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141.
Abstract. Three-weekly transects were done over a 14-month period at Sundays River Beach, a high energy beach in Algoa Bay, South Africa, to determine the life histories, breeding patterns, and fecundities of three intertidal cirolanid isopods. Eurydice longicornis. Pontogeloides latipes , and Excirolana naialensis. E. longicornis exhibits an annual, multivoltine life history with a more extended breeding period than the other two species. P. latipes and E. natalensis both have biennial. univoltine life histories with lower fecundities than E. longicornis. 相似文献
142.
The supralittoral zone of an open sandy beach was dosed with crude oil and changes in the meiofauna monitored. Treatments included weathered and fresh oil on the surface, fresh oil mixed with dispersant on the surface and weathered oil at the water table, all in layers 0·8 cm thick. In all cases the meiofauna was reduced 1 month after dosing but numbers had returned to normal by 5 months except in the site dosed with fresh oil mixed with dispersant. Oil on the surface had greater effects than oil at the water table; fresh oil had a greater effect than weathered oil and fresh oil with dispersant was more toxic than fresh oil alone. Nematodes were least sensitive to the oil and oligochaetes more sensitive, their numbers being correlated with oil concentrations and depth in the substrate. It is concluded that, under all but the heaviest conditions of pollution in their environment, recovery from oil contamination should occur within 5 months in the meiofauna. 相似文献
143.
Summary Metal substitution studies of the stability, structure and chemical bonding of sulfides and sulfosalts lead to significant results, which can be applied to natural parageneses and crystal chemical systematics. Comparison of experiments on stable and metastable phases with thin films provides data, which exceed known geometrical criteria of the sulfosalt systematics. Synthetic and natural phases have been studied with respect to their substitution, bonding chemistry and temperature dependent metal distribution as well as to the structure and orientation of thin films.
With 13 Figures
In memoriam Prof. Dr. V. Kupcik ( 1990) 相似文献
Zusammenfassung Die Untersuchung der Stabilität, Struktur und chemischen Bindung von Sulfosalzen führt zu aussagekräftigen auf natürliche Paragenesen sowie auf die Systematik dieser Verbindungen anwendbaren Resultaten, wenn systematische Substitutionsexperimente angesetzt werden. Diese liefern im Vergleich von stabilen und metastabilen Phasen sowie durch Vergleich mit dünnen Schichten Ergebnisse, die wesentlich über bekannte strukturgeometrische Ansätze zur Sulfosalzsystematik hinausgehen. Es werden synthetische und natürliche Verbindungen bezüglich ihrer Substitution, Bindungschemie und temperaturabhängigen Metallordnung sowie die Orientierung und Struktur von dünnen Schichten diskutiert.
With 13 Figures
In memoriam Prof. Dr. V. Kupcik ( 1990) 相似文献
144.
Anna M. Dymshits Peter I. Dorogokupets Igor S. Sharygin Konstantin D. Litasov Anton Shatskiy Sergey V. Rashchenko Eiji Ohtani Akio Suzuki Yuji Higo 《Physics and Chemistry of Minerals》2016,43(6):447-458
A new synchrotron X-ray diffraction study of chromium oxide Cr2O3 (eskolaite) with the corundum-type structure has been carried out in a Kawai-type multi-anvil apparatus to pressure of 15 GPa and temperatures of 1873 K. Fitting the Birch–Murnaghan equation of state (EoS) with the present data up to 15 GPa yielded: bulk modulus (K 0,T0), 206 ± 4 GPa; its pressure derivative K′0,T , 4.4 ± 0.8; (?K 0,T /?T) = ?0.037 ± 0.006 GPa K?1; a = 2.98 ± 0.14 × 10?5 K?1 and b = 0.47 ± 0.28 × 10?8 K?2, where α 0,T = a + bT is the volumetric thermal expansion coefficient. The thermal expansion of Cr2O3 was additionally measured at the high-temperature powder diffraction experiment at ambient pressure and α 0,T0 was determined to be 2.95 × 10?5 K?1. The results indicate that coefficient of the thermal expansion calculated from the EoS appeared to be high-precision because it is consistent with the data obtained at 1 atm. However, our results contradict α 0 value suggested by Rigby et al. (Brit Ceram Trans J 45:137–148, 1946) widely used in many physical and geological databases. Fitting the Mie–Grüneisen–Debye EoS with the present ambient and high-pressure data yielded the following parameters: K 0,T0 = 205 ± 3 GPa, K′0,T = 4.0, Grüneisen parameter (γ 0) = 1.42 ± 0.80, q = 1.82 ± 0.56. The thermoelastic parameters indicate that Cr2O3 undergoes near isotropic compression at room and high temperatures up to 15 GPa. Cr2O3 is shown to be stable in this pressure range and adopts the corundum-type structure. Using obtained thermoelastic parameters, we calculated the reaction boundary of knorringite formation from enstatite and eskolaite. The Clapeyron slope (with \({\text{d}}P/{\text{d}}T = - 0.014\) GPa/K) was found to be consistent with experimental data. 相似文献
145.
