جریان ثانویه

در مکانیک سیالات جریان ثانویه جریان نسبتاً جزئی است که بر جریان اولیه قرار می گیرد، وقتی جریان اولیه با الگوهای جریانی که با تکنیک‌های ساده تحلیلی سیال غیرلزج قابل پیش‌بینی است با دقت کافی هم‌خوانی دارد.^[۱]^[۲]

منابع

↑ Bowker, Kent A. (1988). "Albert Einstein and Meandering Rivers". Earth Science History. 1 (1): 45. Bibcode:1988ESHis...7...45B. doi:10.17704/eshi.7.1.yk72n55q84qxu5n6. Retrieved 2016-07-01.
↑ In the absence of secondary flow, bend flow seeks to conserve angular momentum so that it tends to conform to that of a free vortex with high velocity at the smaller radius of the inner bank and lower velocity at the outer bank where radial acceleration is lower. Hickin, Edward J. (2003), "Meandering Channels", in Middleton, Gerard V. (ed.), Encyclopedia of Sediments and Sedimentary Rocks, New York: Springer, p. 432 شابک ‎۱−۴۰۲۰−۰۸۷۲−۴

[Einstein-1] Bowker, Kent A. (1988). "Albert Einstein and Meandering Rivers". Earth Science History. 1 (1): 45. Bibcode:1988ESHis...7...45B. doi:10.17704/eshi.7.1.yk72n55q84qxu5n6. Retrieved 2016-07-01.

[2] In the absence of secondary flow, bend flow seeks to conserve angular momentum so that it tends to conform to that of a free vortex with high velocity at the smaller radius of the inner bank and lower velocity at the outer bank where radial acceleration is lower. Hickin, Edward J. (2003), "Meandering Channels", in Middleton, Gerard V. (ed.), Encyclopedia of Sediments and Sedimentary Rocks, New York: Springer, p. 432 شابک ‎۱−۴۰۲۰−۰۸۷۲−۴

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