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Undisturbed Strata Succession Sampling Technology and the Engineering Geological Characteristics of an Atoll in the Southern South China Sea

机译:南海南部环礁未受干扰地层演替采样技术与工程地质特征

摘要

Coral reef calcareous sediment, a special category of rock-soil material, has representative geological structure and environmental characteristics. It is widely distributed in shallow areas of the tropical ocean; therefore the exploration instruments and technologies for engineering geology studies of coral reef calcareous sediments are very different from those used in land or deep-sea. Obtaining undisturbed cores from the Holocene unconsolidated stratum of coral reefs has been a key problem in the field of marine geology and environment surveying. The authors have designed a novel floating drilling platform equipped with a drilling machine, and successfully achieved undisturbed cores from both reef flats (with water depth 0.5 to 2m) and a enclosed lagoon (with water depth 2-12m) of Yongshu Reef (9 degrees 32-9 degrees 42N, 112 degrees 52-113 degrees 04E), southern South China Sea. Based on the detailed observation on the cores and the analysis from engineering geology, Yongshu Reef was split into reef three engineering geological zones: leading edge, reef flat (including outer reef flat, middle reef flat and inner reef flat) and lagoon. The sediments are classified in the stratum as fine sand, medium sand, coarse sand, gravel and weak-cemented reef limestone.
机译:珊瑚钙质沉积物是岩土材料的特殊类别,具有代表性的地质结构和环境特征。它广泛分布在热带海洋的浅海地区。因此,用于珊瑚礁钙质沉积物的工程地质研究的勘探仪器和技术与陆地或深海所用的勘探仪器和技术有很大不同。从全新世未固结的珊瑚礁中获取未扰动的岩心一直是海洋地质和环境调查领域的关键问题。作者设计了一种配备钻床的新型浮式钻井平台,并成功地从永树礁(9度)的礁滩(水深0.5至2m)和封闭泻湖(水深2-12m)中获得了不受干扰的岩心。南海南部32-9度42N,112度52-113度04E)。通过对岩心的详细观测和工程地质分析,将永树礁分为前缘,礁滩(包括外礁滩,中礁滩和内礁滩)和泻湖三个工程地质区。地层中的沉积物分为细砂,中砂,粗砂,砾石和弱水泥礁石灰石。

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