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Featured researches published by G. Hornbruch.


Ground Water | 2009

Evaluation of Combined Direct-Push Methods Used for Aquifer Model Generation

Ralf Köber; G. Hornbruch; Carsten Leven; L. Tischer; Jochen Grossmann; Peter Dietrich; Holger Weiss; Andreas Dahmke

Most established methods to characterize aquifer structure and hydraulic conductivities of hydrostratigraphical units are not capable of delivering sufficient information in the spatial resolution that is desired for sophisticated numerical contaminant transport modeling and adapted remediation design. With hydraulic investigation methods based on the direct-push (DP) technology such as DP slug tests, DP injection logging, and the hydraulic profiling tool, it is possible to rapidly delineate hydrogeological structures and estimate their hydraulic conductivity in shallow unconsolidated aquifers without the need for wells. A combined application of these tools was used for the investigation of a contaminated German refinery site and for the setup of hydraulic aquifer models. The quality of DP investigation and the models was evaluated by comparisons of tracer transport simulations using these models and measured breakthroughs of two natural gradient tracer tests. Model scenarios considering the information of all tools together showed good reproduction of the measured breakthroughs, indicating the suitability of the approach and a minor impact of potential technical limitations. Using the DP slug tests alone yielded significantly higher deviations for the determined hydraulic conductivities compared to considering two or three of the tools. Realistic aquifer models developed on basis of such combined DP investigation approaches can help optimize remediation concepts or identify flow regimes for aquifers with a complex structure.


Journal of Contaminant Hydrology | 2016

Effect of injection velocity and particle concentration on transport of nanoscale zero-valent iron and hydraulic conductivity in saturated porous media.

Tessa J. Strutz; G. Hornbruch; Andreas Dahmke; Ralf Köber

Successful groundwater remediation by injecting nanoscale zero-valent iron (NZVI) particles requires efficient particle transportation and distribution in the subsurface. This study focused on the influence of injection velocity and particle concentration on the spatial NZVI particle distribution, the deposition processes and on quantifying the induced decrease in hydraulic conductivity (K) as a result of particle retention by lab tests and numerical simulations. Horizontal column tests of 2m length were performed with initial Darcy injection velocities (q0) of 0.5, 1.5, and 4.1m/h and elemental iron input concentrations (Fe(0)in) of 0.6, 10, and 17g/L. Concentrations of Fe(0) in the sand were determined by magnetic susceptibility scans, which provide detailed Fe(0) distribution profiles along the column. NZVI particles were transported farther at higher injection velocity and higher input concentrations. K decreased by one order of magnitude during injection in all experiments, with a stronger decrease after reaching Fe(0) concentrations of about 14-18g/kg(sand). To simulate the observed nanoparticle transport behavior the existing finite-element code OGS has been successfully extended and parameterized for the investigated experiments using blocking, ripening, and straining as governing deposition processes. Considering parameter relationships deduced from single simulations for each experiment (e.g. deposition rate constants as a function of flow velocity) one mean parameter set has been generated reproducing the observations in an adequate way for most cases of the investigated realistic injection conditions. An assessment of the deposition processes related to clogging effects showed that the percentage of retention due to straining and ripening increased during experimental run time resulting in an ongoing reduction of K. Clogging is mainly evoked by straining which dominates particle deposition at higher flow velocities, while blocking and ripening play a significant role for attachment, mainly at lower injection velocities. Since the injection of fluids at real sites leads to descending flow velocities with increasing radial distance from the injection point, the simulation of particle transport requires accounting for all deposition processes mentioned above. Thus, the derived mean parameter set can be used as a basis for quantitative and predictive simulations of particle distributions and clogging effects at both lab and field scale. Since decreases in K can change the flow system, which may have positive as well as negative implications for the in situ remediation technology at a contaminated site, a reliable simulation is thus of great importance for NZVI injection and prediction.


Environmental Earth Sciences | 2016

Erratum to: Nanoscale zero-valent iron flakes for groundwater treatment

Ralf Köber; Henner Hollert; G. Hornbruch; M. Jekel; A. Kamptner; N. Klaas; Hanna Maes; K.-M. Mangold; E. Martac; A. Matheis; H. Paar; Andreas Schäffer; H. Schell; Andreas Schiwy; K. R. Schmidt; T. J. Strutz; S. Thümmler; Andreas Tiehm; Jürgen Braun

The original article has been published inadvertently with some errors. Corrected and supporting information is given below. 25 mL of 6 mM sodium boron hydride (NaBH4) was used for the investigations of coatings. The start concentration of iopromide solutions for the reactivity comparison of different particle batches was 2 g/ L (2.5 mmol/L). 725 mg PCE were used for the longterm reactivity column test with the particle production batch B2. Equation 1 should be replaced by the following equation:


Environmental Earth Sciences | 2012

Investigation of the geochemical impact of CO2 on shallow groundwater: design and implementation of a CO2 injection test in Northeast Germany

Anita Peter; Hendrik Lamert; Matthias Beyer; G. Hornbruch; Ben Heinrich; Alexandra Schulz; Helmut Geistlinger; Bernd Schreiber; Peter Dietrich; Ulrike Werban; Carsten Vogt; Hans-Hermann Richnow; Jochen Großmann; Andreas Dahmke


Environmental Earth Sciences | 2014

Nanoscale zero-valent iron flakes for groundwater treatment

Ralf Köber; Henner Hollert; G. Hornbruch; M. Jekel; A. Kamptner; N. Klaas; Hanna Maes; K.-M. Mangold; E. Martac; A. Matheis; H. Paar; Andreas Schäffer; H. Schell; Andreas Schiwy; K. R. Schmidt; T. J. Strutz; S. Thümmler; Andreas Tiehm; Jürgen Braun


Environmental Earth Sciences | 2012

Feasibility of geoelectrical monitoring and multiphase modeling for process understanding of gaseous CO2 injection into a shallow aquifer

Hendrik Lamert; Helmut Geistlinger; Ulrike Werban; Claudia Schütze; Anita Peter; G. Hornbruch; Alexandra Schulz; M. Pohlert; S. Kalia; Matthias Beyer; Jochen Großmann; Andreas Dahmke; Peter Dietrich


Energy Procedia | 2013

Monitoring Approaches for Detecting and Evaluating CO2 and Formation Water Leakages into Near-surface Aquifers☆

Frank Dethlefsen; Ralf Köber; Dirk Schäfer; Said Attia al Hagrey; G. Hornbruch; Markus Ebert; Matthias Beyer; Jochen Großmann; Andreas Dahmke


Energy Procedia | 2011

CO2 leakage test in a shallow aquifer for investigating the geochemical impact of CO2 on groundwater and for developing monitoring methods and concepts

Anita Peter; G. Hornbruch; Andreas Dahmke


Grundwasser | 2007

Schadstoffausbreitung unter Annahme verschiedener kinetischer Ansätze zur Modellierung mikrobiellen Abbaus

Dirk Schäfer; G. Hornbruch; B. Schlenz; Andreas Dahmke


Grundwasser | 2007

Contaminant spreading assuming different kinetic approaches to simulate microbial degradation

Dirk Schäfer; G. Hornbruch; B. Schlenz; Andreas Dahmke

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Peter Dietrich

Helmholtz Centre for Environmental Research - UFZ

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Alexandra Schulz

Helmholtz Centre for Environmental Research - UFZ

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Helmut Geistlinger

Helmholtz Centre for Environmental Research - UFZ

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Hendrik Lamert

Helmholtz Centre for Environmental Research - UFZ

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Ulrike Werban

Helmholtz Centre for Environmental Research - UFZ

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A. Matheis

University of Stuttgart

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