Observable blueshifts near compact objects     

Jeffrey M. Cohen  Mitchell F. Struble  Kay R. Pechenick  Boris Kuharetz 《Astrophysics and Space Science》1982,88(2):307-312

We show that observable blueshifted radiation can emanate from material freely falling toward compact objects. Using a fully relativistic treatment and considering possible blocking of photon trajectories by a neutron star or black hole, we demonstrate that blueshifts are observable.Supported in part by the National Science Foundation.  相似文献   

The Racialization of Difference: Enlarging the Story Field     

Kay Anderson 《The Professional geographer》2002,54(1):25-30

In this article, I explore ways of loosening the interpretive grid of “race” in critical geographical analysis without obscuring that concept's efficacy as a social force. In recent years, social constructivist perspectives on race have brought much evidence to bear on the logics of race/power formations in America and other British settler societies. The risk of petrifying “race” in the analysis of social life and reinscribing the very power that antiracists wish to undo has, however, prompted efforts to reframe the geographical study of race and racism. This article takes up that challenge by exploring an alternative modality of representational power that can be tracked to figurations of humanity and animality in Western cultural process. Such discursive formations take us some way toward understanding the norms and interiorised anxieties out of which racialized whiteness and its subjugated others were, and continue to be, constructed.  相似文献   

Trace element and isotopic variations in a zoned pluton and associated volcanic rocks,Unalaska Island,Alaska: A model for fractionation in the Aleutian calcalkaline suite     

Michael R. Perfit  Hannes Brueckner  James R. Lawrence  Robert W. Kay 《Contributions to Mineralogy and Petrology》1980,73(1):69-87

Trace elements, including rare earth elements (REE), exhibit systematic variations in plutonic rocks from the Captains Bay pluton which is zoned from a narrow gabbroic rim to a core of quartz monzodiorite and granodiorite. The chemical variations parallel those in the associated Aleutian calcalkaline volcanic suite. Concentrations of Rb, Y, Zr and Ba increase as Sr and Ti decrease with progressive differentiation. Intermediate plutonic rocks are slightly enriched in light REE (La/Yb=3.45–9.22), and show increasing light REE fractionation and negative Eu anomalies (Eu/Eu^*=1.03–0.584). Two border-zone gabbros have similar REE patterns but are relatively depleted in total REE and have positive Eu anomalies; indicative of their cumulate nature. Initial ⁸⁷Sr/⁸⁶Sr ratios in 8 samples (0.70299 to 0.70377) are comparable to those of volcanic rocks throughout the arc and suggest a mantle source for the magmas. Oxygen isotopic ratios indicate that many of the intermediate plutonic rocks have undergone oxygen isotopic exchange with large volumes of meteoric water during the late stages of crystallization; however no trace element or Sr isotopic alteration is evident.Major and trace element variations are consistent with a model of inward fractional crystallization of a parental high-alumina basaltic magma at low pressures (6 kb). Least-squares approximations and trace element fractionation calculations suggest that differentiation in the plutonic suite was initially controlled by the removal of calcic plagioclase, lesser pyroxene, olivine and Fe-Ti oxides but that with increasing differentiation and water fugacity the removal of sub-equal amounts of sodic plagioclase and hornblende with lesser Fe-Ti oxides effectively drove residual liquids toward dacitic compositions. Major and trace element compositions of aplites which intrude the pluton are not adequately explained by fractional crystallization. They may represent partial melts derived from the island arc crust. Similarities in Sr isotopes, chemical compositions and differentiation trends between the plutonic series and some Aleutian volcanic suites indicates that shallow-level fractional crystallization is a viable mechanism for generating the Aleutian calcalkaline rock series.LDGO Contribution no. 2964  相似文献   

Radioelements,radiogenic helium and age relationships for groundwaters from the granites at Stripa,Sweden   总被引：1，自引：0，他引：1  

J.N Andrews  I.S Giles  R.L.F Kay  D.J Lee  J.K Osmond  J.B Cowart  P Fritz  J.F Barker  J Gale 《Geochimica et cosmochimica acta》1982,46(9):1533-1543

