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51.
Jonny Rutqvist Ann Bäckström Masakazu Chijimatsu Xia-Ting Feng Peng-Zhi Pan John Hudson Lanru Jing Akira Kobayashi Tomofumi Koyama Hee-Suk Lee Xiao-Hua Huang Mikael Rinne Baotang Shen 《Environmental Geology》2009,57(6):1313-1324
This simulation study shows how widely different model approaches can be adapted to model the evolution of the excavation
disturbed zone (EDZ) around a heated nuclear waste emplacement drift in fractured rock. The study includes modeling of coupled
thermal-hydrological-mechanical (THM) processes, with simplified consideration of chemical coupling in terms of time-dependent
strength degradation or subcritical crack growth. The different model approaches applied in this study include boundary element,
finite element, finite difference, particle mechanics, and elasto-plastic cellular automata methods. The simulation results
indicate that thermally induced differential stresses near the top of the emplacement drift may cause progressive failure
and permeability changes during the first 100 years (i.e., after emplacement and drift closure). Moreover, the results indicate
that time-dependent mechanical changes may play only a small role during the first 100 years of increasing temperature and
thermal stress, whereas such time-dependency is insignificant after peak temperature, because of decreasing thermal stress. 相似文献
52.
Mikael D. Axelsson Ilia Rodushkin Douglas C. Baxter Johan Ingri Björn Öhlander 《Geochemical transactions》2002,3(1):40
A procedure was developed for the determination of element distributions in cross-sections of ferromanganese concretions using
laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The effects of carrier flow rates, rf forward power,
ablation energy, ablation spot size, repetition rate and number of shots per point on analyte intensity were studied. It is
shown that different carrier gas flow rates are required in order to obtain maximum sensitivities for different groups of
elements, thus complicating the optimisation of ICP parameters. On the contrary, LA parameters have very similar effects on
almost all elements studied, thus providing a common optimum parameter set for the entire mass range. However, for selected
LA parameters, the use of compromise conditions was necessary in order to compensate for relatively slow data acquisition
by ICP-MS and maintain high spatial resolution without sacrificing the multielemental capabilities of the technique. Possible
variations in ablation efficiency were corrected for mathematically using the sum of Fe and Mn intensities. Quantification
by external calibration against matrix-matched standards was successfully used for more than 50 elements. These standards,
in the form of pressed pellets (no binder), were prepared in-house using ferromanganese concentrates from a deep-sea nodule
reference material as well as from shallow-marine concretions varying in size and having different proportions of three major
phases: aluminosilicates, Fe- and Mn-oxyhydroxides. Element concentrations in each standard were determined by means of conventional
solution nebulisation ICP-MS following acid digestion. Examples of selected inter-element correlations in distribution patterns
along the cross-section of a concretion are given. 相似文献
53.
I. Sandahl S. Barabash H. Borg E. Yu. Budnik E. M. Dubinin U. Eklund H. Johansson H. Koskinen K. Lundin R. Lundin A. Mostrom R. Pellinen N. F. Pissarenko T. Pulkkinen P. Toivanen A. V. Zakharov 《Annales Geophysicae》1997,15(5):542-552
PROMICS-3 is a plasma experiment flown in the Russian project Interball. It performs three-dimensional (3D) measurements of ions in the energy range 4 eV–70 keV with mass separation and of electrons in the energy range 12 eV–35 keV. The Interball project consists of two main satellites, the Tail Probe and the Auroral Probe, each with one subsatellite. The Interball Tail Probe was launched on 3 August 1995, into a 65° inclination orbit with apogee at about 30 RE. Both main satellites carry identical PROMICS-3 instruments and thus direct comparisons of the particle distributions will be possible once the Auroral Probe is launched. Furthermore, PROMICS-3-Tail is the first instrument measuring the 3D ion distribution function in the magnetospheric boundary layers at high latitudes. In this paper we describe the PROMICS-3 instrument and show initial results from the Tail probe, measurements of the mag-netosheath, plasma sheet, and ring current plasmas. 相似文献
54.
