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D. The dew point read by the hygrometer is very rep resenta2tive of the overall dew point inside the steam generator.

湿度计上的露点读数非常准确地代表了蒸汽发生器内的整个露点。

A step function generator of gas concentration and humidity is firstly presented in this paper.

本文首先提出了气体浓度和湿度的阶跃发生器,在此基础上介绍了气、湿敏传感器的动态校准方法。

Of course, proper storage of a Stradivarius violin in a humidity controlled environment is a foregone conclusion.

当然,一斯特拉迪瓦里小提琴妥善储存在控制环境湿度已成定局。

The results show that humidity does stratify in the space , which is different from mixing ventilation where humidity is constant .

置换通风系统的这一特点,有利于对空调空间进行有效的湿度控制和空调系统的节能。

The simulative model of temperature field and stress field in concrete , Heat and moisture coupling、Parallel simulative calculation of concrete with water pipe cooling、 Parallel feedback analysis of thermal characteristic parameters, and stress intensity factor of induced joint, which are the sixty-four-dollar questions, are studied in this dissertation. The main contents of this dissertation are as follows:(1)Based on the past and current research work, the calculation theory of the transient temperature field and creep stress field of mass concrete which self temperature influence is considered is deduced. The couple effect between the temperature field and humidity field of concrete, is considered on the basis of conservation law of water and energy, and the coupled formulation which coefficient is not constant of the heat and moisture in concrete is deduced. The calculation theory and model which is theoretically strict for solution to thermal problem in concrete with water-cooling pipes are recommended.

本文主要针对混凝土的温度场应力场仿真计算模型、热湿耦合、水管冷却问题的并行仿真、混凝土温度参数并行反演分析以及诱导缝应力强度因子计算等混凝土大坝温度应力数值仿真的关键技术进行了较为深入的研究,全文主要内容如下:(1)在现有研究基础上,推导了考虑自身温度影响的混凝土非稳定温度场和徐变应力场的计算理论;基于水分质量守恒和能量守恒原理考虑混凝土温度场和湿度场的耦合作用,推导了混凝土的变系数热湿耦合方程,并建立了相应的计算模型;引用严密的水管冷却混凝土温度场的计算理论和计算模型,比较了两种简化计算方法用于水管冷却混凝土仿真计算的不足。

Is there a specific environment, in this particular environment, temperature and humidity will have stringent requirements.

是不是有一个特定的环境,在这个特定的环境中,温度和湿度都会有严格的要求。

Based on the ecological characteristics, climate and humidity condition for the vegetation of the sporopollen from the both of the wells, the palaeovegetation types have been reconstructed. The result shows that the paleoclimate changes from tropical semiarid-subhumid climate to subhumid mid subtropical climate to subhumid south subtropical climate.

通过对两口钻井的孢粉植被类型、气温带和干湿度类型及孢粉谱的进一步分析,可将泉头组-青山口组沉积期的气候变化划分为三个演化阶段,自下向上依次为半干半湿的热带气候——半湿润的中亚热带气候——半湿润的南亚热带气候。

The eco-physiological characteristics of drought endurance of Pinus sylvestris var.mongolica were studied under different climatic regions, soil water and leaf water condition.Furthemore,the response and adaptability of trees to water stress was done.The below showed the results. 1 The parameters of drought endurance of P. sylvestris var. mongolica was measure and studied by PV technology in the subhumid, semiarid and arid regions The results indicated the osmotic potentials at water saturation condition and at the initial loss turgor decreased as the climatic drought degree increased,and related linearly with the climatic moisture index.It was proved that the drought endurance of P. sylvetris var. mongolica was varible and the elevation of the osmotic adjust capability was a main way to the adaptation of trees to the drought climatic environment.

本文研究了樟子松(Pinus sylvestris var.mongolica)的主要耐旱生理生态特征在不同地区、不同土壤水分状况和叶水分状况下的变化,进而研究了樟子松对水分胁迫的反应和适应,结果如下: 1 应用 PV 技术对半湿润区、半干旱区和干旱区樟子松耐旱性指标测定研究指出,水饱和总体渗透势和初始失膨点总体渗透势随着气候干旱程度增加而增加,与气候湿度指标呈直线相关,证明了樟子松属于耐旱性可变的树种,渗透调节能力增加是其对干旱气候适应的主要途径。

Therefore, N, S, P and humidity had significant effects on subsurface microbial activity.

因此,N、S、P和湿度对地下环境中微生物的活性有重要影响。

The GPI method assumes that the cloud with brightness temperature below 235K would be rainy, then the area of rain is equal to the coverage of cold cloud below 235K. It may be suitable for most part of China at tropic and subtropic area. But for northern part and plateau area of China, the GPI overestimates precipitation due to lack of enough water vapor.

4GPI方法假定云顶亮温低于235K时,将产生降水,降水区的面积就等于低于235K亮温覆盖的区域,这在热带和中纬度大部分地区可能是适用的,但对我国北方干旱地区以及高原地区,则存在明显的高估,表明有云不一定会有雨,为了修正西北部降水的系统性高估,引入相对湿度修正因子,即在一定温度条件下,加上一定的湿度条件,才能形成降水。

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