Compute the area of the given traverse using DPD and DMD method. COURSE LENGTH (m) BEARING AB 495.85 N 05° 30' E ВС 850.62 N 46° 02' E CD 855.45 S 67° 38 E DE 1020.87 S 12° 25 E EF 1117.26 S 83° 44' W FA 660.08 N 55° 09' W

Q: Problem 1 Determine the magnitude and sense of the couple moment. Given: F = 5 kN 0=30° a=0.5m b=4m…

A: Given Data - F = 5 KN a = 0.5 m b = 4 m c = 2 m d = 1 m Find out -  The Couple Moment ?

Q: using trapezoidal rule

A: Given: f(X)=x3+2  a=0 b=5 To find: Integrate f(x) with respect to x=0 to x=5 using Simpson's 1/3rd…

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Q: For the non-symmetric Z-section shown in Figure Q4 find the position of the horizontal (X) and…

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Q: Find the laplace transform of a given periodic functions; a) sawtooth function

A: Sawtooth function x1t=tut-ut-1ft=x1t+x1t-1+x1t-2+x1t-3 ..........taking laplace transform both…

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Q: 2. Derive an equation that describes the vertical deflection of the beam, y(x), and also calculate…

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Q: Establish the equations for slope and deflection by the double integration method. Determine the…

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Q: Find the particular solution for: y' sin(2y) – cosx = 0, x = -when y = 0 %3D

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Q: Parts AB, BD, DF, and FH have A=4.0 s of your calculations in a table so that lass example). B D F

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Q: The maximum deflection for the cantilever-beam below is no more than 0.03m.Macaulay’s method of…

A: Step 1:

Sediment transport

Sediment transport or Soil transport is the movement of solid particles, usually due to the combination of gravitational forces acting on the sediment, and the movement of the liquid at which the sediment enters. Soil erosion occurs in natural systems where the particles are sandstones (sand, rocks), mud, or clay; the liquid is air, water, or ice; and the gravitational force that works to move particles to the landing surface. Sediment transportation or soil migration due to the movement of liquids occurs in rivers, lakes, lakes, oceans, and other bodies of water as a result of currents and waves. Transportation is also caused by glaciers as they flow, and to places on earth under the influence of wind. Soil erosion due to gravity alone is possible in most sloping areas, including hills, scarves, cliffs, and the continental shelf — the continental boundary of the slope.