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321.
In this paper, the static load plate test and the dynamic load plate test by means of the light falling weight device are
assessed utilizing numerical simulations. Simplified computational models of the tested subsoil and of the testing devices
are developed, which capture the main effects of both the static and the dynamic load plate test. In extensive parametric
studies, the impact of various subsoil conditions on the test results and several sources of error are evaluated and discussed.
Computational test results of the static load plate test and of the dynamic load plate test are set in contrast to an effort
to demonstrate the differences and the common features of the outcomes. 相似文献
322.
323.
Late Miocene increasing exhumation rates in the eastern part of the Alps – implications from low temperature thermochronology
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Andreas Wölfler Walter Kurz Harald Fritz Christoph Glotzbach Martin Danišík 《地学学报》2016,28(5):297-305
A new set of apatite fission‐track and apatite (U–Th)/He data reveals a hitherto undated late Miocene exhumation pulse in the eastern part of the Eastern Alps. While distinct parts of the study area, including the Seckauer Tauern, have been at near surface conditions (<100 °C) since the Eocene, the neighbouring Niedere Tauern experienced enhanced cooling and exhumation in the middle Miocene and again at the late Miocene/Pliocene boundary. Middle Miocene exhumation is interpreted as a result of tectonic escape and convergence that operated simultaneously during lateral extrusion of the Eastern Alps. As the higher late Miocene/Pliocene exhumation rates are restricted to a single tectonic block, namely the Niedere Tauern, we infer a tectonic trigger that is probably related to a change in the external stress field that affected the Alps during this time. 相似文献
324.
It has been widely known that the use of two-frequency Satellite Laser Ranging (SLR) system is limited by stringent precision
requirements of the range measurements and the proper atmospheric model. Owing to the stringent requirements, this SLR system
is impractical for the current requirement of SLR measurements within the framework of global geodetic observing system (GGOS).
If in the future this stringent requirement could be met, this SLR system would be an attractive tool to reduce atmospheric
propagation effects of SLR and would be of great benefit for the next generation of GGOS design. To anticipate possible future
developments of the two-frequency SLR systems, we have developed a new atmospheric correction formula for the two-frequency
SLR measurements. The new formula eliminates the total atmospheric density effect including its gradient and provides two
terms to calculate the curvature effect and the water vapor distribution effect. While the curvature effect can be calculated
by an accurate model, the required information about the water vapor distribution along the propagation path can be calculated
using previous developments of optical delay modeling or alternatively using results from microwave measurements. Theoretical
simulations using the two-frequency systems of the Graz and TIGO-Concepción stations shows that the new formula completely
reduces all propagation effects at any elevation angle above 3° with an accuracy better than 1 mm. However, the required precision
for the difference of the two-frequency SLR measurements, i.e. better than 45 μm for a single epoch, exceeds the capability
of the current state of the art SLR systems. 相似文献
325.
Field Survey of the 27 February 2010 Chile Tsunami 总被引:1,自引:0,他引:1
Hermann M. Fritz Catherine M. Petroff Patricio A. Catal��n Rodrigo Cienfuegos Patricio Winckler Nikos Kalligeris Robert Weiss Sergio E. Barrientos Gianina Meneses Carolina Valderas-Bermejo Carl Ebeling Athanassios Papadopoulos Manuel Contreras Rafael Almar Juan Carlos Dominguez Costas E. Synolakis 《Pure and Applied Geophysics》2011,168(11):1989-2010
On 27 February 2010, a magnitude M w?=?8.8 earthquake occurred off the coast of Chile??s Maule region causing substantial damage and loss of life. Ancestral tsunami knowledge from the 1960 event combined with education and evacuation exercises prompted most coastal residents to spontaneously evacuate after the earthquake. Many of the tsunami victims were tourists in coastal campgrounds. The international tsunami survey team (ITST) was deployed within days of the event and surveyed 800?km of coastline from Quintero to Mehuín and the Pacific Islands of Santa María, Mocha, Juan Fernández Archipelago, and Rapa Nui (Easter). The collected survey data include more than 400 tsunami flow depth, runup and coastal uplift measurements. The tsunami peaked with a localized runup of 29?m on a coastal bluff at Constitución. The observed runup distributions exhibit significant variations on local and regional scales. Observations from the 2010 and 1960 Chile tsunamis are compared. 相似文献
326.
