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  • 551.49
  • 2020-2022  (9)
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  • 2020-2022  (9)
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  • 1
    Publication Date: 2021-06-16
    Description: Large areas of Europe, especially in the Alps, are covered by carbonate rocks and in many alpine regions, karst springs are important sources for drinking water supply. Because of their high variability and heterogeneity, the understanding of the hydrogeological functioning of karst aquifers is of particular importance for their protection and utilisation. Climate change and heavy rainfall events are major challenges in managing alpine karst aquifers which possess an enormous potential for future drinking water supply. In this study, we present research from a high‐alpine karst system in the UNESCO Biosphere Reserve Großes Walsertal in Austria, which has a clearly defined catchment and is drained by only one spring system. Results show that (a) the investigated system is a highly dynamic karst aquifer with distinct reactions to rainfall events in discharge and electrical conductivity; (b) the estimated transient atmospheric CO2 sink is about 270 t/a; (c) the calculated carbonate rock denudation rate is between 23 and 47 mm/1000a and (d) the rainfall‐discharge behaviour and the internal flow dynamics can be successfully simulated using the modelling package KarstMod. The modelling results indicate the relevance of matrix storage in determining the discharge behaviour of the spring, particularly during low‐flow periods. This research and the consequent results can contribute and initiate a better understanding and management of alpine karst aquifers considering climate change with more heavy rainfall events and also longer dry periods.
    Description: The investigated karst system contributes to the transient atmospheric CO2 sink with about 270 t/a. Carbonate denudation rates vary between 23 and 47 mm/1000a. Rainfall‐discharge modelling results indicate the importance of matrix storage particularly during low‐flow periods. image
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: FP7 People: Marie‐Curie Actions http://dx.doi.org/10.13039/100011264
    Keywords: 551.49 ; CO2 sink ; denudation rate ; groundwater ; hydrochemical variability ; karst spring ; rainfall‐discharge model
    Type: article
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  • 2
    Publication Date: 2021-07-21
    Description: Through the release of groundwater, most mountain rivers run year‐round despite their small catchments and sporadic precipitation. This makes mountain ranges important sources of reliable freshwater for downstream populations in many parts of the world. However, due to a lack of ground instrumentation, little is known about groundwater dynamics in mountainous landscapes. Recent research has shown that the amount of moisture trapped in the soil and weathered rocks in the vadose zone can significantly buffer groundwater recharge and runoff but the wider recognition of this effect on major mountain systems has not been yet established. In this study, we test whether the moisture reservoir has an impact on hydrological fluxes in a steep Himalayan catchment during three monsoon seasons. We measured an array of parameters including relative seismic velocity changes from ambient noise correlations. This noninvasive technique allows us to monitor groundwater dynamics in conjunction with classical hydrological measurements. We found that the moisture saturation in the vadose zone controls the onset of groundwater recharge and runoff and therefore determines the annual water availability supplied by monsoon precipitation. We model this dynamic using a surface layer that has a finite storage capacity that controls the connectivity of surface flux to groundwater. The extension of this concept, which is thought to apply widely in flat and undulating landscapes, to steep mountain topography with thin and discontinuous soils underlain by regolith and bedrock has important implications for mountain hydrology.
    Description: Plain Language Summary: The Nepal Himalayas supply essential water resources to a large part of the population of South Asia. Most of this water drains through a mountain groundwater reservoir that is poorly constrained. In steep landscapes, this reservoir is continuously losing water due to gravitational pull. Understanding how the reservoir fills and drains is crucial to the assessment of its sustainability and projection into the future with respect to global climate change. However, the relevant subsurface processes are generally challenging to observe due to limited access to the subsurface, particularly in steep mountain landscapes. We have used seismic ambient noise, ground vibrations continuously recorded by seismometers, to monitor the groundwater dynamics on a spatially integrated scale in a Himalayan valley. We show that the moisture content of a shallow layer controls the transfer of precipitation into the deeper groundwater reservoir during the Indian monsoon seasons. Our study highlights the need to anticipate the effects of changes of land use, soil cover conditions and rainfall regime, due to climate change, to better predict the future of freshwater resources in mountain landscapes.
