首页> 外文会议>第十七届国际结构物大气覆冰会议(IWAIS2017)论文集 >Dynamic Analysis of Multi-span Overhead Electric Transmission Line Considering Induced Ice Shedding
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Dynamic Analysis of Multi-span Overhead Electric Transmission Line Considering Induced Ice Shedding

机译:考虑跨冰的多跨架空输电线路动力学分析

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Overhead transmission lines in cold regions are prone to atmospheric icing hazards.Sudden ice shedding from overhead lines may cause serious electrical faults,such as flashover and short circuit due to insufficient clearance among ground wires,conductors and the earth,and mechanical incidents,such as strand(s)and cable breakage,clamp slippage,insulator rupture and cross-arm and tower deformation,due to large amplitude vibration,unbalanced loads and transient tension of conductors and ground wires.The Finite Element(FE)method is the main way to study the dynamic effects of ice shedding on line components,because of the limitations of analytical methods and physical tests.In early FE studies,ice shedding was modeled by suddenly releasing lumped ice masses from the conductors or overhead ground wires,where the ice shedding amount and location were predefined,and no extra ice deposit(located on other spans for example)was shaken off during the whole cable/line vibration process.However,in reality,more ice deposits may detach from the conductors after the initial ice shedding event.What we call induced ice shedding occurs when the resultant of adhesive force between the cable and the ice deposit and cohesive force within the ice deposit is exceeded by the ice deposit weight and inertia force resulting from the dynamic response of the line.The induced ice shedding will cause the mass,stiffness and damping of the dynamic system to vary with time,leading to a different dynamic response than if there is no further ice detachment.In this study,firstly,the induced ice-shedding effect is modeled in the form of a user-defined subroutine in the FE analysis of a multi-span transmission line section,where the relation among adhesive force,cohesive force,gravity and inertia force is considered to obtain the force balance/imbalance condition that will define whether or not subsequent shedding occurs after the triggering event.Secondly,a comparison of the results obtained without considering induced ice shedding indicates that the dynamic response changes significantly,and the previous method may underestimate or overestimate the threats of ice shedding.Then,the influential factors,initial ice shedding amount and initial ice shedding locations,are studied and the dynamic characteristics of the response are obtained and compared.This paper provides a powerful tool to significantly improve the accuracy of FE simulation of ice-shedding effects on overhead lines,which is important to ensure the mechanical safety and serviceability of transmission lines in cold regions.
机译:寒冷地区的架空输电线路容易造成大气结冰的危险,由于接地线,导体与地面之间的间隙不足,架空线突然结冰可能会导致严重的电气故障,例如飞弧和短路,以及机械事故,例如绞线和电缆断裂,夹具打滑,绝缘子破裂以及横臂和铁塔变形,是由于大振幅振动,不平衡负载以及导体和地线的瞬时张力引起的。有限元方法是由于分析方法和物理测试的局限性,研究了融冰对线路组件的动态影响。在早期有限元研究中,融冰是通过突然从导体或架空地线释放结块的冰块来模拟的,在融冰量中位置和位置是预先定义的,在整个电缆/线路振动过程中,都没有甩掉多余的冰块(例如位于其他跨度上)。现实中,在最初的融冰事件发生后,更多的冰层可能会从导体上脱落。我们所说的感应冰层发生是当电缆与冰层之间的粘着力和冰层内部的内聚力之和超过合力时发生的由于管路的动态响应而产生的重量和惯性力。诱导的冰块脱落将导致动态系统的质量,刚度和阻尼随时间变化,从而导致动态响应与没有进一步冰分离的情况不同。本研究首先在多跨输电线路截面有限元分析中以用户定义的子程序形式对诱发的降冰效果进行建模,其中粘着力,内聚力,重力和惯性力之间的关系为考虑获得力平衡/不平衡条件,该条件将定义触发事件后是否发生后续脱落。其次,比较获得的结果,没有缺点诱发冰的脱落表明动力响应发生了显着变化,而先前的方法可能低估或高估了冰的威胁。然后,研究了影响因素,初始除冰量和初始除冰位置,并研究了其动态特性。本文提供了一个强大的工具,可以显着提高有限元模拟架空线路上降冰效果的准确性,这对于确保寒冷地区输电线路的机械安全性和可维修性具有重要意义。

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