U. Harms, U. Raschke, F. Anselmetti, M. Strasser, V. Wittig, M. Wessels, S. Schaller, S. Fabbri, R. Niederreiter, A. Schwalb
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引用次数: 4
摘要
摘要湖泊沉积物记录了过去的环境条件和变化,是古环境和气候研究的重要内容。访问这些档案的一个主要障碍是从深湖中不受干扰地恢复长岩心。在这项研究中,我们开发并测试了一种新的环保取心工具和模块化驳船,其核心是井下液压锤击先进的活塞取心系统,称为Hipercorig。用于评估该系统性能的试验台是两个冰缘湖泊,Mondsee和Constance,位于阿尔卑斯链的北部边缘。众所周知,这些湖泊很难在沉积物深度超过~ 10米的地方取样,因为密集的冰川沉积物阻碍了更深的取样。这两个湖泊与许多全球湖泊系统相似,在深度上具有坚硬和粗糙的层,因此使用这种新技术获得的经验可以应用于其他湖泊甚至海洋盆地。这两个试验钻井项目的取心深度达63米,在水深达204米的地方进行了成功的取心作业,提供了高质量、连续的取心,采收率达到87%。对Mondsee的63米长的岩芯和康斯坦斯湖的两个20米和24米长的岩芯的初步描述和扫描,提供了新的见解,超越了可追溯到~ 18400 cal BP的北阿尔卑斯前陆冰川消退的开始。
Hipercorig – an innovative hydraulic coring system recovering over 60 m long sediment cores from deep perialpine lakes
Abstract. The record of past environmental conditions and changes archived in lacustrine sediments serves as an important element in paleoenvironmental and climate research. A main barrier in accessing these archives is the undisturbed recovery of long cores from deep lakes. In this study, we have developed and tested a new, environmentally friendly coring tool and modular barge, centered around a down-the-hole hydraulic hammering of an advanced piston coring system, called the Hipercorig. Test beds for the evaluation of the performance of the system were two periglacial lakes, Mondsee and Constance, located on the northern edge of the Alpine chain. These lakes are notoriously difficult to sample beyond ∼ 10 m sediment depths due to dense glacial deposits obstructing deeper coring. Both lakes resemble many global lake systems with hard and coarse layers at depth, so the gained experience using this novel technology can be applied to other lacustrine or even marine basins. These two experimental drilling projects resulted in up to 63 m coring depth and successful coring operations in up to 204 m water depth, providing high-quality, continuous cores with 87 % recovery. Initial core description and scanning of the 63 m long core from Mondsee and two 20 and 24 m long cores from Lake Constance provided novel insights beyond the onset of deglaciation of the northern Alpine foreland dating back to ∼ 18 400 cal BP.