空穴导电

XPS能谱及交流阻抗谱分析显示可能存在氧空穴导电。

The analysis of XPS reveals the possibility of oxyanion hole conduction .

现今我们知道，这些材料的导电过程是所谓空穴导电。

We now believe that these materials conduct by a process known as hole conduction .

这是由于p型半导体空穴导电，而n型半导体则为电子迁移导电，使得表面活性氧物种形成机理不同所致。

These are due to different mechanism of the formation of the partial charged oxygen species on the surface of catalysts .

金属型非晶InSb，以电子导电为主，半导体型非晶InSb则以空穴导电为主。

The electron conduction is dominant in the metal-type amorphous InSb and the hole in semiconductor-type one .

结果表明，金属型非晶态InSb以电子导电为主，半导体型非晶态InSb以空穴导电为主；

Experimental results show that the conduction of the electron is dominative in the metal-type amorphous InSb and the conduction of the hole is dominative in the semiconductor-type amorphous InSb .

在氧气及空气中，以电子空穴导电为主；

Electron-hole conduction is dominant in oxygen or air ;

咔唑类聚合物具有优异的光电性能和空穴导电传输性能，在能源、国防、信息、医疗、环保、农业等领域具有广阔的应用前景。

Polymer with carbazole group has widely been used in energy , national defense , information , medical , environmental protection , agriculture and other areas because of their excellent photoelectric properties and cavities conductive transmission properties .

ESR谱图表明在常温下空气中聚合物中存在有稳定的自由基，为空穴跳跃导电机理。

The results of ESR implied that there was stable radical group in the polymer to confirm that the polymer took hole hopping conduction mechanism .

黄铁矿空穴型导电性与As、Au正相关，与Co、Ni呈明显的负相关，P型和N型导电性是由As/（Co+Ni）值决定的。

The hole type conductance of pyrite appears positive correlation with As , Au , and appears negative correlation with Co , Ni . The P type and N type conductance of pyrites are dominated by As / ( Co + Ni ) value .

对其主要载金矿物黄铁矿的热电性测定，表明黄铁矿为空穴型导电，该矿床剥蚀程度不大，属上部出露。

The pyroelectricity is measured to main carrying - gold mineral pyrite . the result re fleeted that the pyrite is hole conduction , and have calculated deposit to denude no much , belong to upper outcropping .

大多数产于中生代岩体中的中深脉状金矿、火山次火山岩中的金矿床，黄铁矿为“电子心”、“空穴心”混合型导电，个别的为单一的“空穴心”导电。

Most of the pyrites from Mesozoic vein gold deposits and gold deposits hosted in volcanic and sub-volcanic rocks belong to the mixed type of N-type and P-type electric conductivity except a few belonging to simple N-type .