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: Problem 5: Analyze the frame using the following methods. Use the following values: X = 4 kN .…

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Q: Problem 3: Calculate the vertical displacement of E using virtual work method for the truss shown.…

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Q: Consider the beam shown in Egure 1) Take E-29(10) kxi. I-120 in Figure 100 10A 30 100 1001 Part B…

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Q: A P C Using Double Integration Method, find: a) Equation of the Elastic Curve Slope at point C b) c)…

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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…

Q: → Describe how to use the virtual work principle to find the horizontal displacement at D in the…

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Q: 72

A: l = K-P K = 12I1q12+12I1q22+12m2v22 V2 =l1 sin q1+lc2 sin q2q1 K = 12I1q12+12I1q22+12m2q1l1sin…

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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.