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In-situ geotechnical characterization of mixed-grain-size bedforms using a dynamic penetrometer

机译:使用动态渗透仪对混合颗粒尺寸岩床进行原位岩土表征

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摘要

We tested the ability of a small dynamic penetrometer, Nimrod, to infer geotechnical properties of sediment mixtures in the inner shelf. The penetrometer is light and easy to operate, and its operation by scuba divers ensures a greater degree of precision than ship-based penetrometer deployments. We have studied selected positions along a sorted bedform (~ 100 m wide) on the continental shelf off the Coromandel Peninsula close to Tairua, North Island of New Zealand, and additionally took sediment samples at the exact positions of penetrometer impact, also by scuba divers. The derived dynamic penetrometer signatures (i) measured deceleration of the probe and estimated quasi-static bearing capacity as a measure of sediment strength, (ii) reflected changes in grain-size distribution ranging from very fine to very coarse sands, and (iii) revealed the uppermost seafloor stratification (top layer 2-6 cm) potentially being an indicator for sediment dynamics. In this manner, the device proved to be suitable for spatially fine-scaled surveys using divers' support and might deliver complementary information about sediment dynamics, in this case sorted-bedform maintenance.
机译:我们测试了小型动态渗透仪Nimrod推断内层沉积物混合物的岩土特性的能力。渗透仪重量轻且易于操作,与潜水船用渗透仪相比,潜水员的操作可确保更高的精度。我们已经研究了沿着靠近新西兰北岛泰鲁阿的科罗曼德半岛外陆架上排序的床形体(约100 m宽)上选定的位置,并且还通过潜水员在针入度计撞击的确切位置处采集了沉积物样本。得出的动态渗透仪特征(i)测量了探针的减速度并估计了准静态承载力,作为沉积物强度的量度;(ii)反映了从极细砂到极粗砂的粒度分布变化,以及(iii)揭示了最上层的海底分层(顶层2-6厘米)可能是沉积物动力学的指标。以这种方式,该设备被证明适用于在潜水员的支持下进行空间精细测量的情况,并且可以提供有关沉积物动力学的补充信息,在这种情况下,是分类床维护。

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