paradox$57723$ - traduzione in greco
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paradox$57723$ - traduzione in greco

THE THEOREM THAT, FOR INCOMPRESSIBLE AND INVISCID POTENTIAL FLOW, THE DRAG FORCE IS 0 ON A BODY MOVING WITH CONSTANT VELOCITY RELATIVE TO THE FLUID, IN CONTRADICTION TO REAL LIFE, WHERE VISCOSITY CAUSES SUBSTANTIAL DRAG, ESPECIALLY AT HIGH VELOCITIES
D'Alembert's Paradox; D'Alembert paradox; Hydrodynamic paradox; D'Alembert Paradox; D'Alemberts Paradox; D'Alemberts' Paradox; Dalembert's Paradox; Hydrodynamical paradox; Hydrodynamics paradox; D'alembert's Paradox
  • Jean le Rond d'Alembert (1717-1783)
  • Steady and separated incompressible potential flow around a plate in two dimensions,<ref>Batchelor (2000), p. 499, eq. (6.13.12).</ref> with a constant pressure along the two free streamlines separating from the plate edges.
  • wake]],<br>
•5: post-critical separated flow, with a turbulent boundary layer.
  • Pressure distribution for the flow around a circular cylinder. The dashed blue line is the pressure distribution according to [[potential flow]] theory, resulting in d'Alembert's paradox. The solid blue line is the mean pressure distribution as found in experiments at high [[Reynolds number]]s. The pressure is the radial distance from the cylinder surface; a positive pressure (overpressure) is inside the cylinder, towards the centre, while a negative pressure (underpressure) is drawn outside the cylinder.
  • circular]] cylinder in a uniform onflow.

paradox      
n. παράδοξο, παραδοξολογία
coral reef         
  • isotherms]]. Most corals live within this boundary. Note the cooler waters caused by upwelling on the southwest coast of Africa and off the coast of Peru.
  • Ancient coral reefs
  • Deep-water [[cloud sponge]]
  • bay Islands]] are part of the mesoamerican coral reef system. Due to this, the authorities have made huge investments for its preservation.
  • Barrier reef
  • A major coral bleaching event took place on this part of the [[Great Barrier Reef]] in Australia
  • A diversity of corals}}
  • NOAA]] Ocean Education Service. Retrieved January 9, 2010.</ref>
  • Close up of polyps arrayed on a coral, waving their tentacles. There can be thousands of polyps on a single coral branch.
  • Coral fragments growing on nontoxic concrete
  • polyp]] anatomy
  • The three major zones of a coral reef: the fore reef, reef crest, and the back reef
  • Locations of coral reefs
  • [[Coralline algae]] ''[[Lithothamnion]] sp.''
  • Fringing reef at [[Eilat]] at the southern tip of [[Israel]]
  • Table coral, ''[[Acropora]] sp.''
  • Inhabited [[cay]] in the [[Maldives]]
  • A small [[atoll]] in the [[Maldives]]
  • The colour of corals depends on the combination of brown shades provided by their [[zooxanthellae]] and pigmented proteins (reds, blues, greens, etc.) produced by the corals themselves.
  • url=https://www.theguardian.com/environment/interactive/2009/sep/02/coral-world-interactive}}</ref>
  • [[Eastern oyster]]s (''Crassostrea virginica'')
  • Platform reef
  • Coral polyps}}
  • shoals]], that is, it slows down and the wave height increases.
  • Fringing reef
  • Most coral polyps are nocturnal feeders. Here, in the dark, polyps have extended their tentacles to feed on zooplankton.
  • sessile]] and take root on the ocean floor. But unlike plants, corals do not make their own food.<ref>[https://oceanservice.noaa.gov/facts/coral.html Are corals animals or plants?] ''NOAA:  National Ocean Service''. Accessed 11 February 2020. Updated: 7 January 2020.</ref>
  • This map shows areas of [[upwelling]] in red. Coral reefs are not found in coastal areas where colder and nutrient-rich upwellings occur.
  •  [[Zooxanthellae]], the microscopic algae that lives inside coral, gives it colour and provides it with food through photosynthesis
RIDGE OF ROCK IN THE SEA FORMED BY THE GROWTH AND DEPOSIT OF CORAL
Barrier Reef; Coral reefs; Coral Reef; Fringing Reef; Ribbon reef; Deltaic reef; Barrier reefs; Coral-Reefs; Lagoonal reef; Cresentic reef; Planar reef; Coral reef destruction; Apron reef; Formation of coral reefs; Darwin's paradox; Reef habitat zones; Habili; Coral Reef Ecology; Coral reef ecology; Barrier reef; Platform reef; Table reef; Bank reef; Tropical coral reef
κοραλλιότοπος
green tea         
  • ''[[Sencha]]'' green tea, the most popular form of tea in Japan.
  • Four varieties of green tea prior to brewing
  • ''Gakjeochong'', a [[Goguryeo]] tomb, shows a knight drinking tea with two ladies (5-6th century)
  • C}}
  • Georgia]] to support green tea production.
  • Hand-rolling green tea after steaming
  • Tea leaves: ''[[sejak]]'' (green tea), ''[[ujeon]]'' (green tea), and ''[[hwangcha]]'' (yellow tea) from [[Hadong County]]
UNOXIDIZED TEA
Green-tea; Green teas; Green Tea; 綠茶; 绿茶; 緑茶; Health effects of green tea; The green tea; Asian paradox; Green tea extract; Japanese green teas; Japanese green tea; Japanese tea; Green tea catechins; Green tea polyphenols; Green Tea Polyphenols; Green Tea Polyphenol; Green tea polyphenol; Green tea catechin; Green tea extracts; Japanese Tea; Chinese green tea; Nokcha; Beneficial effects of green tea
πράσινο τσάι

