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.     

脑深部神经刺激微电极的表面改性研究

为了提高脑深部刺激电极的生物相容性,降低脑组织的免疫反应,减少或抑制电极周围包裹物的形成,对电极植入端聚氨酯材料进行了表面改性处理.首先用N₂/H₂进行等离子体处理,在电极表面生成活性基团——氨基,再利用电极表面的氨基基团与YIGSR多肽分子发生聚合反应,从而实现在电极表面修饰上对神经细胞具有促进生长作用的多肽分子.改性电极的大鼠植入实验结果发现,改性电极能够在一定程度上减少胶质包裹物的形成,有利于电极与神经细胞之间接触,增加有效刺激体积,证明了电极聚氨酯材料表面接枝聚合生物大分子的可行性,对今后电极表面改性的深入研究具有一定的参考意义.     

深基坑出碴方案比选

深基坑出碴在一些情况下会成为制约工期的关键因素,尤其是复杂地形条件下,在首先满足工期的前提下,还要综合考虑现有机械情况、技术条件和经济效益以及其他作业干扰,这使得深基坑出碴变得更加复杂。文章通过准朔铁路黄河特大桥工程特点,对几种深基坑出碴方案进行了分析对比,综合考虑后选择了履带吊出碴方案。     

深层搅拌桩在深基坑支护工程中的应用

介绍了搅拌桩在南京某复杂土层围护工程中的应用,探讨了质量控制和局部构造措施,指出搅拌桩支护的优势.     

深度脑刺激的精确闭环去同步控制

深度脑刺激(DBS)是治疗帕金森症和癫痫等神经疾病的有效方法之一.针对其开环控制的缺点,以MorrisLecar神经元为节点模拟病态同步神经元网络,提出了基于H∞变论域模糊的DBS闭环控制方法,实现了神经元网络的精确去同步控制.采用变论域模糊逼近神经元非线性动态和H∞抑制逼近误差,利用李雅普诺夫稳定性理论证明控制算法的稳定性并进行了仿真分析.仿真结果验证了所提方案的有效性及鲁棒性,该方法可作为由病态同步引起的神经疾病的一种潜在电刺激治疗方案.     

5A02铝合金板料深冲有限元模拟与实验研究

对5A02铝合金板料深冲过程进行了实验研究,并在率相关晶体塑性本构理论框架下,实现了5A02铝合金板料深冲过程的晶体塑性有限元模拟.研究了深冲过程中的制耳和板厚的分布情况,分析预测了极限拉深系数值;结果表明,晶体塑性有限元法模拟的制耳轮廓的高度和极限拉深系数值与实测值比较吻合,板料的厚度变化与实际情况一致.     

地下连续墙加内撑基坑变形监测分析

广州市轨道交通四号线北延段黄村站为地下两层一岛一侧站台车站,该站所处环境复杂,周围道路交错,交通繁忙而且占据重要地理位置(位于奥体中心主会场的西南侧),所以确定本基坑安全等级为一级.文章就本站在施工期间所观测的测斜、沉降成果,分析了其变化的规律,墙体变形的原因.旨在为以后类似支护结构(连续墙加内支撑)的基坑施工提供指导意见.     

废内燃机油的预处理过程及其产物性质分析

对废内燃机油进行了热处理-蒸馏深拔的预处理研究,结果表明:经过热处理后两种废油40℃的黏度分别降低36.20%和48.79%,杂原子总含量分别降低56.11%和50.25%,杂元素总含量分别降低86.81%和87.12%,基本达到降黏除杂的目的;热处理后的废油经蒸馏深拔后回收利用率达到了89.72%,同时实现了黏度的进一步降低,杂原子和杂元素的进一步脱除,获得了适合加氢改质的原料油。     

新课程下化学教学的反思

新课程下如何实施化学的高效课堂教学?从转变教学思想,科科学把握教学深广度,精心策划教学设计,灵活用用教学策略,作业布置,学习效果的评价方式等方面做了反思与总结.     

深基坑回弹观测及应注意的问题

对平煤集团经调中心进行了基坑回弹观测 ,着重介绍回弹观测的观测方法、观测过程、误差来源、精度分析及观测中应注意的问题