Slow slip generated by dehydration reaction coupled with slip-induced dilatancy and thermal pressurization     

Teruo Yamashita  Alexandre Schubnel 《Journal of Seismology》2016,20(4):1217-1234

Sustained slow slip, which is a distinctive feature of slow slip events (SSEs), is investigated theoretically, assuming a fault embedded within a fluid-saturated 1D thermo-poro-elastic medium. The object of study is specifically SSEs occurring at the down-dip edge of seismogenic zone in hot subduction zones, where mineral dehydrations (antigorite, lawsonite, chlorite, and glaucophane) are expected to occur near locations where deep slow slip events are observed. In the modeling, we introduce dehydration reactions, coupled with slip-induced dilatancy and thermal pressurization, and slip evolution is assumed to interact with fluid pressure change through Coulomb’s frictional stress. Our calculations show that sustained slow slip events occur when the dehydration reaction is coupled with slip-induced dilatancy. Specifically, slow slip is favored by a low initial stress drop, an initial temperature of the medium close to that of the dehydration reaction equilibrium temperature, a low permeability, and overall negative volume change associated with the reaction (i.e., void space created by the reaction larger than the space occupied by the fluid released). Importantly, if we do not assume slip-induced dilatancy, slip is accelerated with time soon after the slip onset even if the dehydration reaction is assumed. This suggests that slow slip is sustained for a long time at hot subduction zones because dehydration reaction is coupled with slip-induced dilatancy. Such slip-induced dilatancy may occur at the down-dip edge of seismogenic zone at hot subduction zones because of repetitive occurrence of dehydration reaction there.  相似文献   

Estuarine flooding in urban areas: enhancing vulnerability assessment     

Santos  Pedro Pinto  Tavares  Alexandre Oliveira  Freire  Paula  Rilo  Ana 《Natural Hazards》2017,93(1):77-95

The assessment of vulnerability provides valuable knowledge in the risk assessment steps of a risk governance process. Given the multiscale, multilevel, and multisectorial aspects of flood risk, the diversified entities that directly and indirectly intervene in risk management require specific outputs from the assessment studies. Urban areas in estuarine margins are particularly exposed and vulnerable to flooding. Such interface conditions are found in the Old City Centre of the Seixal, located in the Tagus estuary, Portugal. Here, two distinct methodologies were applied for the assessment of territorial vulnerability. A regional, lower-scale, methodology explores the application of the statistical procedure based on the SoVI^® at the statistical block level. A second, local and higher-scale, methodology is based in data collected through field matrices at the building and statistical sub-block level. Comparison of results revealed that the lower-scale assessment provides information on the vulnerability drivers at the regional and municipal level. Nevertheless, only at a higher-scale, it is possible to characterize and differentiate the smaller geographical units of analysis that compose the Old City Centre of Seixal. The lower-scale vulnerability assessment allows a strategic response, based on adaptation measures such as spatial planning, institutional capacity building and public awareness. The local level assessment provides more accurate knowledge to support local emergency planning and the allocation of operational and material resources at the urban level. Nevertheless, rather than antagonistic, both models can be considered as complementary, having in mind the requirements of an holistic flood risk governance model.

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Bismuth selenides from St. Andreasberg,Germany: an oxidised five-element style of mineralisation and its relation to post-Variscan vein-type deposits of central Europe     

Cabral  Alexandre Raphael  Ließmann  Wilfried  Jian  Wei  Lehmann  Bernd 《International Journal of Earth Sciences》2017,106(7):2359-2369

International Journal of Earth Sciences - Carbonate veinlets at Roter Bär, a former underground mine in the polymetallic St. Andreasberg vein district of the Harz Mountains, Germany, host...  相似文献   

Characterization of Fault Roughness at Various Scales: Implications of Three-Dimensional High Resolution Topography Measurements     

Thibault Candela  François Renard  Michel Bouchon  Alexandre Brouste  David Marsan  Jean Schmittbuhl  Christophe Voisin 《Pure and Applied Geophysics》2009,166(10-11):1817-1851

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Axial and Radial Permeability Evolutions of Compressed Sandstones: End Effects and Shear-band Induced Permeability Anisotropy   总被引：2，自引：0，他引：2  

Jeremie Dautriat  Nicolas Gland  Jean Guelard  Alexandre Dimanov  Jean L. Raphanel 《Pure and Applied Geophysics》2009,166(5-7):1037-1061

The influence of hydrostatic and uniaxial stress states on the porosity and permeability of sandstones has been investigated. The experimental procedure uses a special triaxial cell which allows permeability measurements in the axial and radial directions. The core sleeve is equipped with two pressure samplers placed distant from the ends. They provide mid-length axial permeability measure as opposed to the overall permeability measure, which is based on the flow imposed through the pistons of the triaxial cell. The core sleeve is also equipped to perform flows in two directions transverse to the axis of the sample. Two independent measures of axial and complementary radial permeability are thus obtained. Both Fontainebleau sandstone specimens with a porosity of about 5.8% to 8% and low permeability ranging from 2.5 mD to 30 mD and Bentheimer sandstone with a porosity of 24% and a high permeability of 3D have been tested. The initial axial permeability values obtained by each method are in good agreement for the Fontainebleau sandstone. The Bentheimer sandstone samples present an axial mid-length permeability 1.6 times higher than the overall permeability. A similar discrepancy is also observed in the radial direction, also it relates essentially to the shape of flow lines induced by the radial flow. All the tested samples have shown a higher stress dependency of overall and radial permeability than mid-length permeability. The effect of compaction damage at the pistons/sample and radial ports/sample interfaces is discussed. The relevance of directional permeability measurements during continuous uniaxial compression loadings has been shown on the Bentheimer sandstone until the failure of the sample. We can efficiently measure the influence of brittle failure associated to dilatant regime on the permeability: It tends to increase in the failure propagation direction and to decrease strongly in the transverse direction.  相似文献   

