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Vortex sheet

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smoothing or regularization parameter in a real fluid. There have been extensive studies on a vortex sheet, most of them by discrete or point vortex approximation, with or without desingularization. Using a point vortex approximation and delta-regularization Krasny (1986) obtained a smooth roll-up of a vortex sheet into a double branched spiral. Since point vortices are inherently chaotic, a Fourier filter is necessary to control the growth of round-off errors. Continuous approximation of a vortex sheet by vortex panels with arc wise diffusion of circulation density also shows that the sheet rolls-up into a double branched spiral.
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The vortex sheet solution as given by the Birkoff-Rott equation cannot go beyond the critical time. The spontaneous loss of analyticity in a vortex sheet is a consequence of mathematical modeling since a real fluid with viscosity, however small, will never develop singularity. Viscosity acts a
1017: 1754:. That is, higher the wavenumber of a Fourier mode, the faster it grows. However, a linear theory cannot be extended much beyond the initial state. If nonlinear interactions are taken into account, asymptotic analysis suggests that for large 889:
This nonlinear integro-differential equation is called the Birkoff-Rott equation. It describes the evolution of the vortex sheet given initial conditions. Greater details on vortex sheets can be found in the textbook by Saffman (1977).
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A flat vortex sheet with periodic boundaries in the streamwise direction can be used to model a temporal free shear layer at high Reynolds number. Let us assume that the interval between the periodic boundaries is of length
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In many engineering and physical applications the growth of a temporal free shear layer is of interest. The thickness of a free shear layer is usually measured by momentum thickness, which is defined as
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As a consequence of Kelvin's circulation theorem, in the absence of external forces on the sheet, the circulation between any two material points in the sheet remains conserved, so
1630: 221: 930: 1805: 737: 677: 416: 389:{\displaystyle {\frac {\partial z^{*}}{\partial t}}=-{\frac {\imath }{2\pi }}\int \limits _{-\infty }^{\infty }{\frac {\gamma (s',t)\mathrm {d} s'}{z(s,t)-z(s',t)}}} 126: 91: 1859: 1832: 1732: 1289: 1046: 922: 606:{\displaystyle \Gamma (s,t)=\int \limits _{0}^{s}\gamma (s',t)\mathrm {d} s'\qquad \mathrm {and} \qquad {\frac {\mathrm {d} \Gamma }{\mathrm {d} s}}=\gamma (s,t)} 462: 2096: 1980:{\displaystyle \theta =\int \limits _{y=-\infty }^{\infty }\left({\frac {1}{4}}-\left({\frac {\left\langle u\right\rangle }{2U}}\right)^{2}\right)\mathrm {d} y} 1772: 1752: 1431: 1313: 717: 697: 436: 186: 166: 146: 880:{\displaystyle {\frac {\partial z^{*}}{\partial t}}=-{\frac {\imath }{2\pi }}\int \limits _{-\infty }^{\infty }{\frac {d\Gamma '}{z(\Gamma ,t)-z(\Gamma ',t)}}} 1861:
decays exponentially. The vortex sheet solution is expected to lose analyticity at the critical time. See Moore (1979), and Meiron, Baker and Orszag (1983).
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Note that the integral in the above equation is a Cauchy principal value integral. The initial condition for a flat vortex sheet with constant strength is
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Drazin, P. G., & Riley, N. (2006). The Navier-Stokes equations: a classification of flows and exact solutions (No. 334). Cambridge University Press.
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denote the strength of the sheet, that is, the jump in the tangential discontinuity. Then the velocity field induced by the sheet is
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is the freestream velocity. Momentum thickness has the dimension of length and the non-dimensional momentum thickness is given by
1632:. The flat vortex sheet is an equilibrium solution. However, it is unstable to infinitesimal periodic disturbances of the form 1587:
Continuous vortex sheet approximation by panel method. Roll-up of a vortex sheet due to an initial sinusoidal perturbation.
