Complementary techniques to assess physical properties of a fine soil irrigated with saline water   总被引：3，自引：2，他引：1  

Angelo Basile  Gabriele Buttafuoco  Giacomo Mele  Anna Tedeschi 《Environmental Earth Sciences》2012,66(7):1797-1807

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Fault architecture in the Main Ethiopian Rift and comparison with experimental models: Implications for rift evolution and Nubia–Somalia kinematics     

Andrea Agostini  Marco Bonini  Giacomo Corti  Federico Sani  Francesco Mazzarini 《Earth and Planetary Science Letters》2011,301(3-4):479-492

The Main Ethiopian Rift (MER) offers a complete record of the time–space evolution of a continental rift. We have characterized the brittle deformation in different rift sectors through the statistical analysis of a new database of faults obtained from the integration between satellite images and digital elevation models, and implemented with field controls. This analysis has been compared with the results of lithospheric-scale analogue models reproducing the kinematical conditions of orthogonal and oblique rifting. Integration of these approaches suggests substantial differences in fault architecture in the different rift sectors that in turn reflect an along-axis variation of the rift development and southward decrease in rift evolution. The northernmost MER sector is in a mature stage of incipient continental rupture, with deformation localised within the rift floor along discrete tectono-magmatic segments and almost inactive boundary faults. The central MER sector records a transitional stage in which migration of deformation from boundary faults to faults internal to the rift valley is in an incipient phase. The southernmost MER sector is instead in an early continental stage, with the largest part of deformation being accommodated by boundary faults and almost absent internal faults. The MER thus records along its axis the typical evolution of continental rifting, from fault-dominated rift morphology in the early stages of extension toward magma-dominated extension during break-up. The extrapolation of modelling results suggests that a variable rift obliquity contributes to the observed along-axis variations in rift architecture and evolutionary stage, being oblique rifting conditions controlling the MER evolution since its birth in the Late Miocene in relation to a constant post ca. 11 Ma ~ N100°E Nubia–Somalia motion.  相似文献   

Recovery of the macrozoobenthic community after severe dystrophic crises in a Mediterranean coastal Lagoon (Orbetello, Italy)   总被引：9，自引：0，他引：9  

Lardicci C  Como S  Corti S  Rossi F 《Marine pollution bulletin》2001,42(3):202-214

The Orbetello lagoon, one of the largest Western Mediterranean lagoons, was affected by high algal blooms and severe anoxic crises in 1992 and 1993, with fish mortality throughout most of the lagoon and a drastic reduction of benthic species. Many measures were undertaken between 1994 and 1996 to remove the severe eutrophication of this lagoon. Such measures included harvesting of the floating seaweed biomass, removal of all wastewater and sea channel enlargement by dredging activity. The aim of the present research was to study the macrozoobenthic assemblage in 1999 and to compare it with previous research in order to assess the recovery of the lagoon. A total of 106 taxa and 45,175 individuals were collected in three areas (sea inlets, western and eastern lagoon) having different organic matter loading during winter and summer. The results of multivariate and correlation analyses indicated that trophic status and its seasonal dynamics were crucial in determining species distribution among the different areas. Moreover, comparison of the macrozoobenthic structure between winter 1995 and 1999 showed differences in species composition and structural parameters in the western and eastern lagoon, where a clear recovery of benthic assemblages was observed in 1999. However, the dominance of opportunistic species in most of the lagoon and the decrease in some structural parameters during summer suggested that this basin still presented signs of disturbance in 1999, six years after the last extended anoxic crises and even after completion of the restoration measures carried out in the environment. It was hypothesized that a secondary disturbance, sustained by a high seasonal release of nutrients from the sediments, could create considerable deviations from the expected improvement in benthic conditions.  相似文献   

Die Matrix der Fische XVI Zweidimensionale papierchromatographische Analyse von Fischschuppenhydrolysaten und Hydrolysaten einiger weiterer Fischorgane     

Ulrich A. Corti  L. Keller 《Aquatic Sciences - Research Across Boundaries》1952,14(2):336-337

Summary The aminoacids in hydrolysates (HCl) of the scales of six different fish-species have been determined by partition paper chromatography (Consden andDent). The scales contain considerable amounts of protein besides hydroxyl apatit and guanin, but none or only minute quantities of carbohydrates. Some of the aminoacids in the liver, air-bladder, kidney and the body muscles of two fish species were investigated.   相似文献   

Die Matrix der Fische XIV. Elektronenmikroskopische Untersuchung von Fischschuppen     

R. Signer  F. v. Beust  Ulrich A. Corti 《Aquatic Sciences - Research Across Boundaries》1951,13(1):31-35

Summary The investigation with an electron-microscope of the scales of the fresh water fish,Leuciscus rutilus L., showed that their ventral “smooth” surface scems to be formed like a corrugated plate with a distance between the ridges of 1–2 μ. The dorsal “rough” side of the scales shows a very fine roughness. It is interrupted by pointed combs of the same structure in a regular distance of 16–27 μ. The thickness of these combs is of about 1 μ at their base, their height of about 5–10 μ. It seems probable that the surface of scales is partially covered with laminas of hyalodentine or guanine.

