Ab initio investigations of the charge transport properties of endohedral M@C₂₀ (M= Na and K) metallofullerenes     

安义鹏  杨传路  王美山  马晓光  王德华 《海洋学报(英文版)》2010,29(11)

Using density functional theory and quantum transport calculations based on nonequilibum Green's function formalism, we investigate the charge transport properties of endohedral M@C₂₀ (M= Na and K) metallofullerenes. Our results show that the conductance of C₂₀ fullerene can be obviously improved by insertion of alkali atom at its centre. Both linear and nonlinear sections are found on the I-V curves of the Au-M@C₂₀-Au two-probe systems. The novel negative differential resistance behaviour is also observed in Na@C₂₀ molecule but not in K@C₂₀.  相似文献   

电厂空冷系统环境气象场要素分析中的几个关键技术     

刘文平  安炜  郭慕萍  茅彧  刘月丽 《气象科技》2008,36(6):814-817

以山西省左权、王曲电厂等为期一年的铁塔气象观测资料和各邻近地面气象站同期观测资料为例,说明如何选取典型年以及相关性较好的对比气象站,通过对电厂空冷梯度的主要气象要素分析,结合选取的对比气象站长时间序列的逐时气象资料,采用相关统计分析并进行回归检验,重建厂址区域风、温场资料,并针对风资料转换中存在的问题进行了探讨.结果表明:在两地风资料相关较差时.利用条件概率结合线性回归以及风矢量相关等方法补充订正厂址区域风资料效果较好.其结果对风、温场历史资料的重建有一定的指导意义.  相似文献   

浅析GPS测量技术在房产基础测绘中的应用          下载免费PDF全文

牟翠伟  安洁 《山东国土资源》2008,24(7)

GPS（Global Positioning System）全球定位系统具有性能好、精度高、应用广的特点。在测绘领域,GPS系统已广泛用于大地测量、工程测量、航空摄影测量及地形测量等各个领域。通过GPS静态测量和GPSRTK测量技术在性能特点、作业方法、技术条件及应用效果的分析,指出GPS技术在房产基础测量中具有传统测量技术无可比拟的优势。  相似文献   

基于弹簧—阻尼理论的海上变电站动力特性研究     

刘兵  陶安  郝俊飞  杨敏  任绅铖 《海洋工程》2024,(2):93-104

近年来,随着海上风电的迅速发展,海上变电站的建设也逐渐兴起。然而,错综复杂、瞬息万变的海洋环境对变电站的安全性和稳定性提出了严峻的挑战,因此有必要加强对变电站分析和研究的重视。为了提高变电站数值模型分析的效率,研究以海上风电场变电站为中心,采用ABAQUS建立了实体土有限元模型和基于弹簧—阻尼理论的有限元模型,以模拟桩土相互作用。随后进行了模态分析、风浪流响应分析和地震响应分析研究。研究结果表明：使用两种模型进行模态分析得出的振型非常相似,频率误差小于5%。此外,在承受风和波流荷载时,两种模型得出的变电站结构响应具有显著的一致性。在地震荷载作用下,两个模型中样本点位移时程曲线的相位频率与测量数据非常接近。值得注意的是,基于弹簧—阻尼理论的模型计算出的振幅与地震波测量数据更为接近。此外,弹簧—阻尼理论方法还大大提高了计算效率。  相似文献   

恩诺沙星在凡纳滨对虾体内的代谢和残留消除规律   总被引：1，自引：0，他引：1  

赵海军  欧安  简纪常  彭树锋 《广东海洋大学学报》2010,30(6)

