Validating Earth and ocean tide models using tidal gravity measurements   总被引：7，自引：0，他引：7  

Trevor F. Baker  Machiel S. Bos 《Geophysical Journal International》2003,152(2):468-485

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Verification of the Contribution of Vehicular Traffic to the Total NMVOC Emissions in Germany and the Importance of the NO3 Chemistry in the City Air     

R. Kurtenbach  R. Ackermann  K. H. Becker  A. Geyer  J. A. G. Gomes  J. C. Lörzer  U. Platt  P. Wiesen 《Journal of Atmospheric Chemistry》2002,42(1):395-411

In 1997 and 1998 several field campaigns for monitoring non-methane volatile organic compounds (NMVOCs) and nitrogen oxides (NO_x) were carried out in a road traffic tunnel and in the city center of Wuppertal, Germany. C₂–C₁₀ aliphatic and aromatic hydrocarbons were monitored using a compact GC instrument. DOAS White and long path systems were used to measure aromatic hydrocarbons and oxygenated aromatic compounds. A formaldehyde monitor was used to measure formaldehyde. Chemiluminescence NO analysers with NO₂ converter were used for measuring NO and NO₂. The high mixing ratios of the NMVOCs observed in the road traffic tunnel, especially 2.9 ppbv phenol, 1.5ppbv para-cresol and 4.4 ppbv benzaldehyde, in comparison with themeasured background concentration clearly indicate that these compounds were directly emitted from road traffic. Para-Cresol was for the first timeselectively detected as primary pollutant from traffic. From the measured data a NMVOC profile of the tunnel air and the city air, normalised to benzene (ppbC/ppbC), was derived. For most compounds the observed city air NMVOC profile is almost identical with that obtained in the traffic tunnel. Since benzene originates mainly from road traffic emission, the comparison of the normalised emission ratios indicate that the road traffic emissions in Wuppertal have still the largest impact on the city air composition, which is in contrast to the German emission inventory. In both NMVOC profiles, aromatic compounds have remarkably large contributions of more than 40 ppbC%. In addtion, total NMVOC/NO_x ratios from 0.6 up to 3.0ppbC/ppb in the traffic tunnel air and 3.4± 0.5 in the city air of Wuppertal were obtained. From the observed para-cresol/toluene and ortho-cresol/toluene ratios in the city air, evidence was found thatalso during daytime NO₃ radical reactions play an important role in urban air.  相似文献   

Exhumation of high-pressure rocks: a review of concepts and processes     

J.P. Platt 《地学学报》1993,5(2):119-133

The exhumation of high-pressure metamorphic rocks requires either the removal of the overburden that caused the high pressures, or the transport of the metamorphic rocks through the overburden. Exhumation cannot be achieved simply by thrusting or strike-slip faulting. It may be caused by erosion of shortened and thickened crust, but this is unlikely to be the only mechanism for exhuming rocks from depths greater than about 20 km. One or more of the following additional mechanisms may be involved. 1 Corner flow of low-viscosity material trapped between the upper and lower plates in a subduction zone can cause upward flow of deeply buried rock, and may explain some occurrences of high-pressure tectonic blocks in mélange. This process does not, however, appear to be adequate to explain the exhumation of regional high-pressure terrains. 2 Buoyancy forces acting directly on metamorphic rock bodies may cause them to rise relative to more dense surroundings. This is likely to be the most important mechanism of exhumation of crustal rocks subducted into the mantle, but cannot explain the emplacement of coherent tracts of high-density metamorphic rock into shallow crustal levels. Some high-pressure blocks emplaced at shallow levels in accretionary terrains may have been entrained in diapiric intrusions of low-density mud or serpentinite. 3 Extension driven by the forces associated with contrasts in surface elevation may explain the exhumation and structural setting of many high-pressure terrains. Extension may occur in the upper part of an accretionary wedge thickened by underplating; or it may affect the whole lithosphere in a region of intracontinental convergence, if surface elevation has been increased by the removal of a lithospheric root. In the second case extension may be accompanied by magmatism and an evolution towards higher temperature during decompression of the metamorphic terrain.  相似文献   

The Chandra view of galaxy mergers     

Nicola J. Brassington  Trevor J. Ponman  rew M. Read 《Monthly notices of the Royal Astronomical Society》2007,377(4):1439-1456

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Erratum to “Environmental control of short-term variation in the plankton community of inner Tokyo Bay, Japan” [Estuar., Coast. Shelf Sci. 78 (2008) 796–810]     

Toru Nakane  Kisaburo Nakata  Heather Bouman  Trevor Platt 《Estuarine, Coastal and Shelf Science》2008,80(4):598

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Extension of a fluctuating plume model of tracer dispersion to a sheared boundary layer and to a large array of obstacles     

Ralph M. Gailis  Alexander Hill  Eugene Yee  Trevor Hilderman 《Boundary-Layer Meteorology》2007,122(3):577-607

