查询词典 I.V.

Type II cells were mainly distributed in layer V of cortex. It appeared that these cells receive the CRF immunostaining fibers terminals afferent from other cells rather than synthesize CRF by themselves. It is probable that type II cells receive afferent fibers from both extracortex and type I cells within layers II -III cortex. Considered that Type I cells morphologically are inhibitory interneuron, we presumed that type I in layer II -III could inhibit activity of type II cells in layer V.

CRF阳性Ⅱ型细胞主要分布在皮层第Ⅴ层，形态学特征显示这类细胞更像是接收来自其它神经元的CRF纤维投射而非自身分泌CRF，证据显示Ⅱ-Ⅲ层CRF神经元纤维可进入第Ⅴ层，考虑到皮层的CRF神经元形态上为抑制性中间神经元，这些结果提示Ⅱ-Ⅲ层CRF神经元能够抑制第Ⅴ层神经元的活动。

According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

由于BOM没有考虑透射太阳辐射的物理过程，研究表明透射太阳辐射对北冰洋的能量收支起到重要作用，因此在BOM模式中引入了对透射太阳辐射的处理；通过对不同水道反照率的数值试验表明海冰厚度对水道反照率的敏感性不强，可能与海冰区水道面积占的比率很小有关；而模式模拟的北极海冰夏季&过度融化&主要源于NCEP再分析资料提供了偏大的太阳短波辐射；对北极海冰的气候变率进行了模拟研究，结果表明：模拟的海冰厚度变化与潜艇探测的海冰吃深度变化具有一致性；模拟和观测的亚欧大陆沿海的年内最大海冰厚度有很好的相关；模拟的海冰移速与长期平均的卫星反演的海冰移速具有相同的速度分布特征；模拟的各个海区海冰面积的变化趋势与卫星反演资料分析的结果基本一致；模拟与观测的主要海洋分区的海冰密集度具有很好的相关：弗瑞姆海峡的海冰体积和面积的输送涉及到海冰密集度、厚度和移动速度，是判断模式模拟能力的一个综合的指标，模式模拟的结果与卫星反演或重建的面积输送、体积输送具有很好的一致性；(5)分析了模拟的北极海冰厚度的气候变率及气候平均表层海流场，结果表明：北极海冰的总体积有显著减少的趋势，北极海冰总体积的变化具有10a际尺度振荡的特点，存在18-20a和12-13a两个主周期；北极海冰的平均厚度在各个海区的变化趋势不同，在巴伦支—喀拉海和巴芬湾—拉布拉多海地区海冰厚度有显著的增加趋势，而其它海区存在减少的趋势；通过对模拟的气候平均表层海流的分析表明，北极河流流量超前弗瑞姆海峡海冰流量7-10年的特征时间尺度与表层海流的气候分布存在着必然联系：(6)利用模拟结果以及中国降水、气温和热带关键区SST资料，讨论了北极各海区海冰平均厚度与中国降水、气温以及热带关键区SST的关系，结果表明：在北极中心海区和楚科奇—波弗特海海冰厚度偏大，在巴伦支—喀拉海以及巴芬湾—拉布拉多海海冰厚度偏小，则中国降水在华南地区、青藏高原和东北北部降水偏少，反之相反；在北极中心海区、东西伯利亚海、楚科奇—波弗特海以及格陵兰海海冰厚度偏小，在巴芬湾—拉布拉多海海冰厚度偏大，则在中国东北地区、高原南部地区和海南岛附近气温偏低，反之相反；另外，北极楚科奇—波弗特海和巴芬湾—拉布拉多海海冰厚度偏大时，在热带中东太平洋海温偏高，而在热带东南印度洋海温偏低。

Two complemented lattices L_1, L_2 are said to be of the same "type" if they have identical sets of tautologies.