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component of the flow velocity is continuous. The discontinuity in the tangential velocity means the flow has infinite
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Once a vortex sheet, it will diffuse due to viscous action. Consider a planar unidirectional flow at
1012:{\displaystyle u={\begin{cases}+U,&{\text{for }}y>0\\-U,&{\text{for }}y<0\end{cases}}} 945: 1292: 25: 191: 58:
The formulation of the vortex sheet equation of motion is given in terms of a complex coordinate
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The integral in the above equation is a Cauchy principal value integral. We now define
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as the integrated sheet strength or circulation between a point with arc length
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components of the flow velocity are discontinuous across the vortex sheet, the
2142:. Momentum thickness can be used to measure the thickness of a vortex layer. 1396:{\displaystyle \omega _{z}=-{\frac {U}{\sqrt {\pi \nu t}}}e^{-y^{2}/4\nu t}} 41: 1583: 33: 51:, vortex sheets tend to be unstable. In particular, they may exhibit 32:, such as in slippage of one layer of fluid over another. While the 659:. The equation of motion of the sheet can be rewritten in terms of 1582: 1261:{\displaystyle u(y,t)={\frac {U}{2{\sqrt {\pi \nu t}}}}\left.} 1433:. Then the equation of motion of the vortex sheet reduces to 1005: 2176:
McGraw-Hill Dictionary of Scientific and Technical Terms
1048:. The velocity discontinuity smooths out according to 2104: 2084: 1995: 1877: 1840: 1813: 1780: 1760: 1740: 1713: 1638: 1597: 1441: 1419: 1324: 1301: 1277: 1057: 1028: 933: 904: 747: 725: 705: 685: 665: 621: 472: 444: 424: 404: 231: 194: 174: 154: 134: 99: 64: 1707:. Linear theory shows that the Fourier coefficient 652:{\displaystyle \mathrm {d} \Gamma /\mathrm {d} t=0} 2134: 2090: 2070: 1979: 1853: 1826: 1799: 1766: 1746: 1726: 1699: 1624: 1573: 1425: 1395: 1307: 1295:. The only non-zero vorticity component is in the 1283: 1260: 1040: 1011: 916: 879: 731: 711: 691: 671: 651: 605: 456: 430: 410: 388: 215: 180: 160: 140: 120: 85: 1734:grows exponentially at a rate proportional to 1834:is a critical value, the Fourier coefficient 8: 93:. The sheet is described parametrically by 1559: 1022:impling the presence of a vortex sheet at 2124: 2109: 2103: 2083: 2029: 2024: 2010: 1994: 1969: 1958: 1931: 1913: 1902: 1888: 1876: 1845: 1839: 1818: 1812: 1791: 1779: 1759: 1739: 1718: 1712: 1679: 1674: 1667: 1657: 1643: 1637: 1596: 1494: 1489: 1475: 1452: 1442: 1440: 1418: 1377: 1371: 1363: 1341: 1329: 1323: 1300: 1276: 1242: 1226: 1220: 1200: 1190: 1185: 1170: 1154: 1148: 1128: 1118: 1113: 1088: 1079: 1056: 1027: 988: 959: 940: 932: 903: 814: 808: 800: 781: 758: 748: 746: 724: 704: 684: 664: 635: 630: 622: 620: 571: 561: 558: 546: 532: 503: 498: 471: 443: 423: 403: 324: 298: 292: 284: 265: 242: 232: 230: 193: 173: 153: 133: 98: 63: 699:by a change of variable. The parameter 2168: 2135:{\displaystyle \theta _{ND}=\theta /L} 24:for a surface across which there is a 1408:Vortex sheet with periodic boundaries 148:is the arclength between coordinate 7: 1625:{\displaystyle z(\Gamma ,0)=\Gamma } 438:and the reference material point 1970: 1903: 1898: 1692: 1675: 1658: 1653: 1619: 1604: 1564: 1540: 1518: 1460: 1445: 1243: 1191: 1171: 1119: 858: 836: 821: 809: 804: 766: 751: 726: 666: 636: 627: 623: 572: 