Figures & data
Figure 1. Homogeneous fluid, vertical jet. Notation and control volume for momentum balance: (a) just after the impact, (b) jet completely formed
![Figure 1. Homogeneous fluid, vertical jet. Notation and control volume for momentum balance: (a) just after the impact, (b) jet completely formed](/cms/asset/0b471515-cca0-4d9f-bd70-681a9d5b89fd/tjhr_a_1579113_f0001_oc.jpg)
Figure 2. Experimental apparatus: (a) diagram of the experimental apparatus, (b) disposition layout of the five pressure transducers on the vertical wall, lengths in centimetres
![Figure 2. Experimental apparatus: (a) diagram of the experimental apparatus, (b) disposition layout of the five pressure transducers on the vertical wall, lengths in centimetres](/cms/asset/305abb92-cd41-47e0-8109-c5c32d7a5e32/tjhr_a_1579113_f0002_ob.jpg)
Figure 4. Sketch of the integration of the pressures. Mixture of water and sediments: C=0.4, , Test M-10
![Figure 4. Sketch of the integration of the pressures. Mixture of water and sediments: C=0.4, F=4.64, Test M-10](/cms/asset/f430939d-732c-4a0e-91fc-711685ca8aeb/tjhr_a_1579113_f0004_oc.jpg)
Figure 5. Example of a pressure and impact force evolution in time. Clear water: , Test W1-53; (a) pressures evolution in time at the five pressure transducers located at different heights along the wall, (b) evolution in time of the impact force, as measured directly by the load cell and indirectly by integrating the pressure transducer measurements
![Figure 5. Example of a pressure and impact force evolution in time. Clear water: F=7.61, Test W1-53; (a) pressures evolution in time at the five pressure transducers located at different heights along the wall, (b) evolution in time of the impact force, as measured directly by the load cell and indirectly by integrating the pressure transducer measurements](/cms/asset/a8b79691-af5f-45b0-9548-93c9e9b4ad4c/tjhr_a_1579113_f0005_oc.jpg)
Figure 6. Dimensionless maximum impact force as a function of the Froude number for clear water and mixture of water and sediments. Comparison between experimental data and as calculated using momentum balance (Eq. Equation6): (a) clear water, (b) water and sediments for different values of solid concentration
![Figure 6. Dimensionless maximum impact force as a function of the Froude number for clear water and mixture of water and sediments. Comparison between experimental data and as calculated using momentum balance (Eq. Equation6S~=12(gρmhi2cosα)+ρmui2hi12(gρmhi2cosα)=1+2Fi2cosα): (a) clear water, (b) water and sediments for different values of solid concentration](/cms/asset/465689b2-3ba2-49eb-89e2-1b8ab65411d6/tjhr_a_1579113_f0006_oc.jpg)
Figure 7. Dimensionless versus Froude number for clear water and mixture of water and sediments. Energy balance solution (Eq. Equation16
) against experimental data: (a) clear water, (b) water and sediments
![Figure 7. Dimensionless (hg)max versus Froude number for clear water and mixture of water and sediments. Energy balance solution (Eq. Equation16(hg)maxhi=1+12cosαFi2) against experimental data: (a) clear water, (b) water and sediments](/cms/asset/eed08cda-b6f8-419b-9676-05a617dc2b0b/tjhr_a_1579113_f0007_oc.jpg)
Figure 10. Jet curvature effect: pressure distribution along the vertical wall. Mixture of water and sediment: , C=0.4, Test M-10: (a) intrinsic coordinates system, (b) flow curvature of the jet
![Figure 10. Jet curvature effect: pressure distribution along the vertical wall. Mixture of water and sediment: F=4.64, C=0.4, Test M-10: (a) intrinsic coordinates system, (b) flow curvature of the jet](/cms/asset/5bb3fb59-ee89-4a35-b799-276ad8750887/tjhr_a_1579113_f0010_oc.jpg)
Figure 11. Clear water: comparison between experimental data and the momentum balance calculated for a reflected wave (Eq. Equation4) and for a vertical jet scheme (Eq. Equation6
)
![Figure 11. Clear water: comparison between experimental data and the momentum balance calculated for a reflected wave (Eq. Equation4S~=S12ρmghi2cosα=1+1.51Ficosα1.25/3) and for a vertical jet scheme (Eq. Equation6S~=12(gρmhi2cosα)+ρmui2hi12(gρmhi2cosα)=1+2Fi2cosα)](/cms/asset/cf5d1a70-bc47-43c5-a2c4-9de47ac5dac2/tjhr_a_1579113_f0011_oc.jpg)