## Historical and technical survey |

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Page 151

These

) 8 5,280 X 4.92 X d, ' " = °-000OT7 "ST " n = Reading values of ft/ and d\ from

Figure 50 and substituting in the above

in ...

These

**equations**are plotted in Figure 50. From**equation**(63): 4(ft/)- „ nnnn77 (ft i') 8 5,280 X 4.92 X d, ' " = °-000OT7 "ST " n = Reading values of ft/ and d\ from

Figure 50 and substituting in the above

**equations**, curves of n and rfi are plottedin ...

Page 162

n To apply this method the distance of the shoreline, rfi, is substituted in

(81), and the

constant for a particular azimuth and is substituted in

...

n To apply this method the distance of the shoreline, rfi, is substituted in

**equation**(81), and the

**equation**is solved for Ti, the terrain factor. This quantity is aconstant for a particular azimuth and is substituted in

**equation**(86) along with the...

Page 251

while for large z one may use asymptotic expansion we shall study the function of

/mo(2) + [z + Dm<>] Um"(z) = 0 , (32) Un°(z) + [2 + D.°] #.'(*) = 0 . (33) 5t 385 1 ...

while for large z one may use asymptotic expansion we shall study the function of

**equation**(19) F(z) — ^0(z) Umo{z) f (31) /g" where //J<2,(«) -♢ >J— e«" " + '"12> • t/mo(2) + [z + Dm<>] Um"(z) = 0 , (32) Un°(z) + [2 + D.°] #.'(*) = 0 . (33) 5t 385 1 ...

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