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991.
The phenomenon of MHD wave refraction is useful in interpreting the properties of the magnetic fluctuations in certain parcels
of solar wind. In the physics of MHD wave refraction, variations in the Alfvén speed VAlf play a dominant role. Here, we compile statistics of the 1-min averages of VAlf at the location of the ACE spacecraft during its first 5 years of operation. We find that monthly distributions of VAlf are close to log-normal, with standard deviations σV as small as 0.11 in the logarithm. Variations in the monthly mean VAlf are correlated significantly with sunspot number. We also compile monthly distributions of the plasma β parameter. The distributions
of both VAlf and β are significantly narrower than they would be if the various solar wind parameters were statistically independent.
In the Tp–VAlf plane, we find a zone of avoidance at low VAlf: for VAlf ≤10 – 15 km/s, there are no samples in the 1-min data that are cooler than Tp = 10 000 – 15 000 K. This feature can be understood in the context of MHD wave refraction, although other explanations are
also possible. 相似文献
992.
A. D. Petford D. E. Blackwell B. S. Collins P. A. Ibbetson E. A. Mallia G. Smith D. Emerson 《Solar physics》1971,19(1):264-269
Tests of the performance of replicas of the latest echelle gratings are reported. 相似文献
993.
994.
We derive upper limits to the radiation temperaturesT
t(k) for emission near the fundamental and second harmonic of the electron plasma frequency in terms of the effective temperature for plasma wavesT
l(k). We findT
t(k)(c/(3)1/2
V
e)3
T
l(k) for emission near the fundamental which differs from the result of Melrose (1970b) by the factor in parentheses. This factor can exceed 4×104 in some plasmas. The conditions under which this limit could be reached are delinated. For emission near the second harmonicT
t(k)T
l(k) since the absorption coefficient in this case can only be positive.The National Center for Atmospheric Research is sponsored by the National Science Foundation. 相似文献
995.
996.
Solute transport through a porous medium is typically modelled assuming the porous medium is rigid. However, many applications exist where the porous medium is deforming, including, municipal landfill liners, mine tailings dams, and land subsidence. In this paper, mass balance laws are used to derive the flow and transport equations for a deforming porous medium. The equations are derived in both spatial and material co‐ordinate systems. Solute transport through an engineered landfill liner is used as an illustrative example to show the differences between the theory for a rigid porous medium, and small and large deformation analysis of a deforming porous medium. It is found that the large deformation model produces shorter solute breakthrough times, followed by the small deformation model, and then the rigid porous medium model. It is also found that it is important to include spatial and temporal void ratio variations in the large deformation analysis. It is shown that a non‐linear large deformation model may greatly reduce the solute breakthrough time, compared to a standard transport analysis typically employed by environmental engineers. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
997.
998.
This paper sets forth the theoretical background and basic numerical expressions for the incorporation of elastic-plastic constitutive equations for ductile rock into a finite element computer code. The derivation of an expression for the total strain rate is performed both for a total stress formulation and for a formulation that employs the concept of effective stress for inelastic behaviour. Specific expressions for the incremental strain rate are presented for the case of a porous material having a quadratic initial yield surface and observing the associated flow rule with a special hardening law for subsequent plastic deformation. A final section of the paper summarizes the expressions required to insert the quadratic yield surface model into a finite element code. 相似文献
999.
1000.
Christopher Potter Peggy Gross Vanessa Genovese Marie-Louise Smith 《Carbon balance and management》2007,2(1):1-11