The broadening of strong lines of Ca⁺, Mg⁺ and Ba⁺ by collisions with neutral hydrogen atoms     

P. S. Barklem  & B. J. O'Mara 《Monthly notices of the Royal Astronomical Society》1998,300(3):863-871

The theory of Anstee &38; O'Mara is extended to the line broadening of transitions of singly ionized atoms by collisions with neutral hydrogen atoms. The theory is used to calculate broadening cross-sections for strong lines of singly ionized calcium, magnesium and barium. The broadening cross-sections calculated are compared with both theoretical and empirical results of other workers.  相似文献   

Additional ultra-high-resolution observations of Ca⁺ ions in the local interstellar medium     

I. A. Crawford  R. Lallement  & B. Y. Welsh 《Monthly notices of the Royal Astronomical Society》1998,300(4):1181-1188

We present ultra-high-resolution (0.35 km s⁻¹ FWHM) observations of the interstellar Ca K line towards seven nearby stars. The spectral resolution was sufficient to resolve the line profiles fully, thereby enabling us to detect hitherto unresolved velocity components, and to obtain accurate measurements of the velocity dispersions ( b values). Absorption components with velocities similar to those expected for the Local Interstellar Cloud (LIC) and the closely associated 'G cloud' were identified towards six of the seven stars. However, in most cases the b values deduced for these components were significantly larger than the b  ≈ 2.2 km s⁻¹ (i.e. T _k ≈ 7000 K, v _t ≈ 1 km s⁻¹) expected for the LIC, and it is argued that this results from the presence of additional, spectrally unresolved, components having similar velocities and physical conditions. For two stars (δ Vel and α Pav) we detect interstellar components with much smaller b values (1.1 ± 0.3 and 0.8 ± 0.1 km s⁻¹, respectively) than are expected for low-density clouds within the Local Bubble. In the case of the narrow α Pav component, we also find an anomalously large Na  i /Ca  ii column density ratio, which is indicative of a relatively high density. Thus it is possible that, in addition to LIC-type clouds, the local interstellar medium contains a population of previously undetected cooler and denser interstellar clouds.  相似文献   

Vertical profiles of Volcanic Aerosol and Polar Stratospheric Clouds Above Kiruna, Sweden: Winters 1993 and 1995     

Terry Deshler  Samuel J. Oltmans 《Journal of Atmospheric Chemistry》1998,30(1):11-23

Vertical profiles of aerosol were measured in February 1993, and January - March 1995 using balloon-borne particle counters released from Kiruna, Sweden. Condensation nuclei (CN) and aerosol with radii 0.15 - 10.0 µm were measured in 8-12 size classes. The three flights in 1993 were within the polar vortex. Temperatures were below polar stratospheric cloud (PSC) threshold temperatures on one flight and a thin PSC was observed. The volcanic aerosol in the 1993 vortex was similar to that in 1992. In 1993, surface areas were 10 - 20 µm2 cm-3 and volumes 1 - 3 µm3 cm-3. In 1995 three of five flights were within the polar vortex. The volcanic aerosol had decreased to 3 - 7 µm2 cm-3 and 0.1 - 0.4 µm3 cm-3. The top of the volcanic aerosol layer in both years was near 500 K potential temperature (~20 km). A thick nitric acid and water PSC was observed in January 1995. In the thickest region of this PSC nearly all CN were observed to be activated, and surface areas of 5 - 10 µm2 cm-3 were calculated. The volumes observed in this PSC were closer to what would be expected for particles composed of nitric acid trihydrate than for ternary solution droplets. In 1993 the opposite was observed, the volumes in the thin PSC were closer to what would be expected for ternary solution droplets.  相似文献   

Mercury in lake sediments of the Precambrian Shield near Huntsville, Ontario, Canada   总被引：10，自引：0，他引：10  

P. E. Rasmussen  D. J. Villard  H. D. Gardner  J. A. C. Fortescue  S. L. Schiff  W. W. Shilts 《Environmental Geology》1998,33(2-3):170-182

