1) Unsteady Water Transportation
非稳态水分传输
2) Unsteady Transportation
非稳态输送
3) unsteady heat transfer
非稳态传热
1.
The analysis and calculation of roof unsteady heat transfer in Ji'nan area
济南地区屋面非稳态传热的分析计算
2.
A mathematic model has been built for the unsteady heat transfer from the kettle to the oil inside.
为此建立了高温超高压釜体到釜腔内液压油的非稳态传热模型 。
3.
The temperature distribution in the adsorption bed was measured and compared with the results calculated with a model of unsteady heat transfer process developed by the authors.
对热参数泵吸附分离床层中的非稳态传热问题进行了理论分析及实验测定,求出了实验范围内的有效导热系数,并给出了从传热角度计算热参数泵吸附分离过程的循环周期时间的关系式。
4) transient heat transfer
非稳态传热
1.
Numerical simulation study on transient heat transfer through the wall made of autoclave-cured aerated concrete;
加气混凝土墙体非稳态传热的数值模拟
2.
Heat transfer of ground heat exchanger for GSHP(3):transient heat transfer characteristic of U-type ground heat exchanger with variable heat flow boundary
地源热泵地埋管换热器传热研究(3):变热流边界条件下单U形地埋管换热器的非稳态传热特性
3.
Some complex transient heat transfer problems are accompanied with hot oil pipelines.
埋地热含蜡原油管道的运行中涉及若干复杂的非稳态传热问题。
5) water transfer
水分传输
1.
Simulation of the water transfer processes of winter wheat field ecosystem using SHAW in Lhasa river valley
基于SHAW模型对拉萨河谷冬小麦农田生态系统水分传输特征的模拟研究
2.
In the loess hilly region in northern Shaanxi Province from June to September,the Simultaneous Heat and Water(CoupModel) model was applied to simulate and study water transfer of Soil-Vegetation-Atmosphere Transfer(SVAT) system in the acacia forest and the potato farmland.
基于野外试验资料,应用CoupModel模型,对陕北黄土丘陵区2006年6~9月份农地(马铃薯)、林地(刺槐林)SVAT系统水分传输进行了模拟。
3.
Researching on water transfer between interfaces of forestry watershed is the focus of interface hydrology and the base of probing the mechanisms of forestry vegetation on hydrological process.
探讨森林植被对水文过程物理机制的研究不可避免地要以森林生态系统为单元 ,以森林生态系统各个界面层次对水分传输和水量转换的影响为基础来进行 ,这也正是目前界面水文学研究的焦点问题。
6) water transport
水分传输
1.
Study on surface water transport in agricultural landscape on the slop lands of red soil (dry season) I.Water transport at soil-atmosphere interface;
红壤坡地农业景观(旱季)地表界面水分传输研究——Ⅰ.土壤大气界面水分传输
2.
Tomato Transpiration and WUE Regulated by Water Transport Path and Size of Shoot and Root under Water Deficit;
水分亏缺下番茄水分传输途径和根冠大小对蒸腾和WUE的调控
3.
Initial water content, precipitation quantity and precipitation intensity are the major factors influencing water transport in litters and moss layer.
初始含水量、降雨量和降雨强度是影响地被物层水分传输的主导因子。
补充资料：非结合水分
分子式：
分子量：
CAS号：
性质：存在于物料表面的润湿水分和物料孔隙中的水分。属于机械结合方式，与物料的结合强度较弱，易于去除。非结合水分所产生的蒸气压与液态水在同温度时所发生的蒸气压相同。
分子量：
CAS号：
性质：存在于物料表面的润湿水分和物料孔隙中的水分。属于机械结合方式，与物料的结合强度较弱，易于去除。非结合水分所产生的蒸气压与液态水在同温度时所发生的蒸气压相同。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条