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411.
Rainer Wolf Mitsuru Ebihara Gerhard R. Richter Edward Anders 《Geochimica et cosmochimica acta》1983,47(12):2257-2270
We have analyzed by RNAA 25 aubrite and 9 diogenite samples for 13 to 29 siderophile, volatile, and lithophile trace elements. Both meteorite classes show a typically igneous siderophile element pattern, with Ir, Os, Re, Ge more depleted than Au, Ni, Pd, Sb. But aubrites tend to have about 10 × higher abundances (10?3 ? 10 ? 4 × Cl for the first 4 and 10?2?10?3 × Cl for the last 4 siderophiles), apparently reflecting smaller metal/silicate distribution coefficients at lowerf(O2), or less complete segregation of metal. Se is surprisingly abundant in aubrites (up to 0.4 × Cl), but Te is less so (), apparently due to its stronger siderophile character. Other volatiles (Ag, Zn, In, Cd, Bi, T1) show depletions intermediate between lunar dunite and the Earth's mantle.Of 7 aubrites analyzed for REE (Ce, Nd, Eu, Tb, Yb, Lu), 6 are depleted in REE (0.08?0.5 × Cl) and 5 show negative Eu anomalies (the exceptions are Bishopville and Mt. Egerton silicate). This supports an igneous origin, as already noted by Boynton and Schmitt (1972). No samples of the complementary, basaltic and feldspathic rocks have been found thus far, but one of our samples of Khor Temiki dark is a candidate for the basalt. It is 5?7 × enriched in REE and only slightly less so in Rb, Cs, and U. Though shocked and enriched in siderophiles to ~0.05 × Cl, it apparently represents a new meteorite class.Three diogenites analyzed for REE show very diverse patterns, from strongly depleted in light REE for Tatahouine (Ce = 0.01 × Cl) to flat for Garland (~2.5 × Cl). The data confirm the trends found by Fukuokaet al. (1977) as well as their interpretations.Factor analysis shows several parallel groupings for aubrites and diogenites: siderophiles (Re, Ir, Os, Pd, Ge), chalcophiles (Se, Te), volatiles (Ag, In, Tl) and incompatibles (U, REE, and Cs or Rb). But there are some differences for elements such as Ni, Sb, Cd, Bi, Au, and Zn, most of which behave more sensibly in aubrites than in diogenites.Several element pairs that differ greatly in volatility (Cs-U, Ge-Ir) correlate closely in aubrites, in approximately Cl-chondrite proportions. These correlations, and other lines of evidence, suggest strongly that aubrites originated by igneous processes in their parent body, not by direct nebular condensation. The source material may have resembled EL chondrites in oxidation state and depletion of refractories, metal, and volatiles. 相似文献
412.
Weather extremes often occur along fronts passing different sites with some time lag. Here, we show how such temporal patterns can be taken into account when exploring inter-site dependence of extremes. We incorporate time lags into existing models and into measures of extremal associations and their relation to the distance between the investigated sites. Furthermore, we define summarising parameters that can be used to explore tail dependence for a whole network of stations in the presence of fixed or stochastic time lags. Analysis of hourly precipitation data from Sweden showed that our methods can prevent underestimation of the strength and spatial extent of tail dependencies. 相似文献
413.
For evaluation of slope stability in materials displaying strain-softening behavior, knowledge concerning the failed state material response is of importance. Here, soft sensitive clay is studied. Such clays behave contractant at failure, which for undrained conditions yields a strain-softening behavior governed by the generation of excess pore water pressure. Strain softening is further linked with material instability and the phenomenon of strain localization. In the case of shear band formation, internal pore pressure gradients are then expected to be present for globally undrained conditions in the sensitive clay due to its low permeability. In the present study, this hypothesis and its implications on the global response and shear band properties are investigated. Utilizing an experimental setup with a modified triaxial cell allowing for shear band formation, the effect of varying the displacement rate is studied. Onset of strain localization is interpreted to occur just before or at the peak shear strength. A strong rate dependency of the softening response is observed. Increasing displacement rates give raised brittleness in terms of the slope of the global softening curve due to accumulating pore pressure. Also, reduced shear band thickness and a shear band inclination approaching 45° are obtained for increasing rates. In the context of slope failure in such materials, the rate dependency in the post-peak state opens up for a large variation in behavior, all depending on time as an important factor. 相似文献
414.
