Runoff and soil loss in biocrusts and physical crusts from the Tabernas Desert (southeast Spain) according to rainfall intensity.

Here, the difference between RC at 60 and 120 mm/h was only marginally significant ( Figure 3A ) when we considered three intensities, but when we plotted four, RC at 120 mm/h was significantly higher than at 60 mm/h and equal to that at 240 mm/h ( Figure 5A ), suggesting that the threshold could be over 77 mm/h and close to 120 mm/h.

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