期刊文献+

双探针型海底热流计数据解算模型选取 被引量:2

Selecting a simplified model for dual-probe seafloor heat-flow meter
下载PDF
导出
摘要 选取适合于双探针型海底热流计数据解算的简化模型,是双探针型海底热流计结构优化的理论基础,对提高海底热流数据解算精度具有重要意义。本文基于脉冲式双探针海底工作的有限元数值模型,对双探针的脉冲加热时间、体生热率、热物性、长度及半径等因素在双探针脉冲法的3个线热源简化模型中所引起的模型误差作了详细的分析和讨论,并以模型误差最小为原则选取简化模型。结果表明:1)脉冲加热有限长线热源(PFLS:pulsed finite line source)模型是双探针脉冲法中较为实用的简化模型,它可消除加热时间和探针长度对介质热物性参数求解的影响;2)在PFLS模型下,探针热导率对待测介质热物性测量的影响可以忽略;而探针间距越大、半径越小及其体积比热容与待测介质越接近,则所求介质热物性的模型误差就越小;在保证温度传感器能有效记录到温度变化的前提下,探针脉冲功率的大小基本不影响介质热物性求解的模型误差。 Selecting an effective and convenient simplified model for dual-probe seafloor heat-flow meter is the theoretical basis for optimizing dual-probe structure, which is very important to improve heat-flow calculation ac- curacy. Basing on the finite element numerical model about seafloor pulsing dual-probe, the authors analyzed in detail how the dual-probe's heat pulse duration, heat generation rate, thermal properties, length and radius affect model errors in three line source simplified models. The selected effective and convenient simplified model is the one whose model errors are the least. The results are as follows: 1 ) in dual-probe heat pulse method, Pulsed Finite Line Source (PFLS) model is a more practical simplified model, in which the model errors from pulse du- ration and probe length can be avoided; 2) in the PFLS model, model errors from probe thermal conductivity can be neglected. In addition, model errors can recede with probe spacing increasing, probe radius decreasing and probe volume heat capacity approaching the surrounding medium. When surrounding medium temperature change can be detected and recoded effectively by the sensor probe, probe heat pulse power cannot affect model errors.
出处 《热带海洋学报》 CAS CSCD 北大核心 2009年第4期28-34,共7页 Journal of Tropical Oceanography
基金 国家高技术研究发展计划(863计划)项目(2006AA09A203) 国家重点基础研究发展973计划项目(2007CB41170104) 国家高技术研究发展计划(863计划)项目(2008AA09Z306) 国土资源部海洋油气资源与环境地质重点实验室基金项目(MRE200804)
关键词 双探针型海底热流计 双探针脉冲法 线热源理论简化模型 有限元数值模拟 Dual-probe seafloor heat-flow meter Dual-probe heat pulse (DPHP) method Line source simpli- fied models Finite element numerical modeling
  • 相关文献

参考文献22

  • 1GERARD R, LANGSETH M G, EWING M. Thermal gradient measurements in the water and bottom sediment of western Atlantic[J]. J Geophys Res, 1962, 67: 785-803.
  • 2CLARK T F, MALCOLM F J, KORGEN B J. An improved Ewing heat probe frame [J]. Mar Geophys Res, 1972, 1: 451-455.
  • 3PFENDER M, VILLINGER H. Miniaturized data loggers for deep sea sediment temperature gradient measurements[J]. Mar Geol, 2002, 186: 557-570.
  • 4徐行,施小斌,罗贤虎,郭兴伟,杨小秋.南海北部海底地热测量的数据处理方法[J].现代地质,2006,20(3):457-464. 被引量:33
  • 5徐行,施小斌,罗贤虎,刘方兰,郭兴伟,沙志斌,杨小秋.南海西沙海槽地区的海底热流测量[J].海洋地质与第四纪地质,2006,26(4):51-58. 被引量:48
  • 6LISTER C R B. Measurement of in situ sediment conductivity by means of a Bullard-type probe [J]. Geophysical Journal International, 1970, 19: 521-532.
  • 7LISTER C R B. The pulse-probe method of conductivity measurement[J]. Geophysical Journal International, 1979, 57: 451-461.
  • 8HYNDMAN R D, DAVIS E E, WRIGHT J A. The measurement of marine geothermal heat flow by a muhipenetration probe digital acoustic telemetry an in-situ thermal conductivity [J]. Mar Geophys Res, 1979, 4: 181-205.
  • 9VILLINGER H, DAVIS E E. A new reduction algorithm for marine heat flow measurements [J]. J Geophys Res, 1987, 92: 12846-12856.
  • 10LISTER C R B, SCLATER J G, DAVIS E E, et al. Heat flow maintained in ocean basins of great age: investigations in the north-equatorial West Pacific [J]. Geophysical Journal International, 1990, 120: 603-630.

二级参考文献126

共引文献84

同被引文献32

引证文献2

二级引证文献8

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部