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Shallow Marine MASW: a Case History and Lessons Learned

机译:浅海洋MASW:案例历史和经验教训

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The concrete spillway associated with a small dam in Rapid City, SouthDakota has evidenced persistent seepage since its construction in the 1970’s. Visualinspection appears to indicate signs of worsening seepage. Geotechnical boringsfrom dam pre-construction as well as modern boring logs taken on either side of thespillway have been consulted; however, budgetary, access, and logistical constraintsrestricted a more in-depth geotechnical boring program. A geophysical investigationwas ordered to better define the subsurface stratigraphy. This data would be used toperform seepage/flow net analysis and determine some remedial solutions to mitigateseepage and extend the life of the structure.Seismic surface wave techniques were employed in a shallow marineenvironment to map depth to bedrock between available boreholes. Hydrophonestreamers with 1m and 3m receiver spacing were used as receiver arrays. MASWand microtremor data were collected using various sources located on both the marine(within the river) and land (adjacent the spillway) sides of the rolling receiver arrays.CMP gathers were constructed using data from four different source-receiver arrayconfigurations. Geotechnical borings were used to constrain the inverse model andverify interpretation of the geophysical data.A traditional means of collecting 2D MASW data utilizes a “walkaway” testto determine a single optimal source-receiver offset per survey profile. We show thatmultiple source-receiver offsets, and receiver-receiver spacings, were necessary togenerate complete surface wave dispersion curves suitable for modeling total depth ofinvestigation. We present challenges observed during the data collection, modelingof the data, and interpretation caused by using this traditionally land-based method ina marine environment.
机译:与南部拉皮德城的一个小水坝相关的混凝土溢洪道 自从1970年代建造以来,达科他州就证明了持续的渗漏。视觉的 检查似乎表明渗流加剧的迹象。岩土钻孔 从大坝的预建以及在两边各取的现代钻孔原木 已咨询溢洪道;但是,预算,访问和后勤方面的限制 限制了更深入的岩土钻孔程序。地球物理调查 被命令更好地定义地下地层。该数据将用于 进行渗流/流网分析并确定一些补救措施以减轻 渗漏并延长结构的使用寿命。 在浅海中采用地震面波技术 在可用钻孔之间将深度映射到基岩的环境。水听器 接收器间距为1m和3m的拖缆用作接收器阵列。马萨诸塞州 和微震数据是使用位于海洋两岸的各种来源收集的 (在河内)和降落(邻近溢洪道)两侧的滚动接收器阵列。 CMP收集是使用来自四个不同源-接收器阵列的数据构建的 配置。岩土工程钻孔用于约束反演模型和 验证对地球物理数据的解释。 收集2D MASW数据的传统方法是利用“走开”测试 确定每个调查资料的单个最佳源接收器偏移量。我们证明 多个源-接收器偏移和接收器-接收器间距对于 生成适合建模总深度的完整的表面波频散曲线 调查。我们提出了在数据收集,建模过程中观察到的挑战 使用这种传统的基于陆地的方法引起的数据和解释 海洋环境。

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