M.J. Truex V.R. Vermeul D.P. Mendoza B.G. Fritz R.D. Mackley M. Oostrom T.W. Wietsma T.W. Macbeth 《Ground Water Monitoring & Remediation》2011,31(1):50-58
Approximately 190 kg of 2 μm‐diameter zero‐valent iron (ZVI) particles were injected into a test zone in the top 2 m of an unconfined aquifer within a trichloroethene (TCE) source area. A shear‐thinning fluid was used to enhance ZVI delivery in the subsurface to a radial distance of up to 4 m from a single injection well. The ZVI particles were mixed in‐line with the injection water, shear‐thinning fluid, and a low concentration of surfactant. ZVI was observed at each of the seven monitoring wells within the targeted radius of influence during injection. Additionally, all wells within the targeted zone showed low TCE concentrations and primarily dechlorination products present 44 d after injection. These results suggest that ZVI can be directly injected into an aquifer with shear‐thinning fluids to induce dechlorination and extends the applicability of ZVI to situations where other emplacement methods may not be viable. 相似文献
327.
Kevin P. Norton Friedhelm von Blanckenburg Roman DiBiase Fritz Schlunegger Peter W. Kubik 《International Journal of Earth Sciences》2011,100(5):1163-1179
Denudation rates from cosmogenic 10Be measured in quartz from recent river sediment have previously been used in the Central Alps to argue that rock uplift occurs
through isostatic response to erosion in the absence of ongoing convergence. We present new basin-averaged denudation rates
from large rivers in the Eastern and Southern European Alps together with a detailed topographic analysis in order to infer
the forces driving erosion. Denudation rates in the Eastern and Southern Alps of 170–1,400 mm ky−1 are within a similar range to those in the Central Alps for similar lithologies. However, these denudation rates vary considerably
with lithology, and their variability generally increases with steeper landscapes, where correlations with topographic metrics
also become poorer. Tertiary igneous rocks are associated with steep hillslopes and channels and low denudation rates, whereas
pre-Alpine gneisses usually exhibit steep hillslopes and higher denudation rates. Molasse, flysch, and schists display lower
mean basin slopes and channel gradients, and, despite their high erodibility, low erosion rates. Exceptionally low denudation
rates are also measured in Permian rhyolite, which has high mean basin slopes. We invoke geomorphic inheritance as a major
factor controlling erosion, such that large erosive glaciers in the late Quaternary cold periods were more effective in priming
landscapes in the Central Alps for erosion than in the interior Eastern Alps. However, the difference in tectonic evolution
of the Eastern and Central Alps potentially adds to differences in their geomorphic response; their deep structures differ
significantly and, unlike the Central Alps, the Eastern Alps are affected by ongoing tectonic influx due to the slow motion
and rotation of Adria. The result is a complex pattern of high mountain erosion in the Eastern Alps, which has evolved from
one confined to the narrow belt of the Tauern Window in late Tertiary time to one affecting the entire underthrust basement,
orogenic lid, and parts of the Southern Alps today. 相似文献
328.
329.
The Casamance estuary, on the coast of Senegal, is an inverse hypersaline estuary: salinity increases landward, and dry season salinity values are up to 172 psu due to the evaporation of seawater. Dissolved inorganic carbon (DIC) concentrations decreased landward as a negative linear function of salinity. Thermodynamic modelling and the absence of CaCO3 in the sediments indicate that this loss of DIC was not due to calcite precipitation in the main water body. The innermost, almost landlocked, waters contained high phytoplankton biomass (50–300 μg chl I?1) and high concentrations of allochthonous dissolved organic carbon. Photosynthetic uptake of DIC and subsequent particulate organic carbon sedimentation is proposed as hypothetical explanation of the relationship between DIC and salinity; localized overheating in shallow waters might also be involved. 相似文献
330.