Riverway dynamic sediment transport capacity calculation method and system
A technology of sediment transport capacity and calculation method, applied in the field of engineering sediment, can solve the problems of limiting the applicability of research results and insufficient attention to impact
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Embodiment 1
[0117] Take the river dynamic sediment transport capacity of Huayuankou-Gaocun section (referred to as Huagao section) in the lower reaches of the Yellow River as an example:
[0118]Taking the Gaocun hydrological station as the representative station of this section of the river, the water and sediment data of the hydrometric station and the topographical changes of the section of the river were collected. According to the measured flood element data, calculate the corresponding flow rate Q(m 3 / s) under the condition of the measured cross-sectional area and the river width B (m) to calculate the corresponding average water depth h (m) of the representative cross-section, take the flow Q as the abscissa, and take the average water depth h as the ordinate. Fit the power function relation h=αQ representing the average water depth h of the section and the discharge Q β ,See figure 2 , according to the fitting results, α=0.141, β=0.350, namely h=0.141Q 0.350 .
[0119] The a...
Embodiment 2
[0124] Take the dynamic sediment transport capacity of the river channel from Gaocun to Aishan in the lower reaches of the Yellow River (referred to as the Gaoai River) as an example:
[0125] Taking the Aishan hydrological station as the representative station of this section of the river, the water and sediment data of the hydrometric station and the topographical changes of the section of the river were collected. According to the measured flood element data, calculate the corresponding flow rate Q(m 3 / s) under the condition of the measured cross-sectional area and the river width B (m) to calculate the corresponding average water depth h (m) of the representative cross-section, take the flow Q as the abscissa, and take the average water depth h as the ordinate. Fit the power function relation h=αQ representing the average water depth h of the section and the discharge Q β ,See Figure 4 , according to the fitting results, α=0.099, β=0.470, namely h=0.099Q 0.470 .
[0...
Embodiment 3
[0131] Take the dynamic sediment transport capacity of the river channel from Aishan to Lijin in the lower reaches of the Yellow River (referred to as the Aili reach) as an example:
[0132] Taking Lijin Hydrological Station as the representative station of this section of the river, collect the water and sediment data of the hydrometric station and the topographical changes of this section of the river. According to the measured flood element data, calculate the corresponding flow rate Q(m 3 / s) under the condition of the measured cross-sectional area and the river width B (m) to calculate the corresponding average water depth h (m) of the representative cross-section, take the flow Q as the abscissa, and take the average water depth h as the ordinate. Fit the power function relation h=αQ representing the average water depth h of the section and the discharge Q β ,See Figure 6 , according to the fitting results, α=0.135, β=0.413, namely h=0.135Q 0.413 .
[0133] The abov...
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