We present a new method for the linking of scarce asteroid astrometry over apparitions, and apply it both to simulated and real data to prove its feasibility. Up to date, there has not been a robust method available to search for linkages between the approximately 50,000 provisionally designated sets of asteroid astrometry spanning less than two days. Unless such a scarce set of astrometry is linked to another set of astrometry, the underlying object can be considered lost as the ephemeris uncertainties are substantial. The new method, which can tackle the challenges, is based on Ranging, which is a fully nonlinear, statistical orbital inversion method. Ranging properly treats astrometric uncertainties and propagates the uncertainty to the resulting orbital-element probability density, which is sampled by a set of orbits. The new orbital-element-space multiple-address-comparison (oMAC) method uses dimensionality-reduction techniques and tree structures to efficiently search for overlapping probability densities in the orbital-element phase space. Overlapping probability densities indicate a candidate linkage between astrometric observation sets. To accept a candidate linkage, we have to find a many-body orbital solution which reproduces the observed positions within the observational uncertainties. To find the linking orbit, we use a multi-step approach starting from a Monte-Carlo generation of possible orbits in a reduced volume of the orbital-element phase space and ending with a least-squares orbital solution, which, in addition to the Sun's gravitation, also takes into account the gravitational influence of the relevant planets. The new multiple-address-comparison method has a loglinear computational complexity, that is, it scales as O(nlogn), where n is the number of included observation sets. It has recently also been implemented for the ephemeris-space multiple-address-comparison (eMAC) method, which is optimized for the short-term linking of scarce astrometry. 相似文献
55.
Peter Jenniskens Jason Utas Qing‐Zhu Yin Robert D. Matson Marc Fries J. Andreas Howell Dwayne Free Jim Albers Hadrien Devillepoix Phil Bland Aaron Miller Robert Verish Laurence A. J. Garvie Michael E. Zolensky Karen Ziegler Matthew E. Sanborn Kenneth L. Verosub Douglas J. Rowland Daniel R. Ostrowski Kathryn Bryson Matthias Laubenstein Qin Zhou Qiu‐Li Li Xian‐Hua Li Yu Liu Guo‐Qiang Tang Kees Welten Marc W. Caffee Matthias M. M. Meier Amy A. Plant Colin Maden Henner Busemann Mikael Granvik 《Meteoritics & planetary science》2019,54(4):699-720
It has been proposed that all L chondrites resulted from an ongoing collisional cascade of fragments that originated from the formation of the ~500 Ma old asteroid family Gefion, located near the 5:2 mean‐motion resonance with Jupiter in the middle Main Belt. If so, L chondrite pre‐atmospheric orbits should be distributed as expected for that source region. Here, we present contradictory results from the orbit and collisional history of the October 24, 2015, L6 ordinary chondrite fall at Creston, CA (here reclassified to L5/6). Creston's short 1.30 ± 0.02 AU semimajor axis orbit would imply a long dynamical evolution if it originated from the middle Main Belt. Indeed, Creston has a high cosmic ray exposure age of 40–50 Ma. However, Creston's small meteoroid size and low 4.23 ± 0.07° inclination indicate a short dynamical lifetime against collisions. This suggests, instead, that Creston originated most likely in the inner asteroid belt and was delivered via the ν6 resonance. The U‐Pb systematics of Creston apatite reveals a Pb‐Pb age of 4,497.1 ± 3.7 Ma, and an upper intercept U‐Pb age of 4,496.7 ± 5.8 Ma (2σ), circa 70 Ma after formation of CAI, as found for other L chondrites. The K‐Ar (age ~4.3 Ga) and U,Th‐He (age ~1 Ga) chronometers were not reset at ~500 Ma, while the lower intercept U‐Pb age is poorly defined as 770 ± 320 Ma. So far, the three known L chondrites that impacted on orbits with semimajor axes a <2.0 AU all have high (>3 Ga) K‐Ar ages. This argues for a source of some of our L chondrites in the inner Main Belt. Not all L chondrites originate in a continuous population of Gefion family debris stretching across the 3:1 mean‐motion resonance. 相似文献
56.
I. Sandahl S. Barabash H. Borg E. Y. Budnik E. M. Dubinin U. Eklund H. Koskinen K. Lundin R. Lundin A. Mälkki R. Pellinen N. F. Pissarenko T. Pulkkinen A. V. Zakharov 《Annales Geophysicae》1999,17(5):659-673
The PROMICS-3 instrument on Interball-2 is nominally identical to the PROMICS-3 instrument on Interball-1. It performs three-dimensional measurements of ions in the energy range 4 eV–70 keV with mass separation and of electrons in the energy range 300 eV–35 keV. Interball-2 was launched on August 29, 1996, into an orbit with the same inclination as that of Interball-1, 63°, but with apogee at 20 000 km. In this study the PROMICS-3 instrument on Interball-2 is briefly described and examples of the first results are presented. Firstly, we report observations of upward moving molecular ions with energies of up to 700 eV at the poleward edge of the auroral oval. Previous observations of outflowing molecular ions have been at lower altitudes and lower energies. Secondly, we show observations of dawnside magnetosheath plasma injections. Using conjugate data from both PROMICS-3 instruments we have found dispersion structures above the morningside auroral oval, which occurred simultaneously with isolated “pockets” of magnetosheath plasma at a distance of XGSM = −14 to −12 RE, which had been injected into the inner part of the low-latitude boundary layer. These isolated plasma structures were sites of strong field-aligned currents and are proposed to be the magnetospheric counterparts of the dispersion structures. 相似文献
57.
