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air layer相关的网络例句

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与 air layer 相关的网络例句 [注:此内容来源于网络,仅供参考]

Based on temperature and salinity data from 17 cruises along the 165°E section during 1984-1988 which were attained by the Sinuo-US cooperative air-sea interaction study and ORSTOM center in Noumea, the anomalous variations of temperature and salinity structures in the upper layer of the ocean in the periods of 1986-1987 E1 Nino and 1984-1985, 1988-1989 La Nina events were analyzed.

使用1984—1989年期间中美海-气相互作用合作研究及法国ORSTOM完成的沿165°E断面共17个航次调查中的温、盐资料,对1986—1987厄尔尼诺(E1Nino)及1984-1985,1988年反厄尔尼诺事件期间海洋上层温、盐结构的变化作了分析。

Firstly, the soil samples are gathered from the same section such as surface layer soil samples gathered from 0cm to 15cm depth and representation on studied object. Secondly, the precondition of tested samples must be the same. This study indicates that the tested samples must be 1mm diameter, over-dried at 40℃ for 24h and airtight cooling for 24h before measured for air-dry samples, and softly planish the surface at measuring. Lastly, the illuminating condition of light must be the same. This study indicates that the testing geometric condition are light source angle 15°, light source distance 30cm and sensor distance 15cm for soil hyperspectra indoor. The surface of white reference must be the same plane of that of sample.

第一个环节的"相同"是指田间土壤样品采集时的剖面位置一致,如表层土都采集0~15cm深度范围内的土壤,且所采集的样品应能尽量具备研究对象的代表性;第二个环节的"相同"是指土壤制备过程中的一些前处理条件应一致,建议土壤光谱测试样品的粒径1mm,风干土壤样品测试前在40℃恒温条件下烘24小时,然后密闭冷却24小时,测试时土壤表面进行稍稍压平处理;第三个环节的"相同"是保证测试光照条件的一致性,建议在50W卤素灯、8°探头角条件下,采用15°的光源照角度、30cm的光源距离和15cm作为室内士壤高光谱测试几何条件,测试时除遵循光谱测试指南的要求外,还须保证参考板表面与测试土壤样品的表面在同一平面上。

Characteristics can not fly; legs was born in the most lower body, it was upright posture; toes webbed; plantigrade sex; forelimbs into flippers; feathers short, in order to reduce friction and turbulence; retention layer of air between the feathers for insulation .

特征为不能飞翔;脚生于身体最下部,故呈直立姿势;趾间有蹼;跖行性;前肢成鳍状;羽毛短,以减少摩擦和湍流;羽毛间存留一层空气,用以绝热。

Punched hole design can further enhance air circulation within shoe to avoid mildew forming in middle layer.

鞋垫采用高密度透气的 OUTHOLITE防滑材料,冲孔设计促进鞋内空气循环,防止中间层霉菌的形成,并具有吸震功能,有效降低脚部扭伤几率。

The interactions among large air voids, the dynamic hydraulic pressure, the non-uniformly distributed load, the overload, the environment condition and the material lead to the deficiency of the adhesion between asphalt and aggregate. The immigration of the asphalt leads to the new bleeding and inside raveling. The pumping and settlement occurred once the water penetrates the whole asphalt layer.

大空隙率、动水压力、荷载的非均布、超载以及气候条件与路面材料的相互作用造成了沥青与集料粘附性的相对不足,面层内部沥青膜剥落后向上部迁移,这是新泛油、内部松散的产生机理;更为严重的情况下,外界水直接贯穿沥青面层对基层顶面的冲刷将诱发泛浆和沉陷。

However, the white pollution has been free, it abuses in the sky, the air brother and brother's clothes punctured the ozone layer, he let the desert sand fly never be stopped, confuse the people's life.

然而,白色污染已经有了自由,它在天空中胡作非为,把空气哥哥和臭氧层弟弟的衣服扎破,他让沙漠上的沙子飞得永远不得停息,搅乱了人民的生活。

In this paper, the structure characteristics of atmospheric boundary layer have been studied over Lanzhou in winter by combining numerical simulation method with analysis of the data which was observed by sounding balloon during the collaborative project "Study on air pollution and countermeasure in Lanzhou" supported by Gansu Government and Chinese Academy of Sciences.

本文利用甘肃省政府和中国科学院的科技合作项目"兰州市大气污染及对策研究"所获得的系留气球探空资料,并且结合数值模拟方法,对兰州市冬季大气边界层温度场特征进行了对比分析,结果表明:在没有特殊天气过程的典型冬季代表性时段,山谷城市兰州逆温边界层结构无论白天或夜间都存在,而且经常出现多层逆温和白天的脱地逆温情况,只有当冷空气过境时,逆温现象才减弱或消失;与观测结果相比较可以看出,数值模拟结果基本上反应了温度场的主要特征。

The top layer, when exposed to air, will harden faster than the underlayer.

这样,外面的漆层可以接触空气,于是硬化速度比下层快。

Puts forward the method of covering the cooling ceiling with the diathermanous film having high penetration rate for long wave radiation, and there being a layer of air or vacuum between the ceiling undersurface and the film.

提出了一种避免结露和下降气流的方法:用对长波具有高透过性的薄膜密封包裹冷却顶板,该薄膜和冷却顶板下表面之间保留一空气或真空夹层。

The seasonal variation of the upper layer heat content is controlled jointly by both the dynamic process and the net heat flux from the sea surface, and it can be mainly attributed to the air-sea interaction.

由动力过程和海表净热通量共同控制,2种作用都有明显的季节变化特征,并且随区域的变化两者贡献有所变化;西南季风爆发前,上层海洋热含量最大值的出现,是之前几个月动力作用和海表净热通量共同加热的结果。

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