全光纤安防系统模式识别混合编程的实现

介绍了宽域全光纤监控预警系统及光纤扰动信号模式识别算法.利用小波包分解对信号进行分解与重构,并提取各频段内信号分量能量谱作为特征向量;应用综合考虑观测数据和确定性先验知识的BVC-RBF神经网络实现信号分类,提高了网络的泛化能力.利用Matlab引擎、动态链接库(DLL)、组件对象模型(COM)3种混合编程方法将Mat...     

基于模糊数学和粒子群算法的边坡参数反分析

传统的利用边坡位移进行力学参数反分析的方法构造的目标函数较为简单.为了体现滑坡土体的不同性质,文中在传统优化方法的基础上,分析了滑坡体内部土体的位移特点,并将滑坡土体分为滑坡床、滑坡面和滑坡体3个类别.然后分别利用模糊数学和粒子群算法求得不同位置土体对3个类别的隶属度以及3个类别的位移权重,并根据土体的隶属度和3个类别...     

高取代度木聚糖衍生物的理化性质

以从麦草中分离得到的木聚糖为原料、丙烯酰胺为醚化剂、碱为催化剂、丁醇/水为反应介质制备了带有高取代度双官能团的木聚糖衍生物.采用13C核磁共振表征了木聚糖衍生物的结构.利用平行板流变仪和同步热分析仪对木聚糖衍生物与原木聚糖的动态流变性能和热稳定性进行测试,结果表明:与原木聚糖溶液相比,木聚糖衍生物溶液呈现较低的粘度,剪...     

剩余压紧力条件下滑靴副的油膜特性及功耗

在考虑滑靴高速旋转时底面会形成热楔支承力的基础上,利用求解高次微分方程的研究方法建立了剩余压紧力状态下柱塞泵的滑靴底面的油膜模型,通过Matlab编程精确描述了剩余压紧力状态下滑靴油膜的动态特性,并以此为基础研究了滑靴的油膜厚度与负载、转速的关系,推导了滑靴高速运行所造成的功耗损失,同时分析了负载和转速变化对滑靴功耗损...     

两种基于苯并咪唑衍生物配体的新型铱(Ⅲ)配合物的合成及发光性能研究

合成了新型配体N-异丙基-2-苯基苯并咪唑(bi)和N-异丙基-2-(4-氟苯基)苯并咪唑(fbi),并用它们与三氯化铱和乙酰丙酮反应,制备了相应的环金属铱(Ⅲ)配合物发光材料(bi)2Ir(acac)和(fbi)2lr(acac)(acac=乙酰丙酮).对其结构用1H NMR和元素分析方法进行了表征,研究了配合物的UV-vis,荧光光谱及电化学性质.两种材料的最大发光波长分别位于514 nm和493nm.电化学研究表明,在苯环上引入氟原子后,配合物的HOMO和LUMO间能隙增大(分别为O.12 eV和0.15 eV),与最大发光波长蓝移结果吻合.     

山东省湿地面积变化及其生态价值分析

笔者利用三期中国湿地数据,首次定量化研究山东省湿地在1990年、2000年2008年间的变化趋势,并对生态价值变化进行分析.结果显示,山东省湿地自然湿地从1990到2008年减少达到1 966.48 km2,减幅达到37.58%,面积变化先急促后迟缓.山东省湿地生态系统服务功能价值从1990年的374.82亿元,到2000年减少到333.18亿元,然而到2008年增长到了 373.38亿元,先减少后增加,同湿地面积变化趋势一致,这在总量上的增长,完全是人工湿地的增长,自然湿地一直在减少.     

Mitochondrial DNA variation analysis suggests extreme low genetic diversity in Guizhou snub-nosed monkeys （Rhinopithecus brelichi）

Guizhou snub-nosed monkey (Rhinopithecus brelichi) is a unique, endangered primate in China, mainly distributed in Fanjing Mountain National Natural Reserve, Guizhou Province, in an area of 275 km2. Recently, habitat loss and fragmentation have caused population isolation. To assess genetic diversity within this species and its population structure, we sequenced 400 bp of the hypervariable I segment from the mitochondrial DNA control region for 128 individuals. Only one haplotype was identified from these individuals. Compared with other primate species, R. brelichi can be regarded as a species with very low genetic diversity, which further adds to the conservation concern.     

