胃癌术中区域动脉灌注联合腹腔缓释化疗的临床研究

目的探讨胃癌术中区域动脉灌注联合腹腔缓释化疗的临床效果。方法将80例进展期胃癌患者随机分为治疗组和对照组,治疗组于胃癌根治术中经肿瘤的主要供血动脉灌注含5-氟尿嘧啶和丝裂霉素的生理盐水灌注液,术毕将5-Fu缓释剂植入肿瘤病灶区域、吻合口周围及淋巴回流区等区域。对照组术中不进行腹腔内干预性治疗。结果两组术后复发及转移率、3年和5年生存率的差异较大,有统计学意义,治疗组优于对照组。结论胃癌术中区域动脉灌注联合腹腔缓释化疗应用于临床,疗效肯定,具有推广应用价值。     

Continental subduction channel processes: Plate interface interaction during continental collision

The study of subduction-zone processes is a key to development of the plate tectonic theory. Plate interface interaction is a basic mechanism for the mass and energy exchange between Earth＇s surface and interior. By developing the subduction channel model into continental collision orogens, insights are provided into tectonic processes during continental subduction and its products. The continental crust, composed of felsic to mafic rocks, is detached at different depths from subducting continental lithosphere and then migrates into continental subduction channel. Part of the subcontinental lithospheric mantle wedge, composed of perido- tile, is offscrapped from its bottom. The crustal and mantle fragments of different sizes are transported downwards and upwards inside subduction channels by the corner flow, resulting in varying extents of metamorphism, with heterogeneous deformation and local anatexis. All these metamorphic rocks can be viewed as tectonic melanges due to mechanical mixing of crust- and man- lie-derived rocks in the subduction channels, resulting in different types of metamorphic rocks now exposed in the same orogens. The crust-mantle interaction in the continental subduction channel is realized by reaction of the overlying ancient subcontinental lithospheric mantle wedge peridotite with aqueous fluid and hydrous melt derived from partial melting of subducted continental basement granite and cover sediment. The nature of premetamorphic protoliths dictates the type of collisional orogens, the size of ultrahigh-pressure metamorphic terranes and the duration of ultrahigh-pressure metamorphism.     

Diachroneity of continental subduction and exhumation: Constraints from the Permian-Triassic HP metamorphic terrane in the Tongbai orogen, central China

High-pressure （HP） metamorphic terrane in the Tongbai orogen comprises two HP slices （I and II） and a tectonic m61ange zone in the northeast and a blueschist-greenschist zone in the southwest. HP slice I is represented by the northern and southern eclogite zones on the two sides of the Tongbaishan antiform. HP slice II is represented by retrograded eclogite-bearing metamorphic en- claves in Cretaceous gneissic granites in the Tongbai Complex. U-Pb, Lu-Hf, Rb-Sr and 4Ar/39Ar multichronometric data indi- cate that the peak metamorphism of HP slice I took place at -255 Ma, whereas the metamorphic ages of HP slice II are as young as 232-220 Ma. By contrast, the tectonic melange zone near the suture was metamorphosed at -256 Ma. Such a diachroneity of dif- ferent slices across the direction of the orogen in the Hong＇an-Dabie-Sulu HP/UHP terrane is ubiquitous, and it can be interpreted by a syn-subduction detachment/exhumation model. Furthermore, the metamorphic age of HP slice I in the Tongbai orogen is older than that of the equivalent HP slice in the Hong＇an orogen by ~15 Ma, suggesting that the diachroneity may have also ex- isted along the direction of the orogen. A seesaw-type subduction/exhumation model is proposed to explain this age disparity and the subduction of the South China Block becomimg shallower towards the west.     

