Route the following upstream inflow hydrograph through a downstream flood control channel using the Muskingum method. The channel reach has a proportionality coefficient of 1.25 hr and a weighting factor of 0.3 Stop routing after completing the 20-hour time step. Time (hr) 1 2 W|N 3 st 4 5 69 6 7 8 9 10 Inflow (cfs) 90 140 208 320 440 550 640 680 690 630 Time (hr) 11 12 13 14 15 16 17 18 19 20 18 Inflow (cfs) 570 470 390 360 330 250 180 130 100 90

Q: Time (hrs) 0 12 24 36 48 60 72 84 96 108 Inflow Discharge (m3/hr) 20 191 249 164 110 82 62 48 32 28…

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Q: 2) For the watershed in the Figure 1, using mean annual precipitations in Table 1, Table1 Annual…

A: StationsPrecipitation (mm/year)A86B96C126D136E106F96G106H116I126J126K106L116M121N126O136P126

Q: Q2) The hourly rainfall intensity data during a storm are as follows 01 2 3 45 6 7 89 10 Time (hrs)…

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Q: Given the following 30-minute UH for a 1676-acre watershed, use the S-hydrograph method to derive a…

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Q: 086) Ordinates of a 2-hour unit hydrograph are given in the table below. Using these, derive a…

A: Derive 4-hr UH using S-curve method.

Q: Three inches of runoff produced the hydrograph below. Find the unit hydrograph. What value goes in…

A: Using the concept of hydrography, we can write relation as- unit hydrograph at a particular…

Q: 9.3 cm 172 164 10.5 cm 42 12.8 cm 156 10.9 cm 14.2 cm 124 Basin boundary D150 12.2 cm 36 116 14.0 cm…

A: Thiessen polygon method is a common method of weighing the rain gauge observation according to the…

Q: Muskingum parameters of k and x

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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.