Re-examination of the temperature-dependent relationship between δ<Superscript>18</Superscript>O<Subscript>diatoms</Subscript> and δ<Superscript>18</Superscript>O<Subscript>lake water</Subscript> and implications for paleoclimate inferences     

Julien Crespin  Florence Sylvestre  Anne Alexandre  Corinne Sonzogni  Christine Paillès  Marie-Elodie Perga 《Journal of Paleolimnology》2010,44(2):547-557

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Assessing drought in the drylands of northeast Brazil under regional warming exceeding 4 °C     

Marengo  Jose A.  Cunha  Ana Paula M. A.  Nobre  Carlos A.  Ribeiro Neto  Germano G.  Magalhaes  Antonio R.  Torres  Roger R.  Sampaio  Gilvan  Alexandre  Felipe  Alves  Lincoln M.  Cuartas  Luz A.  Deusdará  Karinne R. L.  Álvala  Regina C. S. 《Natural Hazards》2020,103(2):2589-2611

Natural Hazards - Historically, during periods of extreme drought, food security in the drylands of the semiarid region of Northeast Brazil (NEB) is under severe risk due to agricultural collapse....  相似文献   

Testing models of step formation against observations of channel steps in a steep mountain stream     

Antonius Golly  Jens M. Turowski  Alexandre Badoux  Niels Hovius 《地球表面变化过程与地形》2019,44(7):1390-1406

Steep streams often feature a step-pool morphology where the steps determine channel stability and dissipate the stream's energy, and thus are important for local flow hydraulics and bedload transport. Steps also play a key-role for the coupling of channels and adjacent hillslopes by controlling hillslope stability. Although step-pool systems have been investigated in various modelling and experimental efforts, the processes of step formation and destruction remain under debate. Theories of step formation consider a wide range of dominant drivers and fall into three groups favouring hydraulic controls ( HC ), granular interactions during flow ( GI ) or random drivers ( RD ) as relevant factors for step location. A direct evaluation of these models with field observations is challenging, as step formation cannot be directly observed. Based on the physical mechanisms of the various formation models we derive diagnostic morphometric parameters and test them with a field data set from a steep stream in Switzerland. Our results suggest that one class of alluvial steps form due to jamming in narrow and narrowing sections of the channel, while steps in wide and widening sections form around rarely mobile keystones. These two models of step formation apply in our study reach at the same time in different locations of the channel. A third class of steps is forced by logs. Such steps are typically located close to the original growth position of the tree and therefore reflect strong channel-hillslope coupling. Wood-forced steps make up a minor fraction of the step population, but contribute significantly to the cumulative step height and are therefore relevant to reach-scale flow resistance of the channel. © 2019 John Wiley & Sons, Ltd.  相似文献   

Inorganic nitrogen uptake and related enzymatic activity in the seagrass Zostera noltii     

Ana Alexandre  João Silva  Rui Santos 《Marine Ecology》2010,31(4):539-545

The preferential inorganic nitrogen source for the seagrass Zostera noltii was investigated in plants from Ria Formosa, South Portugal. Rates of ammonium and nitrate uptake were determined at different concentrations of these nutrients (5, 25 and 50 μm ), supplied simultaneously (NH₄NO₃) or separately (KNO₃ and NH₄Cl). The activity of the enzymes nitrate reductase (NR) and glutamine synthetase (GS) was also assessed. The results showed that ammonium is the preferential inorganic nitrogen source for Z. noltii, but, in the absence of ammonium, the species also has a high nitrate uptake capacity. The simultaneous availability of both inorganic nitrogen forms enhanced the uptake rate of ammonium and decreased the uptake rate of nitrate compared to when only one of the nitrogen forms was supplied. The activity of both enzymes was much higher in the leaves than in the roots, highlighting the importance of the leaves as primary reducing sites in the nitrogen assimilation process.  相似文献   

Additive effects of climate change and human hunting explain population decline and extinction in cave bears     

Alessandro Mondanaro  Mirko Di Febbraro  Marina Melchionna  Francesco Carotenuto  Silvia Castiglione  Carmela Serio  Simone Danisi  Lorenzo Rook  Jose Alexandre F. Diniz‐Filho  Pasquale Raia 《Boreas: An International Journal of Quaternary Research》2019,48(3):605-615

Cave bears (Ursus spelaeus) are an iconic component of the European late Quaternary Ice Age megafauna. Recent demographic analyses based on cave bear mtDNA sequences and refined radiocarbon dating indicate that cave bear population size and genetic diversity started to decline some 50 kilo years ago (kya). Hence, neither the coldest phase of the last glaciation (started some 24 kya), nor the colonization of Europe by Palaeolithic hunters (started some 45 kya) coincides with the beginning of population decline. Here, we reconstructed cave bear climatic niche evolution through time. Then, we performed spatially explicit population viability analyses to assess cave bear demographics through time in response to climatic changes, human effects on bear survival and their combination. We found that climate change was responsible for a 10‐fold decrease in cave bear population size after 40 kya. However, climate change on its own could not explain U. spelaeus extinction at 24 kya. Additional negative effects consistent with human population expansion are required to explain both U. spelaeus' retreat from eastern Europe since 40 kya and its final extinction.  相似文献