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CORPS EVALUATION OF FLUID MUD MEASUREMENT AND THE DEFINITION OF NAVIGABLE DEPTH

机译:泥浆测量的企业评估和可导航深度的定义

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摘要

The U.S. Army Engineer Research and Development Center (ERDC) has responsibility under the Innovative Technologies (IT) Focus Area of the Dredging Operation and Environmental Research (DOER) Program to identify and evaluate innovative dredging and dredged material management technologies. An IT work unit, Fluid Mud Measurement and the Definition of Navigable Depth, will identify, demonstrate, and evaluate both established and emerging fluid mud measurement technologies, and also evaluate existing navigable depth definitions and project management practices. Results from these evaluations will be used to improve Corps fluid mud characterization capabilities, develop criteria for defining the limiting depth for safe navigation in areas with fluid mud, and formulate engineering recommendations for potential Corps implementation of a navigable depth policy. Fluid mud can be characterized as suspensions with density gradations that range from slightly greater than that of the overlying water in its upper layers, to that of stiff, dense lower layers. Fluid mud densities can range from 1050 to 1350 g/1, with concentrations ranging from 50 to 500 g/1 or 2-13 percent solids by volume, and consist of silt and clay-sized material with clay minerals and organic material (Teeter 1997). Furthermore, navigable depth is defined as the limiting depth in fluid mud areas at which vessels can navigate freely, without serious loss in speed or maneuverability and without incurring damage to hull or hull appendages (PIANC 1982). No standardized method exists in the Corps to survey fluid mud. The Corps Engineer Manual 1110-2-1003 Hydrographic Surveying (2001) states "when the upper sediment layer is not well consolidated, the three major depth measurement methods used in the Corps (sounding pole, lead line, and acoustic echo sounding) will generally not correlate with one another, or perhaps not even give consistent readings from one time to the next when the same type of instrument or technique is used." This ambiguity in determining depth has hindered Corps-wide optimization of maintenance dredging in fluid mud areas. This paper describes the work unit and results of investigations to date. While various technologies are currently being identified, a preliminary field demonstration of an acoustic characterization system is described to illustrate just one of the types of fluid mud measurement systems that the work unit may ultimately select for detailed evaluation. The SILAS software suite (developed by Sterna Survey Services of The Netherlands) was demonstrated in the Gulfport, Mississippi, navigation channel in 2002. This software samples the unaltered return signal from a low frequency hydrographic survey depth sounder and, with calibration input from an acoustical probe with a known signature, finds the variances present along the signal path and purportedly converts those changes into density and viscosity information using onsite calibration factors.
机译:在疏Dr作业和环境研究(DOER)计划的创新技术(IT)重点领域下,美国陆军工程师研究与开发中心(ERDC)负责识别和评估创新的疏and和疏material材料管理技术。一个IT工作部门,“流体泥浆测量和可导航深度的定义”,将识别,演示和评估已建立和正在出现的流体泥浆测量技术,还将评估现有的可导航深度定义和项目管理实践。这些评估的结果将用于提高兵团的泥浆特征化能力,制定标准来定义在有泥浆的地区安全航行的极限深度,并为工程兵实施可航行深度政策制定工程建议。流体泥浆的特征在于其悬浮液的密度等级范围从其上层的上覆水的密度稍大于上层的坚硬致密的下层。流体泥浆的密度范围为1050至1350 g / 1,浓度范围为50至500 g / 1或按体积计2%的固体,由淤泥和粘土大小的材料以及粘土矿物和有机材料组成(Teeter 1997) )。此外,可航行深度定义为在船上可以自由航行,不会严重损失速度或机动性且不会损坏船体或船体附件的流体泥浆区域中的极限深度(PIANC 1982)。兵团没有标准化的方法来测量流体泥浆。 《兵团工程师手册》 1110-2-1003 Hydrographic Surveying(2001)指出:“当上层沉积层没有很好地固结时,兵团中使用的三种主要深度测量方法(测深杆,引出线和回声测深)通常会当使用相同类型的仪器或技术时,彼此之间没有相互关联,或者甚至一次都无法给出一致的读数。”确定深度的模棱两可阻碍了全军范围内对泥浆区疏maintenance的最佳维护。本文介绍了迄今为止的工作单位和调查结果。尽管目前正在识别各种技术,但已描述了声学表征系统的初步现场演示,以说明工作单位最终可能选择进行详细评估的流体泥浆测量系统中的一种。 SILAS软件套件(由荷兰的Sterna Survey Services开发)于2002年在密西西比州的格尔夫波特的导航通道中进行了演示。该软件对低频水文测深仪的原样返回信号进行采样,并通过声学输入进行校准具有已知特征的探头,可以找到沿信号路径出现的变化,并据称可以使用现场校准因子将这些变化转换​​为密度和粘度信息。

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