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电阻率

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It was found that the resistivity of the TiO2, thin films deposited on Ti and Ti substrates increased non-linearly with the increase of the thickness of the films and varied in the range from conductor or semiconductor to nonconductor, respectively. The conducting layer thickness of the films deposited on different substarte materials is different and the films deposited on glass are nonconductors.

结果表明,沈积在Ti和Si基底上的TiO2薄膜的电阻率随著膜厚的增加而非线性增大,分别经历了导体、半导体到绝缘体或半导体到绝缘体的电阻率范围的变化过程, TiO2薄膜导电层厚度也不相同,沈积在玻璃表面TiO2薄膜为绝缘体。

The measurements of the transport properties indicate that the crystal exhibits a semiconductor behavior with p-type carriers and the thermal activation energy was estimated to be about 0.18 eV.

我们测量了制备样品的电阻率和热电势特性,样品表现出典型的p型半导体行为。经对电阻率和热电势数据的拟合,得到样品的热激活能△=0.16-0.18eV。

Finally, the problems and the application prospects of the electrical resistivity study are discussed.

并讨论了土的电阻率理论研究中存在的问题,展望了土电阻率理论的研究与应用前景。

The resistivity of iron is almost six times as much as that of copper.

铁的电阻率几乎是铜的6倍。(或译成:铁的电阻率几乎比铜的大5倍。

Volume and surface resistivity measurements are dependent on several factors.

电阻率和表面电阻率的测量决定于几个因素。

Complex resistivity phase detection is one of the development trend of complex resistivity logging technology.

电阻率相位检测技术是目前复电阻率测井技术的一个主要的发展方向。

In this paper, we establish a method to determine the resitivities of the earth and diameter of invaded zone simutaneously,using the deep and shallow apparent resitivitics,and propose a new algorithm. The main advantages of our method is that the selection of the initial value is need not, but in proviously work, it is nescssary and it must close to real values.

成功地解决了由双侧向测井深、浅视电阻率同时反演地层真电阻率和等效侵入带直径问题,建立了可靠的反演算法,此算法的最主要优点在于它不依赖于初值的选取,因而是真正具有工程实用价值的算法。

Another way to study on stability of high temperature superconductor is using finite element method.

本文提出了两种测量电阻率的方法,并得到Bi2223/Ag超导带材的电阻率与温度的非线性特性曲线,这对研究高温超导体的失超传播过程以及有限元分析都有重要的实际意义。

So we can inverse telluric current structure of medium according to the response, that is, the resistivity and distribution of underground rock and mineral.

电法勘探的理论基础是不同岩石矿物的电阻率不同,不同地电结构的场响应不同,因此我们可以由观测的场响应反演出介质的地电结构,即地下岩石矿物的电阻率及分布。

The theoretical foundation of electrical prospecting is that the resistivity of different rocks and minerals are different, and different fields have different responses to telluric current structure. So we can inverse telluric current structure of medium according to the response, that is, the resistivity and distribution of underground rock and mineral.

电法勘探的理论基础是不同岩石矿物的电阻率不同,不同地电结构的场响应不同,因此我们可以由观测的场响应反演出介质的地电结构,即地下岩石矿物的电阻率及分布。

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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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