    Description: Key Points: Passive seismic interferometry reveals detailed insights into subsurface water storage variability in the Nepal Himalayas Vadose zone moisture saturation controls river discharge generation in a steep mountain landscape Freshwater delivery from high mountains is strongly dependent on subsurface conditions, which are rarely considered in these environments
    Description: GFZ HART program
    Keywords: 551.49 ; Himalayas ; mountain hydrology ; seismic noise | subsurface moisture ; summer monsoon ; vadose zone
    Type: article
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  • 3
    Publication Date: 2021-06-27
    Description: The water loss in packed beds was studied spatially and time‐resolved via magnetic resonance imaging on the pore scale. The packed beds were measured under water‐saturated and unsaturated conditions, while the magnetic resonance method allowed a quantitative differentiation between air, liquid, and solid phases exploring the native contrast of the named phases without additional contrast agents. Beside a qualitative image comparison, subsequent quantitative image processing allowed for a detailed spatially resolved determination of water distribution, the differentiation between water transport processes, and the quantification of liquid clusters in 3‐D. Results are presented for two packed beds that show significant differences in their evaporation and drainage dynamics, which are mainly determined by the physical properties of the packed beds. The water loss of the packed bed of 2–4 mm quartz particles reached a level below interpretability after 18.2 hr; meanwhile, a successive decrease of the largest liquid cluster volume from 82.5 to 0.7 mm3 was observed. The water content of the packed bed of 2 mm glass spheres was still observable after 70.9 hr. During the experiment, no significant changes in the structure of the liquid clusters were measured. The current work displays the applicability of magnetic resonance imaging for pore‐scale investigations without the addition of contrast agents.
    Description: Key Points: Pore‐scale investigations were performed by MRI without additional contrast agents Dominant water loss processes were differentiated. Liquid clusters were analyzed within the 3‐D data sets.
    Description: German Research Foundation (DFG) http://dx.doi.org/10.13039/501100001659
    Keywords: 551.49 ; MRI ; evaporation ; percolation ; liquid cluster
    Type: article
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  • 4
    Publication Date: 2021-07-04
    Description: High‐performance numerical codes are an indispensable tool for hydrogeologists when modeling subsurface flow and transport systems. But as they are written in compiled languages, like C/C++ or Fortran, established software packages are rarely user‐friendly, limiting a wider adoption of such tools. OpenGeoSys (OGS), an open‐source, finite‐element solver for thermo‐hydro‐mechanical–chemical processes in porous and fractured media, is no exception. Graphical user interfaces may increase usability, but do so at a dramatic reduction of flexibility and are difficult or impossible to integrate into a larger workflow. Python offers an optimal trade‐off between these goals by providing a highly flexible, yet comparatively user‐friendly environment for software applications. Hence, we introduce ogs5py, a Python‐API for the OpenGeoSys 5 scientific modeling package. It provides a fully Python‐based representation of an OGS project, a large array of convenience functions for users to interact with OGS and connects OGS to the scientific and computational environment of Python.
    Description: German Federal Environmental Foundation http://dx.doi.org/10.13039/100007636
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: 551.49 ; hydrogeology ; subsurface flow ; modeling ; software
    Type: article
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  • 5
    Publication Date: 2021-07-04
    Description: For simulating reactive transport on aquifer scale, various modeling approaches have been proposed. They vary considerably in their computational demands and in the amount of data needed for their calibration. Typically, the more complex a model is, the more data are required to sufficiently constrain its parameters. In this study, we assess a set of five models that simulate aerobic respiration and denitrification in a heterogeneous aquifer at quasi steady state. In a probabilistic framework, we test whether simplified approaches can be used as alternatives to the most detailed model. The simplifications are achieved by neglecting processes such as dispersion or biomass dynamics, or by replacing spatial discretization with travel‐time‐based coordinates. We use the model justifiability analysis proposed by Schöniger, Illman, et al. (2015, https://doi.org/10.1016/j.jhydrol.2015.07.047) to determine how similar the simplified models are to the reference model. This analysis rests on the principles of Bayesian model selection and performs a tradeoff between goodness‐of‐fit to reference data and model complexity, which is important for the reliability of predictions. Results show that, in principle, the simplified models are able to reproduce the predictions of the reference model in the considered scenario. Yet, it became evident that it can be challenging to define appropriate ranges for effective parameters of simplified models. This issue can lead to overly wide predictive distributions, which counteract the apparent simplicity of the models. We found that performing the justifiability analysis on the case of model simplification is an objective and comprehensive approach to assess the suitability of candidate models with different levels of detail.
    Description: Plain Language Summary: In groundwater, chemical substances like nitrate are transported and undergo chemical reactions. Understanding such reactive transport processes plays a key role in securing our water resources and drinking water. We use computer models for understanding such reactive transport processes and for simulating their future behavior. In such models, we make many scientific decisions on which processes should be included and in what degree of detail. Here, we face a trade‐off: Usually, a complex model with many mathematical terms resolves many details of the process. Yet, such complex models require lots of data for calibration and lots of time for the computer simulation. In contrast, a simple model with fewer details comes with less effort in both respects. However, it might neglect important parts of the process. For the example of nitrate decay, we use a probabilistic approach to find the best simplification for a comparatively detailed reference model. Our results show that, in certain cases, it is justified to employ a simpler model instead of a complex alternative without deteriorating modeling results. Alongside, we explain how difficult it can be to define realistic parameter ranges for simplified models.
