Highly conductive and transparent Al-doped ZnO （AZO） thin films were prepared from a zinc target containing Al （1.5 wt.%） by direct current （DC） and radio frequency （RF） reactive magnetron sputtering. The stru...Highly conductive and transparent Al-doped ZnO （AZO） thin films were prepared from a zinc target containing Al （1.5 wt.%） by direct current （DC） and radio frequency （RF） reactive magnetron sputtering. The structural, optical, and electrical properties of AZO films as-deposited and submitted to annealing treatment （at 300 and 400℃, respectively） were characterized using various techniques. The experimental results show that the properties of AZO thin films can be further improved by annealing treatment. The crystallinity of ZnO films improves after annealing treatment. The transmittances of the AZO thin films prepared by DC and RF reactive magnetron sputtering are up to 80% and 85% in the visible region, respectively. The electrical resistivity of AZO thin films prepared by DC reactive magnetron sputtering can be as low as 8.06 x 10-4 Ωcm after annealing treatment. It was also found that AZO thin films prepared by RF reactive magnetron sputtering have better structural and optical properties than that prepared by DC reactive magnetron sputtering.展开更多
We present a case study of applying MT （magnetotellurics） and CSAMT （controlled source audio-frequency magnetotelluries） for geophysical exploration in Jiangxia （江夏）, which is located in new industrial develop...We present a case study of applying MT （magnetotellurics） and CSAMT （controlled source audio-frequency magnetotelluries） for geophysical exploration in Jiangxia （江夏）, which is located in new industrial developing suburb, where artificial noises are severe. In order to know deep buried structure, fracture status, and characteristics of underground geothermal development about 2 km, we acquired MT and CSAMT data to image subsurface structure through inversion and joint interpretation. The electrical terms of the 2D MT inversion can be divided into three ranges of resistivity values： （1） a highly resistive （〉350 ~.m） layer mainly characteristic of limestone, dolomitic limestone, leuttrite, silicarenite, and packsand; （2） an intermediate resistivity （250-350 Ω·m） layer mainly constituted by siliceous shale, siltstone, battie, and ampelitic limestone; and （3） a low resistivity （20-250 Ω·m） layer, from surface to-100 m, which is related to lacustrine alluvium of Quaternary period; the deep low resistivity layer is interpreted to be representative of the geothermal field. The result of the 2D CSAMT inversion reveals two layers of different electrical resistivities： （1） the first resistive layer （20-250 Ω·m）, which is related to lacustrine alluvium of Quaternary period and the heat source, and （2） the second resistive layer （250-3 000Ω·m）. The heat source appears to be bounded within the middle of exploration area and shows the N-S trend. Its depth ranges from more than 1.2 to less than 0.7 km, and its resistivity values range from 20 to 250 Ω·m in the northeast part of Jiangxia. Comparing the results of MT and CSAMT method, the positive anomalies are similar and can be assumed to be generated by the same source.展开更多
基金the Program for New Century Excellent Talents in Universities, MOE, China (No. NCET-05-0764)the Tackle Key Problems on Scientific Technology Foundation of Chongqing Municipality (Nos. CSTC2005AA4006-A6 and CSTC2004AC4034)+2 种基金the Natural Science Foundation of Chongqing Municipality (No. CSTC2005BA4016)China Postdoctoral Science Foundation (No. 2005037544)the Inno-base for Graduates of Chongqing University (No. 200506Y1B0240131).
文摘Highly conductive and transparent Al-doped ZnO （AZO） thin films were prepared from a zinc target containing Al （1.5 wt.%） by direct current （DC） and radio frequency （RF） reactive magnetron sputtering. The structural, optical, and electrical properties of AZO films as-deposited and submitted to annealing treatment （at 300 and 400℃, respectively） were characterized using various techniques. The experimental results show that the properties of AZO thin films can be further improved by annealing treatment. The crystallinity of ZnO films improves after annealing treatment. The transmittances of the AZO thin films prepared by DC and RF reactive magnetron sputtering are up to 80% and 85% in the visible region, respectively. The electrical resistivity of AZO thin films prepared by DC reactive magnetron sputtering can be as low as 8.06 x 10-4 Ωcm after annealing treatment. It was also found that AZO thin films prepared by RF reactive magnetron sputtering have better structural and optical properties than that prepared by DC reactive magnetron sputtering.
基金supported by the National Natural Science Foundation of China (No. 40974040)the Deep Exploration in China (No. SinoProbe-01-03-02)the Ministry of Land and Resources of China
文摘We present a case study of applying MT （magnetotellurics） and CSAMT （controlled source audio-frequency magnetotelluries） for geophysical exploration in Jiangxia （江夏）, which is located in new industrial developing suburb, where artificial noises are severe. In order to know deep buried structure, fracture status, and characteristics of underground geothermal development about 2 km, we acquired MT and CSAMT data to image subsurface structure through inversion and joint interpretation. The electrical terms of the 2D MT inversion can be divided into three ranges of resistivity values： （1） a highly resistive （〉350 ~.m） layer mainly characteristic of limestone, dolomitic limestone, leuttrite, silicarenite, and packsand; （2） an intermediate resistivity （250-350 Ω·m） layer mainly constituted by siliceous shale, siltstone, battie, and ampelitic limestone; and （3） a low resistivity （20-250 Ω·m） layer, from surface to-100 m, which is related to lacustrine alluvium of Quaternary period; the deep low resistivity layer is interpreted to be representative of the geothermal field. The result of the 2D CSAMT inversion reveals two layers of different electrical resistivities： （1） the first resistive layer （20-250 Ω·m）, which is related to lacustrine alluvium of Quaternary period and the heat source, and （2） the second resistive layer （250-3 000Ω·m）. The heat source appears to be bounded within the middle of exploration area and shows the N-S trend. Its depth ranges from more than 1.2 to less than 0.7 km, and its resistivity values range from 20 to 250 Ω·m in the northeast part of Jiangxia. Comparing the results of MT and CSAMT method, the positive anomalies are similar and can be assumed to be generated by the same source.
