润楠雄配子体发育的超微结构研究 Ⅲ.营养细胞和生殖细胞的形成

对润楠(Machilus pingii Cheng ex Yang)花粉生殖细胞和营养细胞的形成进行了观察.结果如下:(1)随着小孢子核向(?)方向迁移,胞质的线粒体和前质体显著增多;由于大液泡的存在,细胞器偏向核的一侧分布.(2)小孢子有丝分裂末期,胞质中出现较多的高尔基体和微管.(3)生殖细胞(?)抵达花粉内壁后,生殖细胞和营养细胞的胞质中出现大量与壁平行排列的粗面内质网.随着生殖细胞壁的加厚, 生殖细胞的局部与营养细胞核相贴近,贴近区域的生殖细胞质中出现交织成网的内质网.(4)游离的生殖细胞具,胞质中仅有少量细胞器;营养细(?)中储存有大量的淀粉粒.从观察结果推测:影响润楠生殖细胞在花粉内进一步分裂的因素可能有三种:一是生殖细胞壁留存的时间;二是营养细胞和生殖细胞本身的代谢状况;三是营养细胞核对生殖细胞的作用.     

不同条件下麝香石竹玻璃苗的诱导形成及其生理特性研究

研究了不同培养基及外植体条件下麝香石竹玻璃苗的诱导形成及玻璃苗部分生理特性。本文研究认为：麝香石竹玻璃的形成是培养基和外植体因素相互作用的结果，培养基极端的水分环境可能是导致玻璃苗形成的外在原因。     

山东临沂煤田本溪组Profusulinella带层位的发现及其地质意义

本文首次证实山东临沂煤田本溪组的层位均属于Profusulinella带,而华北地区本溪组普遍发育的Fusulina—Fusulinella带则在本区缺失。文中共记述了蜓类7属42种和亚种,其中包括6个新种。另外还对其在古地理、构造方面的意义作了讨论。     

三元配合物La(Et2 dtc)3(phen)的热化学性质

目的研究三元配合物La(Et2dtc)3(phen)的热化学性质.方法采用了微量热法和燃烧法.结果铜试剂(NaEt2dtc·3H2O)和邻菲咯啉(phen·H2O)与水合氯化镧(LaCl3·3.94H2O)在无水乙醇中反应,制得三元固态配合物La(Et2dtc)3(phen).在298.15 K下测得了该配合物的液相生成反应的焓变△rHθm(l),为(-8.801±0.043)kJ/mol,计算了固相生成反应的焓变△rHθm(s),为(70.428±0.293)kJ/mol;配合物的恒容燃烧能△cU为(-17 455.98±7.98)kJ/mol,其标准燃烧焓△cHθm和标准生成焓△fHθm经计算分别为(-17 475.19±7.98)kJ/mol,(-1 257.78±8.84)kJ/mol.结论IR光谱表明该配合物中La3+与3个NaEt2dtc中的6个硫原子双齿配位,同时与邻菲咯啉中的2个氮原子双齿配位,配位数为8.     

Simulation of sub micron particle formation and growth during combustion processes

Recently ,hazardscausedbysuspendedparticu latematter (SPM ) ,especiallybyparticleswithdiam etersmallerthan 1.0 μm (PM 1.0 ) (calledsub mi cronparticles) ,havereceivedmuchattentionintheenvironmentalresearch[1] .Combustion processcaninherentlyresultintheformationofsub micronparti clesanditisamajorsourceofatmosphericloadingofsuch particles .Thesecombustiondevicesincludesmelters,coalcombustion ,waste to energyincinera tors ,andcementkilns .Althoughenvironmentalreg ulationsaredesignedandusedunde…     

Petrological implication of wagnerite-Ma5bc in the quartzofeldspathic gneiss, Larsemann Hills, East Antarctica

