Some useful results on initial node locations for near-equatorial circular satellite orbits     

Ahmed Kamel  Richard Tibbitts 《Celestial Mechanics and Dynamical Astronomy》1973,8(1):45-73

Perturbation theory based on Lie transforms is used to obtain a second-order long period solution for inclination and right ascension of ascending node, of near-equatorial circular satellite orbits. The solution includes the average effects of the Earth's oblateness and the luni-solar perturbations. Three algorithms, useful in mission analysis, are then given. The first algorithm finds the initial node location that results in a decrease of inclination to zero and it also finds the corresponding time to arrive at this zero inclination. The second algorithm determines the initial nodal band that maintains the orbital inclination below a specified value for a given time interval. The third algorithm obtains the initial node location that maximizes the time in which the satellite can be maintained within a given inclination tolerance without the use of any active control and it also obtains the corresponding maximum time. The results of the first and the third algorithms are given for 24-h near-equatorial circular satellite orbits and are cast in simple closed forms.  相似文献   

Stability of a compressible fluid cylinder ambient with a bounded conducting medium under general varying magnetic fields     

Ahmed E. Radwan 《Astrophysics and Space Science》1990,172(2):305-314

The stability of a compressible fluid cylinder pervaded by a longitudinal uniform magnetic field-ambient with a bounded conducting medium of negligible inertia penetrated with general varying vacuum magnetic fields has been developed. The stability criterion describing the stability characteristics of that model is derived and discussed analytically in general terms. The axial fields have always stabilizing influences. The azimuthal vacuum field has a destabilizing effect, however, it becomes minimal if the perturbed and the unperturbed vacuum fields are not orthogonal. The magnetodynamic instability of the fluid jet is modified in the presence of the fluid compressibility. The stabilizing influence due to the latter may be realized more clearly on utilizing the numerical methods for investigating the eigenvalue relation.Several reported works can be recovered as limiting cases with appropriate simplifications.  相似文献   

Nonaxisymmetric magnetogravitational instability of a streaming fluid cylinder ambient with a tenuous medium pervaded by transverse varying fields     

Ahmed E. Radwan 《Astrophysics and Space Science》1992,187(2):241-260

The stability of a self-gravitating streaming fluid cylinder acting upon the electromagnetic force ambient with a tenuous medium of negligible inertia but pervaded by a transverse varying fields, has been developed. The stability criterion is derived, discussed analytically and the results are verified numerically. The cylinder is purely self-gravitating unstable in small axisymmetric domain and stable in all the rest states. modes while the transverse field exterior the cylinder is stabilizing or destabilizing according to restrictions in the asymmetric modes and purely destabilizing in the symmetric one. The streaming has a strong destabilizing influence and that influence is independent of the kind of the perturbation and wavelengths. Both the streaming and the electromagnetic influences increase the gravitational axisymmetric unstable domain and shrink those of stability in the axisymmetric and non-axisymmetric perturbations. Moreover, the stabilizing character of the Lorentz force of some states, is physicaly interpreted, will not be able to suppress the gravitational instability because the gravitational instability of sufficiently long waves will persist.  相似文献   

Tropospheric,stratospheric and mesospheric ozone observed using the Umkehr method     

Christian Meunier  Ahmed Bekaddour  Pierre Marche  Pierre Jouve 《Planetary and Space Science》1983,31(7):729-730

Ozone vertical profiles have been obtained above the “Observatoire de Haute-Provence” from 9 to 19 June 1981, with both conventional and short Umkehr methods: the mesospheric and stratospheric ozone variability has been found to be very small while the ozone variability was large in the troposphere and maximum at the tropopause level.  相似文献   

Organic matter diagenesis in the anoxic sediments of saanich inlet,British Columbia,Canada: a case for highly evolved community interactions     

S.I. Ahmed  S.L. King  J.R. Clayton 《Marine Chemistry》1984,14(3):233-252

Cytochrome c and ferricyanide reducing activities are measured in a Desulfovibrio desulfuricans (strain ATCC No. 17990) that indicate that the APS reductase activity is constitutive. This enzymatic activity is also measured in a Saanich Inlet isolate identified as Desulfovibrio salexigens (Saanich). Successful measurement of the Cytochrome c reducing activity was also made in the sediment extracts from Saanich Inlet, and this activity was found to be present in sediments as deep as 50 cm. Bacterial biomass distributions were estimated using measurements of ATP in the Saanich Inlet sediments. ETS activity measurements correlated well with the in situ [³⁵S]-SO₄^2? reduction rate measurements; both of the methods showing a subsurface maximum in activity at a depth of about 10 cm. However, some differences between the results obtained from these two procedures were also found, e.g., the in situ [³⁵S]-SO₄^2? reduction activity approximated zero values at or near 25 cm depth, while 5–10% of the surface ETS activity was present at a depth of as much as 50 cm. The hypothesis presented is that the subsurface maximum may be due to the anaerobic oxidation of methane by [³⁵S]-SO₄^2? ions as mediated by the sulfate-reducing bacteria. A discussion of the strong interactive relationships between a variety of organisms in an ecosystems context, so necessary in bringing about organic matter diagenesis in anoxic marine environments, is also presented.  相似文献   

