Fig. 3
From: Influence of particle size on non-Darcy seepage of water and sediment in fractured rock
![Fig. 3](http://media.springernature.com/full/springer-static/image/art%3A10.1186%2Fs40064-016-3778-9/MediaObjects/40064_2016_3778_Fig3_HTML.gif)
Scatter plot of angle strain rate—shear stress (0.061–0.080 mm)
From: Influence of particle size on non-Darcy seepage of water and sediment in fractured rock
Scatter plot of angle strain rate—shear stress (0.061–0.080 mm)