Fluctuating plume models provide a useful conceptual paradigm in the understanding of plume dispersion in a turbulent flow. In particular, these models have enabled analytical predictions of higher-order concentration moments, and the form of the one-point concentration probability density function (PDF). In this paper, we extend the traditional formalism of these models, grounded in the theory of homogeneous and isotropic turbulent flow, to two cases: namely, a simple sheared boundary layer and a large array of regular obstacles. Some very high-resolution measurements of plume dispersion in a water channel, obtained using laser-induced fluorescence (LIF) line-scan techniques are utilised. These data enable us to extract time series of plume centroid position (plume meander) and dispersion in the relative frame of reference in unprecedented detail. Consequently, experimentally extracted PDFs are able to be directly compared with various theoretical forms proposed in the literature. This includes the PDF of plume centroid motion, the PDF of concentration in the relative frame, and a variety of concentration moments in the absolute and relative frames of reference. The analysis confirms the accuracy of some previously proposed functional forms of model components used in fluctuating plume models, as well as suggesting some new forms necessary to deal with the complex boundary conditions in the spatial domain.  相似文献   

Archaean tectonics in the Agnew supracrustal belt,Western Australia     

J.P. Platt  P.D. Allchurch  R.W.R. Rutland 《Precambrian Research》1978,7(1):3-30

The Agnew supracrustal belt consists of a greenstone sequence (interlayered metabasalt, differentiated gabbroic sills, ultramafic bodies, and black volcanogenic sediment) unconformably overlain by granitoid-clast conglomerate and meta-arkose. The base of the preserved sequence is intruded by grey tonalite with a crudely concordant upper contact, and by small discordant bodies of leucogranite.An early deformation (D1) produced isoclinal folds and a regional penetrative foliation. These structures were probably gently dipping when formed. D2 produced large-scale NNW-trending upright folds, a regional foliation, and a vertical N-trending ductile fault on the west side of the belt. D2 structures indicate a combination of ENE-WSW shortening, and right-lateral shear along the ductile fault. Both D1 and D2 were accompanied by metamorphism under upper greenschist to lower amphibolite facies conditions.The interpreted sequence of tectonic events is (1) deposition of the greenstone sequence on an unknown basement; (2) intrusion of large volumes of tonalite, separating the supracrustal rocks from their basement; (3) erosion of mafic rocks and tonalite to produce the clastic sedimentary sequence; (4) the first deformation; (5) intrusion of small volumes of leucogranite; (6) the second deformation.The bulk of the granitoid rocks were emplaced before the first recognisable deformation. Thus the granitoid magma cannot have been produced by partial melting of previously downbuckled ‘greenstone belt’ rocks, nor can the large-scale upright folds (D2) be a result of forceful emplacement of the magma — two common postulates for Archaean terrains. The D2 folds are closely related to the ductile fault bounding the zone: these structures, which give the present N-trending tectonic belt its form, are the youngest features in the terrain.  相似文献   

Aeolian Sky packaged chemicals pollution incident     

Trevor R. Dixon  T.J. Dixon 《Marine pollution bulletin》1981,12(2):53-56

Three and a half thousand packages of chemicals, including at least 956 containing hazardous substances were washed ashore on to the beaches of southern England. They were believed at the time to have come from the wreck of the Aeolian Sky. There is now a strong suspicion that half the packages, including 32 canisters of arsenic trichloride, were lost from the deck cargo of another vessel in the English Channel. Despite difficulties in identifying the contents of many unlabelled chemical packages found on the shore, most were recovered during clearance operations by Local Authorities. Although there was no evidence of any ecological damage, 20 people were taken to hospital for treatment or precautionary medical examinations following contact with opened or leaking packages. This incident raised questions regarding international reporting procedures, liability and compensation arrangements following losses of packaged chemical cargoes at sea.  相似文献   

Alarming growth in tanker casualties     

Trevor R. Dixon 《Marine pollution bulletin》1979,10(3):68-69

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Prior exposure to Cu contamination influences the outcome of toxicological testing of Fucus serratus embryos     

Nielsen HD  Burridge TR  Brownlee C  Brown MT 《Marine pollution bulletin》2005,50(12):1675-1680

Brown seaweeds are often employed in single species toxicity testing to study the association between the pollutant and the biota in contaminated marine habitats. We have used Fucus serratus (Phaeophyta) from one Cu resistant and one non-resistant population to evaluate the effect of prior exposure to metal pollution on toxicological endpoints. Analysis of comparative toxicity was conducted for embryo rhizoid elongation and adult relative growth rate (RGR). Algae that had previously been exposed to Cu expressed consistently lower levels of sensitivity to Cu than those that had no history of exposure to the pollutant. For both non-resistant and resistant populations rhizoid length was a more sensitive endpoint than adult RGR. While early life history stages of brown algae are generally regarded as being pollution-sensitive and inhibition of spore and embryo rhizoid elongation is frequently used as endpoints in bioassays, the test results may be affected by prior exposure of the parent algae to the pollutant. We conclude that the effect of prior exposure should be considered when comparing endpoints between studies and when selecting material for future testing.  相似文献