在26±2℃水温下,每天投喂含有恩诺沙星药物的饲料,研究恩诺沙星在凡纳滨对虾Litopenaeus vanname肌肉、肠和肝胰脏组织中的代谢和残留消除规律。残留药物用乙腈提取,液相色谱串联质谱仪检测。结果表明:恩诺沙星在凡纳滨对虾体内可代谢为环丙沙星,对虾体内同时有恩诺沙星和环丙沙星两种药物残留;环丙沙星在肌肉、肝胰脏和肠组织中的消除时间分别为6、8、10 d,而恩诺沙星在这三组织中的消除时间则为12、14、16 d。建议把肠作为该药残留监控的靶组织,凡纳滨对虾的休药期不少于16 d。  相似文献   

GNSS����ƽ̨���ݴ���Ŀɿ��Է���   总被引：1，自引：0，他引：1  

许长辉  王坚  高井祥  安韦 《大地测量与地球动力学》2009,29(1):114-118

????????????????GNSS?????????????????????????????????????????????????????????????????????????????????GPS????GLONASS?????????????????????????Galileo???????????η?????????澫??????????????????????????????????????????????  相似文献   

Migration rate of river bends estimated by tree ring analysis for a meandering river in the source region of the Yellow River     

Cheng Liu  An Liu  Yun He  Yuehong Chen 《国际泥沙研究》2021,36(5):593-601

Meandering rivers have dynamic evolution characteristics of lateral migration and longitudinal creeping movement, and studies on the migration rate of meandering rivers have both scientific and practical significance for understanding the evolution process. A river source region often is sparsely populated and lacks long-term monitoring data, making it difficult to estimate the migration rate of river bends. In the source region of the Yellow River, located in the northeastern part of the Qinghai-Tibet Plateau, China, meandering rivers have extensively developed. Combined with field investigation and sampling in the source region in 2016 and 2017, 9 river bends in the middle Baihe River were selected to attempt estimation of migration rates of the river bends using tree ring analysis. The tree core and disc samples were collected using an increment borer and a crosscut saw, and the ages of the trees were estimated based on tree ring analysis. A method for estimating the migration rate of river bends based on the relation between positions and ages of trees grown on the point bars in inner banks is proposed. The estimated migration rates of the 9 river bends of the Baihe River ranged 0.38–6.10 m/yr, and the migration rates were found to be related to the flow rate, channel slope, height of the outer bank, and width of the river valley. The maximum migration rate was determined to be at the No. 9 River Bend where the ratio of the meander-bend radius to the channel width (R/W) was 2.31, which is consistent with previous findings that the bend migration is most rapid in the ‘migration phase’. The proposed method for estimating the migration rate of river bends provides a potential alternative option for future study on the morphodynamic process of a meandering river.  相似文献   

Modification of the Sm–Nd isotopic system in garnet induced by retrogressive fluids          下载免费PDF全文

Shi‐Chao An  Shu‐Guang Li  Zhen Liu 《Journal of Metamorphic Geology》2018,36(8):1039-1048

Garnet, as a major constitutive mineral of eclogite, is important for Sm–Nd dating of eclogite due to its high Sm/Nd ratio and its stability during retrogression. However, a comprehensive study of the petrography, mineral chemistry, garnet water content, and Sm–Nd isotopic composition of eclogites from the Bixiling massif, Central Dabie Zone (CDZ), reveals significant modification of the Sm–Nd isotopic system in garnet as a result of retrogression. This problem constitutes a challenge for Sm–Nd dating of the Bixiling eclogites, with the Sm–Nd isochron ages of 218 ± 4 to 210 ± 9 Ma reported in the literature being younger than 226 ± 3 Ma, which is the generally accepted peak metamorphic age of the CDZ. Petrographic analysis reveals heterogeneity in colour within single fractured garnet grains. There are light‐pink garnet (Grt‐P) and red garnet (Grt‐R) types that possess distinct chemical compositions. Compared to Grt‐P, Grt‐R has higher Fe and andradrite contents but lower Al and grossular contents. Grt‐P also has lower water contents (15–35 ppm) than Grt‐R (34–65 ppm), which, together with the spatial association between Grt‐R and fractures, suggests that the colour change is related to fluid alteration. Grt‐P is an ultra‐high‐pressure (UHP) mineral, and Grt‐R is the product of the interaction between Grt‐P and a fluid during retrogression. Moreover, Grt‐R features lower Sm and Nd contents but higher Sm/Nd ratios than Grt‐P. The Sm–Nd isochrons defined by UHP minerals (Grt‐P+Omp+Rt or Grt‐P+Cpx+WR) from three eclogite samples yield consistent ages of 226.0 ± 3.8 Ma, 225.0 ± 3.9 Ma and 226.2 ± 6.9 Ma, which are identical to the peak metamorphic age of 226 ± 3 Ma for the CDZ. The retrogressed garnet (i.e., Grt‐R), omphacite and rutile, together define a pseudoisochron with younger ages of 218.9 ± 5.9 to 202.8 ± 4.8 Ma, which are geologically meaningless. The increase in the Sm/Nd ratio with constant or lower ¹⁴³Nd/¹⁴⁴Nd ratios during the transformation of Grt‐P to Grt‐R was probably the cause of these younger ages.  相似文献   

