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Ground Penetrating Radar for Detecting Underground Pipe Buried in Different Type Materials

机译:用于探测埋在不同类型材料中的地下管道的探地雷达

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Ground Penetrating Radar (GPR) propagate electromagnetic (EM) wave that reacts to electromagnetic properties changes across the subsurface materials, for example, sand, granite, concrete, beach sand, clay, plastic material, etc., use to profile underground material. Before GPR invented, engineers, rely on the excavation process to determine what lies beneath the ground surface. Excavation is an expensive and time-consuming endeavour, but it does not always detect every object underground. GPR, by comparison, is faster, more accurate, and less costly than enable to penetrate most materials with few exceptions. This study meant to evaluate whether different types of material underneath, can cause an impact on the image display of the underground profile for human interpretation. GPR with a central frequency of 250 MHz - used to capture the image of pipes buried in six samples of different soil types and one of it is a ready mix concrete. There are two metals and two plastic pipes running through the material at the depth 0.5m and 1m respectively were buried on site. A few pieces of plywood used as the separator between them. Each GPR data, of pipes buried in six different soil material displayed as a two-dimensional array of value called radargram. The array with a specific value and location show the intensity of the reflected wave for each soil that reflected the signal. The vertical direction of radargram displays it travel time for depth measurement, once the signal velocities are known and the horizontal direction is linear distance on the ground surface.
机译:探地雷达(GPR)传播电磁波(EM),该电磁波对地下材料(例如沙子,花岗岩,混凝土,海滩沙子,粘土,塑料等)的电磁特性变化起反应,用于对地下材料进行轮廓分析。在GPR发明之前,工程师们依靠挖掘过程来确定地下的东西。开挖是一项昂贵且费时的工作,但并非总能探测到地下的所有物体。相比之下,GPR比能够穿透大多数材料的例外情况更快,更准确且成本更低。这项研究旨在评估下面不同类型的材料是否会影响地下剖面的图像显示,以供人类解释。 GPR的中心频率为250 MHz-用于捕获埋在六个不同土壤类型的样本中的管道的图像,其中之一是预拌混凝土。在现场埋有分别穿过深度为0.5m和1m的两条金属和两条塑料管。几块胶合板用作它们之间的分隔物。每个GPR数据都显示了埋在六种不同土壤材料中的管道的二维值数组,称为雷达图。具有特定值和位置的阵列显示每种反射信号的土壤的反射波强度。一旦知道信号速度并且水平方向是在地面上的线性距离,雷达图的垂直方向将显示其行进时间以进行深度测量。

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