The solution of radioelements and radiogenic ⁴He by groundwaters in fractured rocks is dependent upon the radioelement distribution in the rock matrix and the extent of the rock-water interface. The ${}^{234}\text{U}{}^{238}\text{U}$ activity ratio and the dissolved U, Rn and He contents of such groundwaters respond to changes in the flow regime with time. Although ${}^{234}\text{U}{}^{238}\text{U}$ activity ratios change with groundwater residence time as a consequence of ²³⁴Th-recoil induced solution of ²³⁴U, the activity ratio is strongly influenced by the U distribution within fractures, by the extent of the rock-water interface and by the amount of ²³⁸U in solution. A model for the quantitative evaluation of these effects is presented.Groundwaters from depths up to 880 m in the Stripa granite have variable dissolved uranium contents and ${}^{234}\text{U}{}^{238}\text{U}$ activity ratios. The uranium geochemistry is primarily determined by variations in flow path rather than by groundwater age.Dissolved radiogenic ⁴He in the groundwaters increases with their depth of origin, and is dependent upon the U content of the granite and upon its fracture porosity. It increases with groundwater residence time but movement of ⁴He by diffusion and transport processes make the actual groundwater age indeterminate.  相似文献   

Surface charge evolution of mineral-organic complexes during pedogenesis in Hawaiian basalt     

Jon Chorover  Mary Kay Amistadi 《Geochimica et cosmochimica acta》2004,68(23):4859-4876

Changes in surface charge of soil particles that accompany mineral transformations during soil formation were measured for a humid tropical chronosequence in Hawaiian basalt ranging in lava flow age from 0.3 to 4100 kiloyears (ky). Parent mineralogy is dominated by glass, olivine, pyroxene, and feldspar, whereas poorly crystalline (PC) weathering products (allophane, microcrystalline gibbsite, ferrihydrite) accumulate in early to intermediate weathering stages (through 400 ky), and crystalline secondary minerals (kaolinite, gibbsite, goethite) are dominant in the oldest (1400 and 4100 ky) soils. Detailed characterization of the solid phase was accomplished with chemical extractions, X-ray diffraction analysis, and molecular spectroscopy (FTIR and ¹³C MAS NMR). Simultaneous proton titration and background ion adsorption measurements were made on LiCl saturated soils over a range in pH (2-9) and ionic strength (0.001 and 0.01 M LiCl). Dependence of variable surface charge on solution composition reflects the changing nature of mineral-organic interactions over the course of pedogenesis. Points of zero net proton charge (PZNPC) ranged from 3.4 to 6.2 and 2.0 to 5.8 at 0.001 and 0.01 M ionic strength (I), respectively. Intermediate-aged soils containing the highest mass concentration of humified soil organic matter (SOM) and its complexes with PC minerals gave rise to the steepest charging curves (largest pH dependence) and highest PZNPC values. Surface charge properties of these soils most closely reflected their weakly acidic Al and Fe hydroxide constituents, which is consistent with metal hydroxide saturation of organic functional groups, rather than organic coating of mineral surfaces. Charging curves were less steep and PZNPC values were lower for the older soils, consistent with SOM coating of more crystalline goethite, kaolinite, and gibbsite surfaces in a soil system less impacted by labile Al and Fe.  相似文献   

A stochastic physical system approach to modeling river water quality     

W. F. Curi  T. E. Unny  J. J. Kay 《Stochastic Hydrology and Hydraulics》1995,9(2):117-132

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Tholeiitic Aleutian arc plutonism: The Finger Bay pluton,Adak, Alaska     

Suzanne Mahlburg Kay  Robert W. Kay  Hannes K. Brueckner  James L. Rubenstone 《Contributions to Mineralogy and Petrology》1983,82(1):99-116

The earliest representatives in the sequence of Tertiary to Recent magmatic rocks on Adak island in the central Aleutians, are the Finger Bay Volcanics and associated small shallow-level gabbroic intrusives. The tholeiitic Finger Bay pluton (gabbro to quartz monzodiorite) is among the least altered representatives of this earliest period. The field relations, mineralogy, and geochemistry of the Finger Bay pluton contrast with the more recent calcalkaline plutons in the arc (e.g. on Adak, Hidden Bay pluton: 33 m.y. and on Kagalaska, Kagalaska pluton: 15 m.y.). Compared with the Hidden Bay pluton, the Finger Bay pluton is smaller (8 km² versus 100 km²), has a greater proportion of gabbro (84% versus 5%), has a somewhat different mineralogy, and has higher whole rock and mafic mineral FeO/MgO ratios, higher K₂O, and higher concentrations of incompatable elements in rocks of equivalent SiO₂ (particularly for the more siliceous units). Magmatic amphibole occurs only in the most siliceous units in the Finger Bay pluton, whereas it is common in the calc-alkaline plutons. Except for the size, these differences parallel those between tholeiitic and calc-alkaline volcanic rocks from the active Aleutian volcanic centers. Textural, miner-alogical, and trace element analyses indicate that mixing of magmas and gabbros generated some of the rocks of intermediate (monzodiorite) composition in the Finger Bay pluton. Most of the differences in magmatic trends between the calc-alkaline and tholeiitic plutons are attributed to the physical conditions of magmatic evolution in the crust, rather than to differences in initial magmatic types. This conclusion rests on the similarity of fractionation-independent isotope ratios and trace element ratios in Aleutian magmas of all ages. In particular, compared to magmas of the north Pacific ocean basin (MORB, oceanic islands), Aleutian magmas show excess enrichment of Ba, K, Rb, and U relative to REE and high ²⁰⁷Pb/²⁰⁴Pb ratios for a given ²⁰⁶Pb/²⁰⁴Pb ratio. Recognition of tholeiitic series plutons in the arc provides direct evidence for magmatic conditions accompanying fractionation, and serves to emphasize the diversity of magmatic trends that are found over time and space at convergent plate margins.  相似文献   

