ENGINEERING GEOLOGICAL EVALUATION OF YANGLUO YANGTZE BRIDGE, WUHAN
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摘要: 武汉阳逻长江大桥桥址区断层和褶皱发育, 襄樊-广济断裂带位置不清.在初勘阶段, 针对不同的桥型方案, 运用多种勘探手段进行了同等深度的勘察.勘探结果表明, 在勘探深度范围内, 没有发现襄樊-广济断裂从桥址区通过, 仅在K80+530 m和K81+860 m处发现两正断层, 其中F1对三塔斜拉桥桥型方案的中塔影响较大, F2处于南引桥部位, 对大桥的影响较小.从地质条件方面考虑, 阳逻长江大桥选用悬索桥方案比较合适, 如果采用斜拉桥方案, 则中塔位置需要向南移.Abstract: The main engineering problems were represented in the paper: developing faults, fold strata and unclear belt of Xiangfan-Guangji fracture. In elementary period, comprehensive geological methods were applied in the exploration of the bridge site at the same depth for different samples. As a result, no belt of Xiangfan-Guangji fracture was prospected, and only two faults were found at K80+530 m and K81+860 m. The F1 fault of them had a great influence on the three-tower rope scheme, while the F2 fault in the south bridge approach had little. So, the scheme of rope bridge was better if only geological conditions were considered. If the sample of stiff bridge was selected, the middle tower must be moved to the south.
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表 1 不同岩土层参数
Table 1. Parameters of different rocks and strata
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