气体扩散电极制备条件与氧还原反应活性关系的研究

在改变催化层中聚四氟乙烯(PTFE)、造孔剂含量和热压压力等条件下制备气体扩散电极,通过计时电位法、阴极极化曲线对气体扩散电极进行测定,并将其结果用最小二乘法拟合得出电极的制备条件与氧气还原反应电化学参数之间的关系。电化学测试结果表明,各种条件下制备的电极的阴极极化过程都符合Rho提出的半经验公式规律;当气体扩散电极催化层PTFE面密度3.33mg/cm²、造孔剂(NH₄)HCO₃面密度1.05mg/cm²以及热压压力3.69MPa时,气体扩散电极的氧还原活性最佳。     

班公湖－怒江缝合带侵入岩地球化学和年代学特征及形成构造背景

对西藏纳屋错地区班公湖－怒江缝合带西段的侵入岩进行岩石地球化学和锆石 U-Pb年龄测定,并与缝合带以外南面岩浆弧侵入岩进行对比。岩石地球化学分析表明,缝合带内侵入岩样品均属于钙碱性和高钾钙碱性系列,隶属于岛弧型岩浆岩类。稀土元素球粒陨石标准化分布模式均表现出 LREE 富集、HREE 相对亏损的右倾模式,痕量元素原始地幔标准化蛛网图显示样品总体上富集大离子不相容元素（HFSE）Rb、K、Ba,亏损高场强元素（LILE）Nb、Ta、Ti、P,体现了钙碱性系列岩体的特征和演化趋势;年代学分析表明,带内侵入岩的成岩时代集中在早白垩世（104．5～141．7 Ma B．P．）;进一步的构造环境对比分析表明,所有侵入岩样品均属于岛弧型-大陆碰撞型花岗岩类,但缝合带内岩浆岩属性为同碰撞花岗岩,缝合带具由钙碱性向高钾钙碱性演化的特征和趋势,形成于受逆掩构造或地壳剪切作用的造山时期,处于威尔逊旋回的“陆陆碰撞造山-山带剥蚀”阶段,认为班-怒缝合带西段存在双向俯冲的碰撞造山构造背景。     

基于频率调制二元编码光栅相位测量剖面术

分析传统的频率调制正弦光栅用于3步相移相位测量剖面术时,系统非线性对测量精度的影响,提出采用二元频率调制光栅,提高3步相移相位测量剖面术计算绝对相位测量精度的方法.完成了分别采用传统正弦频率调制光栅投影和基于Floyd-Steinberg二元编码频率调制光栅投影的相移剖面术的绝对相位计算结果对比.结果表明,采用正弦频率调制光栅模板的3步相移算法对系统的非线性敏感,而二元编码频率调制光栅模板既保持了利用单组条纹投影就可计算条纹绝对相位的优点,又不受系统非线性的影响,大大提高了基于频率调制光栅的相移剖面术的测量精度.计算机模拟和实验验证了所提方法的有效性.     

前列腺增生症合并腹股沟疝同期手术治疗31例体会

探讨前列腺增生并腹股沟疝同期行经尿道前列腺电切术与无张力疝修补术治疗的效果及经验。对31例前列腺增生合并腹股沟疝患者行同期经尿道前列腺电切术及无张力疝修补术。31例无大出血、切口感染及电切综合征等并发症发生,平均术后住院时间为11d,随访1~3年。均排尿顺畅,无疝复发及其它并发症。采用同期经尿道前列腺电切术及无张力疝修补术治疗前列腺增生并腹股沟疝安全有效,避免了二次手术痛苦,减少了费用,适宜在基层农村选择应用。     

一次性与常规根管治疗术治疗急性牙髓炎的效果对比分析

探讨一次性与常规根管治疗术治疗急性牙髓炎的效果。选取于本院进行治疗的急性牙髓炎患者100例,并随机分为观察组和对照组各50例。对照组行常规根管治疗术,观察组行一次性根管治疗术。观察并记录两组患者的手术成功率以及一年后病情的复发情况。观察组手术成功率显著高于对照组(P0.05),复发率明显低于对照组(P0.05)。一次性根管治疗术治疗急性牙髓炎可有效提高患者临床治疗效果,值得临床推广。