Spatial and temporal variability of 0‐ to 5‐m soil–water storage at the watershed scale          下载免费PDF全文

Zihuan Fu  Yunqiang Wang  Zhisheng An  Wei Hu  Khan M.G. Mostofa  Xuezhang Li  Bingxia Liu 《水文研究》2018,32(16):2557-2569

Dynamic relationships among rainfall patterns, soil water distribution, and plant growth are crucial for sustainable conservation of soil and water resources in water‐limited ecosystems. Spatial and temporal variation in deep soil water content at a watershed scale have not yet been characterized adequately due to the lack of deep soil water data. Deep soil–water storage (SWS) up to a depth of 5 m (n = 73) was measured at 19 sampling occasions at the LaoYeManQu watershed on the Chinese Loess Plateau (CLP). At a depth of 0–1.5 m, the annual mean SWS was highly correlated with rain intensity, and the correlation decreased with depth, but within the layers at 1.5–5.0 m, the changes in SWS indicated a lag between precipitation and the replenishment of soil water. Geostatistical parameters of SWS were also highly dependent on depth, and the mean SWS presented similar spatial structures in two adjacent layers. Temporal stability of SWS as indicated by mean relative difference, standard deviation of the relative difference (SDRD), and mean absolute bias error (MABE) was significantly weaker at the shallow than at deeper layers. Soil separates and organic carbon content controlled the spatial pattern of SWS at the watershed scale. One representative location (Site 57) was identified to estimate the mean SWS in the 1‐ to 5‐m layer of the watershed. Semivariograms of the SDRD and MABE were best fitted by an isotropic spherical model, and their spatial distributions were depth‐dependent. Both temporal stability and spatial variability of SWS increased over depth. This study is helpful for deep SWS estimation and sustainable management of soil and water on the CLP, and for other similar regions around the world.  相似文献   

极地冰下生物地球化学过程研究进展     

马红梅  孙波  姜苏  安春雷  史贵涛  李院生 《地球科学进展》2012,27(2):147-153

已有的研究结果表明:极地冰下存在生命活动的证据。生物地球化学过程以其独特的视角,从生物学和地球化学学科交叉的角度,对于诠释冰下环境微生物生存及其对全球气候的影响提供了一条新途径。目前对于冰下生命的研究多集中在温型冰川和多温型冰川,关于冷型冰川冰下环境的生物起源、生存条件、能源转化方式和生物体的空间分布特征及种属关系等研究均还处在起步阶段。在简要阐述冰下化学风化机理发展历程的基础上,对近年应用生物地球化学过程研究极地冰下环境的研究成果进行总结和分析。此外,针对该领域目前研究上的空白和热点,分别对利用生物地球化学过程研究冰下环境微生物生存和繁衍,冰下温室气体释放,重大古气候事件探索及星际生命探索等科学命题进行展望。  相似文献