TY - GEN
T1 - Analysis of ground-penetrating radar signal reflected from the water volume influenced by sediment concentration
AU - Wang, Hau Wei
AU - Hong, Jian Hao
AU - Huang, Chin Jer
N1 - Funding Information:
This study is based on work supported by the Ministry of Science and Technology, Taiwan (Grant no. MOST 104-2625-M-492-010-). We thank the MOST for funding this study. (MOST 104-2625-M-492-010-).
Publisher Copyright:
© 2016 Taylor & Francis Group, London.
Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2016
Y1 - 2016
N2 - The feasibility of using a Ground-Penetrating Radar (GPR) to obtain river cross-sections was verified by many researches. In Taiwan, the Sediment Concentration (SC) in rivers is always in the order of several hundred parts per million, which increases to more than 30,000 ppm during rainfall. The water depth calculated using GPR may be influenced by the SC as the radio waves pass through the water volume. In this study, we investigated the effects of SC on the transmittance ability of GPR signals. The clay in the Shihmen reservoir was preliminarily used as the sediment material. The SC ranged from freshwater to 35,759 ppm, and the experiments were conducted at two temperature ranges. The results indicated that the water depth measured using GPR was strongly affected by the SC and the water temperature. We recommend that such data as the chemical properties of the sediment, SC, and water temperature in the field be recorded when measuring the cross-section by using GPR.
AB - The feasibility of using a Ground-Penetrating Radar (GPR) to obtain river cross-sections was verified by many researches. In Taiwan, the Sediment Concentration (SC) in rivers is always in the order of several hundred parts per million, which increases to more than 30,000 ppm during rainfall. The water depth calculated using GPR may be influenced by the SC as the radio waves pass through the water volume. In this study, we investigated the effects of SC on the transmittance ability of GPR signals. The clay in the Shihmen reservoir was preliminarily used as the sediment material. The SC ranged from freshwater to 35,759 ppm, and the experiments were conducted at two temperature ranges. The results indicated that the water depth measured using GPR was strongly affected by the SC and the water temperature. We recommend that such data as the chemical properties of the sediment, SC, and water temperature in the field be recorded when measuring the cross-section by using GPR.
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U2 - 10.1201/9781315644479-57
DO - 10.1201/9781315644479-57
M3 - Conference contribution
AN - SCOPUS:85015312773
SN - 9781138029132
T3 - River Flow - Proceedings of the International Conference on Fluvial Hydraulics, RIVER FLOW 2016
SP - 345
EP - 350
BT - River Flow - Proceedings of the International Conference on Fluvial Hydraulics, RIVER FLOW 2016
A2 - Constantinescu, George
A2 - Garcia, Marcelo
A2 - Hanes, Dan
PB - CRC Press/Balkema
T2 - International Conference on Fluvial Hydraulics, RIVER FLOW 2016
Y2 - 11 July 2016 through 14 July 2016
ER -