基于数字地磁资料的滤波幅相法初步应用研究

根据地磁垂直分量日变化畸变异常的周期特征, 应用FHD磁力仪分钟值观测资料, 通过富氏拟合滤出1~3 h的日变化,突出垂直分量日变化中的畸变变化, 直接获取了幅相法异常。 新方法只需单台的垂直分量分钟值观测资料, 克服了原有幅相法需要参考台资料的缺陷, 方便了异常提取, 拓展了数字地磁观测资料的应用范围。     

GRACE时变重力场的滤波理论及质量变化分析

正由于GRACE(gravity recovery and climate experiment)时变重力场模型直接解算质量变化时存在较大的误差,需要对其进行相应的滤波处理,提高质量变化的反演精度。本文总结了GRACE监测全球与区域质量变化的研究进展,分析了最新时变重力场模型的精度及其滤波方法;提出了基于重力位系数协方差阵的时变重力场滤波方法;分析了南极冰盖的质量变化、亚马孙流域陆地水质量和海平面变化。本文的研究成果及创新点主要包括以下几个方面:     

化感物质抑制短裸甲藻的机理研究

文章通过研究邻苯二甲酸二丁酯(DBP)对短裸甲藻的活性氧自由基(ROS,主要为H_2O_2)水平、过氧化标志产物丙二醛(MDA)含量以及对细胞亚显微结构的影响,初步揭示DBP抑制短裸甲藻的机理,为沿海赤潮的控制和有效防治提供有力的支持。研究结果表明,DBP通过引起短裸甲藻细胞内活性氧自由基的过度积累而引起膜质过氧化,与不添加DBP的对照组相比,在低浓度DBP(0.1mg/L)的影响下,H_2O_2含量前48h变化比较平稳,48h以后逐渐下降。而在高浓度DBP(10mg/L)的影响下,H_2O_2含量变化波动明显,暴露72h后,H_2O_2含量达到248.24nmol·(10~7cells)~(-1),约是对照组的4.67倍。过氧化标志产物MDA在低浓度DBP(0.1mg/L)处理后暴露24h分别出现峰值0.23μmol·(10~9cells)~(-1)、0.28μmol·(10~9cells)~(-1),高浓度DBP(10 mg/L)处理MDA含量24h后持续上升,72h时高达0.351μmol·(10~9 cells)-1,约是对照组的2.32倍。同时DBP可以引起短裸甲藻细胞结构受损,表现在叶绿体、线粒体等细胞器变模糊,细胞空泡化,原生质膜皱缩,细胞脂质体(黑色颗粒)明显增多等,初步认为过氧化损伤为化感物质作用机理。     

郑氏大力丸制备工艺及质量标准研究

目的：研究郑氏大力丸的制备工艺和质量标准中药物的薄层鉴别方法。方法：从丸剂自动化生产角度考察郑氏大力丸生产工艺的可行性,并建立熟地黄和人参专属性强、简便的薄层鉴别方法。结果：郑氏大力丸的生产工艺为：在出条口直径5mm,推料速度与切丸速度500r/min的条件下,以纯化水为粘合剂制成含水量28.6%的软材后进行制丸;郑氏大力丸中熟地黄、人参薄层鉴别方法重现性良好。结论：郑氏大力丸制备工艺合理、质量标准良好,可以应用于生产。     

红藤瘀痛洗药的皮肤毒性和安全性研究

目的：研究红藤瘀痛洗药经皮肤给药的毒性和安全性。方法：选用家兔进行皮肤急性毒性实验及皮肤刺激性实验,选用豚鼠进行皮肤过敏性实验,观察红藤瘀痛洗药的皮肤用药的急性毒性反应及皮肤刺激性、过敏性。结果：红藤瘀痛洗药高剂量、正常剂量对完整及破损家兔皮肤均未见急性毒性反应;红藤瘀痛洗药高剂量、正常剂量对家兔皮肤均未见刺激反应;红藤瘀痛洗药对豚鼠皮肤未见过敏反应。结论：红藤瘀痛洗药经皮肤给药无明显的毒性反应,安全性良好。     

西藏纳木错及其入湖河流溶解有机碳和总氮浓度的季节变化

为深入理解纳木错湖水及入湖河流中溶解有机碳（DOC）和总氮（TN）浓度的季节变化特征及其影响因素,于2012-2013年不同季节对纳木错2个站点及流域内21条主要入湖河流进行采样及分析,采用统计学方法初步探讨纳木错水体和21条河流DOC和TN浓度季节变化特征.结果表明,河流DOC平均浓度范围为0.763~1.537 mg/L,TN平均浓度范围为0.179~0.387 mg/L.21条入湖河流DOC浓度在春末夏初和夏季达到高值,冬季为低值,TN浓度季节变化趋势大体上与DOC浓度相反.湖泊水体DOC和TN浓度范围分别为2.42~8.08和0.237~0.517 mg/L,明显分别高于河水中的浓度.湖泊DOC浓度季节变化趋势与河流一致,而TN浓度无明显的季节性变化.河水DOC浓度的季节变化和空间差异受控于河流的补给方式,湖水DOC浓度受湖泊内部藻类等水生植物活动和河流外源输入的影响.DOC等有机质的分解是影响纳木错流域湖水和河水TN浓度的重要原因.     

