Difference between revisions of "Tutorial M10 005 Results QGIS"

From Tuflow
Jump to navigation Jump to search
 
(2 intermediate revisions by the same user not shown)
Line 8: Line 8:
 
<li>Open the TUFLOW Viewer.
 
<li>Open the TUFLOW Viewer.
 
<li>Select File > Load Results. Navigate to the '''Module_10\TUFLOW\runs''' and open both '''M10_5m_004.tcf''' and '''M10_5m_005.tcf'''.
 
<li>Select File > Load Results. Navigate to the '''Module_10\TUFLOW\runs''' and open both '''M10_5m_004.tcf''' and '''M10_5m_005.tcf'''.
<li>Select the 'Water Level' map output type in the Result Type panel and toggle on 'Maximum'. Inspect the difference in water levels between M10_5m_004 and M10_5m_005:<br>
+
<li>Select the 'Water Level' map output type in the Result Type panel and toggle on 'Maximum'. Inspect the difference in water levels between '''M10_5m_004''' and '''M10_5m_005''':<br>
 
<br>
 
<br>
[[File:Animation M10 005 Results 01.gif]]<br>
+
{{Video|name=Animation_M10_005_Results_01.mp4|width=1230}}<br>
 
<br>
 
<br>
 
<li>Use the Plot Cross Section tool to see the cross section of the water level and bed level at the the edge of the flood extent.  
 
<li>Use the Plot Cross Section tool to see the cross section of the water level and bed level at the the edge of the flood extent.  
<li>Compare the M10_5m_004 and M10_5m_005 results. The curvature of water level in M10_5m_005 demonstrates the Non-Newtonian fluid qualities. The viscosity of the fluid has changed, becoming more solid, due to the shear force as the fluid moves down the catchment:<br>
+
<li>Compare the '''M10_5m_004''' and '''M10_5m_005''' results. The curvature of water level in '''M10_5m_005''' demonstrates the Non-Newtonian fluid qualities. The viscosity of the fluid has changed, becoming more solid, due to the shear force as the fluid moves down the catchment:<br>
 
<br>
 
<br>
[[File:Animation M10 005 Results 02.gif]]<br>
+
{{Video|name=Animation_M10_005_Results_02.mp4|width=1230}}<br>
 
</ol><br>
 
</ol><br>
  

Latest revision as of 11:26, 15 August 2023

Introduction

QGIS is used to view the water using Non-Newtonian fluids. The results are compared to Newtonian fluids from Part 4. For viewing of the 2D map results, see Module 1.

Method

Inspect water levels of the non-Newtownian outputs:

  1. Open the TUFLOW Viewer.
  2. Select File > Load Results. Navigate to the Module_10\TUFLOW\runs and open both M10_5m_004.tcf and M10_5m_005.tcf.
  3. Select the 'Water Level' map output type in the Result Type panel and toggle on 'Maximum'. Inspect the difference in water levels between M10_5m_004 and M10_5m_005:



  4. Use the Plot Cross Section tool to see the cross section of the water level and bed level at the the edge of the flood extent.
  5. Compare the M10_5m_004 and M10_5m_005 results. The curvature of water level in M10_5m_005 demonstrates the Non-Newtonian fluid qualities. The viscosity of the fluid has changed, becoming more solid, due to the shear force as the fluid moves down the catchment:



Conclusion

  • The water level outputs of the Non-Newtonian fluid were inspected and compared to a Newtonian fluid from Part 4.
  • For further functionality, see TUFLOW Viewer.


Up
Go-up.png Back to Module 10 Main Page