首页> 外文会议>International conference on port and ocean engineering under arctic conditions >ANALYSIS OF BOREHOLE JACK ICE STRENGTH DATA USING QUANTILE REGRESSION
【24h】

ANALYSIS OF BOREHOLE JACK ICE STRENGTH DATA USING QUANTILE REGRESSION

机译:使用量子回归分析钻孔插孔冰强数据

获取原文

摘要

The magnitude of ice strength is a topic that impacts the design of offshore structures and the use of ice as a construction material (ISO, 2010). There is a large body of confined compressive strength values on old ice, first year and fresh water ice obtained using Borehole Jack (BHJ) measurements in Ihe field. In some cases the corresponding values of ice temperature and ice salinity have been obtained. The ice strength measurements have often been analysed by plotting the BHJ ice strength as a function of the brine volume and performing least-squares analysis on the data. This approach has had limited success mainly due to the large scatter in the data. In least-squares analysis, the scatter is treated as an aspect that is to be minimised so that the underlying trend can be quantified. Using quantile regression in contrast, the scatter is treated as an essential part of the data. In this paper we use the quantile regression method to generate values of the BHJ strength at quantiles, from 0.05 to 0.95, using 236 strength measurements from multi-year, first-year and flooded ice. The analysis showed that the ice strength can be modelled using a linear function of root brine volume. The Normal, Log-normal, Gamma and Gumbel probability distributions were tested as suitable models for the generated quantiles. The Normal distribution was found to match the quantiles with the lowest RMS error. From the calibrated probability distribution, BHJ pressure at other quantiles can be obtained. For example at the 0.99 quantile (1% probability of exceedence) and at zero brine volume, the ice strength is 53.5 MPa. The calibrated probability distribution of the BHJ ice strength is compared with the recommendations contained in ISO 19906.
机译:冰强的幅度是影响海上结构的设计和冰作为建筑材料的主题(ISO,2010)。在IHE领域中使用钻孔插孔(BHJ)测量获得的旧冰,第一年和淡水冰上存在大量狭窄的压缩强度值。在某些情况下,已经获得了相应的冰温和冰盐的值。通常通过将BHJ冰强度作为盐水体积的函数绘制并对数据进行最小二乘分析来分析冰强度测量。这种方法的成功有限,主要是由于数据的大散布。在最小二乘分析中,将散射视为要最小化的方面,使得可以量化潜在的趋势。相比之下,使用量子回归,将散点视为数据的重要组成部分。在本文中,我们使用量化的回归方法在量数,从多年,一年和洪水冰的236强度测量产生0.05至0.95的量级的BHJ强度的值。分析表明,可以使用根盐水体积的线性函数来建模冰强度。正常,逻辑正常,伽马和伸缩概率分布被测试为生成的定量的合适模型。发现正常分布与最低RMS误差的定量匹配。从校准的概率分布,可以获得其他量子的BHJ压力。例如,在0.99分量物(1%的概率)和零盐水体积时,冰强度为53.5MPa。将BHJ冰强的校准概率分布与ISO 19906中所含的建议进行比较。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号