掺铒SiO_x1.54μm强的室温光致发光

采用等离子化学汽相淀积方法，改变SiH_4和N_2O的流量比制备含有不同氧浓度的SiO_x。用离子注入方法将铒掺入SiO_x,经300～935℃快速热退火，在波长1.54μ处观察到很强的室温光致发光(PL)。发光强度随氧含量和激发功率增加而增加，与SiO_x的微结构有非常密切的关系。对可能的发光机理进行了讨论。

a-SiCx∶H和β-SiC中Er缺陷结构及其1.54μm发光探索

材料科学开放实验室基金,光学信息技术科学教育部开放实验室基金

掺铒a-Si∶H,O薄膜1.54μm光致发光和微结构

国家自然科学基金,国家攀登计划

铒、氧共注a-Si:H和a-SiCx:H的1.54μm光致发光

在a-Si:H和a-SiCx:H中共注稀土铒和氧。300 ℃和400 ℃热退火后,测得了来自发光中心Er~(3+)内层4f电子跃迁的1.54 μm光致发光。400 ℃是较好的退火温度。随着碳含量的增加,发光强度逐渐减弱,这可能是由于碳的引入减弱了间隙氧退火时的迁移能力所致。

Er离子在Inp、GaAs和Si中的1.54μm特征发光峰

分别在InP、GaAs和Si中以7×10＜′14＞和1×10＜′15＞cm＜′－2＞的剂量进行Er离子注入, 并采用闭管、快速和炉退火等热处理。低温光致发光（PL）、反射式高等电子衍射和卢瑟福背散射实验研究表明, 上述样品中Er＜′3＋＞离子特征发光的中心波长均出现在1．5μm处, 其中InP的发光峰最强, 而注入损伤的恢复是影响Er＜′3＋＞发光的重要因素之一。卢瑟福背散射分析进一步证实退火后Er原子在Si中向表面迁移, 而在InP中的外扩散较小, 并比较了Er在InP和Si晶格中的占位情况。图7参12

1.54 mu m near-infrared photoluminescent and electroluminescent properties of a new Erbium (111) organic complex

The crystal structure of Er(PM)(3)(TP)(2) [PM = 1-Phenyl-3-methyl-4-isobutyryl-5-pyrazoloiie, TP = triphenyl phosphine oxide] was reported and its photoluminescence properties were studied by UV-vis absorption, excited, and emission spectra. The Judd-ofelt theory was introduced to calculate the radiative transition rate and the radiative decay time of 3.65 ms for the I-4(13/2) -> I-4(15/2) transition of Er3+ ion in this complex.

1.54 mu m infrared photoluminescence and electroluminescence from an erbium organic compound

Infrared emission at 1.54 mu m excited optically and electrically from an erbium organic compound tris(acetylacetonato)(1,10-phenanthroline) erbium [Er(acac)(3)(phen)] is observed. The rare-earth complex is dispersed into a polymer matrix of poly(N-vinylcarbazole) (PVK) to fabricate an electroluminescent (EL) device with an ITO/PVK:Er(acac)(3)(phen)/Al:Li/Ag structure, where ITO represents indium-tin-oxide-coated glass. The device shows infrared EL emission at 1.54 mu m, which suggests a simple and cheap method to obtain a light source for 1.54-mu m-wavelength devices in optical communications. (C) 2000 American Institute of Physics. [S0021-8979(00)00301-7].

Sedimentation rates and provenance analysis in the Southwestern Okinawa Trough since the mid-Holocene

As a high-sedimentation rate depocenter along the path of the Kuroshio Current, the southwesternmost part of the Okinawa Trough is a key area to understand the Kuroshio history and sediments transportation. A 34.17-m-long sediment core was obtained by the advanced piston corer of Marco Polo/IMAGES XII MARION DUFRESNE during the May 2005 from the Southern Okinawa Trough at site MD05-2908. The recovered sediments were analyzed by AMS C-14 dating, coarse size fraction (> 63 mu m) extraction and moisture content determination in order to study its sedimentation flux and provenance. The depth-age relationship of core MD05-2908 was well constrained by 17 C-14 dating points. The sediments span across the mid-Holocene (6.8 ka B.P.) and have remarkablely high sedimentation rates between 1.8 and 21-2 m/ka, which is well consistent with the modern observations from sediment traps. We identified five 70-200 a periods of abnormally rapid sedimentation events at 6790-6600 a B.P., 5690-5600 a B.P., 4820-4720 a B.P., 1090-880 a B.P., and 260-190 a B.P., during which the highest sedimentation rate is up to 21-2 m/ka. In general, the lithology of the sediments were dominated by silt and clay, associated with less than 5% coarse size fraction (a parts per thousand << 63 mu m). As the most significant sediment source, the Lanyang River in northeastern Taiwan annually deliver about 10Mt materials to the coastal and offshore region of northeast Taiwan, a portion of which could be carried northward by currents toward the study area. Therefore, we concluded that the 5 abnormally rapid sedimentation events may be related to intensified rainfall in Taiwan and thus increased materials to our study area at that time. However, a few extreme-rapid sedimentation events cannot be explained by normal river runoff alone. The large earthquakes or typhoons induced hyperpycnal discharge of fluvial sediment to the ocean may also act as a potential source supply to the Okinawa Trough.