 Long sediment cores (>1 m) were collected from eight Precambrian Shield lakes in southern Ontario, Canada and analyzed for mercury (Hg), loss-on-ignition (LOI), and a suite of 36 other elements. Results indicated at least 100-fold variation in sediment Hg concentrations between lakes in close proximity (from 450 ppb), comparable to the variation reported for lakes across the whole of Canada. Strong areal correlations between Hg concentrations and LOI (r ² =0.77), between Hg and other trace element concentrations (Pb, Zn, Cd, Sb, As, Br), and similarities in the vertical concentration profiles of Hg and LOI, all point to the importance of organic matter in the release, transport and redistribution of metals in watershed systems. The spatial pattern of Hg concentrations in deep, precolonial sediments (>20 cm) was found to mirror the pattern of Hg concentrations in modern surface sediments, an observation that was confirmed in a follow-up survey (r ² =0.85;n=25 lakes), indicating that natural processes govern the unequal distribution of Hg among these lakes. Between-lake differences in surface sediment Hg concentrations normalized to organic carbon (Hg/C) were also reflected by Hg concentrations in smallmouth bass normalized to 35 cm length (R ² =0.63;n=15 lakes). The latter relationship suggests that smallmouth bass and lake sediment indicators provide mutually supportive information regarding Hg loading to the lacustrine environment from geological sources in the watershed system. Received: 31 October 1996 · Accepted: 27 May 1997  相似文献   

Ocean Data Assimilation Using Intermittent Analyses and Continuous Model Error Correction   总被引：1，自引：0，他引：1  

Bohua Huang  James L. Kinter III  Paul S. Schopf 《大气科学进展》2002,19(6):965-992

A new data insertion approach is applied to the Derber and Rosati ocean data assimilation(ODA) system,a system that uses a variational scheme to analyze ocean temperature and provide ocean model corrections continuously.Utilizing the same analysis component as the original system,the new approach conducts analyses to derive model corrections intermittently at once-daily intervals.A technique similar to the Incremental Analysis Update(IAU) method of Bloom et al.is applied to incorporate the corrections into the model gradually and continuously.This approach is computationally more economical than the original.A 13-year global ocean analysis from 1986 to 1998 is produced using this new approach and compared with an analysis based on the original one.An examination of both analyses in the tropical Pacific Ocean shows that they have qualitatively similar annual and interannual temperature variability.Howerver,the new approach produces smoother monthly analyses.Moreover,compared to the independent observations from current meters,the new equatorial currents are significantly better than the original analyses,not only in maintaining the mean state but also in capturing the annual and interannual variations.  相似文献   

VELOCITY AND SUSPENSION CONCENTRATION IN SEDIMENT-MIXED FLUID     

B.S.MAZUMDER  K.GHOSHAL 《国际泥沙研究》2002,17(3)

1 INTRODUCTION AND REVIEW Numerous investigations related to vertical velocity and suspension concentration distributions have been undertaken to the steady, uniform, open channel turbulent flow. The problems of sediment mixed water flows are of direct interest to the practical situations in the field of river sedimentation, coastalsediment transport and in the field of two-phase flow in particular. In hydraulic open channel flow, the vertical velocity profile is usually described by…  相似文献   

Siting criteria for heat extraction from hot dry rock; Application to Switzerland     

