Application of short-range photogrammetry for monitoring seepage erosion of riverbank by laboratory experiments

• Published in: Journal of hydrology (Amsterdam) 2018-03, Vol.558, p.380-391
• Main Authors: Masoodi, A., Noorzad, A., Majdzadeh Tabatabai, M.R., Samadi, A.
• Format: Article
• Language: English
• Subjects: Groundwater; Kinect; Monitoring; Riverbank erosion; Seepage; Short-range photogrammetry
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2018.01.051

•Estimation of erosion is of great importance due to negative effects on the river.•Scanning spatiotemporal variations of riverbank erosion to quantify seepage erosion.•Propose an innovative approach to monitor riverbank erosion using Kinect.•Investigation of variation trend of riverbank induced by seepage in laboratory. Temporal and spatial monitoring play a significant role in evaluating and examining the riverbank morphology and its spatiotemporal changes. Unlike the terrestrial laser scanners, other previously used methods such as satellite images, total station surveying, and erosion pins have limited application to quantify the small-scale bank variations due to the lack of rapid survey and resolution in data acquisition. High cost, lack of availability, specialized equipment and hard movement of laser scanners make it necessary to develop new accurate, economical and easily available methods. The present study aims to test the Kinect photogrametric technology for measuring and assessing riverbank variations in laboratory environment. For this purpose, three models of layered soil blocks for three different levels of groundwater (i.e. 24, 34 and 44 cm) were designed to investigate the seepage erosion behavior experimentally. The results indicate the high accuracy of Kinect in measuring the bank erosion cavity dimensions (i.e., 0.5% error) with high spatial resolution data (i.e. 300,000 points per frame). The high speed of Kinect in riverbank scanning enables the analysis of time variations of mechanisms such as seepage erosion which occurs rather rapidly. The results confirmed that there is a power relationship between the seepage gradient and the time of the bank failure with a determination coefficient of 0.97. Moreover, an increase in the level of groundwater on the riverbank increases the rate of undercutting retreat that caused more rapid failure of the riverbank.