146.
The calcium isotopic composition of NIST SRM 915b and 1486 provided by the National Institute of Standards and Technology was analysed. The δ44/40Ca values of the two reference materials relative to NIST SRM 915a were: NIST SRM 915b =+0.72 ± 0.04‰ and NIST SRM 1486 =?1.01 ± 0.02‰. NIST SRM 1486 did not require any chemical separation prior to measurement. 相似文献
147.
148.
Design of Pressure Relief Valves for Protection of Steel-Lined Pressure Shafts and Tunnels Against Buckling During Emptying 总被引:1,自引:1,他引:0
Using high-strength steels for pressure shafts and tunnel liners and taking into account significant rock mass participation
allows the design of comparatively thin steel liners in hydropower projects. Nevertheless, during emptying of waterways, these
steel linings may be endangered by buckling. Compared with traditional measures such as increased steel liner thickness and
stiffeners, pressure relief valves are a very economical solution for protection of steel liners against critical external
pressure and therefore buckling during emptying. A calculation procedure has been developed for the design of the required
number and arrangement of pressure relief valves, and this has been used successfully in practice. Systematic model tests
enabled the assumptions of the design method to be verified. 相似文献
149.
Penelope J. WOZNIAKIEWICZ Hope A. ISHII Anton T. KEARSLEY Mark J. BURCHELL Philip A. BLAND John P. BRADLEY Zurong DAI Nick TESLICH Gareth S. COLLINS Mike J. COLE Sara S. RUSSELL 《Meteoritics & planetary science》2011,46(7):1007-1024
Abstract– Samples returned from comet 81P/Wild 2 by the Stardust mission provided an unequaled opportunity to compare previously available extraterrestrial samples against those from a known comet. Iron sulfides are a major constituent of cometary grains commonly identified within cometary interplanetary dust particles (IDPs) and Wild 2 samples. Chemical analyses indicate Wild 2 sulfides are fundamentally different from those in IDPs. However, as Wild 2 dust was collected via impact into capture media at approximately 6.1 km s?1, it is unclear whether this is due to variation in preaccretional/parent body processes experienced by these materials or due to heating and alteration during collection. We investigated alteration in pyrrhotite and pentlandite impacted into Stardust flight spare Al foils under encounter conditions by comparing scanning and transmission electron microscope (SEM, TEM) analyses of preimpact and postimpact samples and calculating estimates of various impact parameters. SEM is the primary method of analysis during initial in situ examination of Stardust foils, and therefore, we also sought to evaluate the data obtained by SEM using insights provided by TEM. We find iron sulfides experience heating, melting, separation, and loss of S, and mixing with molten Al. These results are consistent with estimated peak pressures and temperatures experienced (approximately 85 GPa, approximately 2600 K) and relative melting temperatures. Unambiguous identification of preserved iron sulfides may be possible by TEM through the location of Al‐free regions. In most cases, the Ni:Fe ratio is preserved in both SEM and TEM analyses and may therefore also be used to predict original chemistry and estimate mineralogy. 相似文献
150.
Pavel Raška Vilém Zábranský Jakub Dubišar Antonín Kadlec Alena Hrbáčová Tomáš Strnad 《Natural Hazards》2014,70(1):705-732
During the last two decades, documentary data (written and iconographic sources) have been increasingly employed in geomorphologic research aiming at reconstruction of territorial distribution, temporal occurrence and social and economic impacts of various geomorphologic hazards. The goal of this paper is to broaden the previous discussion (Glade et al. The use of historical data in natural hazard assessments. Kluwer, Dordrecht, 2001) of the methodological constraints on the use of documentary data for geomorphologic hazard research. Using the interdisciplinary approach of geomorphology, historiography and medial studies, we firstly summarise the major finding of papers that have employed various types of documentary data sources to study geomorphologic hazards in different regions. In the second section, we present case studies from the Czech Republic resulting from the ongoing research project that is devoted to the assessment of the potential of documentary data to reconstruct past occurrences of and mitigation strategies for geomorphologic hazards. Finally, we discuss three main methodological issues emerging from our research: (a) problems emerging from the positivist approach to documentary data sources and the necessity for critical analyses of documentary data sources based on modern historiographic approaches, (b) constraints arising from the combination of documentary data from different spatiotemporal scales and (c) lacks in the use of documentary data to study local-based adaptation strategies to cope with geomorphologic hazards. 相似文献