一个具有最小元O及最大元I的格L，如果在其中又定义了一个单值的1元运算&′&能适合O′=I，I′'=O，则称L为一可补格，一个命题演算良构式A(设只含命题连接词A，V，～)，如果命它的变数在L中任意取值且将A，V，～分别解释为L中的运算∩，U，′时，A永远得到值I，则称A为L上的恒I式，当两个可补格L_1，L_2上的恒I式集相同时，称L_1，L_2为同型的，本文就是讨论可补格按同型关系分类的问题，所得结果如下：定理设有限可补格L_2适合条件：，存在一良构式A能使则任一可补格L_1与L_2同型的一个充分必要条件是：(A_1)。

March 14, 2000 L a 'st Tue s 'day a 'fternoon' Con'sul Gen' e ral Da'vid Hopper, the he a d of v i ' s a op' e ra'tions at the Am e 'rican Em'bassy, came to Peking U'niver'sity wi th three oth 'er v i ' s a of'ficers to explain' the "se'crets" of apply'ing for a US stu'dent v i ' s a, and were wel'comed by the stu'dents.

3月14日上周二下午，美国驻华使馆总领事贺德炜先生带着三名签证官，一行四人来到北京大学，向大学生们宣讲申请赴美留学签证的&秘诀&，受到大学生们的欢迎。

With the increase of establishment years, most of plant communities on the grasslands showed a "V" type change trend in their quantities, i.e., high-low-high, hut the forbs biomass had a "Λ" type change trend and the sedge biomass increased gradually. Soil nutrients presented a "V" type hut soil hulk density presented a "Λ" type change trend, bile soil pH presented a decreasing trend. Most of soil microbial physiological groups and microbial biomass carbon showed a "V" type change trend, phosphorus-dissolving bacteria showed a "Λ" type change trend, denitrifying bacteria decreased gradually, while cellulose-decomposing bacteria showed an increasing trend.

结果表明：随着人工草地建植年限的增加，植物群落的数量特征多呈高－低－高、杂类草生物量低－高－底、莎草生物量增加的趋势；土壤养分变化为高－低－高、容重为低－高－底、pH呈下降趋势；土壤中多数微生物的数量及微生物生物量碳含量的变化为高－低－高，纤维素分解菌数量逐渐升高，而反硝化菌数量逐年下降，溶磷菌数量呈低－高－低的动态变化。

The result in this part also accorded to that of HPLC in the second chapter(The totle content of uridine、hypoxanthosine、guanosine、adenosine in the counterfeits and adulterations was lower than 1.99mg/g, the content of adenosine was lower than 0.44 mg/g).

混淆品及伪品中I 、II、III、V四个核苷的总量介于1.219 mg/g～1.803 mg/g，V的含量介于0.364 mg/g～0.423 mg/g，与第二章高效液相的研究结果吻合（混淆品及伪品四个核苷成分的总量小于1.99 mg/g，V的含量小于0.44mg/g）。

The result in this part accorded to that of HPLC in the second chapter(The totle content of uridine、hypoxanthosine、guanosine、adenosine in Cordyceps sinensis .was higher than 2.50mg/g, the content of adenosine was higher than 0.75 mg/g). The totle content of uridine、hypoxanthosine、guanosine、adenosine in the counterfeits and adulterations was from 1.219 mg/g to1.803mg/g ,the content of adenosine was from 0.364 mg/g to0.423 mg/g .

应用HPLC-MS对冬虫夏草及其混淆品与伪品进行二级质谱定量分析，结果显示，冬虫夏草中I 、II、III、V四个核苷的总量介于2.473 mg/g～2.830 mg/g，V的含量介于0.850 mg/g～1.009 mg/g，与第二章高效液相的研究结果吻合（冬虫夏草四个核苷成分的总量大于2.50mg/g，V的含量大于0.75 mg/g）。

All the number ruff people in facted with each H .I.V.

今天大约有500万人在亚洲被感染了艾滋病毒导致艾滋病。

It is a polymeric coupling agent that reacts with degraded polymers to restore the original molecular weight as well as I.V. and melt viscosity.

它是通过与已降解聚合物进行化学反应，恢复其原来的分子量和特性粘度，增大熔融粘度。

Children of treatment group were treated by genciclovir with 5 mg/kg i.v.

有关治疗CP儿童CMV感染的报道不多，本研究观察更昔络韦治疗CP儿童CMV感染的疗效。1资料与方法1.1临床资料2002年1月~2004年12月在我院儿童脑瘫康复中心治疗的36例CMV感染CP病例，CP诊断符合2004年全国小儿脑性瘫痪的定义、诊断条件及分型标准[3]，CMV感

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。