82 research outputs found

    Toward a general calibration of the Swiss plate geophone system for fractional bedload transport

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    Substantial uncertainties in bedload transport predictions in steep streams have encouraged intensive efforts towards the development of surrogate monitoring technologies. One such system, the Swiss plate geophone (SPG), has been deployed and calibrated in numerous steep channels, mainly in the Alps. Calibration relationships linking the signal recorded by the SPG system to the intensity and characteristics of transported bedload can vary substantially between different monitoring stations, likely due to site-specific factors such as flow velocity and bed roughness. Furthermore, recent flume experiments on the SPG system have shown that site-specific calibration relationships can be biased by elastic waves resulting from impacts occurring outside the plate boundaries. Motivated by these findings, we present a hybrid calibration procedure derived from flume experiments and an extensive dataset of 308 direct field measurements at four different SPG monitoring stations. Our main goal is to investigate the feasibility of a general, site-independent calibration procedure for inferring fractional bedload transport from the SPG signal. First, we use flume experiments to show that sediment size classes can be distinguished more accurately using a combination of vibrational frequency and amplitude information than by using amplitude information alone. Second, we apply this amplitude-frequency method to field measurements to derive general calibration coefficients for 10 different grain-size fractions. The amplitude-frequency method results in more homogeneous signal responses across all sites and significantly improves the accuracy of fractional sediment flux and grain-size estimates. We attribute the remaining site-to-site discrepancies to large differences in flow velocity and discuss further factors that may influence the accuracy of these bedload estimates.ISSN:2196-632XISSN:2196-631

    1,2,3-Trifluoro­benzene

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    In the title compound, C6H3F3, weak electrostatic and dispersive forces between C(δ+)—F(δ−) and H(δ+)—C(δ−) groups are at the borderline of the hydrogen-bond phenomenon and are poorly directional and further deformed in the presence of π–π stacking inter­actions. The mol­ecule lies on a twofold rotation axis. In the crystal structure, one-dimensional tapes are formed via two anti­dromic C—H⋯F hydrogen bonds. These tapes are, in turn, connected into corrugated two-dimensional sheets by bifurcated C—H⋯F hydrogen bonds. Packing in the third dimension is furnished by π–π stacking inter­actions with a centroid–centroid distance of 3.6362 (14) Å

    1,3-Difluoro­benzene

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    The weak electrostatic and dispersive forces between C(δ+)—F(δ−) and H(δ+)—C(δ−) are at the borderline of the hydrogen-bond phenomenon and are poorly directional and further deformed in the presence of other dominant inter­actions, e.g. C—H⋯π. The title compound, C6H4F2, Z′ = 2, forms one-dimensional tapes along two homodromic C—H⋯F hydrogen bonds. The one-dimensional tapes are connected into corrugated two-dimensional sheets by further bi- or trifrucated C—H⋯F hydrogen bonds. Packing in the third dimension is controlled by C—H⋯π inter­actions

    DebrisInterMixing-2.3: a finite volume solver for three-dimensional debris-flow simulations with two calibration parameters. Part 2: Model validation with experiments

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    Here, we present validation tests of the fluid dynamic solver presented in von Boetticher et al. (2016), simulating both laboratory-scale and large-scale debris-flow experiments. The new solver combines a Coulomb viscoplastic rheological model with a Herschel-Bulkley model based on material properties and rheological characteristics of the analyzed debris flow. For the selected experiments in this study, all necessary material properties were known - the content of sand, clay (including its mineral composition) and gravel as well as the water content and the angle of repose of the gravel. Given these properties, two model parameters are sufficient for calibration, and a range of experiments with different material compositions can be reproduced by the model without recalibration. One calibration parameter, the Herschel-Bulkley exponent, was kept constant for all simulations. The model validation focuses on different case studies illustrating the sensitivity of debris flows to water and clay content, channel curvature, channel roughness and the angle of repose. We characterize the accuracy of the model using experimental observations of flow head positions, front velocities, run-out patterns and basal pressures.Peer ReviewedPostprint (published version

    Ökologische Belastungsgrenzen von Ökosystemen: Entwicklung von ökologischen Belastungsgrenzen – Critical Loads – verschiedener Ökosysteme in Abhängigkeit von Klimawandel und Luftschadstoffen im polnisch-sächsischen Grenzraum

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    Klimawandel und Luftverschmutzung stellen zwei der größten Herausforderungen zum Schutz der Ökosysteme und zum Erhalt der biologischen Vielfalt dar. Zur Bewertung der Auswirkungen im polnisch-sächsischen Grenzraum dient das Konzept der ökologischen Belastungsgrenzen – Critical Loads (CL) genannt. CL beschreiben Grenzwerte für luftgetragene Schadstoffeinträge (Stickstoff und Schwefel), bei deren Einhaltung keine schädigenden Wirkungen auf empfindliche Ökosysteme zu erwarten sind. Der Bericht dokumentiert die für verschiedene Ökosystemtypen in Abhängigkeit von Klima- und Depositionsänderungen ermittelten CL sowie deren Überschreitung. Während die Belastungssituation durch versauernd wirkende Stoffeinträge zu vernachlässigen ist, stellt die Eutrophierung aufgrund von Stickstoffeinträgen ein hohes Risiko für die Ökosysteme dar. Maßnahmen zur Luftreinhaltung der letzten Jahrzehnte bewirken, dass der Anteil von Ökosystemen zunimmt, in denen CL eingehalten werden. Dem gegenüber erhöht sich allerdings die Empfindlichkeit der Ökosysteme hinsichtlich Eutrophierung durch die prognostizierten klimatischen Änderungen deutlich

    Показатели токсичности промышленных отходов

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    Безотходное производство - новая тенденция в промышленности всего мира. Продукция, получаемая из вторсырья, считается экологичной. Данное направление приветствуется в обществе. Но прежде чем приступить к переработке любой отход проходит оценку на пригодность для дальнейшего использования и токсичность. В зависимости от класса отхода применяется инструментальные методы (химические, физические и физико-химические) или биологические (биоиндикация, биотетирование).Wasteless production is a new trend in the industry of the whole world. Products derived from recyclables are considered environmentally friendly. This direction is becoming popular. Before recycling wastes pass the toxicity assessment. Permission or renouncemen will be issued after verification. Depending on the class of waste, instrumental methods (chemical, physical and physico-chemical), biological methods (bioindication, biotesting) are used

    Preliminary Comparison of Two-Way Satellite Time and Frequency Transfer and GPS Common-View Time Transfer During the INTELSAT Field Trial

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    For a decade and a half Global Positioning System (GPS) common-view time transfer has greatly served the needs of primary timing laboratories for regular intercomparisons of remote atomic clocks. However, GPS as a one-way technique has natural limits and may not meet all challenges of the comparison of the coming new generation of atomic clocks. Two-way satellite time and frequency transfer (TWSTFT) is a promising technique which may successfully complement GPS. For two years, regular TWSTFT's have been performed between eight laboratories situated in both Europe and North America, using INTELSAT satellites. This has enabled an extensive direct comparison to be made between these two high performance time transfer methods. The performance of the TWSTFT and GPS common view methods are compared over a number of time-transfer links. These links use a variety of time-transfer hardware and atomic clocks and have baselines of substantially different lengths. The relative merits of the two time-transfer systems are discussed
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