L. Rybach  P. Bodmer  N. Pavoni  St. Mueller 《Pure and Applied Geophysics》1978,116(6):1211-1224

For selecting possible hot dry rock extraction sites for geothermal energy applications, the following criteria have been considered: (i) depth to the crystalline basement, (ii) temperatures at depth, (iii) pattern of regional stress field and (iv) natural permeability (=degree of fracturing) of basement rocks. A contour map of the basement topography is presented. From outcrops at the nothern border of Switzerland (crystalline rocks of the Black Forest massif, mainly granites and gneisses of Hercynian age) the basement dips gently toward the SE under the Mesozoic and Tertiary sediments of the Molasse Basin and reaches its maximum depth (7 km) underneath the front of the Alps. Some 30 km further SE the basement rocks appear at the surface (Aar- and Gotthard-massif, Penninic units), where they are deformed and fractured to a great extent. Temperature-depth profiles have been obtained by model calculations. Locally increased heat product on (in granite batholiths) at the base of the Molasse Basin, combined with the blanketing effect of the overlying sediments, could raise the temperatures to 150–170°C at a depth of 5 km. According to earthquake fault-plane solutions (P-axes) the regional stress field in the area of the Swiss Alps and in its northern Foreland is characterized by the maximum horizontal compression oriented N(150±20)°E in the upper crust.In situ stress determinations (overcoring experiments) show that considerable excess horizontal compressive stress is present in the Alpine crust (up to 200 bar). The deep Alpine tunnels exhibited considerable fracturing of crystalline rocks at depths greater than 1–2 km. Information about the degree of fracturing has also been obtained by refraction profiles. The velocitydepth functions show lower than normal velocities in the uppermost 1.5 km, indicating that the rocks there are fractured. A 30–40 km wide region, running along the axis of the Molasse Basin (which coincides with the majority of the population and most of the industry of Switzerland) would provide the best hot dry rock sites.Paper presented at the Second NATO-CCMS Meeting on Dry Hot Rock Geothermal Energy, 28–30 June 1977, Los Alamos, New Mexico, USA. Contribution No. 198, Institute of Geophysics ETH Zurich.  相似文献   

Deep seismic soundings in southern Spain     

Working Group for Deep Seismic Sounding in Spain – 《Pure and Applied Geophysics》1977,115(3):721-735

Summary In 1974 and 1975 deep seismic sounding experiments were carried out in the area of the Betic Cordillera in southern Spain. A network of crustal seismic profiles was established with shotpoints at sea close to Cádiz, Adra and Cartagena and on land at Alquife near Guadix. The lengths of the profiles range from 50 km near Alquife to 440 km for the main profile between Cádiz and Cartagena parallel to the strike of the Betic Cordillera. The main profile was supplemented by a reversed recording line close to the Mediterranean coast between Adra and Cartagena and another one perpendicular to the main tectonic strike from Adra towards the north. The first interpretation of the data indicates considerable variation in the crustal thickness. A preliminary inversion leads to a three-layered model of the crust. The mean compressional velocity is about 5.1 km/s down to a depth of 4 km. Below this the velocity is 6.13 km/s from 4 to 16 km where it increases to 7.14 km/s. TheP _n-velocity is 8.18 km/s. The crust-mantle boundary is reached at a depth of 27 km near Cartagena and lies 32 km deep near Adra, Underneath the gravity minimum of the Betic Cordillera the crust-mantle boundary is found at a depth of about 36 km. Below the Betic zone a pronounced zone of low velocity with 7.7 km/s seems to exist in the depth range from 40 to 60 km.Contribution No. 4, Grupo de Trabajo de Perfiles Sismicos, Comisión Española del Proyecto Geodinámico, C.S.I.C., Madrid, Spain.Contribution No. 139, Geophysical Institute, University of Karlsruhe, Hertzstrasse 16, D-75 Karlsruhe 21, Germany.Contribution No. 217, Institut de Physique du Globe, Université Paris VI, 4 Place Jussieu, F-75230 Paris Cedex 05, France.Contribution No. 11, Instituto y Observatorio de Marina, San Fernando (Cádiz), Spain.Contribution No. 163, Institute of Geophysics, Swiss Federal Institute of Technology, ETH-Hönggerberg, CH-8093 Zürich, Switzerland.  相似文献   

GRB 060418 and 060607A: the medium surrounding the progenitor and the weak reverse shock emission     

Z. P. Jin  Y. Z. Fan † 《Monthly notices of the Royal Astronomical Society》2007,378(3):1043-1048

We provide a remedy for a recently published formulation of the Voigt function by reformulating the function into a single proper integral with a damped sine integrand. The present formulation clears up concerns highlighted about the original formulation. The reduction of the Voigt function to a single proper integral enables the use of algorithms available in the literature and included in many software packages to integrate the function and to evaluate the line profile with relative simplicity and superior accuracy. Evidence of the usefulness and superior accuracy of the new formulation is provided.  相似文献   

Variation in the primary and reprocessed radiation from an orbiting spot around a black hole   总被引：1，自引：0，他引：1  

M. Dov&#;iak  V. Karas  G. Matt  R. W. Goosmann 《Monthly notices of the Royal Astronomical Society》2008,384(1):361-369

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