Measuring and modeling of a three-dimensional tracer transport in a planted soil column

Schroeder, Natalie [Forschungszentrum Juelich, Agrosphere, Germany] Javaux, Mathieu [UCL] Haber-Pohlmeier, Sabina [4inst. technical and macromolecular chemistry, RWTH Aachen University, Germany] Pohlmeier, Andreas [Forschungszentrum Juelich, Agrosphere, Germany] Huber, Katrin [Forschungszentrum Juelich, Agrosphere, Germany] Vereecken, Harry [Forschungszentrum Juelich, Agrosphere, Germany] Vanderborght, Jan [Forschungszentrum Juelich, Agrosphere, Germany] et al.[show all]

Water flow from soil to root is driven by the plant transpiration and an important component of the hydrological cycle. The model R-SWMS combines three-dimensional (3D) water flow and solute transport in soil with a detailed description of root structure in three dimensions [1,2]. This model offers the possibility to calculate root water and solute uptake and flow within the roots, which enables explicit studies with respect to the distribution of water and solutes around the roots as well as local processes at the root-soil interface. In this study, we compared measured data from a tracer experiment using Magnetic Resonance Imaging (MRI) with simulations in order to assess the distribution and magnitude of the water uptake of a young lupine plant. An aqueous solution of the Gadolinium-complex (Gd-DTPA2-) was chosen as a tracer, as it behaves conservatively and is ideally suited for MRI. Water flow in the soil towards the roots can thus be visualized by following the change in tracer concentrations over time. The data were obtained by MRI, providing high resolution 3D images of the tracer distribution and root architecture structures by using a spin echo pulse sequence, which is strongly T1- weighted to be tracer sensitive [3], and T2 –weighted for root imaging [4]. This experimental setup was simulated using the 3D high-resolution numerical model R-SWMS. The comparison between MRI data and the simulations showed extensive effects of root architecture parameters on solute spreading. Although the results of our study showed the strength of combining non-invasive measurements and 3D modeling of solute and water flow in soil-root systems, where the derivation of plant hydraulic parameters such as axial and radial root conductivities is possible, current limitations were found with respect to MRI measurements and process description.