Chemical kinetic performance losses for a hydrogen laser thermal thruster

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/77288/1/AIAA-25927-132.pd

Resonant dipole-dipole interaction in the presence of dispersing and absorbing surroundings

Within the framework of quantization of the macroscopic electromagnetic field, equations of motion and an effective Hamiltonian for treating both the resonant dipole-dipole interaction between two-level atoms and the resonant atom-field interaction are derived, which can suitably be used for studying the influence of arbitrary dispersing and absorbing material surroundings on these interactions. The theory is applied to the study of the transient behavior of two atoms that initially share a single excitation, with special emphasis on the role of the two competing processes of virtual and real photon exchange in the energy transfer between the atoms. In particular, it is shown that for weak atom-field interaction there is a time window, where the energy transfer follows a rate regime of the type obtained by ordinary second-order perturbation theory. Finally, the resonant dipole-dipole interaction is shown to give rise to a doublet spectrum of the emitted light for weak atom-field interaction and a triplet spectrum for strong atom-field interaction.Comment: 15 pages, 1 figure, RevTE

General Overview of Black Hole Accretion Theory

I provide a broad overview of the basic theoretical paradigms of black hole accretion flows. Models that make contact with observations continue to be mostly based on the four decade old alpha stress prescription of Shakura & Sunyaev (1973), and I discuss the properties of both radiatively efficient and inefficient models, including their local properties, their expected stability to secular perturbations, and how they might be tied together in global flow geometries. The alpha stress is a prescription for turbulence, for which the only existing plausible candidate is that which develops from the magnetorotational instability (MRI). I therefore also review what is currently known about the local properties of such turbulence, and the physical issues that have been elucidated and that remain uncertain that are relevant for the various alpha-based black hole accretion flow models.Comment: To be published in Space Science Reviews and as hard cover in the Space Sciences Series of ISSI: The Physics of Accretion on to Black Holes (Springer Publisher

Relações do parâmetro S para algumas propriedades físicas de solos do sul do Brasil Relationships of the S parameter of some physical properties of soils of southern Brazil

O parâmetro S representa o valor da inclinação da curva de retenção de água no seu ponto de inflexão. Um aumento nos valores de S indica uma ampla distribuição de tamanho de poros, condizente com condições estruturais que estabelecem um adequado funcionamento físico do solo. Neste trabalho, testou-se a sensibilidade do parâmetro S, proposto na literatura, em relação a algumas propriedades físicas de solos do Sul do Brasil. O parâmetro S não se relacionou com o teor de argila total, nem com o teor de argila dispersa dos sete solos utilizados neste trabalho. Para o grupamento dos solos argilosos e muito argilosos, o parâmetro S apresentou decréscimo exponencial com o aumento da densidade do solo e um crescimento exponencial com o aumento da matéria orgânica do solo. Nesses solos, a água disponível às plantas aumentou de forma linear (ADP= 3,19*S) passando pela origem e a pressão de pré-consolidação reduziu exponencialmente com o aumento do valor de S. Conclui-se que o parâmetro S apresentou sensibilidade para determinar a qualidade física dos solos de textura argilosa e muito argilosa.<br>The S index corresponds to the slope of the soil water retention curve at its inflection point. A high S value indicates the presence of structural pores, which are essential for a good soil physical condition. The objective of this study was to evaluate the sensitivity of the index of soil physical quality (S), as proposed in the literature for some physical properties of soils from Southern Brazil. In the seven soils used here, no relationship was found between clay and water dispersible clay content with soil physical quality index S. However, in soils with high clay content, the S index decreases with an increase in soil bulk density and increases with an increase in soil organic matter content. For a given texture class, plant available water increased linearly (PAW= 3.19*S) to the origin and the preconsolidation pressure decreased exponentially with the increasing S index. The S index is sensitive to be used as an index of soil physical quality for soils with a high clay content