566: 562: 553: 550: 547: 533: 473: 405: 325: 293: 288: 250: 235: 14: 557: 545: 2059: 2041: 1613: 1601: 1556: 1553: 1536: 1527: 1515: 1509: 1217: 1204: 1145: 1132: 1073: 1061: 871: 854: 845: 833: 600: 588: 529: 512: 488: 476: 380: 363: 354: 342: 321: 304: 210: 198: 115: 103: 1: 216:{\displaystyle \gamma (s,t)} 168:and a reference point, and 53:Kelvin–Helmholtz instability 2209:Fluid dynamic instabilities 894:Diffusion of a vortex sheet 2225: 1800:{\displaystyle t<t_{c}} 732:{\displaystyle \Gamma } 672:{\displaystyle \Gamma } 411:{\displaystyle \Gamma } 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1041:{\displaystyle y=0} 917:{\displaystyle t=0} 457:{\displaystyle s=0} 44:on a vortex sheet. 2132: 2088: 2068: 2020: 1977: 1851: 1824: 1797: 1764: 1744: 1724: 1697: 1622: 1589: 1571: 1423: 1393: 1305: 1281: 1258: 1181: 1109: 1038: 1009: 1004: 914: 877: 729: 709: 689: 669: 649: 603: 454: 428: 408: 386: 213: 178: 158: 138: 118: 83: 20:is a term used in 2091:{\displaystyle U} 2037: 2018: 1952: 1921: 1767:{\displaystyle k} 1747:{\displaystyle k} 1483: 1467: 1426:{\displaystyle 1} 1357: 1356: 1308:{\displaystyle z} 1102: 1099: 991: 962: 875: 794: 773: 712:{\displaystyle s} 692:{\displaystyle t} 580: 431:{\displaystyle s} 384: 278: 257: 181:{\displaystyle t} 161:{\displaystyle z} 141:{\displaystyle s} 2216: 2188: 2185: 2179: 2173: 2141: 2139: 2138: 2133: 2128: 2117: 2116: 2097: 2095: 2094: 2089: 2077: 2075: 2074: 2069: 2035: 2033: 2028: 2019: 2011: 2006: 1986: 1984: 1983: 1978: 1973: 1968: 1964: 1963: 1962: 1957: 1953: 1951: 1943: 1932: 1922: 1914: 1906: 1901: 1860: 1858: 1857: 1852: 1850: 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742: 721: 720: 719:is replaced by 701: 700: 681: 680: 661: 660: 617: 616: 570: 560: 537: 515: 468: 467: 440: 439: 420: 419: 400: 399: 366: 338: 329: 307: 300: 270: 249: 238: 234: 227: 226: 190: 189: 170: 169: 150: 149: 130: 129: 95: 94: 60: 59: 22:fluid mechanics 12: 11: 5: 2222: 2220: 2212: 2211: 2206: 2204:Fluid dynamics 2196: 2195: 2190: 2189: 2180: 2167: 2166: 2164: 2161: 2160: 2159: 2154: 2147: 2144: 2131: 2127: 2123: 2120: 2115: 2112: 2108: 2087: 2067: 2064: 2061: 2058: 2055: 2052: 2049: 2046: 2043: 2040: 2032: 2027: 2023: 2017: 2014: 2009: 2005: 2002: 1999: 1976: 1972: 1967: 1961: 1956: 1950: 1947: 1942: 1939: 1936: 1930: 1925: 1920: 1917: 1911: 1905: 1900: 1897: 1894: 1891: 1887: 1883: 1880: 1848: 1844: 1821: 1817: 1794: 1790: 1786: 1783: 1763: 1743: 1721: 1717: 1694: 1691: 1688: 1685: 1682: 1677: 1670: 1666: 1660: 1655: 1652: 1649: 1646: 1642: 1621: 1618: 1615: 1612: 1609: 1606: 1603: 1600: 1569: 1566: 1562: 1558: 1555: 1552: 1549: 1545: 1542: 1538: 1535: 1532: 1529: 1526: 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564: 555: 552: 549: 543: 540: 535: 531: 528: 525: 521: 518: 514: 511: 506: 501: 497: 493: 490: 487: 484: 481: 478: 475: 464:in the sheet. 453: 450: 447: 427: 407: 382: 379: 376: 372: 369: 365: 362: 359: 356: 353: 350: 347: 344: 341: 335: 332: 327: 323: 320: 317: 313: 310: 306: 303: 295: 290: 287: 283: 276: 273: 269: 264: 261: 255: 252: 245: 241: 237: 212: 209: 206: 203: 200: 197: 177: 157: 137: 117: 114: 111: 108: 105: 102: 82: 79: 76: 73: 70: 67: 30:fluid velocity 13: 10: 9: 6: 4: 3: 2: 2221: 2210: 2207: 2205: 2202: 2201: 2199: 2184: 2181: 2177: 2172: 2169: 2162: 2158: 2155: 2153: 2150: 2149: 2145: 2143: 2129: 2125: 2121: 2118: 2113: 2110: 2106: 2085: 2065: 2062: 2056: 2053: 2050: 2047: 2044: 2038: 2030: 2025: 2021: 2015: 2012: 2007: 