unsteady-state conditions
1Stall (flight) — For other uses, see stall. In fluid dynamics, a stall is a reduction in the lift coefficient generated by a foil as angle of attack increases. This occurs when the critical angle of attack of the foil is exceeded. The critical angle of attack is… …
2Veldwezelt-Hezerwater — is a Palaeolithic archaeological site in Belgium. ContextThe successive archaeological excavation campaigns at Veldwezelt Hezerwater, Belgium provide important remains of at least five separate Middle Palaeolithic valley settlements. It is… …
3Viktor Dilman — Viktor Vasilyevich Dilman, also spelled Dil man (Russian: Виктор Васильевич Дильман, born March 11, 1926 in Proskurov (now Khmel’nitskiy), Ukrainian SSR, Soviet Union) is a Russian scientist performing research for USPolyResearch. He is best… …
4POLIAKHOV — RUSSIA (see also List of Individuals) 17.12.1906 Kiev/RU 27.1.1987 Moscow/RU Nikolai Nikolaevich Poliakhov graduated from the Moscow University in 1929 and started there at the Central Aero hydromechanic Institute TsAGI as a scientist. He moved… …
5Continuous stirred-tank reactor — CSTR symbol The continuous stirred tank reactor (CSTR), also known as vat or backmix reactor, is a common ideal reactor type in chemical engineering. A CSTR often refers to a model used to estimate the key unit operation variables when using a… …
6Permeability (earth sciences) — Permeability in the earth sciences (commonly symbolized as κ , or k ) is a measure of the ability of a material (typically, a rock or unconsolidated material) to transmit fluids. It is of great importance in determining the flow characteristics… …
7Navier–Stokes equations — Continuum mechanics …
8Fluid dynamics — Continuum mechanics …
9Bernoulli's principle — This article is about Bernoulli s principle and Bernoulli s equation in fluid dynamics. For Bernoulli s Theorem (probability), see Law of large numbers. For an unrelated topic in ordinary differential equations, see Bernoulli differential… …
10glacier — glaciered, adj. /glay sheuhr/, n. an extended mass of ice formed from snow falling and accumulating over the years and moving very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of… …
