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air temperature相关的网络例句

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与 air temperature 相关的网络例句 [注:此内容来源于网络,仅供参考]

The results show that the atmosphere has a big influence on the thermal stability of C_(60).C_(60) begins to decompose at 423.5℃in the air,the deomposed peak temperature is 668.5℃,but very stable in the helium atmosphere,only sublimate,the crystal shape of C_(60) has a certain influence to its thermal stability.The synthesized nine kinds of nitro-fullerene derivatives all have good thermal stability and their decomposed peak temperatures all exceed 350℃.The thermal explosion temperature for 5 seconds delay of product 4 is 253℃.The category,number and position of nitryl group in nitro-fullerene derivatives all have influence on their thermal stability.

利用差热分析仪和DSC-TG综合热分析仪对C_(60)及其硝基衍生物的热稳定性进行了研究,结果表明,环境气氛对C_(60)热稳定性影响很大,C_(60)在空气中423.5℃开始分解,放热峰值温度为668.5℃,在氦气中很稳定,仅表现为升华,C_(60)的晶型对其热稳定性也有一定的影响;合成得到的九种硝基富勒烯衍生物都具有较好的热稳定性,分解峰值温度均高于350℃;产物4的5秒爆发点测试结果为253℃。

During the winter months, the mean temperature is lower than other regions located on the same latitude, due to the expansion of high-pressure air masses formed over inland Siberia, whose strong northwesterly winds bring dry, cold air into Korea.

冬天 (12-2 月)受地形影响。由于寒冷的西伯利亚高气压和偏西风影响温度比同纬度的其他国家要低。

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。

Presents the design of heating ventilating and air conditioning systems in which low temperature hot water floor panel heating systems in winter,variable refrigerant volume split air conditioning systems in summer,and central ventilation systems through all-year are adopted.

介绍了该工程的供暖系统、空调系统及通风系统的设计。冬季采用低温热水地板辐射供暖,夏季采用变制冷剂流量多联分体式空调系统供冷,全年采用集中新风系统供给新风。

Everyone knows that the temperature of the air is a physical quantity.It is easy to measure.The humidity of the air is also a very important physical quantity .

众所周知空气的温度是比较容易测量的物理量,而空气湿度则是一个非常重要的而又难以测量的物理量。

This thesis is mainly concerned with mechanism of air preheater after-burning and air preheater hot spots detection technique based on image of temperature field.

本文主要研究了电站锅炉空气预热器发生二次燃烧的机理以及基于温度场分布图的空预器热点检测系统。

It is very important problem how to detect aggregate fuels and sediments temperature on air preheater parts surface effectively in order to prevent air preheater from fire.

如何有效地检测空气预热器表面的燃料油污沉积物的温度,是防止空气预热器表面起火所必须考虑的问题。

The pressure ridge partly moved to southeast, it led to the cold air stream more moved to southeast, and the strong cold wave broke out. The water vapor from Caspian sea to Bslkhash lake accumulated at the upper of north Xinjiang, and it provided the water vapor condition for the cold wave. The ECMWF numerical forecast product accurately predicted the evolution trend of circulation (the position, intensity, path and speed of ground surface cold high pressure) of height field in this cold wave process. The predicted temperature at 850 hPa had good corresponding relation with the actual lowest temperature.

高压脊部分东南垮,导致强冷空气大举东南下,强寒潮天气暴发;里海到巴尔喀什湖的水汽在北疆上空聚积,为这次寒潮天气提供了水汽条件;ECMWF数值预报产品在这次强寒潮天气过程中准确的预报了高度场的环流场演变趋势,地面冷高压的位置、强度、路径和移速;850 hPa格点温度预报值与最低温度实况值具有很好的对应关系。

The temperature distributions of the gas , air and heat surface in the regenerative air heater at different operating conditions are procurable with this solution .

由该方法可以得到不同工况下空气预热器内部烟气,空气及其受热面的温度沿轴向和周向的分布情况。

Rna - Rns, see "Partitioning of net radiation", for multiple plants the fraction of radiation to each plant is calculated in the radiation section, see "Partitioning of radiation between plants", es is the vapour pressure at saturation, ea is the actual vapour pressure,ρa is air density, cp is the specific heat of air at constant pressure, Lν is the latent heat of vaporisation,Δ is the slope of saturated vapour pressure versus temperature curve,γ is the psychrometer "constant", rs is an "effective" surface resistance and ra is the aerodynamic resistance.

潜在蒸腾量 Etp 根据Monteith(1965)给出的彭曼联合方程形式计算:式中: Rn 为对于蒸腾的有效净辐射量(也就是 Rna - Rns ,见"净辐射划分"-Partitioning of net radiation,对于多重植被,每一株植物的辐射比率的计算见辐射一节的"植物间的辐射划分"Partitioning of radiation between plants); es 为饱和水气压;ea 为实际水气压;ρa 为空气密度; cp 为常压下的空气比热;Lν为汽化潜热;Δ为与温度曲线饱和水气压关系曲线斜率;γ为干湿球湿度计"常数";rs 为"有效"表面阻力;ra 为气动阻力。

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