105 research outputs found

    The General Requirements of Work

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    Dynamical models for sand ripples beneath surface waves

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    We introduce order parameter models for describing the dynamics of sand ripple patterns under oscillatory flow. A crucial ingredient of these models is the mass transport between adjacent ripples, which we obtain from detailed numerical simulations for a range of ripple sizes. Using this mass transport function, our models predict the existence of a stable band of wavenumbers limited by secondary instabilities. Small ripples coarsen in our models and this process leads to a sharply selected final wavenumber, in agreement with experimental observations.Comment: 9 pages. Shortened version of previous submissio

    Frequency Response of Stationary Internal Wave Probes

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    Promoter opening (melting) and transcription initiation by RNA polymerase I requires neither nucleotide beta,gamma hydrolysis nor protein phosphorylation.

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    With some bacterial RNA polymerases and in eukaryotic RNA polymerase II, DNA melting during initiation requires the coupling of energy derived from beta,gamma hydrolysis of ATP. A detailed analysis of this possible requirement for eukaryotic RNA polymerase I reveals no such requirement. However, in some cases, beta,gamma non-hydrolyzable derivatives (beta,gamma imido or methylene) of nucleotide substrates have been found to significantly inhibit transcription initiation because of their inefficient use as the first nucleotide of the transcript. In addition, the results presented here show that protein kinase activity is not required as an integral part of transcription initiation by RNA polymerase I. Prior phosphorylation of proteins participating in the process is not ruled out

    Vertical Diffusion in Shallow Waters

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