity, the dispersion-like term, Dψ, defined by a classical, velocity-independent dispersivity, and the so-called time constant, τ, to unity. We also argue that for small-scale heterogeneous advection (HA) and mobile-immobile mass transfer (MIMT) CTRW transition time distributions, ψ(t), are unaffected by mean flow velocity. To experimentally test these claims, we re-analyze two bench-scale transport experiments—one for HA, one for MIMT—each performed at multiple flow rates in otherwise identical conditions, and show it is possible to simultaneously explain all breakthrough curves in each, subject to the above constraints. We compare our calibrations with earlier efforts for the same data sets. In the HA calibration we identify a ψ(t) of the same functional form as previous authors, and which yielded breakthrough predictions essentially identical to theirs, but with greatly differing parameters. This illustrates how values of individual CTRW parameters may not map one-to-one onto underlying physics. We recommend reporting complete model descriptions, discuss how the simplified approach assists in this and other theoretical considerations.
KW - Laplace transform
KW - continuous-time random walk
KW - mass transfer
KW - model calibration
KW - solute transport
KW - upscaling
UR - http://www.scopus.com/inward/record.url?scp=85130608983&partnerID=8YFLogxK
U2 - 10.1029/2021WR031350
DO - 10.1029/2021WR031350
M3 - Article
AN - SCOPUS:85130608983
SN - 0043-1397
VL - 58
JO - Water Resources Research
JF - Water Resources Research
IS - 5
M1 - e2021WR031350
ER -