Definizione

liar paradox
<philosophy> A sentence which asserts its own falsity, e.g. "This sentence is false" or "I am lying". These paradoxical assertions are meaningless in the sense that there is nothing in the world which could serve to either support or refute them. Philosophers, of course, have a great deal more to say on the subject. ["The Liar: an Essay on Truth and Circularity", Jon Barwise and John Etchemendy, Oxford University Press (1987). ISBN 0-19-505944-1 (PBK), Library of Congress BC199.P2B37]. (1995-02-22)

Wikipedia

D'Alembert's paradox

In fluid dynamics, d'Alembert's paradox (or the hydrodynamic paradox) is a contradiction reached in 1752 by French mathematician Jean le Rond d'Alembert. D'Alembert proved that – for incompressible and inviscid potential flow – the drag force is zero on a body moving with constant velocity relative to the fluid. Zero drag is in direct contradiction to the observation of substantial drag on bodies moving relative to fluids, such as air and water; especially at high velocities corresponding with high Reynolds numbers. It is a particular example of the reversibility paradox.

D’Alembert, working on a 1749 Prize Problem of the Berlin Academy on flow drag, concluded: "It seems to me that the theory (potential flow), developed in all possible rigor, gives, at least in several cases, a strictly vanishing resistance, a singular paradox which I leave to future Geometers [i.e. mathematicians - the two terms were used interchangeably at that time] to elucidate". A physical paradox indicates flaws in the theory.

Fluid mechanics was thus discredited by engineers from the start, which resulted in an unfortunate split – between the field of hydraulics, observing phenomena which could not be explained, and theoretical fluid mechanics explaining phenomena which could not be observed – in the words of the Chemistry Nobel Laureate Sir Cyril Hinshelwood.

According to scientific consensus, the occurrence of the paradox is due to the neglected effects of viscosity. In conjunction with scientific experiments, there were huge advances in the theory of viscous fluid friction during the 19th century. With respect to the paradox, this culminated in the discovery and description of thin boundary layers by Ludwig Prandtl in 1904. Even at very high Reynolds numbers, the thin boundary layers remain as a result of viscous forces. These viscous forces cause friction drag on streamlined objects, and for bluff bodies the additional result is flow separation and a low-pressure wake behind the object, leading to form drag.

The general view in the fluid mechanics community is that, from a practical point of view, the paradox is solved along the lines suggested by Prandtl. A formal mathematical proof is lacking, and difficult to provide, as in so many other fluid-flow problems involving the Navier–Stokes equations (which are used to describe viscous flow).