Zircon U-Pb ages of granites at Changba and Huangzhuguan in western Qinling and implications for source nature

Mesozoic granitoids are widespread in the Qinling-Dabie-Sulu orogenic belt. Precise U-Pb dating on these granitoids can reveal the evolution of the continental collision orogen and thus provide information on the nature of magma sources. This study presents zircon LA-ICP-MS U-Pb dating and whole-rock geochemical analyses for two intrusions at Changba and Huangzhuguan in western Qinling. Zircon U-Pb ages for central and marginal phases of the Huangzhuguang intrusion are 214±1 Ma and 213±3 Ma, respectively. Zircons from the Changba intrusion yield a dominant cluster with an U-Pb age of 213±2 Ma. Collectively, these ages are younger than ages of 220 to 240 Ma for ultrahigh-pressure metamorphism due to the continental collision between the South China Block and the North China Block, corresponding to syn-exhumation magmatism. Some inherited zircons occur in the Changba intrusion, yielding a weighted mean of ²⁰⁶Pb/²³⁸U ages at 757±14 Ma. This indicates that the Changba intrusion has the crustal source of mid-Neoproterozoic ages and a tectonic affinity to the South China Block. Geochemically, the two intrusuons are both rich in LILE and LREE but depleted in HFSE and HREE, similar to arc-type igneous rocks. The Huangzhuguang intrusion exhibits linear correlations between SiO₂ and the other major oxides, implying chemical evolution from a cognate magma source. It contains mafic enclaves, suggesting possible mixing of felsic-mafic magmas. The Changba granite is rich in Si and K but poor in Fe and Mg as well as has a high value of Fe*, suggesting strong differentiation of granitic magma. Therefore, the two intrusions were derived from the Late Triassic anatexis of the continental crust of different compositions in the northern margin of South China Block. This process may be coupled with exhumation of the subducted continental crust in the stage of late collision.     

The occurrence and significance of C25HBI in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin,NW China

The saline lacustrine deposit of the Oligocene Lower Ganchaigou Formation is the main source rock for the Western Qaidam Basin,NW China.In this study,abundant highly branched isoprenoids with 25 carbon atoms (C25HBI) were detected in the upper section of the Lower Ganchaigou Formation.C25HBI is a biomarker for diatoms,and can provide information regarding biogeochemical processes during production and preservation of sedimentary organic matter.The carbon isotopic values of C25HBI in these source rocks were in the range of-18‰ to-20‰.The relative enrichment in 13C of C25HBI suggests that these isoprenoids were derived from diatom blooms.In this case,the diatoms used HCO3-as an additional carbon source to dissolved CO2 in water column due to their high biological productivity.Conversely,the diatom blooms indicated an abundant nutrient supply to the environment and high primary productivity.Thus,the occurrence of 13C-enriched C25HBI could be an ideal marker for good source rocks.The decreased concentration of CO2(aq) in the water column induced by diatom blooms can result in an enrichment in 13C of organic matter synthesized by primary producers.This may be a possible reason for the occurrence of 13C-enriched organic matter in the Cenozoic source rocks of the Western Qaidam Basin.Previous studies have shown that the high carbon number n-alkanes sourced from diatoms have no carbon preference.Hence,the sources of n-alkanes in regional source rocks are complex,and should be considered when discussing the sources of organic matter in future studies.     

Carbon and hydrogen isotopic compositions and their evolutions of gases generated by herbaceous swamp peat at different thermal maturity stages

Coalbed methane (CBM) accumulation models include continuous gas accumulation and staged gas accumulation.However,studied on the geochemical characteristics and indices to evaluate staged accumulation CBM are lacking.This study for the first time obtained the carbon and hydrogen isotopic compositions of methane and ethane generated at different evolution stages using thermal simulation of samples prepared by treating an herbaceous swamp peat at different temperatures.The results showed that the carbon isotopic compositions of methane and ethane were obviously affected by the thermal evolution level of the starting sample,while the hydrogen isotopic compositions were closely related to the maturity of gases.The carbon and hydrogen isotopic compositions of gases generated by coal-forming organic matter with Ro values from 1.2%,1.7%,2.4%,3.2% and 3.7% to 5.2% were determinated.The relationship between Ro values and the carbon and hydrogen isotopic compositions of gases generated by coal-forming organic matter at different evolution stages as well as the carbon or hydrogen isotopic relationships between methane and ethane were established.The results provide a scientific basis for studying the genesis of CBM generated at different maturity intervals and understanding the geochemical characteristics of staged accumulation CBM.These results were applied to a case study on CBM from the southern Qinshui basin,and it was found that the CBM accumulated after the Middle Jurassic and was characteristic of staged gas accumulation.This is consistent with the result of geological studies,and further showed that the results of thermal simulation experiments are very important for evaluating the genesis of natural CBM.