An estimate of the duct life time from low latitude ground observations of whistlers at Varanasi     

P. N. Khosa  Lalmani  M. M. Ahmed  V. K. Rawal 《Earth, Moon, and Planets》1983,28(3):329-333

The observed periodicity in the whistler occurrence rate recorded at our low latitude ground station at Varanasi (geomagnetic latitude, 14°55'N) is interpreted in terms of duct life time at lowL values. Power spectrum analysis of the whistler data yields a period of about 50 min for the growth and decay of ducts. Further dispersion analysis of the whistlers has qualitatively confirmed the existence of separate ducts during the period of observations.  相似文献   

Relationship of environmental geochemistry to soil degradation in Helwan catchment, Egypt   总被引：1，自引：0，他引：1  

Ahmed A. Melegy 《Environmental Geology》2005,48(4-5):524-530

Environmental geochemistry plays an important role in understanding the distribution of major cations (Ca²⁺, Mg²⁺, Na⁺, K⁺) in Helwan catchment, south Cairo, Egypt. Evaluation of soil mechanical erosion rate, depletion rate, exchangeable rates of base cations and sodium adsorption ratios are essential for understanding soil degradation problems in the representative Helwan catchment. Soil erosion is a natural process. It often becomes a problem when human activity causes it to occur much faster than under natural conditions. The results of the mechanical erosion rate of soil and the exchangeable rates of base cations are 1845 and 80.3 kg ha⁻¹ yr⁻¹, respectively. The high intensity of the mechanical erosion rate is probably attributed to the high specific surface area of the studied type of Vertisol, intensive application of fertilizer and industrial activities. Mechanical erosion of soil, exchangeable rate of base cations and the depletion rate of base cations are almost inexhaustible sources of sodium, and all these increase the problem of sodic soils and may affect plant productivity in Helwan catchment.  相似文献   

L'upwelling de la côte atlantique du Maroc entre 1994 et 1998     

Ahmed Makaoui  Abdelattif Orbi  Karim Hilmi  Soukaina Zizah  Jamila Larissi  Mohammed Talbi 《Comptes Rendus Geoscience》2005,337(16):1518

The pelagic ecosystem of the Moroccan Atlantic coast is influenced by the spatiotemporal variability of upwelling. The changes in the physicochemical and biological parameters as well as their interrelationship and regrouping by the principal components analysis allowed us to subdivide the Atlantic coast in four active areas: two areas located at the north of Cape Juby (28°N), characterised by a summery activity and two areas located at the south, active permanently, with a variable intensity. To cite this article: A. Makaoui et al., C. R. Geoscience 337 (2005).  相似文献   

Fluid inclusions in chromite from a pyroxenite dike of the Pindos ophiolite complex     

Ahmed Al-Boghdady  Maria Economou-Eliopoulos 《Chemie der Erde / Geochemistry》2005,65(2):191-202

Chromitite occurrences in the Pindos ophiolite complex are located in elongated dunite bodies hosted in harzburgite of the mantle sequence, and show a compositional variation from high-Al to high-Cr type. Although the majority of the chromite ores is characterized by paucity in fluid inclusions, abundant fluid inclusions were found in chromite hosted by a coarse-grained pyroxenite dike at the Spanos Valley, Pindos complex. Chromite occurs in highly variable proportion in an orthopyroxene matrix or as inclusions in orthopyroxenes. Its composition is homogeneous and has an average Cr/(Cr+Al) ratio 0.73.The investigation of chromitites revealed the presence of primary and secondary fluid inclusions. The primary inclusions are of following types: Three-phase solid-liquid-gas, three-phase liquid-liquid-gas, two-phase liquid-gas and one-phase octahedron crystal-shaped. The secondary fluid inclusions are two-phase liquid-gas and mono-phase fluid inclusions.The presence of fluid inclusions in chromite aggregates hosted in orthopyroxenite dikes, in combination with the trace element contents in chromite concentrates and the mineralogical composition of the dikes may indicate that an aqueous phase separated from the magma.  相似文献   

Reply to the discussion to “On the evolution of salt diapirs in Tunisian Atlas” by Christopher J. Talbot     

Chokri Jallouli  Mongi Chikhaoui  Ahmed Brahem  Mohamed Moncef Turki  Kevin Mickus  Ramdhane Benassi 《Tectonophysics》2005,406(3-4):255-258

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