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首页> 外文期刊>Australian Geomechanics >GIS-BASED BACK ANALYSIS OF RIVERBANK INSTABILITY IN-THE LOWER RIVER MURRAY
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GIS-BASED BACK ANALYSIS OF RIVERBANK INSTABILITY IN-THE LOWER RIVER MURRAY

机译:基于GIS的下游河床不稳定逆向分析。

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Over the last 4 years or so, unprecedented low river levels, combined with current loading conditions, have adversely contributed to more than 137 riverbank collapse-related incidents and a long term metastable condition along the Lower River Murray, which have recently been considered as the dominating factors inducing bank collapse. With high resolution aerial photographs and digital elevation models (DEMs), this study has established the riverbank geometry prior to collapse of 26 2-dimensional cross section models. Based on government inventories, the collapsed riverbank sections were identified and vectorized using visual interpretation under ArcGIS. In order to obtain appropriate soil parameters for the study area, 5 back analytical models have been conducted at collapsed riverbank sections adjacent to Long Island Marina, Murray Bridge, South Australia. The slope stability analysis software SVSlope was employed in the back-analysis with soil data obtained from two nearby site investigations. Factors of safety were calculated to examine the potential for riverbank collapse with respect to varying river levels. The results indicate that, when the river levels return to 0 to 0.5 m AHD, a portion of the riverbank is close to collapse, whereas a large proportion of the banks remain quasi stable. A raised and maintained high river level will improve the stability but to a limited extent. Several remedial works may need to be conducted when the river level is about to decrease.
机译:在过去的四年左右的时间里,前所未有的低河水位,加上当前的装载条件,已导致超过137例与河岸倒塌相关的事件和长期处于亚瑞河沿岸的亚稳态条件,最近被认为是造成这种情况的主要原因。导致银行倒闭的主导因素。借助高分辨率的航空照片和数字高程模型(DEM),本研究已经确定了26个二维横截面模型崩溃之前的河岸几何形状。根据政府清单,在ArcGIS下使用可视化解释对塌陷的河岸断面进行识别和矢量化。为了获得适合研究区域的土壤参数,在南澳大利亚州墨累桥长岛码头附近的塌陷河岸段进行了5种反向分析模型。边坡稳定性分析软件SVSlope用于从两个附近现场调查获得的土壤数据的反分析中。计算了安全因素,以检查在变化的河流水位下河岸倒塌的可能性。结果表明,当河流水位恢复到0至0.5 m AHD时,一部分河岸将近崩溃,而大部分河岸则保持准稳定。升高并保持较高的河流水位将在一定程度上改善稳定性。当河流水位即将下降时,可能需要进行数项补救工作。

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