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<br />CASE 6 SCOUR AT A8lJ1lIIENTS WHEN a/y.. > 25 <br /> <br />Field data for scour at abutments for various size streams are scarce, but data <br />collected at rock dikes on th. Mississippi indicate the equilibrium scour depth <br />for large a/y.. values can be esti~ted by equation 10: <br /> <br />0.33 <br /> <br />y. = 4 F.... <br /> <br />(11) <br /> <br />Y.. <br /> <br />The data a..e scatte..ed, p..ima..ily because equilibrium depths were not measu..ed. <br />Dunes as la..ge as 20 to 30 feet high move down the Mississippi and associated <br />time fa.. dune movement is ve..y large in cOlParison to time ..equired to form <br />live-bed local scour hol.s. Neve..theless, it is believed that th.se data <br />..ep...sent th. limit in scal. fo.. scou.. depths as compa..ed to labo..atory data <br />and enables useful ext..apolation of laboratory studies to field installations. <br /> <br />Acco..dingly, It is ..ecommended that equations 3 th..ough 10 be applied fa.. <br />abutments with 0 < a/y.. < 25 and equation 11 be used fa.. a/y.. > 25. <br /> <br />CASE 7 ABUTMENTS SKElIED TO llIE STREAM <br /> <br />With skewed c..ossings, the app..oach embankment that is angled downst..eaa has <br />the depth of scou.. ..educed because of the st..eamlining effect. Conve..sely, the <br />app..oach embankment which is angled upstre.. will have a deepe.. scour hole. <br />The calculated scou.. depth should be adjusted In acco..dance with the curve of <br />Flgu..e 3.14. which is patte..ned afte.. Ahmad (1953). <br /> <br />.. 1.4 <br />. <br />.c: <br />.. 1.2 <br />.. <br />01: <br />... 1.0 <br />Ii <br />.1 <br />Xi Il <br />..... .6 <br />0_ <br />-e! .4 U <br />DoO I ~. <br />-II: .2 I <br />.... I <br />0'" /, <br />0.2 0 <br />... 0 45 110 135 110 <br />.. <br />~ of inclinAtion, c#l, de,. <br /> An,le <br /> <br /> <br />FIGURE 4.11. Scou.. estimate adjustment fa.. skew. <br /> <br />38 <br /> <br />, <br /> <br />.. <br />. <br />(. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />