基于车载激光扫描的带状地物表面快速重建

根据带状地物空间形态特征以及车载激光扫描系统对带状地物数据采集的特点,提出对相邻两条扫描线数据构建三角网进而完成整个带状地物表面快速重建方法。该方法充分利用了每条扫描线获取带状地物横截面的特点,相邻两条扫描线构建的三角网能准确地反映其所覆盖的狭长条带区域的形态结构,把所有狭长条带连接起来便能准确地描述整个带状地物的形态结构。在网格构建过程中自动建立点、线、面间的拓扑关系或隐含拓扑关系,查询和动态更新操作都限制在非常狭小的范围内,便于快速重建。     

临沂市温泉（井）成热机制分析及找热方向研究

临沂市地处鲁西隆起南部,地热资源丰富。该文介绍了临沂市的地层、岩浆岩、构造、地热背景、主要控热断裂及20余眼温泉(井)的情况和分布。通过分析汤头温泉、白塔地热井、汤坊崖地热井、铜井地热井、松山地热井、新村地热井、西高都地热井等主要温泉(井)的控热断裂、成热机制,认为该区地热主要分布在沂沭断裂带与NW向深大断裂交会处,地下水补给多沿NW—SE断裂,热源以深大断裂沟通深部热源,水温、水量较好地热井均处在沂沭断裂带沂水-汤头断裂以西的、控热断裂为张性断裂或的张扭性断裂凹陷区内。结合临沂市区域地质构造特点,认为蒙山断裂与鄌郚-葛沟断裂深部交会处,尼山断裂、峄城断裂与鄌郚-葛沟断裂交会处为地热勘探靶区。     

一种水产动物病毒现场检测免疫芯片的制备与应用

采用原子力显微镜对氨基化玻片及6种不同方法修饰玻片进行表面特征分析,并比较了硝酸纤维素(NC)膜、PVDF膜以及以上不同修饰玻片对抗体的固定效率、固定效果,最终选择琼脂糖修饰玻片作为芯片载体。将纯化后的兔抗血清(捕获抗体)点样至琼脂糖修饰玻片上,制备免疫芯片,与待检样品(病毒感染的靶器官组织)匀浆液孵育形成复合物,该复合物被辣根过氧化物酶(HRP)标记的特异性单克隆抗体(单抗)识别,经底物显色,得到肉眼可见的检测结果。通过改变芯片制备及应用过程中的具体条件参数,对各条件进行了优化,并采用生物素-链亲和素(BAS)标记特异性单抗作为检测抗体以提高检测灵敏度。基于此夹心免疫分析原理制备的WSSV、LCDV现场检测免疫芯片,病毒的最低检出量分别为82.50ng/ml、0.88μg/ml,在一定的抗原浓度范围内,病毒浓度的对数值与信号强度呈线性关系;采用BAS放大检测信号后,病毒的最低检出量为12.38ng/ml、0.22μg/ml。该免疫芯片与酶联免疫吸附法(ELISA)及免疫荧光法(IFAT)对同种样品的检测结果高度一致。     

内湾沉积物生物硅化学测定法的实验条件探讨

对国内外已经建立的几种生物硅的测定方法进行简要的评述,并详细地对内湾沉积物中生物硅化学提取法的条件选取进行实验探讨,对低生物硅含量的内湾沉积物测定提出了较优的条件。     

基于孔压静力触探(CPTU)测试的连云港海相粘土前期固结压力确定方法研究

首先回顾了基于孔压静力触探(CPTU)测试确定前期固结压力的方法,通过连云港海相粘土场地进行的CPTU试验资料,以室内固结试验得到的前期固结压力作为参考值评估了经验方法预测前期固结压力的有效性。最简单的方法是直接建立前期固结压力和净锥尖阻力的关系,同时也是最有效的方法。     