Ann-Kristin Eriksson Wiklund Sandra VilhelmssonStig Johan Wiklund Britta Eklund 《Estuarine, Coastal and Shelf Science》2009
The invasive polychaete genus, Marenzelleria and the native amphipod, Monoporeia affinis are food and habitat competitors in the Baltic Sea. Previous studies have shown that moderate densities of Marenzelleria can affect the behaviour of M. affinis. To examine the short-term interactive effects of interspecific habitat choice and environmental contaminants a series of habitat colonisation experiments were performed. The contaminants examined included harbor sediments and sediment spiked with the antifouling substances, Cu, Zn and Irgarol. Polychaetes and amphipods were exposed to contaminants in single-species and two-species experiments. In spiked-sediment experiments, M. affinis showed clear dose-dependent response. These experiments verified that behavioural response of M. affinis to different habitats is a sensitive method for testing toxicity under controlled conditions. In experiments with three different harbor sediments and reference sediment both species showed the lowest preference for the reference sediment. This sediment also had the lowest content of quality food, indicating that factors such as food quality and quantity may override the disturbing effects of contaminants in natural sediments. The presence of Marenzelleria spp. did not affect amphipod habitat choice, indicating no short-term effects, which implies that both species can co-exist provided sufficient food is available. 相似文献
58.
Björn Öhlander Barbara Müller Mikael Axelsson Lena Alakangas 《Journal of Geochemical Exploration》2007
Metals released from oxidation and weathering of sulphide minerals in mine tailings are to a high degree retained at deeper levels within the tailings themselves. To be able to predict what could happen in the future with these secondarily retained metals, it is important to understand the retention mechanisms. In this study an attempt to use laser ablation high-resolution ICP-MS (LA-ICP-SMS) to quantify enrichment of trace elements on pyrite surfaces in mine tailings was performed. Pyrite grains were collected from a profile through the pyrite-rich tailings at the Kristineberg mine in northern Sweden. At each spot hit by the laser, the surface layer was analyzed in the first shot, and a second shot on the same spot gave the chemical composition of the pyrite immediately below. The crater diameter for a laser shot was known, and by estimating the crater depth and total pyrite surface, the total enrichment on pyrite grains was calculated. Results are presented for As, Cd, Co, Cu, Ni and Zn. The results clearly show that there was an enrichment of As, Cd, Cu and Zn on the pyrite surfaces below the oxidation front in the tailings, but not of Co and Ni. Arsenic was also enriched on the pyrite grains that survived in the oxidized zone. Copper has been enriched on pyrite surfaces in unoxidized tailings in the largest amount, followed by Zn and As. However, only 1.4 to 3.1% of the Cd and Zn released by sulphide oxidation in the oxidized zone have been enriched on the pyrite surfaces in the unoxidized tailings, but for As and Cu corresponding figures are about 64 and 43%, respectively. There were many uncertainties in these calculations, and the results shall not be taken too literally but allowed the conclusion that enrichment on pyrite surfaces is an important process for retention of As and Cu below the oxidation front in pyrite rich tailings. Laser ablation is not a surface analysis technique, but more of a thin layer method, and gives no information on the type of processes resulting in enrichment on the pyrite surfaces. Although only pyrite grains that appeared to be fresh and without surface coatings were used in this study, the possibility that a thin layer of Fe-hydroxides occurred must be considered. Both adsorption to the pyrite directly or to Fe-oxyhydroxides may explain the enrichment of As, Cd, Cu and Zn on the pyrite surfaces, and, in the case of Cu, also the replacement of Fe(II) by Cu(II) in pyrite. 相似文献
59.
60.
Maryline Moulin Daniel Aslanian Mikael Evain Anglique Leprêtre Philippe Schnurle Fanny Verrier Joseph Thompson Philippe De Clarens Sylvie Leroy Nuno Dias 《地学学报》2020,32(3):205-214
The Natal Valley, offshore Mozambique, is a key area for understanding the evolution of East Gondwana. Within the scope of the integrated multidisciplinary PAMELA project, we present new wide‐angle seismic data and interpretations, which considerably alter Geoscience paradigms. These data reveal the presence of a 30‐km‐thick crust that we argue to be of continental nature. This falsifies all the most recent palaeo‐reconstructions of the Gondwana. This 30‐km‐thick continental crust 1,000 m below sea level implies a complex history with probable intrusions of mantle‐derived melts in the lower crust, connected to several occurrences of magmatism, which seems to evidence the crucial role of the lower continental crust in passive margin genesis. 相似文献