一维复式排列量子线阱的集体激发

利用流体力学方法计算了1+1维复式排列量子阱的集体激发谱.     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

淮南矿区深部岩巷典型围岩参数反分析研究!

基于典型巷道的表面收敛位移,通过进化神经网络方法进行了淮南矿区典型围岩类型的物性参数反分析研究.采用反分析得到的参数,通过数值正分析得到了和实测基本吻合的深部位移结果.表明通过反分析研究,基本得到了反映典型围岩类型的物性参数.     

GaAlN/GaN量子阱中电子的激发态极化

考虑了纤锌矿结构材料的各向异性造成的内建电场的作用，计算了GaN／GaAlN量子阱内电子的激发态极化．结果表明．电子偶极矩改变随Al浓度的增加非线性减小．一般情况下激发态极化产生的电场强度远小于内建电场．可忽略不记，但当n取较大值(10^19／cm^3以上)时，即材料被重掺杂时，激发态极化产生的电场强度对内建电场的影响不能忽略．     

卡洼掌井田勘探工程实践

为了开发宁缠煤田东部卡洼掌矿区的煤炭资源,在充分利用已往勘探成果的基础上,采用钻探、槽探、坑探、地球物理测井、地质填图、采样测试等多种勘查手段,提高了对煤炭资源的控制程度、开采技术条件的查明程度及勘探精度,为矿井建设可行性研究和初步设计提供了可靠的地质依据。     

低渗透油气藏水平井压裂优化设计

介绍了水平井压裂裂缝的形态、压裂水平井的渗流特征、压后产能预测;探讨了裂缝条数、裂缝长度和裂缝导流能力的优化以及不同的裂缝布局和不同位置的裂缝对压后产量的影响.通过X井水加喷砂压裂位置测井数据进行压裂裂缝模拟,优化设计与现场施工的加砂量和排量比较一致.     

基于利益机制的校企深度合作研究

高职校企合作已经取得一定的成效,但是就目前的发展状况来看,校企合作从深度和广度上来说都到了一个瓶颈阶段,究其原因在于,参与各方缺乏一个有效的利益约束和激励机制。因此,明确参与各方的责权利,以利益共同体为研究视角,对于深化校企合作有重要的意义。     

人类学仪式视阈下的藏族母语小说——以藏文小说《肩胛骨之魂》为例

在人类学仪式理论的框架中,藏文小说文本《肩胛骨之魂》可以看作一个“阈限”仪式,从文本的“深描”和来自这个社会的成员那里可以得到这种回应。这篇小说至少承载了一种人类学的想像,通过人类学仪式理论来理解和研究这部作品,便于区别“魔幻现实主义”这种对藏族文学作品较刻板化的研究视角。     

激发数学学习兴趣的策略

针对多数学生对学习数学有枯燥、乏味的感觉，阐述了必须在教学中采用生动的富有感染力的教学方法，以激发学生对数学学习的浓厚兴趣，使学生在提出问题和解决问题中养成善于思考，勇于探索的良好品质。