Karin Mossberg Sonnek Tomas Mårtensson Ester Veibäck Peter Tunved Håkan Grahn Pontus von Schoenberg Niklas Brännström Anders Bucht 《Natural Hazards》2017,88(3):1565-1590
In this study, we analyse and discuss the possible impacts on the Swedish society of a volcanic eruption on Iceland, emitting ash particles and large quantities of sulphur dioxide. A scenario was developed, based on the historical Laki eruption of 1783–1784, to describe the content of a potential sulphur fog over time in Sweden. Due to its high complexity and the many uncertainties in the underpinning scientific data, the scenario was developed using a cross-disciplinary approach incorporating experts from different scientific fields. An analysis of the impacts of the hazard on human health, environment and technical equipment was then performed and, finally, representatives from national authorities assessed the overall societal challenges in responding to the consequences of a massive volcanic eruption. The analysis shows that it is the peak concentrations of sulphur dioxide and sulphuric acid rather than the longer periods of moderate concentrations that contribute most to the negative consequences for human health and environment. Altogether, three societal challenges were identified: the ability to compile and disseminate relevant information fast enough, to perform continuous measurements of concentrations of different substances in affected areas and to meet the large demand for medical care. 相似文献
415.
Mwajuma Ibrahim Lingwanda Anders Prästings Stefan Larsson Dalmas L. Nyaoro 《Geomechanics and Geoengineering》2017,12(2):137-151
One of the essential inputs in settlement prediction models is the soil modulus, which may be obtained from laboratory tests or estimated from in situ measurements. The total uncertainty in predicting the confined modulus of a sandy soil is quantified with data from side-by-side in situ testing using the standard penetration test, the static cone penetration test, the light dynamic probing and the laboratory oedometer test. To estimate transformation errors, correlations are proposed between in situ and laboratory data. The results indicate that similar magnitudes of total uncertainties are associated with the in situ methods, which are approximately twice as high as those from the direct oedometer method. The quantified uncertainties are an important input for reliability-based designs of foundations under similar soil conditions. 相似文献
416.
417.
Kirsten Zickfeld Anders Levermann M. Granger Morgan Till Kuhlbrodt Stefan Rahmstorf David W. Keith 《Climatic change》2007,82(3-4):235-265
We present results from detailed interviews with 12 leading climate scientists about the possible effects of global climate
change on the Atlantic Meridional Overturning Circulation (AMOC). The elicitation sought to examine the range of opinions
within the climatic research community about the physical processes that determine the current strength of the AMOC, its future
evolution in a changing climate and the consequences of potential AMOC changes. Experts assign different relative importance
to physical processes which determine the present-day strength of the AMOC as well as to forcing factors which determine its
future evolution under climate change. Many processes and factors deemed important are assessed as poorly known and insufficiently
represented in state-of-the-art climate models. All experts anticipate a weakening of the AMOC under scenarios of increase
of greenhouse gas concentrations. Two experts expect a permanent collapse of the AMOC as the most likely response under a
4×CO2 scenario. Assuming a global mean temperature increase in the year 2100 of 4 K, eight experts assess the probability of triggering
an AMOC collapse as significantly different from zero, three of them as larger than 40%. Elicited consequences of AMOC reduction
include strong changes in temperature, precipitation distribution and sea level in the North Atlantic area. It is expected
that an appropriately designed research program, with emphasis on long-term observations and coupled climate modeling, would
contribute to substantially reduce uncertainty about the future evolution of the AMOC. 相似文献
418.
Anders Lindh 《Contributions to Mineralogy and Petrology》1976,54(4):315-327
Dihedral angles between two grains of quartz and one of pyrrhotite, sphalerite resp. hematite are measured at triple junctions. An approach to equilibrium is noted. The sulphides have dihedral angles greater than 120 ° and the oxide less than 120 °. No significant influence of sphalerite composition on dihedral angle can be proved. It is concluded that the average grain boundary energy between two grains of quartz is smaller than that between quartz and a sulphide but greater than that between quartz and hematite. Sulphide — biotite interfaces are found to be parallel to the biotite cleavage. Parallelism is concluded to meet a requirement of minimum grain boundary energy. Assuming random distribution of grains, the interfacial area between sulphides and transparent minerals is found to be too small in comparison with that between sulphides. The sulphide clustering, observed and inferred, is suggested to depend on a combination of grain boundary energy and epitaxial growth, but may to some extent be inherited from the ore-generation stage. 相似文献