Sediment modeling using laboratory-scale rainfall simulator and laser precipitation monitor

V G Jadhao; Ashish Pandey; S K Mishra

doi:10.1016/j.envres.2023.116859

Sediment modeling using laboratory-scale rainfall simulator and laser precipitation monitor

Environ Res. 2023 Nov 15;237(Pt 1):116859. doi: 10.1016/j.envres.2023.116859. Epub 2023 Aug 8.

Authors

V G Jadhao¹, Ashish Pandey², S K Mishra³

Affiliations

¹ Department of Water Resources Development and Management, Indian Institute of Technology Roorkee, Roorkee, 247667, Uttarakhand, India. Electronic address: jgunvantrao@wr.iitr.ac.in.
² Department of Water Resources Development and Management, Indian Institute of Technology Roorkee, Roorkee, 247667, Uttarakhand, India. Electronic address: ashish.pandey@wr.iitr.ac.in.
³ Department of Water Resources Development and Management, Indian Institute of Technology Roorkee, Roorkee, 247667, Uttarakhand, India. Electronic address: s.mishra@wr.iitr.ac.in.

PMID: 37562739
DOI: 10.1016/j.envres.2023.116859

Abstract

The characterization of a rainfall simulator provides an excellent opportunity to study the potential of soil erosivity without waiting for natural rain. But, precise instrumentation is required to estimate the parameters, which is seldom available. To overcome this problem, the empirical and conceptual relationships obtained through physically-based modeling help to correlate the rain parameters contributing to soil erosion. The present laboratory study used five pressurized nozzles of different capacities and a Laser Precipitation Monitor (LPM) to generate different rain intensities (21.0-79.0 mm h^-1) and to register drop size distribution, respectively. The sediment transportation induced by rain and runoff was measured with an erosion flume of 2.50 × 1.25 × 0.56 m with an adjustable longitudinal slope. The spatial uniformity, drop size distribution, drop velocity, and kinetic energy were used to evaluate the simulator's performance. The different rain erosivity parameters were correlated and tested statistically using linear and non-linear regression analysis. The rain simulation experiments of different intensities at different pressure ranges were performed on flat, 5, 10, and 15% slopes of the erosion flume to evaluate rain characteristics and record the surface runoff and sediment yield. The median drop sizes produced during the simulator ranged from 0.38 to 2.11 mm, coinciding with natural rain. The empirical relationships were developed to correlate surface discharge and sediment yield with rain intensity by optimizing the parameters for further study of experimental field plots of different slopes. The observed and estimated rain erosivity parameters showed a significant relationship (R² = 0.75 to 0.93; P < 0.001) in multiple regression analysis, and the metrics used to test the developed regression equations showed lower MAE, MSE, and RMSE errors indicating the adequacy of the relationships. The results indicated that the simulator helps to understand the complex task of soil erosion with hydrologic and geomorphic processes in laboratory experimentation with sufficient accuracy in measuring sediment transport events.

Keywords: Drop size distribution; Kinetic energy; Rainfall simulation; Sediment yield model.