Application of entropy analysis of in situ droplet-size spectra in evaluation of oil chemical dispersion efficacy

In situ droplet-size distributions were measured using a laser in situ scattering and transmissiometry (LISST-100X) particle size analyzer during the evaluation of natural and chemical dispersion efficiency of crude oils under different wave and current conditions. An entropy grouping of the in situ dispersed oil droplet-size spectra has classified the multi-modal droplet-size distributions into different groups based on similar droplet-size spectra characteristics within groups and distinction between groups. A generalized linear logistic regression model was fitted to analyze the effects of a number of factors and their interactions on the grouping of oil droplet-size spectra. The grouped results corresponded to the oil dispersion efficiency at different levels. This new method for droplet-size distribution data analysis can have significant implication in field evaluation of natural and chemical dispersion efficiency of oil.     

损伤谱在结构抗震性能评估中的应用

改进能力谱法可以较好地评估结构抗震性能,在工程中得到了广泛的应用.本文在此基础上指出,由改进能力谱方法求得的延性是结构的延性需求,并不是结构的实际延性能力,不能以此代表结构在罕遇地震作用下的实际抗震能力.其次,基于弹塑性损伤反应谱(简称"RD谱"),结合模态Pushover分析,提出了基于RD谱的能力谱分析方法,通过R...     

Strength reduction factors for seismic analyses of buildings exposed to near-fault ground motions

To estimate the near-fault inelastic response spectra, the accuracy of six existing strength reduction factors (R) proposed by different investigators were evaluated by using a suite of near-fault earthquake records with directivity-induced pulses. In the evaluation, the force-deformation relationship is modelled by elastic-perfectly plastic, bilinear and stiffness degrading models, and two site conditions, rock and soil, are considered. The R-value ratio (ratio of the R value obtained from the existing R-expressions (or the R-μ-T relationships) to that from inelastic analyses) is used as a measurement parameter. Results show that the R-expressions proposed by Ordaz & Perez-Rocha are the most suitable for near-fault ground motions, followed by the Newmark & Hall and the Berrill et al. relationships. Based on an analysis using the near-fault ground motion dataset, new expressions of R that consider the effects of site conditions are presented and verifi ed.     

连云港海域表层海水温度、盐度变化的多重分形分析

以1996—2008年的连云港海域表层海水温度、盐度的日观测数据为基础,运用多重分形分析方法对该海域温度、盐度的时间演变特征进行了研究。结果表明,在所研究的时间尺度内,温度和盐度均具有统计标度不变性,表现出较弱的多重分形特征;多重分形谱形态参数的计算结果表明,温度和盐度的变化均存在着下降的趋势,并且盐度随时间变化的复杂性、不规则性和不均匀性要较温度显著。研究结果对于连云港海域海洋环境系统动力过程的理解和预报模式的改进具有参考意义。     

安徽官山两种坡缕石粘土的成分与红外吸收谱

本文采用多种成分分析手段对官山两种不同颜色坡缕石全粘土进行了研究。全粘土湿化学分析扣除SiO2含量计算得到的坡缕石阳离子数与电子探针获得的阳离子数一致。配位八面体阳离子计算表明，粉红色坡缕石为三八面体矿物，灰白色坡缕石是介于三八面体矿物和二八面体矿物间的中间类型。X射线粉末衍射的K值法对全粘土矿物定量分析有着较高的精度，同时用电子探针波谱可准确测定坡缕石粘土的成分。官山两种不同颜色含坡缕石的全粘土红外吸收谱能反映其中坡缕石的吸收谱特征。对X射线光电子能谱研究表明两种不同颜色的坡缕石中的铁主要是Fe^3 ，这与全岩湿化学分析的结果是一致的，同时也还可以作为电子探针成分分析的补充。     

我国土壤光谱线之研究

通过对我国各地的土壤光谱反射率的分析表明,无论在二维或多维空间中,确有土壤光谱线存在,但不是严格的一条直线,而是有适当宽度的带。不宜用全国统一的一条土壤光谱线来作植被分析。讨论了不同土壤光谱线对绿度及植被覆盖度估计的误差。还论述了土壤光谱反射率主成分分析的结果及其物理意义。     

The effect of horizontal resolution on gravity waves simulated by the GFDL “SKYHI” general circulation model

To examine the effects of horizontal resolution on internal gravity waves simulated by the 40-level GFDL SKYHI general circulation model, a comparison is made between the 3° and 1° resolution models during late December. The stratospheric and mesospheric zonal flows in the winter and summer extratropical regions of the 1° model are much weaker and more realistic than the corresponding zonal flows of the 3° model. The weaker flows are consistent with the stronger Eliassen-Palm flux divergence (EPFD).The increase in the magnitude of the EPFD in the winter and summer extratropical mesospheres is due mostly to the increase in the gravity wave vertical momentum flux convergence (VMFC). In the summer extratropical mesosphere, the increase in the resolvable horizontal wavenumbers accounts for most of the increase in the gravity wave VMFC. In the winter extratropical mesosphere, the increase of VMFC associated with large-scale eastward moving components also accounts for part of the increase in the gravity wave VMFC.The gravity waves in the summer and winter mesosphere of the 1° model are associated with a broader frequency-spectral distribution, resulting in a more sporadic time-distribution of their VMFC. This broadening is due not only to the increase in resolvable horizontal wavenumbers but also occurs in the large-scale components owing to wave-wave interactions. It was found that the phase velocity and frequency of resolvable small-scale gravity waves are severely underestimated by finite difference approximations.