向海湿地自然保护区鸟类多样性评价方法的比较研究

鸟类多样性是评价湿地生态环境质量极其敏感的指标。向海湿地自然保护区地处半干旱区,受气候和人为影响,生态环境变化极为剧烈,因此,寻求一种行之有效且简单易行的鸟类多样性评价手段,对于及时了解湿地生态环境质量的动态变化信息,提出湿地和鸟类多样性的管理和保护对策至关重要。稀疏标准化法是一种建立在物种-面积关系上的生物多样性评价方法,主要用于区域尺度上的生物多样性评估。运用改进的稀疏标准化程序,利用多年调查和收集的鸟类数据,来评价和分析向海自然保护区鸟类多样性及其变化,结合香农-威纳多样性指数和均匀度指数,分析了两种方法获取结果的相关性。评估结果表明:稀疏标准化法获取的鸟类多样性和均匀度信息与传统的香农-威纳多样性指数和Pielou均匀度指数间具有显著的相关关系,可以用于鸟类的多样性和均匀度评价,且具有科学、直观、运算简捷、快速等优势。     

Element mobility during continental collision: insights from polymineralic metamorphic vein within UHP eclogite in the Dabie orogen

Metamorphic dehydration and partial melting are two important processes during continental collision. They have significant bearing on element transport at the slab interface under subduction‐zone P–T conditions. Petrological and geochemical insights into the two processes are provided by a comprehensive study of leucocratic veins in ultrahigh‐pressure (UHP) metamorphic rocks. This is exemplified by this study of a polymineralic vein within phengite‐bearing UHP eclogite in the Dabie orogen. The vein is primarily composed of quartz, kyanite, epidote and phengite, with minor accessory minerals such as garnet, rutile and zircon. Primary multiphase solid inclusions occur in garnet and epidote from the both vein and host eclogite. They are composed of quartz ± K‐feldspar ± plagioclase ± K‐bearing glass and exhibit irregular to negative crystal shapes that are surrounded by weak radial cracks. This suggests their precipitation from solute‐rich metamorphic fluid/melt that involved the reaction of phengite breakdown. Zircon U–Pb dating for the vein gave two groups of concordant ages at 217 ± 2 and 210 ± 2 Ma, indicating two episodes of zircon growth in the Late Triassic. The same minerals from the two rocks give consistent δ¹⁸O and δD values, suggesting that the vein‐forming fluid was directly derived from the host UHP eclogite. The vein is much richer in phengite and epidote than the host eclogite, suggesting that the fluid is associated with remarkable concentration of such water‐soluble elements as LILE and LREE migration. Garnet and rutile in the vein exhibit much higher contents of HREE (2.2–5.7 times) and Nb–Ta (1.8–2.0 times) than those in the eclogite, indicating that these normally water‐insoluble elements became mobile and then were sunken in the vein minerals. Thus, the vein‐forming agent would be primarily composed of the UHP aqueous fluid with minor amounts of the hydrous melt, which may even become a supercritical fluid to have a capacity to transport not only LILE and LREE but also HREE and HFSE at subduction‐zone metamorphic conditions. Taken together, significant amounts of trace elements were transported by the vein‐forming fluid due to the phengite breakdown inside the UHP eclogite during exhumation of the deeply subducted continental crust.     

西藏仲巴地区的一个晚泥盆世菊石动物群

晚泥盆世菊石相地层,国内以往仅见于东北的大兴安岭和黔南地区。本文记述的材料采自西藏仲巴地区柴曲(河)两岸的巨日桑群下段,菊石化石包括?Lobotornoceras sp.,Sporadoceras sp.,S.pompeckji Wedekind,S.of.biferum(Phillips),Cheiloceras sp.等属种,时代为晚泥盆世法门早期。     

大震前短周期瑞利面波的前兆异常特性

<正> 本文试图从实际观测资料中寻找大震前短周期瑞利面波的某些前兆异常特性,并从理论上加以分析讨论。初步结果表明,瑞利面波的群速、相速及波形、频谱等在大震前均可能显示出一定的前兆异常特性。     

流动注射分光光度法同时测定水中挥发酚及氰化物

在单针进样器的基础上，增加一个三通流路同时进样，在线消解-流动注射分光光度法测定水中挥发酚及氰化物。实验结果表明，挥发酚浓度在0mg/L～0．2mg／L、氰化物浓度在0mg/L～0．5mg／L范围内具有良好的线性关系。通过在线气体扩散分离技术，提高了分析速度，每小时可完成12个～15个样品的分析。方法的相对标准偏差〈5％，回收率在90．4％～108．5％之间。