贮藏介质含水量为60%有利于保持东方百合鳞茎的新鲜饱满状态；
For fresh keeping of Lily bulbs, 60% was proved as the suitable relative water content in packing media;
本文就含水的倾斜多孔介质层在侧向加热条件下流体热对流稳定性问题进行试验研究。
A experimental investigation on the stability of thermal convection in a sloping porous Medium under lateral heating is reported.
在研究了电容式传感器的原理和含水介质导电浴盆效应的基础上提出了用电容式传感器来测量粮食水分的原理。
Measuring principle of grain's moisture is proposed the basis of electric conductivity bathtub effect of moisture containing mediums, and capacitive sensor.
通过脉冲试验，采用测站脉冲响应曲线及流量衰减曲线分析，对后寨河流域含水介质结构进行了研究。
Based on pulse test, the pulse response curve and flow recession curve are analysed for studying the structure of karst aquifer medium.
高效复合菌与石油配水一起进入模拟地下含水介质的反应器，在反应器前部均能形成一个稳定的生物带。
The hybrid microorganism in-flowed into the reactor imitating the aquifer media with the petroleum wastewater, and it could form a steady microorganism zone in the foreside of the reactor.
岩溶含水介质结构类型在一定程度上决定了岩溶地下水的富集与运移规律。
The structural type of karst water-bearing media determines the storage capacity and movement features to a certain extent.
在分析研究化验资料的基础上，探讨了储层存在多孔介质、微细孔隙水等产生低含水油层的原因。
Based on the analysis and research on test results, it discusses the existence of low water-cut oil layers due to porous media and pore water in micro pores of reservoir.
白垩系砂岩是鄂尔多斯高原的主要含水介质，对区内工农业、居民用水具有的重要的作用。
Cretaceous sandstone, the main aquifer in Ardos plateau, plays an important role in supplying industry and agriculture using water and inhabitant drinking-water.
前者主要是被污染地下水中阴离子替代组成含水层介质骨架的矿物晶格中阴离子，生成新的矿物相的过程。
The metasomatic process is mostly the substitution of anions in the crystal lattice of minerals making up the matrix of aquifers by anions from polluted groundwater to form new mineral facies.
该模型能反映漏斗中心水位的动态特性，且不要求均衡区承压含水层为各项同性的均匀透水介质；
The model can reflect the dynamic characteristics of the water stage at the cone center, and it does not require artesian aquifers in balance regions to be of homogeneous media.
并对含水介质结构、边界条件及地下水流态进行了研究，建立了水文地质概念模型，构建了三维地下水流数学模型。
Based on aquifer characteristics, boundary condition and groundwater flow regime, the hydro geologic concept model and the three-dimensional groundwater flow simulation mathematical model was built.
对不同的土样进行了一系列的室内试验，试验表明，模型能很好地描述非饱和土介质介电常数与体积含水量之间的关系。
From the experimental results, it was found out that the relation curves of soil samples were almost consistent with each other and fittd the model well.
木材干燥的控制过程就是控制窑内介质温度和湿度来使木材含水率降低到某一期望值的过程。
The control process of wood drying is the same as the process of controlling medium's temperature and humidity in a kiln in order to reduce water ratio of wood to some expected value.
为充分体现矿井裂隙水系统的强烈非均质性和不连续特征，运用广义多重介质理论，系统地研究了范各庄煤系含水介质。
For fully representing the characteristics of fractured rock masses, such as strong nonhomogeneity and discontinuousness, the media are studied with generalized multiple porous media theory.
前言：介绍了DR AST IC模型的七个评价因子：地下水埋深、含水层净补给量、含水层介质类型、土壤类型、地形坡度、包气带介质i的影响和含水层的导水系数。
The paper introduces seven factor of DRASTIC model: Depth of water table, Net recharge, Aquifer media, Soil media, Topography, Impact of Vadose Zone and Hydraulic Conductivity.
由于水、油介电特性差异较大，导致电磁波在不同含水率的油水混合介质中传播时的相位系数有很大不同。
There is so much a different dielectric property between oil and water that the phase constants are quite different when electromagnetic wave travels in them.
这些结果表明，高含水量(85%)，可能增加小型基底真菌却减少了的孔隙介质和因此的传热传质。
These results indicate that the higher moisture level (85%), probably increased substrate availability to the fungus but reduced the porosity of the medium and hence the heat and mass transfer.
研究结果表明：对于成层介质中的渗流计算，可用等效的各向同性的均质含水层代替不同透水性介质组成的层状岩土层。
The results show that the equivalent isotropic homogeneous aquifer can substitute the layers consisted of different water-permeable media for seepage flow calculation in the layered media.
在该模型的基础上研究了电磁波与非饱和土介质的相互作用，建立了非饱和土介质介电常数与体积含水量之间的关系模型。
Then the relationship between dielectric constant and volume water content or pore ratio of unsaturated soil was established. Different kinds of soil samples were tested.
研究的影响因素主要包括含水率、质量、功率和吸波介质，经过分析得到了各个因素影响微波加热的能力。
The main influence factors are water-content coefficient, capacity factors, mass and microwave absorbing materials, and the capability of every factor is obtained by analyzing the results.
研究的影响因素主要包括含水率、质量、功率和吸波介质，经过分析得到了各个因素影响微波加热的能力。
The main influence factors are water-content coefficient, capacity factors, mass and microwave absorbing materials, and the capability of every factor is obtained by analyzing the results.
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