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  • 1
    In: Journal of Geophysical Research: Earth Surface, American Geophysical Union (AGU), Vol. 125, No. 10 ( 2020-10)
    Abstract: Thermokarst lake taliks may refreeze when inundated with seawater, even under floating ice conditions Salt rejection from lagoon ice formation and seasonal isolation from the sea cause hypersaline conditions below the lagoon's ice cover Subaquatic ice‐bearing permafrost formation suggests that not all subsea ice‐bearing permafrost is former terrestrial permafrost
    Type of Medium: Online Resource
    ISSN: 2169-9003 , 2169-9011
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2020
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2138320-0
    SSG: 16,13
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 2017
    In:  Journal of Applied Geophysics Vol. 146 ( 2017-11), p. 167-177
    In: Journal of Applied Geophysics, Elsevier BV, Vol. 146 ( 2017-11), p. 167-177
    Type of Medium: Online Resource
    ISSN: 0926-9851
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2017
    detail.hit.zdb_id: 1110469-7
    SSG: 16,13
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  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 2012
    In:  Journal of Applied Geophysics Vol. 78 ( 2012-3), p. 44-51
    In: Journal of Applied Geophysics, Elsevier BV, Vol. 78 ( 2012-3), p. 44-51
    Type of Medium: Online Resource
    ISSN: 0926-9851
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2012
    detail.hit.zdb_id: 1110469-7
    SSG: 16,13
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  • 4
    Online Resource
    Online Resource
    Elsevier BV ; 2022
    In:  Journal of Applied Geophysics Vol. 196 ( 2022-01), p. 104519-
    In: Journal of Applied Geophysics, Elsevier BV, Vol. 196 ( 2022-01), p. 104519-
    Type of Medium: Online Resource
    ISSN: 0926-9851
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2022
    detail.hit.zdb_id: 1110469-7
    SSG: 16,13
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  • 5
    Online Resource
    Online Resource
    Environmental and Engineering Geophysical Society ; 2007
    In:  Journal of Environmental and Engineering Geophysics Vol. 12, No. 2 ( 2007-06), p. 173-184
    In: Journal of Environmental and Engineering Geophysics, Environmental and Engineering Geophysical Society, Vol. 12, No. 2 ( 2007-06), p. 173-184
    Abstract: We investigate the influence of uncorrelated high frequency Gaussian noise on the accuracy and reliability of first-break arrival time picks. Using a reliable automatic picking algorithm based on the Akaike information criterion (AIC) and systematically noise contaminated synthetic data, allows us to develop a characteristic relation between the mis-pick (i.e., the error in the picked arrival time) and the signal-to-noise (S∕N) ratio for a specific waveform. For typical near-surface crosshole georadar survey setups, we further study the impact of such noise-related picking errors on tomographically reconstructed velocity images. Using synthetic and field data examples, results of tomographic inversions illustrate that significant velocity distortions can be introduced by noise-related mis-picking. In addition, we show that, under favorable conditions, it is possible to correct the noise-related picking errors prior to inversion.
