Hodneland, Erlend

Hodneland, Erlend


T: +47 924 63 756

M: erho@norceresearch.no


  • PDE Based Algorithms for Smooth Watersheds

    Hodneland, Erlend; Xue-Cheng Tai, and Henrik Kalisch

    Watershed segmentation is useful for a number of image segmentation problems with a wide range of practical applications. Traditionally, the tracking of the immersion front is done by applying a fast sorting algorithm. In this work, we explore a continuous approach based on a geometric description of the immersion front which gives rise to a partial differential equation.

  • Physical models for simulation and reconstruction of human tissue deformation fields in dynamic MRI

    Hodneland, Erlend; Hanson E, Munthe-Kaas AZ, Lundervold A, Nordbotten JM.

    Medical image registration can be formulated as a tissue deformation problem, where parameter estimation methods are used to obtain the inverse deformation. However, there is limited knowledge about the ability to recover an unknown deformation. The main objective of this study is to estimate the quality of a restored deformation field obtained from image registration of dynamic MR sequences.

  • Quantifcation of single-kidney function and volume in living kidney donors using dynamic contrast-enhanced MRI

    Eikefjord E; Hodneland, Erlend; Andersen E, Svarstad E, Lundervold A, Rørvik J

    The objective of our study was to investigate whether dynamic contrast-enhanced MRI (DCE-MRI) can detect differences and potential adaption in single-kidney parenchymal volume, blood flow, glomerular filtration rate (GFR), and filtration fraction in the remaining kidney of healthy donors compared with nondonors. Further, we evaluated the agreement in donor GFRs measured using DCE-MRI versus serum clearance of iohexol.

  • Upscaling of Nonisothermal Reactive Porous Media Flow under Dominant Péclet Number: The Effect of Changing Porosity

    C. Bringedal; ; S. Pop, and F. A. Radu Read More: http://epubs.siam.org/doi/abs/10.1137/15M1022781

    Motivated by rock-fluid interactions occurring in a geothermal reservoir, we present a two-dimensional pore scale model of a thin strip consisting of void space and grains, with fluid flow through the void space. Ions in the fluid are allowed to precipitate onto the grains, while minerals in the grains are allowed to dissolve into the fluid, taking into account the possible change in the aperture of the strip that these two processes cause.