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平整冰层
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  ice-sheet
     The air and water temperature distributions of January in Bohai from historical statistic data as well as the design ice thickness of different ice periods are organized using a mesh of 1/6 latitude × 1/6 longitude in Bohai. The ice-sheet physical and mechanical parameter distributions of different ice periods in Bohai are thus obtained.
     将渤海历史资料归纳的冬季气温分布、水温分布和不同重现期冰厚度分布资料放入渤海1/6经度和1/6纬度的网格内,从而获得渤海不同重现期平整冰层的物理和力学参数分布。
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  “平整冰层”译为未确定词的双语例句
     As samples, the distributions of ice sheet design thickness, compressive strength, flexural strength, shear strength and elastic modulus for ice periods of 25, 50 and 100 years are presented.
     作为实例,给出渤海25、50、100年重现期的平整冰层设计厚度分布、压缩强度分布、弯曲强度分布、剪切强度分布和弹性模量分布。
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  相似匹配句对
     Temper Rolling for Cold-rolled Strip
     冷轧带钢的平整轧制
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     A Mathematical Research for Ground Leveling System
     土地平整系统算法研究
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     Development of instrument in measuring thickness of ice layer on Huanghe River
     黄河冰层厚度测量仪的研制
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     A study on thermal expanding force of confined ice sheet
     约束冰层温度膨胀力的研究
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     As samples, the distributions of ice sheet design thickness, compressive strength, flexural strength, shear strength and elastic modulus for ice periods of 25, 50 and 100 years are presented.
     作为实例,给出渤海25、50、100年重现期的平整冰层设计厚度分布、压缩强度分布、弯曲强度分布、剪切强度分布和弹性模量分布。
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  ice-sheet
Our data corroborate the view that the repeated occurrence of YD-type event was not an "accident", possibly resulted from the coupling of ice-sheet and oceanic/atmospheric circulations.
      
Two numerical methods for solving the full steady ice-sheet equations in axi-symmetric flow are described.
      
The reason may be related to overestimated ice-sheet thickness and glaciation period in the north.
      
Ice-sheet drainage of glacial detritus into the sea involves size fractionation by ice-margin winnowing on a giant scale caused by the lower density of meltwater entering cold seawater.
      
That is, under the warmer conditions inferred to have prevailed prior to the opening of the Drake Passage, conditions would still have been favorable for the maintenance of an Antarctic ice-sheet.
      
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A new division of ice engineering sub-areas is set up based on the ice physical and mechanical parameters distributions in Bohai. The characteristic of the division shows that the load on the vertical structures with same diameter or width is (equal) in a same division area. Therefore, the new division index becomes the product of a uniform ice sheet design thickness and peak compressive strength at different return periods. To obtain these physical and mechanical parameters, we use history data to set up the...

A new division of ice engineering sub-areas is set up based on the ice physical and mechanical parameters distributions in Bohai. The characteristic of the division shows that the load on the vertical structures with same diameter or width is (equal) in a same division area. Therefore, the new division index becomes the product of a uniform ice sheet design thickness and peak compressive strength at different return periods. To obtain these physical and mechanical parameters, we use history data to set up the expressions of a uniform ice sheet or ice sample temperature, salinity and density with air temperature, water temperature, ice period and ice thickness. Then ice porosity is obtained. Later ice peak compressive strength is calculated by using the experimental relationship of Bohai ice peak compressive strength and porosity. At last, the ice sheet physical and peak compressive strength distributions at different return periods in Bohai are developed from ice sample results. The new ice engineering sub-areas at different return periods are obtained with the help of the new division index. The new ice sub-areas in return periods of 25-, 50- and 100-year are given as samples.

根据渤海海冰物理和力学参数分布建立渤海海冰工程分区。其特点是将作用到相同直径或宽度的直立结构物上冰的作用力范围相同的区域划分为同一分区内,因此不同重现期设计冰厚度和峰值压缩强度之积作为区划指标。为了获得不同重现期渤海海冰物理和力学性质参数,利用渤海历史资料建立用气温、水温、冰期和冰厚表达非变形平整冰层和冰样温度、盐度、密度的关系,进而获得冰的孔隙率;利用渤海海冰单轴压缩强度同孔隙率的试验关系计算相应峰值压缩强度;然后发展渤海不同重现期平整冰层物理和力学参数的平面分布。在此基础上以新区划指标做不同重现期的海冰工程分区。作为新区划的实例,给出25、50、100年重现期的渤海海冰工程分区。

The expressions for vertical profiles of ice sheet temperature, salinity and density using historical air temperature, water temperature, ice period and ice thickness of Bohai are set up. The vertical profile of ice porosity is also obtained. The compressive strength, flexural strength, shear strength and elastic modulus of the ice sheet are calculated using the experimental relationships of Bohai ice mechanical parameters and porosity. The air and water temperature distributions of January in Bohai from historical...

The expressions for vertical profiles of ice sheet temperature, salinity and density using historical air temperature, water temperature, ice period and ice thickness of Bohai are set up. The vertical profile of ice porosity is also obtained. The compressive strength, flexural strength, shear strength and elastic modulus of the ice sheet are calculated using the experimental relationships of Bohai ice mechanical parameters and porosity. The air and water temperature distributions of January in Bohai from historical statistic data as well as the design ice thickness of different ice periods are organized using a mesh of 1/6 latitude × 1/6 longitude in Bohai. The ice-sheet physical and mechanical parameter distributions of different ice periods in Bohai are thus obtained. As samples, the distributions of ice sheet design thickness, compressive strength, flexural strength, shear strength and elastic modulus for ice periods of 25, 50 and 100 years are presented.

利用渤海历史资料建立由气温、水温、冰期和冰厚表达平整冰层温度、盐度、密度的垂直剖面,进而获得冰的孔隙率垂直剖面。在此基础上通过渤海冰力学参数同孔隙率的试验关系计算出相应冰层峰值压缩强度、峰值弯曲强度、峰值剪切强度和弹性模量。将渤海历史资料归纳的冬季气温分布、水温分布和不同重现期冰厚度分布资料放入渤海1/6经度和1/6纬度的网格内,从而获得渤海不同重现期平整冰层的物理和力学参数分布。作为实例,给出渤海25、50、100年重现期的平整冰层设计厚度分布、压缩强度分布、弯曲强度分布、剪切强度分布和弹性模量分布。

 
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