By Chia-Shun Yih
Read or Download Stratified flows PDF
Similar physics books
This ebook goals to make extensively obtainable an comprehensible facts of the notorious spin-statistics theorem. This widely recognized yet little-understood theorem is meant to provide an explanation for the truth that electrons obey the Pauli exclusion precept. This truth, in flip, explains the periodic desk of the weather and their chemical homes.
While in 1957 Chen Ning Yang, together with his colleague Tsung Dao Lee, steered that, in layman's phrases, the suitable- and left-handed easy parts of subject behaved otherwise, and while scan proven that the legislation of nature do distinguish among a process and its replicate photograph, our wisdom of basic actual ideas took one of many unexpected turns that have characterised its heritage.
- The Free-Lagrange Method
- Introduction to General Relativity
- Das elegante Universum: Superstrings, verborgene Dimensionen und die Suche nach der Weltformel
- Physics Reports vol.184
- Physics of Amphiphilic Layers: Proceedings of the Workshop, Les Houches, France February 10–19, 1987
Additional resources for Stratified flows
From such work the grooves appear to represent an intermediate stage in the deepening and, under some circumstances, the rounding of an originally wide and uniformly shallow channel (AbdelRahman, 1963; Mosley, 1973; Shepherd and Schumm, 1974), but the nature of the erosion processes, and the role if any of secondary flow in the initiation and growth of the structures, remain undescribed. The fossil record of erosional grooves and ridges in fluviatile sediments is not extensive. B. King’s ( 1927) larger forms.
The furrows between ridges are broad and range from shallow and flatbottomed to deep and rounded. Some furrows are smooth and even along their length, whereas bthers have a coarsely granular appearance. Many furrows are crossed transversely at fairly regular intervals by evenly spaced curved ridges that are concave downcurrent and bound shallow flute-like hollows, the arrangement with the main ridges creating a ladder-like effect. M. Anderson, 1976). (e,g. , 1975) reveal lines of convergence and divergence amongst the ridges which allow them to be divided between linear zones in each of which a similar orientation is maintained.
1-23. Geometry of tidal current ridges (data of Off, 1963). g. D. Caston, 1972). g. Gohren, 1971; Park, 1974). M. Ball, 1967; Houboult, 1968; Park, 1974). Many prove to be wholly constructional features, resting on a level substrate which extends beneath them between exposures on the floors of the adjacent channels. Multiple internal reflectors are commonly evident, dipping in the same direction and at a similar gentle slope to the steeper side of the ridge. Evidently the banks grow or move partly in the same direction as the steeper face.