磁黄铁矿在纳米碳管生长中的作用

本文采用天然磁黄铁矿矿物－六方磁黄铁矿和单斜磁黄铁矿分别作催化剂,引入电弧法生长纳米碳管,发现二者具有截然不同的催化效果。在此基础上,探讨了在合成纳米碳管实验中磁黄铁矿的催化作用及催化机理。     

遥感模拟图像应用于不同传感器光谱性能分析

研究利用高光谱成像数据,用数字的方法定量模拟了SPOT－HRV、CBERS-CCD、Landsat5-TM和NOAA14-AVHRR类似波段的空中表面反射率及地面光谱反射率图像,并利用这些图像对上述传感器相应波段的光谱响应、大气影响特性用基于反射率和基于归一化植被指数（NDVI）的方法进行了定量的比较分析。研究表明,由于传感器类似波段的光谱响应不同,因而由其计算的反射率和NDVI之间均存在明显差异,这种差异是大气改正所无法完全消除的。多传感器定量分析时需要进行相应的辐射改正。     

改进快速模拟退火方法进行AVO岩性参数反演

以广义波乐兹曼的吉布斯（Ｂｏｌｔｚｍａｎｎ－Ｇｉｂｂｓ）统计理论为基础,将数认（ｎｕｍｃｒａｌ）和依赖于温度的似柯西（Ｇａｕｃｈｙ）分布相结合建立一种新的扰动模型,改进接受概率,提出了一种非常快速模拟退火法（ｖｅｒｙ ｆａｓｔ ｓｉｍｕｌａｔｅｄ ａｎｎｅａｌｉｎｇ）。通过多参数的振幅随炮检距变化（ＡＶＯ）的合成数据和实际投资试算结果表明,该方法能在高温下进行大范围内的搜寻,解的稳定性好和抗随机干     

非接触式六自由度运动测量与分析方法

本文提供了一种非接触式六自由度运动测量与分析方法。首先应用位置测量仪（ＰＳＤ）对安置在模型上的红外线发光源（ＬＥＤ）进行测量,然后用所编制的软件计算出模型的六个自由度运动情况。该方法避免了接触式测量仪对模型作用一定的力而产生的误差,同时具有较高的位置解析度与频率响应能力,测量结果精度较高。该方法可同时测量空间三个点的运动坐标从而可用计算机求得模型在空间的六个自由度运动情况。测量与分析结果令人满意。     

多伦地区晚侏罗世火山活动节律研究

多伦地区的晚侏罗世火山岩地层,可划分为满克头鄂博、玛尼吐、白音高老三个火山活动小旋回,通过对其岩石组成、岩相、结构构造及其变化的研究,从地球历史演化的阶段性、周期性和不可逆性的角度,探讨了该区晚侏罗世火山活动节律特征,进而从时空尺度对火山活动节律的级别和特征进行了划分和厘定,并探讨了不同级别节律的成因。     

山东沂水郯庐断裂带中段中生代火山岩特征及演化

山东沂水地区位于郯庐断裂带中段,中生代火山活动强烈。早期主要为一套高钾钙碱性系列的中型火山岩,年龄为110--125Ma,按安山岩K60估算的地壳厚度为58--62km,说明当时具造山岩石圈根,其代表的构造环境为活动大陆边缘。晚期为一套钾玄岩系列的中酸性火山岩及少量基性火山岩,年龄为69--101Ma,该期火山岩铕异常不明显,δEu=0.92（平均）,反映该期火山作用是在可能存在山根的条件下,在地幔岩石圈减薄、拉伸下形成的。郯庐断裂带内一套厚度达3200m的晚白垩世大盛群河湖相沉积岩,是造山带去根后地壳进一步拉张、伸展,在断陷盆地重兴冲冲的产物。     

江苏里下河地区降水与水位的关系

洪涝是里下河地区汛期的主要灾害,也是当地各级政府防范的重点。洪涝灾害的发生,与降水前的水位有着密切的关系,作者根据里下河地区的特殊水系和地形,研究确定出降水量与水位的定量关系。根据降水的预报,得出雨后的最高水位预报值,防汛部门可根据预报结果,提前采取必要的措施,减少洪涝灾害的影响。     

Hydrodynamics of suspended particulate matter in the tidal freshwater zone of a macrotidal estuary (the Seine Estuary, France)

The effects of fortnightly, semidiurnal, and quaterdiurnal lunar tidal cycles on suspended particle concentrations in the tidal freshwater zone of the Seine macrotidal estuary were studied during periods of medium to low freshwater flow. Long-term records of turbidity show semidiurnal and spring-neap erosion-sedimentation cycles. During spring tide, the rise in low tide levels in the upper estuary leads to storage of water in the upper estuary. This increases residence time of water and suspended particulate matter (SPM). During spring tide periods, significant tidal pumping, measured by flux calculations, prevents SPM transit to the middle estuary which is characterized by the turbidity maximum zone. On a long-term basis, this tidal pumping allows marine particles to move upstream for several tens of kilometers into the upper estuary. At the end of the spring tide period, when the concentrations of suspended particulate matter are at their peak values and the low-tide level drops, the transport of suspended particulate matter to the middle estuary reaches its highest point. This period of maximum turbidity is of short duration because a significant amount of the SPM settles during neap tide. The particles, which settle under these conditions, are trapped in the upper estuary and cannot be moved to the zone of maximum turbidity until the next spring tide. From the upper estuary to the zone of maximum turbidity, particulate transport is generated by pulses at the start of the spring-neap tide transition period.     

胶东大庄子金矿地质特征与成因探讨

大庄子金矿是我国首次发现赋存于胶东变质岩中大规模韧-脆性剪切带内的蚀变岩型及石英脉型金矿床.金矿化与绢英岩化、黄铁矿化、硅化和碎裂岩化有关.矿体受韧-脆性剪切带、黄铁绢英岩化、晚元古代晚期角闪岩相变质岩的共同控制.矿石矿物组合以自然金-金属硫化物-架状硅酸盐为主的组合类型.矿床属于在韧-脆性剪切作用下,与含金量较高的下元古界荆山群变质岩的形成、演化有成因联系的蚀变、重熔、交代中温动力热液改造型金矿床.     

WAVELET CHARACTERISTICS OF RAINFALL VARIATION IN THE THREE GORGE REGION OF CHANGJIANG RIVER*

Making the climatic diagnosis of Changjiang Three Gorge Region by the maximum entropy spectrum analysis and wavelet analysis,we discovered that the main periods of the annual and wintertime precipitation variation in the east subregion differ from that in the west subregion.The former is a period of about 2 years,and the latter is about 5-6 years.Their wavelet patterns are also apparently different between two subregions:the alternate positive and negative wavelet patterns for the west,but not so regular for the east.These provide a climatic background for the implementation of Three Gorge Project.We also found that the historical reason of the main periods by combing synthetically spectrum analysis and wavelet analysis could be realized.In addition we suggest a gist of the climate forecast by analogy analysis based on the 2-dimensional wavelet figures.