辽宁省大伙房水库及入库河流水质空间特征与河库水质关系

入库河流与水库存在空间上的连续性,河流污染物输入是水库水质恶化的主要原因,对大伙房水库及其入库支流61个采样点的水质状况进行调查,并运用聚类分析和主成分分析对大伙房水库及入库支流的水质空间特性和主要污染物进行分析.聚类分析显示,按照水质相似性将大伙房水库及入库支流水质可分为上游区、下游区和库区3个典型空间区域.分别对3个区域进行主成分分析,结果显示:入库支流上游区和下游区水质主要影响因素为氨氮、总氮和化学需氧量,库区影响水质的主要因素为温度、p H值、浊度、溶解氧、电导率、氨氮和总氮.对上游、下游和库区水质均有显著影响的因子为氨氮和总氮,上游区、下游区和库区氨氮浓度均值分别为0.06、0.10和0.19 mg/L,总氮浓度均值分别为0.13、0.16和0.26 mg/L.入库河流下游区对水库水质影响较大,受社河和浑河污染物输入的影响,大伙房水库水质在空间上呈现社河入库区水质优于浑河入库区水质.并且库区氨氮和总氮浓度均与距岸边距离呈负相关,溶解氧和p H值均与距入库口距离呈负相关,表明入库河流污染物输入和环库区面源污染均对大伙房水库水质产生一定影响.     

兰勃特投影向高斯投影转换程序编制及难点分析

为了解决兰勃特投影向高斯投影转换中存在的难题,如:如何从兰勃特投影的平面坐标求大地坐标,高斯正算中经度的确定等,更好地促进兰勃特投影地图的应用,本文在对两种投影理论研究的基础之上,采用C#语言进行编程实现兰勃特投影向高斯投影转换.结果表明所编制的程序切实可行,且具有科学性.本研究的程序可以为测绘生产单位提供一种选择.     

纳木错水温变化及热力学分层特征初步研究

水温变化是湖泊的重要物理特性,对湖泊的水质特征、湖水能量循环、水生生态系统研究具有重要意义.基于不同季节的实地观测资料,分析青藏高原高海拔、深水大湖纳木错的水温变化特征及季节差异,并着重分析湖水热力学分层的季节变化.结果显示纳木错中部、东部两个湖盆冬季封冻,夏季存在稳定分层,春、秋季混合,是一个典型双季对流、完全混合型湖泊.但两个湖盆水温变化与热力学分层又有各自的特征,东部浅湖盆湖水在春季升温快,夏季分层与秋季翻转均比中部湖盆早,且秋季翻转时水温也比中部湖盆高.初步分析认为两个湖盆不同的湖盆形状及水深分布可能是造成其热力学特征差异的主要原因.     

INFLUENCE OF PUMPING ON FOUR-COMPONENT BOREHOLE STRAIN AT TAI'AN SEISMIC STATION AND ITS INTERFERENCE MECHANISM

Four-component borehole strainmeter (FCBS) is one kind of high-precision borehole strain observation instruments invented in China. As a kind of near-surface deformation observation instrument, FCBS is also easily disturbed by the external environment factors. As a common factor, pumping has significant influence on FCBS observation. Existing studies mostly identify the pumping interference from the perspective of observation curve morphology, relatively few studies focus on its interference mechanism. In order to truly capture earthquake precursor information, it is necessary to study the interference mechanism. In recent years, RZB-3 type FCBS at Tai'an seismic station has been seriously affected by pumping, so it is necessary and also feasible to study the interference mechanism of pumping. Since the influence of pumping interference on borehole strainmeter is common, this work would be very practical and be used for reference by other borehole strain observation stations. We find that the original observation curves and observed surface strain, shear strain from RZB-3 type FCBS at Tai'an seismic station have the characteristics of synchronous change with the borehole water level, in which the linear correlation coefficient between the two observed shear strain curves and borehole water level reached 0.70 and 0.82 respectively. We further find that the principal strain direction of borehole and borehole water level after normalization meet the nonlinear function as y=1.217arctan(x)^0.224-0.284. The above phenomenon indicates that the observation of RZB-3 type FCBS at Tai'an seismic station is significantly affected by the borehole water level, and the influence is more obvious and the gradient is larger at the stage of low water level. Pumping interference often appears in low water level stage and changes the rock pore pressure state. Statistics show that pumping interference affects the borehole strain state. To investigate the interference mechanism of pumping to RZB-3 type FCBS at Tai'an seismic station, we take a known pumping as an example, in which we study the principal strain state of the borehole in three periods of normal pumping, interruption of pumping and resuming pumping respectively. During each period, we solve 3 parameters of the principal plane strain state, i.e. the maximum principal strain rate, the minimum principal strain rate and the maximum principal strain direction from four observation equations of FCBS by nonlinear iterative least squares algorithm. On the other hand, concentrated load model (CLM) is used to simulate the mechanical mechanism of pumping. Firstly, the depth of FCBS relative to pumping source and the concentrated load at pumping source are inversed, then, the strain state surrounding the pumping well, including the state at RZB-3 borehole, is simulated by forward modeling. By comparing these results, we find that: (1)The concentrated load at pumping source inversed by CLM during periods of normal pumping and resuming pumping are both located at or near the bottom of the pumping well, which is consistent with the actual situation, indicating that mechanism and degree of the influence of pumping on borehole strain are well simulated by CLM. (2)The observed strain state is consistent with the simulation result of pumping interference by forward modeling, indicating that the principal strain state of borehole calculated based on observation of FCBS reflects the true strain state of borehole under different pumping states.(3)The inversed concentrated load at pumping source during pumping periods is significant greater than the load of the pumped water, indicating that the pumping process has more significant influence on the pore pressure of rocks than the load of the pumped water. Even though CLM is an approximate simulation since it's based on some elastic assumptions, the interference mechanism of pumping on RZB-3 type FCBS at Tai'an seismic station is well explained, which is maybe very helpful for studying the influence of pumping interference on other deformation instruments, locating the unknown pumping source and studying the characteristics of pore pressure of rocks.