Large Column Setup for flow and heat transport experiments
The laboratory setup illustrated in Fig 1. can be used to study one-dimensional (1D) heat and solute tracer transport through a cylinder-shaped sample (length 1.5 m, inner diameter 0.29 m) at seepage velocities of va = 1 ‑ 50 m d‑1 and at temperatures of 5 – 70 °C.
Figure 1
Schematic experimental setup of the column. The refrigerated bath circulators serve as a hot and cold water storage. The volume flow is controlled by an eight-channel peristaltic pump. The red dots mark the positions of the Pt100 temperature sensors. The column can be installed in a vertical and horizontal configuration.
To enable an instant change between hot-water injection and cold-water injection, two refrigerated bath circulators (Witeg WCR-P22) are used. The two devices have an accuracy of ± 0.1 K. They can be used independently for heating and cooling and served here as cold and hot water tanks. An eight-channel peristaltic pump (Ismatec Ecoline) is used to control the volume flow into the column. A three-way valve is installed at each of the inflow tubes close to the column to allow tempering of the tubes without injection into the column. Furthermore, the three-way valves are used to inject a solute tracer.
A soil sample can be inserted in the acrylic glass column (Fig 2.).
Figure 2
A vertically movable perforated stabilization plate mounted on the lid prevented shifting of the sample during tilting of the column (Fig. 3). The column is thermally insulated by a 5-cm-thick layer of K‑Flex 25 (l = 0,034 W m-1 K-1) insulation. In addition, the inflow tubes are thermally insulated by a K‑Flex tube (wall thickness 10 mm). A tank at the end of the outflow tubes is installed to ensure the same pressure level at each outflow tube. A tank at the outflow is used to determine the volume flow through the column.
Figure 3
Further descriptions and results of the experiments can be found in the following publication:
Gossler, M. A., Bayer, P., Zosseder, K. (2019): Experimental investigation of thermal retardation and local thermal non-equilibrium effects on heat transport in highly permeable, porous aquifers, Journal of Hydrology. https://doi.org/10.1016/j.jhydrol.2019.124097