    Type of Medium: Online Resource
    ISSN: 1083-1363 , 1943-2658
    Language: English
    Publisher: Environmental and Engineering Geophysical Society
    Publication Date: 2007
    detail.hit.zdb_id: 2114966-5
    detail.hit.zdb_id: 2252108-2
    SSG: 16,12
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  • 6
    Online Resource
    Online Resource
    Society of Exploration Geophysicists ; 2012
    In:  GEOPHYSICS Vol. 77, No. 1 ( 2012-01), p. R19-R32
    In: GEOPHYSICS, Society of Exploration Geophysicists, Vol. 77, No. 1 ( 2012-01), p. R19-R32
    Abstract: Particle swarm optimization (PSO) is a relatively new global optimization approach inspired by the social behavior of bird flocking and fish schooling. Although this approach has proven to provide excellent convergence rates in different optimization problems, it has seldom been applied to inverse geophysical problems. Until today, published geophysical applications mainly focus on finding an optimum solution for simple, 1D inverse problems. We have applied PSO-based optimization strategies to reconstruct 2D P-wave velocity fields from crosshole traveltime data sets. Our inversion strategy also includes generating and analyzing a representative ensemble of acceptable models, which allows us to appraise uncertainty and nonuniqueness issues. The potential of our strategy was tested on field data collected at a well-constrained test site in Horstwalde, Germany. At this field site, the shallow subsurface mainly consists of sand- and gravel-dominated glaciofluvial sediments, which, as known from several boreholes and other geophysical experiments, exhibit some well-defined layering at the scale of our crosshole seismic data. Thus, we have implemented a flexible, layer-based model parameterization, which, compared with standard cell-based parameterizations, allows for significantly reducing the number of unknown model parameters and for efficiently implementing a priori model constraints. Comparing the 2D velocity fields resulting from our PSO strategy to independent borehole and direct-push data illustrated the benefits of choosing an efficient global optimization approach. These include a straightforward and understandable appraisal of nonuniqueness issues as well as the possibility of an improved and also more objective interpretation.
    Type of Medium: Online Resource
    ISSN: 0016-8033 , 1942-2156
    RVK:
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2012
    detail.hit.zdb_id: 2184-2
    SSG: 16,13
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  • 7
    Online Resource
    Online Resource
    Society of Exploration Geophysicists ; 2020
    In:  GEOPHYSICS Vol. 85, No. 3 ( 2020-05-01), p. A19-A23
    In: GEOPHYSICS, Society of Exploration Geophysicists, Vol. 85, No. 3 ( 2020-05-01), p. A19-A23
    Abstract: Earth and environmental sciences rely on detailed information about subsurface processes. Whereas geophysical techniques typically provide highly resolved spatial images, monitoring subsurface processes is often associated with enormous effort and, therefore, is usually limited to point information in time or space. Thus, the development of spatial and temporal continuous field monitoring methods is a major challenge for the understanding of subsurface processes. We have developed a novel method for ground-penetrating-radar (GPR) reflection monitoring of subsurface flow processes under unsaturated conditions and applied it to a hydrological infiltration experiment performed across a periglacial slope deposit in northwest Luxembourg. Our approach relies on a spatial and temporal quasicontinuous data recording and processing, followed by an attribute analysis based on analyzing differences between individual time steps. The results demonstrate the ability of time-lapse GPR monitoring to visualize the spatial and temporal dynamics of preferential flow processes with a spatial resolution in the order of a few decimeters and temporal resolution in the order of a few minutes. We observe excellent agreement with water table information originating from different boreholes. This demonstrates the potential of surface-based GPR reflection monitoring to observe the spatiotemporal dynamics of water movements in the subsurface. It provides valuable, and so far not accessible, information for example in the field of hydrology and pedology that allows studying the actual subsurface processes rather than deducing them from point information.
    Type of Medium: Online Resource
    ISSN: 0016-8033 , 1942-2156
    RVK:
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2020
    detail.hit.zdb_id: 2184-2
    SSG: 16,13
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  • 8
    Online Resource
    Online Resource
    Society of Exploration Geophysicists ; 2002
    In:  GEOPHYSICS Vol. 67, No. 5 ( 2002-09), p. 1516-1523
    In: GEOPHYSICS, Society of Exploration Geophysicists, Vol. 67, No. 5 ( 2002-09), p. 1516-1523
    Abstract: We have used a combination of surface ground‐penetrating radar (GPR) profiling, crosshole radar tomography, and natural gamma‐ray logging to characterize a gravelly braided stream deposit. In a gravel pit, we conducted a survey using 300‐MHz surface GPR, 250‐MHz crosshole radar, and densely sampled gamma‐ray logging at single‐borehole locations. After excavation, we validated the geophysical results by comparison with the sedimentological and hydrogeological information obtained from the corresponding outcrop wall. We found the visual lithofacies boundaries agreed very well with the images provided by applied geophysical techniques. Our results illustrate how GPR reflector images are improved using tomographic velocity information. In addition, the structural interpretation of tomographic velocity fields is guided by the GPR reflector images in combination with natural gamma‐ray logging results. Groundwater flow and transport modeling was also performed on different subsurface models. The hydrogeological response of parameter distributions derived from a digitized outcrop image are compared with the response of a parameter field derived from the combined geophysical data and with the response of a simple block interpolation between the boreholes. Comparison of cumulative particle arrival times (breakthrough curves) indicates that the characterization of an appropriate real aquifer would benefit from incorporating high‐resolution geophysical data into the analysis.
