TY - JOUR

T1 - Drainage in heterogeneous sand columns with different geometric structures

AU - Vasin, M.

AU - Lehmann, P.

AU - Kaestner, A.

AU - Hassanein, R.

AU - Nowak, Wolfgang

AU - Helmig, Rainer

AU - Neuweiler, Insa

N1 - Funding information: The authors wish to acknowledge the assistance of Eberhard Lehmann and Gabriel Frei from the Paul Scherrer Institute, Villingen, Switzerland. The financial support of the German Federal Ministry of Education and Research (BMBF) and the German Research Foundation (Project Ne 824/2-2) are gratefully acknowledged.

PY - 2008/1/26

Y1 - 2008/1/26

N2 - This paper discusses multi-step drainage experiments in two heterogeneously packed sand columns (10 × 10 × 20 cm3). Different packing structures were generated using two different sand types. One purpose of the study was to test the influence of packing structures on the movement of water. The second purpose was to assess the quality of predictions for the outflow curves in both columns made with an upscaled model. The heterogeneous structures of the columns can be considered as two opposing extremes. The first column was packed with a random arrangement of two sand types that is not stochastically homogeneous and where a cluster running through the column exists for both materials. The second column was packed with a periodic pattern of coarse-sand inclusions in a fine-sand background and has a clearly defined unit cell. The depth-averaged (2D) spatial distribution of the water content in the columns was monitored during the whole multi-step outflow experiment using neutron radiography. The 3D water content was measured at the steady states by neutron tomography. The experimental results are compared with the model predictions of an upscaled model derived with the homogenization theory. The parameters for the upscaled model are calculated from the hydraulic parameters of the two sand types. These hydraulic parameters were first identified in independent measurements on samples of the two individual sand types, separately. Additionally, the hydraulic parameters of both sands were identified by fitting a numerical model to the measured outflow curves. The different column structures showed a significant effect on water retention and the effective retention function, as water was trapped in the coarse-sand inclusions of the periodic structure. We included this trapping effect in the effective retention function of the upscaled model with an apparent air entry pressure. Contrary to the retention, the different packing structures had no large effect on the dynamic behavior of the outflow. The effective conductivity of the columns is therefore not significantly influenced by the structure. The upscaled models predicted the movement of the averaged water content in the two columns well. This confirms the applicability of upscaled models even if the underlying requirements are not strictly met.

AB - This paper discusses multi-step drainage experiments in two heterogeneously packed sand columns (10 × 10 × 20 cm3). Different packing structures were generated using two different sand types. One purpose of the study was to test the influence of packing structures on the movement of water. The second purpose was to assess the quality of predictions for the outflow curves in both columns made with an upscaled model. The heterogeneous structures of the columns can be considered as two opposing extremes. The first column was packed with a random arrangement of two sand types that is not stochastically homogeneous and where a cluster running through the column exists for both materials. The second column was packed with a periodic pattern of coarse-sand inclusions in a fine-sand background and has a clearly defined unit cell. The depth-averaged (2D) spatial distribution of the water content in the columns was monitored during the whole multi-step outflow experiment using neutron radiography. The 3D water content was measured at the steady states by neutron tomography. The experimental results are compared with the model predictions of an upscaled model derived with the homogenization theory. The parameters for the upscaled model are calculated from the hydraulic parameters of the two sand types. These hydraulic parameters were first identified in independent measurements on samples of the two individual sand types, separately. Additionally, the hydraulic parameters of both sands were identified by fitting a numerical model to the measured outflow curves. The different column structures showed a significant effect on water retention and the effective retention function, as water was trapped in the coarse-sand inclusions of the periodic structure. We included this trapping effect in the effective retention function of the upscaled model with an apparent air entry pressure. Contrary to the retention, the different packing structures had no large effect on the dynamic behavior of the outflow. The effective conductivity of the columns is therefore not significantly influenced by the structure. The upscaled models predicted the movement of the averaged water content in the two columns well. This confirms the applicability of upscaled models even if the underlying requirements are not strictly met.

KW - Connected structures

KW - Effective parameters

KW - Heterogeneous media

KW - Multi-step outflow experiments

KW - Richards equation

KW - Upscaling

UR - http://www.scopus.com/inward/record.url?scp=50349093629&partnerID=8YFLogxK

U2 - 10.1016/j.advwatres.2008.01.004

DO - 10.1016/j.advwatres.2008.01.004

M3 - Article

AN - SCOPUS:50349093629

VL - 31

SP - 1205

EP - 1220

JO - Advances in water resources

JF - Advances in water resources

SN - 0309-1708

IS - 9

ER -