@misc{ToetzkeKardjilovMankeetal.2017,
  author    = {T{\"o}tzke, Christian and Kardjilov, Nikolay and Manke, Ingo and Oswald, Sascha},
  title     = {Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-402237},
  pages     = {9},
  year      = {2017},
  abstract  = {Water infiltration in soil is not only affected by the inherent heterogeneities of soil, but even more by the interaction with plant roots and their water uptake. Neutron tomography is a unique non-invasive 3D tool to visualize plant root systems together with the soil water distribution in situ. So far, acquisition times in the range of hours have been the major limitation for imaging 3D water dynamics. Implementing an alternative acquisition procedure we boosted the speed of acquisition capturing an entire tomogram within 10 s. This allows, for the first time, tracking of a water front ascending in a rooted soil column upon infiltration of deuterated water time-resolved in 3D. Image quality and resolution could be sustained to a level allowing for capturing the root system in high detail. Good signal-to-noise ratio and contrast were the key to visualize dynamic changes in water content and to localize the root uptake. We demonstrated the ability of ultra-fast tomography to quantitatively image quick changes of water content in the rhizosphere and outlined the value of such imaging data for 3D water uptake modelling. The presented method paves the way for time-resolved studies of various 3D flow and transport phenomena in porous systems},
  language  = {en}
}
@article{ToetzkeKardjilovMankeetal.2017,
  author    = {T{\"o}tzke, Christian and Kardjilov, Nikolay and Manke, Ingo and Oswald, Sascha},
  title     = {Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography},
  series = {Scientific reports},
  volume    = {7},
  journal   = {Scientific reports},
  publisher = {Macmillan Publishers Limited},
  address   = {London},
  issn      = {2045-2322},
  doi       = {10.1038/s41598-017-06046-w},
  year      = {2017},
  abstract  = {Water infiltration in soil is not only affected by the inherent heterogeneities of soil, but even more by the interaction with plant roots and their water uptake. Neutron tomography is a unique non-invasive 3D tool to visualize plant root systems together with the soil water distribution in situ. So far, acquisition times in the range of hours have been the major limitation for imaging 3D water dynamics. Implementing an alternative acquisition procedure we boosted the speed of acquisition capturing an entire tomogram within 10 s. This allows, for the first time, tracking of a water front ascending in a rooted soil column upon infiltration of deuterated water time-resolved in 3D. Image quality and resolution could be sustained to a level allowing for capturing the root system in high detail. Good signal-to-noise ratio and contrast were the key to visualize dynamic changes in water content and to localize the root uptake. We demonstrated the ability of ultra-fast tomography to quantitatively image quick changes of water content in the rhizosphere and outlined the value of such imaging data for 3D water uptake modelling. The presented method paves the way for time-resolved studies of various 3D flow and transport phenomena in porous systems.},
  language  = {en}
}
@article{ToetzkeCermakNadezhdinaetal.2017,
  author    = {T{\"o}tzke, Christian and Cermak, Jan and Nadezhdina, Nadezhda and Tributsch, Helmut},
  title     = {Electrochemical in-situ studies of solar mediated oxygen transport and turnover dynamics in a tree trunk of Tilia cordata},
  series = {iForest - Biogeosciences and Forestry},
  volume    = {10},
  journal   = {iForest - Biogeosciences and Forestry},
  number    = {2},
  publisher = {SISEF - The Italian Society of Silviculture and Forest Ecology},
  address   = {Potenza},
  issn      = {1971-7458},
  doi       = {10.3832/ifor1681-010},
  pages     = {355 -- 361},
  year      = {2017},
  abstract  = {Platinum electrodes were implanted into the xylem of a lime tree (Tilia cordata) stem and solar- induced electrochemical potential differences of up to 120 mV were measured during the vegetative period and up to 30 mV in winter. The time dependent curves were found to be delayed with respect to solar radiation, sap flow activity, temperature and vapor pressure deficit. A general equation for the potential difference was derived and simplified by analyzing the effect of temperature and tensile strength. The potential determining influence of oxygen concentration on the respective location of the platinum electrode was identified as the principal phenomenon measured. A systematic analysis and investigation of the observed periodic oxygen concentration signals promises new information on sap flow, oxygen diffusion through tree tissues and on oxygen consumption related to the energy turnover in tree tissues.},
  language  = {en}
}
@article{HaberPohlmeierToetzkeOswaldetal.2017,
  author    = {Haber-Pohlmeier, Sabina and T{\"o}tzke, Christian and Oswald, Sascha and Lehmann, Eberhard and Bl{\"u}mich, Bernhard and Pohlmeier, Andreas},
  title     = {Imaging of root zone processes using MRI T-1 mapping},
  series = {Microporous and mesoporous materials : zeolites, clays, carbons and related materials},
  volume    = {269},
  journal   = {Microporous and mesoporous materials : zeolites, clays, carbons and related materials},
  publisher = {Elsevier},
  address   = {Amsterdam},
  issn      = {1387-1811},
  doi       = {10.1016/j.micromeso.2017.10.046},
  pages     = {43 -- 46},
  year      = {2017},
  abstract  = {Noninvasive imaging in the root soil compartment is mandatory for improving knowledge about root soil interactions and uptake processes which eventually control crop growth and productivity. Here we propose a method of MRI T-1 relaxation mapping to investigate water uptake patterns, and as second example, in combination with neutron tomography (NT), property changes in the rhizosphere. The first part demonstrates quantification of solute enrichment by advective transport to the roots due to water uptake. This accumulation is counterbalanced by net downward flow and dispersive spreading. One can furthermore discriminate between zones of high accumulation patterns and zones with much less enrichment. This behavior persists over days. The second part presents the novel combination of MRI with neutron tomography to couple static, proton density information of roots and their interface to the surrounding soil with information about the local water dynamics, reflected by NMR relaxation times. The root soil interface of a broad bean plant is characterized by slightly increasing MRI and NT signal intensity but decreasing T-1 relaxation time indicating locally changed soil properties.},
  language  = {en}
}