    Description: Key Points: We compare a set of four simplified models against a reference model for reactive transport at quasi steady state on aquifer scale. A Bayesian model justifiability analysis helps identifying the most suitable model simplification strategy. The proposed analysis reveals the difficulty of reasonably constraining parameter priors for simplified models.
    Description: DFG http://dx.doi.org/10.13039/501100001659
    Keywords: 551.49 ; conceptual uncertainty ; reactive transport ; Bayesian model comparison ; model complexity
    Type: article
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  • 6
    Publication Date: 2021-10-29
    Description: In this study, we demonstrate by numerical density-dependent groundwater flow and transport modelling how transient beach morphology and regular storm floods that are typical for high-energy beaches change this classical picture of a subterranean estuary. The model results suggest that the variable beach morphology and seasonal storm floods lead to strong spatiotemporal variability of hydrodynamic and transport patterns reaching several 10th of meters into the subsurface, thereby distorting the classical salinity stratification. We believe that these findings are particularly relevant for sandy high-energy beaches which are commonly present at global coastlines.
    Keywords: 551.49 ; subterranean estuary ; pore water flow ; numerical modeling
    Type: map
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  • 7
    Publication Date: 2021-12-03
    Description: Micro-macro models for dissolution processes are derived from detailed pore-scale models applying upscaling techniques. They consist of flow and transport equations at the scale of the porous medium (macroscale). Both include averaged time- and space-dependent coefficient functions (permeability, porosity, reactive surface, and effective diffusion). These are in turn explicitly computed from the time- and space-dependent geometry of unit cells and by means of auxiliary cell problems defined therein (microscale). The explicit geometric structure is characterized by a level set. For its evolution, information from the transport equations solutions is taken into account (micro-macro scales). A numerical scheme is introduced, which is capable of evaluating such complex settings. For the level-set equation a second-order scheme is applied, which enables us to accurately determine the dynamic reactive surface. Local mesh refinement methods are applied to evaluate Stokes type cell problems using P2/P1 elements and a Uzawa type linear solver. Applications of our permeability solver to scenarios involving static and evolving geometries are presented. Furthermore, macroscopic flow and transport equations are solved applying mixed finite elements. Finally, adaptive strategies to overcome the computational burden are discussed. We apply our approach to the dissolution of an array of dolomite grains in the micro-macro context and validate our numerical scheme.
    Keywords: 551.49 ; 550.724 ; porous media ; reactive flow ; dissolution processes ; modeling
    Language: English
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  • 8
    Publication Date: 2021-11-30
    Description: We have used stable water isotopes (δ18O, δ2H) in combination with lumped-parameter modeling for characterizing unsaturated flow in two lysimeters vegetated with maize. The lysimeters contained undisturbed soil cores dominated by sandy gravel (Ly1) and clayey sandy silt (Ly2). Stable water isotopes were analyzed in precipitation and lysimeter outflow water over about 3 years. The mean transit time of water T and dispersion parameter PD, obtained from modeling, were higher for the silt soil in Ly2 than for the gravel soil in Ly1 (T of 362 vs. 129 d, PD of 0.7 vs. 0.12). The consideration of preferential flow (PF) paths could substantially improve the model curve fits, with 13 and 11% contribution of PF for Ly1 and Ly2 as best estimates. Different assumptions were compared to estimate the input function, that is, stable water isotope content in the recharging water. Using the isotopic composition of precipitation as input (no modification) resulted in reasonable model estimations. Best model fits for the entire observation were obtained by weighting the recharging isotopes according to average precipitation within periods of 3 and 6 months, in correspondence to changing vegetation phases and seasonal influences. Input functions that consider actual evapotranspiration could significantly improve modeling at some periods, however, this led to deviations between modeled and observed δ18O at other periods. This may indicate the influence of variable flow, so that dividing the whole observation period into hydraulically characteristic sub-periods for lumped-parameter modeling (which implements steady-state flow) is recommended for possible further improvement.
