1) water transmission
水的传输
2) water transport
水传输
1.
Electrochemical Investigation on Water Transport Behavior of Organic Coatings and Degradation Mechanism of Coated-metals;
有机涂层中水传输与涂层金属失效机制的电化学研究
2.
And the water transport kinetics was introduced in the paper.
介绍了水在有机涂层中的存在形式和传输动力学及涂层组元(颜填料、助剂)对涂层中水传输的影
3.
In the present article water transport behaviors in actual trend were reviewed.
介绍在实际吸水过程中 ,涂层中水传输的特性及其影响因素 。
3) 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。
4) water and heat transfer
水热传输
1.
A new simulation method of decompose-coordination for solving the water and heat transfer model in GSVAC was presented.
该文以干旱区绿洲-荒漠交错带为研究对象,以质量守恒原理与能量平衡原理为基础,建立了潜水-土壤-植被-大气系统中水分与热量传输模式,并提出了求解潜水-土壤-植被-大气系统的数值模拟分解-协调新方法,用天山北麓三工河流域绿洲-荒漠交错带的实测资料验证了水热传输模型的可靠性。
5) 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：地下水水资源评价(见水资源评价)
地下水水资源评价(见水资源评价)
d ixiashui shuiziyuan Ping】ia地下水水资源评价见水资源评价。
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