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13. Mitteilung siehe diese Zeitschrift,13, 29–30 (1951).  相似文献   

La «Matrix» des Poissons VI. Etudes oscillographiques sur la détermination du caractère nocif de différentes eaux usées de provenance industrielle     

Ulrich A. Corti 《Aquatic Sciences - Research Across Boundaries》1951,13(2):358-364

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Re‐orientation of the extension direction and pure extensional faulting at oblique rift margins: comparison between the Main Ethiopian Rift and laboratory experiments     

Giacomo Corti  Melody Philippon  Federico Sani  Derek Keir  Tesfaye Kidane 《地学学报》2013,25(5):396-404

In this study, we draw on a unique combination of well‐resolved fault‐slip data and earthquake focal mechanisms to constrain spatial variations in style of faulting in the obliquely extending Main Ethiopian Rift, East Africa. These data show that both boundary and internal faults – oblique and orthogonal to the plate divergence (PD) respectively – exhibit almost pure dip‐slip motion, and indicate significant local deflection in orientation of the extension direction at rift margins. Scaled analogue models closely replicate the multidisciplinary observations from the rift and suggest that the process is controlled by the presence of a deep‐seated, pre‐existing weakness – oblique to the direction of PD – that is able to cause a local rotation in the orientation of the extension direction at rift margins. Minor counterclockwise block rotations are required to accommodate the difference in slip direction along the different fault systems, as supported by existing and new palaeomagnetic data from the rift.  相似文献   

An international program on Silk Road Disaster Risk Reduction——a Belt and Road initiative (2016-2020)     

Lei Yu  Cui Peng  Amar Deep Regmi  Virginia Murray  Alessandro Pasuto  Giacomo Titti  Muhammad Shafique  Tilak Priyadarshana D. G 《山地科学学报》2018,15(7):1383-1396

Belt and Road Initiative (BRI) is a Chinese national strategy which calls for cooperative economic, political and cultural exchange at the global level along the ancient Silk Road. The overwhelming natural hazards located along the belt and road bring great challenges to the success of BRI. In this framework, a 5-year international program was launched to address issues related to hazards assessment and disaster risk reduction (DRR). The first workshop of this program was held in Beijing with international experts from over 15 countries. Risk conditions on Belt and Road Countries (BRCs) have been shared and science and technology advancements on DRR have been disseminated during the workshop. Under this program, six task forces have been setup to carry out collaborative research works and three prioritized study areas have been established. This workshop announced the launching of this program which involved partners from different countries including Pakistan, Nepal, Russia, Italy, United Kingdom, Sri Lanka and Tajikistan. The program adopted the objectives of Sendai Framework for Disaster Risk Reduction 2015–2030 and United Nation Sustainable Development Goals 2030 and was implemented to assess disaster risk in BRCs and to propose suitable measures for disaster control which can be appropriate both for an individual country and for specific sites. This paper deals with the outcomes of the workshop and points out opportunities for the near future international cooperation on this matter.  相似文献   

Experimental models of extension of continental lithosphere weakened by percolation of asthenospheric melts     

Giacomo Corti  Marco Bonini  Fabrizio Innocenti  Piero Manetti  Giovanni B. Piccardo  Giorgio Ranalli 《Journal of Geodynamics》2007,43(4-5):465-483

Analogue models are used to investigate extension of a continental lithosphere weakened by asthenospheric melts percolating through the upper mantle, a process that has been hypothesised to control the opening of the Ligurian Tethys. Models were performed in a centrifuge apparatus and reproduced, by using materials such as sand and viscous mixtures, extension of 60-km thick, three-layer continental lithosphere floating above the asthenosphere. The percolated lithospheric mantle was assumed to be characterised by a rheological behaviour similar to that of the asthenosphere. Two sets of experiments investigated the influence on deformation of (1) the thickness of the percolated mantle and the associated strength contrast between the normal and weakened lithosphere, and (2) the lateral width of the weakened zone. Model results suggest that mantle percolation by asthenospheric melts is able to promote strong localised thinning of the continental lithosphere, provided that a significant thickness of the lithospheric mantle is weakened by migrating melts within a narrow region. Strain localisation is maximised for percolation of the whole lithospheric mantle and strong strength contrast between the normal and weakened lithosphere. Under these conditions, the thickness of the lithosphere may be reduced to less than 12 km in 3 Ma of extension. Conversely, localised thinning is strongly reduced if the thickness of the percolated zone is ≤1/3 of the thickness of the whole lithospheric mantle and/or the lithosphere is weakened over wide regions. Overall, model results support the working hypothesis that mantle percolation by asthenospheric melts is a controlling factor in the transition from distributed continental deformation to localised oceanic spreading.  相似文献   

Laser Induced Breakdown Spectroscopy applications to meteorites: Chemical analysis and composition profiles     

M. Dell’Aglio  A. De Giacomo  R. Gaudiuso  G.S. Senesi 《Geochimica et cosmochimica acta》2010,74(24):7329-7339

A fast procedure for chemical analysis of different meteorites is presented, based on LIBS (Laser Induced Breakdown Spectroscopy). The technique is applied to several test cases (Dhofar 019, Dhofar 461, Sahara 98222, Toluca, Sikhote Alin and Campo del Cielo) and can be useful for rapid meteorite identification providing geologists with specific chemical information for meteorite classification. Concentration profiles of Fe, Ni and Co are simultaneously detected across the Widmanstätten structure of the iron meteorite Toluca with a view to determining cooling rates. The LIBS analysis of meteorites is also used as a laboratory test for analogous studies on the respective parent bodies (Mars, asteroids) in space exploration missions where one clear advantage of the proposed technique is that no direct contact with the sample is required.  相似文献