Characterization of rainfall generated by dripper‐type rainfall simulator using piezoelectric transducers and its impact on splash soil erosion | Zendy

Abd Elbasit Mohamed A. M. | Zendy; Yasuda Hiroshi | Zendy; Salmi Atte | Zendy; Anyoji Hisao | Zendy

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Characterization of rainfall generated by dripper‐type rainfall simulator using piezoelectric transducers and its impact on splash soil erosion

Author(s) -

Abd Elbasit Mohamed A. M.,

Yasuda Hiroshi,

Salmi Atte,

Anyoji Hisao

Publication year - 2010

Publication title -

earth surface processes and landforms

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.294

H-Index - 127

eISSN - 1096-9837

pISSN - 0197-9337

DOI - 10.1002/esp.1935

Subject(s) - splash , environmental science , erosion , intensity (physics) , hydrology (agriculture) , disdrometer , soil science , geology , meteorology , geotechnical engineering , precipitation , geomorphology , physics , quantum mechanics , rain gauge

Rainfall erosivity represents the primary driver for particle detachment in splash soil erosion. Several raindrop erosivity indices have been developed in order to quantify the potential of rainfall to cause soil erosion. Different types of rainfall simulators have been used to relate rainfall characteristics to soil detachment. However, rainfall produced by different rainfall simulators has different characteristics, specifically different relationships between rainfall intensity and rainfall erosivity. For this reason, the effect of rainfall characteristics produced by a dripper‐type rainfall simulator on splash soil erosion ( D s ) has been investigated. The simulated rainfall kinetic energy ( KE ) and drop size distribution ( DSD ) were measured using piezoelectric transducers, modified from the Vaisala RAINCAP ® rain sensor. The soil splash was evaluated under various simulated rainfall intensities ranging from 10 to 100 mm h −1 using the splash‐cup method. The simulated rainfall intensity ( I ) and kinetic energy relationship ( I – KE ) was found to be different from natural rainfall. The simulated rainfall intensity and splash soil erosion relationship ( I – D s ) also followed this same trend. The I – KE relationship was found to follow the natural rainfall trend until the rainfall intensity reached 30 mm h −1 and above this limit the KE started to decrease. This emphasizes the importance of the I – KE relationship in determining the I ‐ D s relationship, which can differ from one rainfall simulator to another. D s was found to be highly correlated with KE ( r = 0·85, P < 0·001), when data produced by the rainfall intensity ranged from 10 to 100 mm h −1 . However, when the threshold rainfall intensity (30 mm h −1 ) was considered, the correlation coefficient further improved ( r = 0·89, P = 0·001). Accordingly, to improve the soil splash estimation of simulated rainfall under various rainfall intensities the I–KE characterization relationship for rainfall simulators has to be taken into account. Copyright © 2010 John Wiley & Sons, Ltd.

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