2003: 2000: 1997: 1987: 1974: 1965: 1959: 1954: 1948: 1945: 1940: 1937: 1934: 1928: 1923: 1918: 1915: 1909: 1895: 1892: 1889: 1885: 1881: 1878: 1870: 1866: 1862: 1846: 1842: 1819: 1815: 1792: 1788: 1784: 1781: 1761: 1741: 1719: 1715: 1689: 1686: 1683: 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Let 175: 155: 135: 112: 109: 106: 100: 80: 77: 74: 71: 68: 65: 56: 54: 50: 45: 43: 39: 35: 31: 27: 26:discontinuity 23: 19: 2183: 2171: 1988: 1871: 1867: 1863: 1774:and finite 1590: 1435: 1411: 1270: 1021: 897: 888: 741: 614: 466: 397: 225: 57: 46: 18:vortex sheet 17: 15: 2152:Vortex ring 739:. That is, 2198:Categories 2163:References 34:tangential 2122:θ 2107:θ 2022:∫ 1924:− 1904:∞ 1899:∞ 1896:− 1886:∫ 1879:θ 1693:Γ 1687:π 1681:ı 1659:∞ 1654:∞ 1651:− 1641:∑ 1620:Γ 1605:Γ 1565:Γ 1541:Γ 1531:− 1519:Γ 1507:π 1504:⁡ 1487:∫ 1478:ı 1473:− 1461:∂ 1454:∗ 1446:∂ 1386:ν 1365:− 1351:ν 1348:π 1339:− 1327:ω 1279:ν 1235:ν 1202:− 1192:∞ 1183:∫ 1179:− 1163:ν 1139:− 1130:− 1120:∞ 1111:∫ 1094:ν 1091:π 990:for  978:− 961:for  859:Γ 849:− 837:Γ 822:Γ 810:∞ 805:∞ 802:− 798:∫ 791:π 784:ı 779:− 767:∂ 760:∗ 752:∂ 727:Γ 667:Γ 628:Γ 586:γ 567:Γ 510:γ 496:∫ 474:Γ 406:Γ 358:− 302:γ 294:∞ 289:∞ 286:− 282:∫ 275:π 268:ı 263:− 251:∂ 244:∗ 236:∂ 196:γ 42:vorticity 2146:See also 2004:⟩ 1998:⟨ 1941:⟩ 1935:⟨ 1807:, where 1568:′ 1544:′ 862:′ 825:′ 542:′ 520:′ 371:′ 334:′ 312:′ 47:At high 1291:is the 128:where 2036:  1989:where 1271:where 38:normal 2078:and 1785:< 997:< 968:> 679:and 1501:cot 28:in 2200:: 924:, 55:. 16:A 2130:L 2126:/ 2119:= 2114:D 2111:N 2086:U 2066:x 2063:d 2060:) 2057:t 2054:, 2051:y 2048:, 2045:x 2042:( 2039:u 2031:L 2026:0 2016:L 2013:1 2008:= 2001:u 1975:y 1971:d 1966:) 1960:2 1955:) 1949:U 1946:2 1938:u 1929:( 1919:4 1916:1 1910:( 1893:= 1890:y 1882:= 1847:k 1843:A 1820:c 1816:t 1793:c 1789:t 1782:t 1762:k 1742:k 1720:k 1716:A 1690:k 1684:2 1676:e 1669:k 1665:A 1648:= 1645:k 1617:= 1614:) 1611:0 1608:, 1602:( 1599:z 1561:d 1557:) 1554:) 1551:t 1548:, 1537:( 1534:z 1528:) 1525:t 1522:, 1516:( 1513:z 1510:( 1496:1 1491:0 1481:2 1470:= 1464:t 1450:z 1421:1 1403:. 1389:t 1383:4 1379:/ 1373:2 1369:y 1361:e 1354:t 1344:U 1336:= 1331:z 1303:z 1256:. 1252:] 1248:s 1244:d 1238:t 1232:4 1228:/ 1222:2 1218:) 1214:y 1211:+ 1208:s 1205:( 1198:e 1187:0 1176:s 1172:d 1166:t 1160:4 1156:/ 1150:2 1146:) 1142:y 1136:s 1133:( 1126:e 1115:0 1106:[ 1097:t 1086:2 1082:U 1077:= 1074:) 1071:t 1068:, 1065:y 1062:( 1059:u 1036:0 1033:= 1030:y 1000:0 994:y 984:, 981:U 971:0 965:y 955:, 952:U 949:+ 943:{ 938:= 935:u 912:0 909:= 906:t 872:) 869:t 866:, 855:( 852:z 846:) 843:t 840:, 834:( 831:z 818:d 788:2 776:= 770:t 756:z 707:s 687:t 647:0 644:= 641:t 637:d 632:/ 624:d 601:) 598:t 595:, 592:s 589:( 583:= 577:s 573:d 563:d 554:d 551:n 548:a 539:s 534:d 530:) 527:t 524:, 517:s 513:( 505:s 500:0 492:= 489:) 486:t 483:, 480:s 477:( 452:0 449:= 446:s 426:s 381:) 378:t 375:, 368:s 364:( 361:z 355:) 352:t 349:, 346:s 343:( 340:z 331:s 326:d 322:) 319:t 316:, 309:s 305:( 272:2 260:= 254:t 240:z 211:) 208:t 205:, 202:s 199:( 176:t 156:z 136:s 116:) 113:t 110:, 107:s 104:( 101:z 81:y 78:i 75:+ 72:x 69:= 66:z

Index

fluid mechanics
discontinuity
fluid velocity
tangential
normal
vorticity
Reynolds numbers
Kelvin–Helmholtz instability
kinematic viscosity

Vortex ring
Burgers vortex sheet
McGraw-Hill Dictionary of Scientific and Technical Terms
Categories
Fluid dynamics
Fluid dynamic instabilities

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