1.
The influenceof formation temperature decreasing on formation pressure in Sulige Gasfield
地层温度的降低对苏里格气田地层压力的影响
2.
Characteristics of temperature, humidity and wind velocity profiles in the surface layer in sunshiny day in spring in the Taklimakan Desert hinterland;
塔中春季晴天近地层温度、湿度和风速廓线特征
3.
A Method for Calculating the Formation Temperature during Acidizing the Matrix of Sandstone
砂岩基质酸化地层温度的数值计算方法
4.
A New Method of Determining Formation Temperature
地层温度确定的新方法及实际指导意义探讨
5.
Characteristics of Wind Velocity,Temperature and Humidity Profiles of Near-surface Layer in Tengger Desert
腾格里沙漠近地面层风、气温、湿度特征
6.
Estimation of the Making-up Temperature of Geothermy Water and the Thermal Reservoir Temperature in the Guanzhong Basin
关中盆地地下热水接受补给时温度及热储层温度的估算
7.
The CO_2 Flux of Soils and the CO_2 Concentration of Surface Layer at Arid Region in Temperate Zone;
温带干旱地区近地层CO_2浓度和土壤CO_2通量
8.
Crack Mechanism and Controlling Technique of High-rise Building Basement Wall;
高层建筑地下室侧墙温度裂缝机理及控制技术
9.
Groundwater Age and Recharge Temperature in the Quantenary Aquifers in North China Plain;
华北平原第四系含水层地下水年龄与补给温度
10.
Research on the Optimum Insulation Thickness of the External Wall for Residential Buildings in Changsha Region
长沙地区居住建筑外墙保温层最佳厚度的研究
11.
Anslysis of Actual Measure and Numerical Simulation for Freeze Temperature Field in Cretaceous Stratum
白垩系地层冻结温度场实测与数值模拟分析
12.
Value of CO_2 Density Logging under Formation Conditions
地层温压条件下CO_2密度测井响应值研究
13.
vertical gradients of salinity and temperature
盐度和温度作垂直分层
14.
stratification of temperature and salinity
温度与盐度的分层状况
15.
Retrieval of Land Surface and Soil Temperature in Different Bare Soil Layers from EOS/MODIS Images;
基于EOS/MODIS数据的地表温度反演及多层土温估算研究
16.
Study on Temperature Field and Plan of the Heat Presearvation and Insulation Layer on the Extra-Long Highway Tunnel in High Attitude and Cold Zones;
高寒地区特长公路隧道温度场及保温隔热层方案研究
17.
meat thermometer
测定肉内层温度的温度计
18.
To a very large extent, the temperature of the earth is determined by the amount of solar heat which the atmosphere can keep .
在很大程度上，地球的温度取决于大气层所能保持的太阳的热量。