1) moisture field
水分场
1.
Dynamic test of moisture field in soil under supplying water;
补水条件下土体水分场的动态测试
2.
The similarity criteria of the artificial freeze temperature field(TF) and moisture field(MF) are inferred.
根据相似理论推导出人工冻结温度场和水分场模型试验相似准则。
3.
Based on an observation on the moisture field and temperature field changing with time in freezing soil, this paper makes a numerical simulation of the test results by citing the heat-moisture coupling model of one dimension vertical freezing soil system established by Doctor Flerchinger and the correlative relation equation and boundary condition.
在观测正冻土冻结过程中水分场和温度场随时间变化规律的基础上 ,引用Flerchinger建立的垂直一维冻土系统水、热流耦合模型及相关的联系方程和边界条件对所测的结果进行数值模拟 ,证明其模型在工程上的准确性与适用性 。
2) water field
水分场
1.
According to heat transfer, filtration theory and mechanics of frozen soil, a mathematics model and its control equation were put forward, which is of the coupling problem of temperature field, water field and stress fields.
根据传热学、渗流理论及冻土力学提出了带相变的温度场、水分场和应力场耦合问题的数学力学模型及其控制方程。
3) scattered flow field of karstic water
岩溶水分散流场
4) horizontal wind decomposition
水平风场分解
5) horizontal component of the earth magnetic field
地磁场水平分量
1.
The method that measuring horzontal component of the earth magnetic field with digital quantometer is introdnces,the computational formule are given,systematic error are discussed,the advantages of the this method with tangent galvanometer measuring horizontal component of the earth magnetic field are simply expounded.
介绍了用数字冲击电流计测量地磁场水平分量的方法,给出了计算公式,对系统误差进行了讨论,简述了该方法与用正切电流计法测量地磁场水平分量的优点。
6) triangular method of horizontal magnetic field intensity
水平磁场分量
1.
This paper expounds the principle, the method and application results for determining the depth of underground pipeline using triangular method of horizontal magnetic field intensity.
本文阐述了利用水平磁场分量确定地下管线深度的原理方法以及应用效果。
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