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Determination of global ice loads on the ship using the measured full-scale motion data

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초록

This paper describes the whole procedures to determine ice-induced global loads on the ship using measured full-scale data in accordance with the method proposed by the Canadian Hydraulics Centre of the National Research Council of Canada. Ship motions of 6 degrees of freedom (dof) are found by processing the commercial sensor signals named Motion Pak II under the assumption of rigid body motion. Linear accelerations as well as angular rates were measured by Motion Pak II data. To eliminate the noise of the measured data and the staircase signals due to the resolution of the sensor, a band pass filter that passes frequencies between 0.001 and 0.6 Hz and cubic spline interpolation resampling had been applied. 6 dof motions were computed by the integrating and/or differentiating the filtered signals. Added mass and damping force of the ship had been computed by the 3-dimensional panel method under the assumption of zero frequency. Once the coefficients of hydrodynamic and hydrostatic data as well as all the 6 dof motion data had been obtained, global ice loads can be computed by solving the fully coupled 6 dof equations of motion. Full-scale data were acquired while the ARAON rammed old ice floes in the high Arctic. Estimated ice impact forces for two representative events showed 7e15 MN when ship operated in heavy ice conditions.

Abstract

This paper describes the whole procedures to determine ice-induced global loads on the ship using measured full-scale data in accordance with the method proposed by the Canadian Hydraulics Centre of the National Research Council of Canada. Ship motions of 6 degrees of freedom (dof) are found by processing the commercial sensor signals named Motion Pak II under the assumption of rigid body motion. Linear accelerations as well as angular rates were measured by Motion Pak II data. To eliminate the noise of the measured data and the staircase signals due to the resolution of the sensor, a band pass filter that passes frequencies between 0.001 and 0.6 Hz and cubic spline interpolation resampling had been applied. 6 dof motions were computed by the integrating and/or differentiating the filtered signals. Added mass and damping force of the ship had been computed by the 3-dimensional panel method under the assumption of zero frequency. Once the coefficients of hydrodynamic and hydrostatic data as well as all the 6 dof motion data had been obtained, global ice loads can be computed by solving the fully coupled 6 dof equations of motion. Full-scale data were acquired while the ARAON rammed old ice floes in the high Arctic. Estimated ice impact forces for two representative events showed 7e15 MN when ship operated in heavy ice conditions.

참고문헌 (5)

  1. 정성엽, "전자기 유도 장비를 이용한 북극해 해빙의 두께측정", 대한조선학회 논문집, 49(2), pp.189~195 (2012), 대한조선학회[DOI]
  2. 정성엽, "여름철 Chukchi Borderland 부근 해빙 재료특성 계측", 대한조선학회 논문집, 49(1), pp.45~51 (2012), 대한조선학회
  3. MOTAN: a Novel Approach for Determining Ice-induced Global Loads on Ships, "Johnston, Michelle", MARI-TECH, 1~17 (2003)
  4. Jsystron Donner Inertial, "Motion Pak II, Low Cost-6 Degree of Freedom, Multi-Axis Inertial Sensing System User's Guide", ~
  5. Vegte, Joyce Van De, "Fundamentals of Digital Signal Processing with Cdrom" (2001), Prentice Hall PTR

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