Health, Safety and Environmental Risks of Underground Co2 Storage – Overview of Mechanisms and Current Knowledge     

Kay Damen  André Faaij  Wim Turkenburg 《Climatic change》2006,74(1-3):289-318

CO₂ capture and storage (CCS) in geological reservoirs may be part of a strategy to reduce global anthropogenic CO₂ emissions. Insight in the risks associated with underground CO₂ storage is needed to ensure that it can be applied as safe and effective greenhouse mitigation option. This paper aims to give an overview of the current (gaps in) knowledge of risks associated with underground CO₂ storage and research areas that need to be addressed to increase our understanding in those risks. Risks caused by a failure in surface installations are understood and can be minimised by risk abatement technologies and safety measures. The risks caused by underground CO₂ storage (CO₂ and CH₄ leakage, seismicity, ground movement and brine displacement) are less well understood. Main R&D objective is to determine the processes controlling leakage through/along wells, faults and fractures to assess leakage rates and to assess the effects on (marine) ecosystems. Although R&D activities currently being undertaken are working on these issues, it is expected that further demonstration projects and experimental work is needed to provide data for more thorough risk assessment.  相似文献   

The melting of floating ice raises the ocean level     

Peter D. Noerdlinger  Kay R. Brower 《Geophysical Journal International》2007,170(1):145-150

It is shown that the melting of ice floating on the ocean will introduce a volume of water about 2.6 per cent greater than that of the originally displaced sea water. The melting of floating ice in a global warming will cause the ocean to rise. If all the extant sea ice and floating shelf ice melted, the global sea level would rise about 4 cm. The sliding of grounded ice into the sea, however, produces a mean water level rise in two parts ; some of the rise is delayed. The first part, while the ice floats, is equal to the volume of displaced sea water. The second part, equal to 2.6 per cent of the first, is contributed as it melts. These effects result from the difference in volume of equal weights of fresh and salt water. This component of sea rise is apparently unrecognized in the literature to date, although it can be interpreted as a form of halosteric sea level change by regarding the displaced salt water and the meltwater (even before melting) as a unit. Although salinity changes are known to affect sea level, all existing analyses omit our calculated volume change. We present a protocol that can be used to calculate global sea level rise on the basis of the addition of meltwater from grounded and floating ice; of course thermosteric volume change must be added.  相似文献   

Measuring Ω₀ from the entropy evolution of clusters     

Scott T. Kay  Richard G. Bower 《Monthly notices of the Royal Astronomical Society》1999,308(3):664-676

In this paper we have extended the entropy-driven model of cluster evolution developed by Bower in order to be able to predict the evolution of galaxy clusters for a range of cosmological scenarios. We have applied this model to recent measurements of the evolution of the L _x− T normalization and X-ray luminosity function in order to place constraints on cosmological parameters. We find that these measurements alone do not select a particular cosmological framework. An additional constraint is required on the effective slope of the power spectrum to break the degeneracy that exists between this and the background cosmology. We therefore include a theoretical calculation of the Ω₀ dependence on the power spectrum, based on the cold dark matter paradigm, which infers Ω₀<0.55 (0.1<Ω₀<0.7 for Ω₀+Λ₀=1), at the 95 per cent confidence level. Alternatively, an independent measurement of the slope of the power spectrum from galaxy clustering requires Ω₀<0.6 (Ω₀<0.65 for Ω₀+Λ₀=1), again to 95 per cent confidence. The rate of entropy evolution is insensitive to the values of Ω₀ considered, although it is sensitive to changes in the distribution of the intracluster medium.  相似文献