    Type of Medium: Online Resource
    ISSN: 0016-8033 , 1942-2156
    RVK:
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2002
    detail.hit.zdb_id: 2184-2
    SSG: 16,13
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  • 9
    Online Resource
    Online Resource
    Society of Exploration Geophysicists ; 2018
    In:  GEOPHYSICS Vol. 83, No. 5 ( 2018-09-01), p. E335-E345
    In: GEOPHYSICS, Society of Exploration Geophysicists, Vol. 83, No. 5 ( 2018-09-01), p. E335-E345
    Abstract: In near-surface geophysics, small portable loop-loop electromagnetic induction (EMI) sensors using harmonic sources with a constant and rather small frequency are increasingly used to investigate the electrical properties of the subsurface. For such sensors, the influence of electrical conductivity and magnetic permeability on the EMI response is well-understood. Typically, data analysis focuses on reconstructing an electrical conductivity model by inverting the out-of-phase response. However, in a variety of near-surface applications, magnetic permeability (or susceptibility) models derived from the in-phase (IP) response may provide important additional information. In view of developing a fast 3D inversion procedure of the IP response for a dense grid of measurement points, we first analyze the 3D sensitivity functions associated with a homogeneous permeable half-space. Then, we compare synthetic data computed using a linear forward-modeling method based on these sensitivity functions with synthetic data computed using full nonlinear forward-modeling methods. The results indicate the correctness and applicability of our linear forward-modeling approach. Furthermore, we determine the advantages of converting IP data into apparent permeability, which, for example, allows us to extend the applicability of the linear forward-modeling method to high-magnetic environments. Finally, we compute synthetic data with the linear theory for a model consisting of a controlled magnetic target and compare the results with field data collected with a four-configuration loop-loop EMI sensor. With this field-scale experiment, we determine that our linear forward-modeling approach can reproduce measured data with sufficiently small error, and, thus, it represents the basis for developing efficient inversion approaches.
    Type of Medium: Online Resource
    ISSN: 0016-8033 , 1942-2156
    RVK:
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2018
    detail.hit.zdb_id: 2184-2
    SSG: 16,13
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  • 10
    In: GEOPHYSICS, Society of Exploration Geophysicists, Vol. 71, No. 3 ( 2006-05), p. H33-H44
    Abstract: Inversions of an individual geophysical data set can be highly nonunique, and it is generally difficult to determine petrophysical parameters from geophysical data. We show that both issues can be addressed by adopting a statistical multiparameter approach that requires the acquisition, processing, and separate inversion of two or more types of geophysical data. To combine information contained in the physical-property models that result from inverting the individual data sets and to estimate the spatial distribution of petrophysical parameters in regions where they are known at only a few locations, we demonstrate the potential of the fuzzy [Formula: see text] -means (FCM) clustering technique. After testing this new approach on synthetic data, we apply it to limited crosshole georadar, crosshole seismic, gamma-log, and slug-test data acquired within a shallow alluvial aquifer. The derived multiparameter model effectively outlines the major sedimentary units observed in numerous boreholes and provides plausible estimates for the spatial distributions of gamma-ray emitters and hydraulic conductivity.
    Type of Medium: Online Resource
    ISSN: 0016-8033 , 1942-2156
    RVK:
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2006
    detail.hit.zdb_id: 2184-2
    SSG: 16,13
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