    Keywords: 551.49 ; groundwater flow modeling
    Language: English
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  • 9
    Publication Date: 2021-12-20
    Description: Aus drei Gebieten von Berlin (West), die einen geologisch verschiedenen, aber jeweils ziemlich homogenen Aufbau besitzen, wurden ca. 60 Grundwasserstandsganglinien und klimatologische Datenreihen analysiert. Das Ziel ist es, das allgemeine zeitliche Verhalten der Grundwasseroberfläche dieser Gebiete zu beschreiben und in Verbindung damit die Grundwasserneubildung zu berechnen. Grundlage der Untersuchung sind die Trend- und die Spektralanalyse. Bei der Trendanalyse wurden Polynome 3. Grades auf ihre Anwendung als Trendfunktion hin überprüft. Es zeigte sich, dass eine gute Approximation des langfristigen Verhaltens der Grundwasseroberfläche häufig nur durch Polynome 2. oder 3. Grades gegeben ist. Erst dann ist auch für einen begrenzten zukünftigen Zeitraum eine genaue Prognostizierung des mittleren Grundwasserstandes möglich und somit auch eine Abschätzung, wie sich zu künftige Grundwasserentnahmen auswirken können. Für die Spektralanalyse wurde aufgrund einer vergleichenden Darstellung von drei Berechnungsmethoden das auf der Theorie der stochastischen Prozesse basierende und von BLACKMAN & TUKEY (1959) erweiterte Verfahren zur Analyse der hier vorliegenden Zeitreihen als das am besten geeignete angesehen. Für die Untersuchung wurde ein entsprechendes EDV-Programm erstellt. Die Spektralanalyse ergab zwei Periodenbereiche, die sowohl in den Grundwasserstandsganglinien als auch in den klimatologischen Reihen Vorkommen. Vorherrschend sind Schwingungen, die durch 60 - 80-monatige Perioden in einer allgemeinen Form quantifiziert werden können. Daneben ist eine Jahresperiode vorhanden, die allerdings in den Grundwasserstandsganglinien nur teilweise, abhängig vom Flurabstand der Grundwasseroberfläche, nachzuweisen ist. Abhängig vom Auftreten der mehrjährigen und jährlichen Perioden setzt sich auch die Grundwasserneubildung aus zwei Anteilen zusammen. Als Bezugsgröße wurde die als klimatische Wasserbilanz definierte Größe (Niederschlag minus potentieller Evapotranspiration) angesehen. Bei tieferliegender Grundwasseroberfläche ist nur der Anteil aus dem langzeitlichen Schwingungsverlauf vorstehend aufgeführter Größe anzusetzen, während bei nachweisbarer Jahresperiode und damit geringerem Flurabstand der Grundwasseroberfläche noch ein Anteil aus jährlicher Versickerungsrate hinzukommt. Mit dem Phasenspektrum wird die Zeitverschiebung zwischen gleichen Perioden in klimatologischen Reihen und Grundwasserstandsganglinien ermittelt.
    Description: ABSTRACT: Approximately 60 groundwater level markings and climatological data were analyzed from three areas in Berlin (West) whose structures, although geologically different, are all rather homogeneous. It is the goal of this investigation to describe the general temporal behavior of the water table of these areas and to calculate, in regard to the temporal behavior, the formation of new groundwater. The basis of this investigation is trend and spectral analysis. Polynômes 3rd degree were utilized in the trend analysis in order to determine their applicability as trend functions. It was found that a good approximation of the long-term behavior of the water table is frequently given only by polynomes of the 2nd or 3rd degree. Just then, is a precise prognosis of the average groundwater level for a limited time span possible and therefore also an estimate of what effects future ground water removal can have. On the basis of a comparative description of three (mathematical) methods, the procedure based on the Theory of Stochastic Processes and enlarged by BLACKMANN & TUKEY ( 1959 ) was chosen as best suited for the analysis of this time series. A corresponding computer program was written for the investigation. The spectral analysis showed two periods that appeared both in the groundwater level markings and in the climatic series. Prevalent are oscillations exhibiting 60 - 80 month periods. In addition, a yearly period was found that is, however, only partially existent in the groundwater level markings and depends upon the water table field distance. The formation of new groundwater is composed of two parts depending upon the occurrence of the several year period and of the yearly period. As correlation, quantity defined as climatic water-balance (precipitation minus potential evapotranspirations) chosen. In case the groundwater table should lie deeper, only the part from the long-termillation course, which consists of the aforesaid quantity, should be taken into account. The time lag between the same periods in climatic series and groundwater level markings were ascertained the phase spectrum.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: 551.49 ; Hydrogeologie einzelner Regionen ; Berlin, Brandenburg, Sachsen-Anhalt und Mecklenburg-Vorpommern {Geologie} ; FID-GEO-DE-7
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