Mg dominantmineralsofwagnerite triplite group,i.e.(Mg,Fe,Mn)2(PO4)(F,OH),arerelativelyrare,buthavebeenfoundinawidevariety ofgeologicenvironments,includingmetamorphic rocksofallgrades[1]suchasquartz carbonateveinsof hydrothermalorigin,pegmatites,kyanite quartzite,micaschist,sillimanitegneiss,andmagnetiteores.Uptonow,wagneriteispresentmainlyasthe Ma2bcpolytype,anaccessorymineralincalcium poorrocks[2,5]inwhichapatite,ifpresent,oftenoc cursasretrograderimaroundwagnerite.Henriques[6]reportedasma…     

基于AMl量化参数的卤代甲烷Δ_fH_m~θRBF—NN模型的构建

应用G98W程序包中的AMl方法对45个卤代甲烷分子进行优化计算,所得中心碳原子的静电荷密度(Qc)、分子的最高占据轨道能级(HOMO)和最低空轨道能级(LUMO)量化参数作为径向基人工神经网络的输入向量,选用df=10,eg=10-3对卤代甲烷ΔfHθm进行建模,所建模型预测值与其实验值吻合得很好.故这一新方法具有一定的参考价值.     

机动目标空间合群仿真

为了解决空间合群和战场中的事件检测问题，提出了一种新的机动目标的空间群生成算法．该算法通过一级融合获得的信息来定义特征相似度，即归属相似度、位置相似度和速度相似度，并将这些相似度再次融合以求得合群结果．由于测量空间的不确定性被映射到了模糊相似度空间，因此通过模糊匹配机制可解决测量空间的不确定性问题．仿真结果表明，所提算法能实时完成多个级别的空间合群融合，其计算复杂度也比较低，而且在空间合群的态势评估中获得了比较好的结果．     

Abnormal high pressure in Kuqa foreland thrust belt of Tarim basin: Origin and impacts on hydrocarbon accumulation

Following analyses of the abnormal high pressure distribution characteristics, based on the geological characteristics, tectonic stress field and physical simulation, we investigated the formation mechanisms of abnormal high pressure and its impacts on hydrocarbon accumulation in the Kuqa foreland thrust belt. The abnormal high pressure appears at the bottom of the Paleogene and obviously exists in the Triassic and Jurassic. However, the pressure coefficient in the Triassic and Jurassic is lower than that in the Cretaceous and at the bottom of the Paleogene. Horizontally, the abnormal high pressure distribution is characterized by E-W orientation zoning. The maximum pressure coefficient lies in the Kelasu-Dongqiu-Dina tectonic zones in the center of the Kuqa foreland thrust belt and decreases away from the tectonic zones. The formation of abnormal high pressure was mainly related with the intense tectonic compression in the Early Pleistocene time, and tectonic uplifting, undercompaction and hydrocarbon generation were secondary factors contributing to abnormal high pressure. Under the rapid and intense tectonic compression in the Early Pleistocene, the rock framework firstly undertook 1/4 of the compression stress and the other was borne by the pore fluids. Due to the presence of great seal of gypsum-salt or gypsum-mudstone beds in the Paleogene, the pressure of pore fluids increased rapidly and led to the abnormal high pressure in the Kuqa foreland thrust belt. The abnormal high pressure has important impacts on hydrocarbon accumulation. It is one of the necessary conditions for formation of large oil and gas fields in the Kuqa foreland thrust belt.     

蠕变地层套管等效破坏载荷分析

蠕变地层套管损坏的主要原因是套管外壁受到蠕变地层的非均匀载荷作用，套管本体抵抗非均匀载荷能力远远低于套管抗挤强度而产生缩径变形。通过分析蠕变地层套管非均匀载荷的分布形式，并考虑在该非均匀载荷作用下套管的强度特征及固井水泥环力学性能对套管抗非均匀载荷影响的基础上，采用有限单元法，分析了蠕变地层套管本体、固井套管组合体的等效破坏载荷。结果表明，非均匀载荷作用下套管的抗载能力迅速下降，提高固井水泥性能，切实保证固井质量将显著提高套管抵抗非均匀载荷的能力。