长距离稀疏参考站下网络RTK电离层误差内插模型精度分析     

邓健  赵兴旺  张爱国 《测绘科学技术学报》2015,(3):236-240

针对现有内插模型是否能够满足长距离稀疏参考站下电离层误差内插精度要求的问题,以线性内插模型、距离相关内插模型作为研究对象,首先结合误差传播定律从理论上比较两种内插模型对参考站间电离层延迟估值误差的抗差性;然后选取多组距主参考站不同距离的实例数据,分析比较模型内插精度的变化规律。实例结果表明:LIM模型内插精度分布较均匀,且优于DIM模型;对比中长距离(100 km),在长距离稀疏参考站下,模型内插精度明显降低,特别是对于电离层误差波动范围较大的卫星,其内插偏差超过±3 cm的达到50%以上。  相似文献   

高温裂解在线测试高氯酸盐氧同位素方法研究   总被引：1，自引：0，他引：1  

方玲  周爱国  李小倩  刘运德  张梦南 《地质学报》2015,89(10):1832-1840

高温裂解在线测试高氯酸盐氧同位素的方法与技术,能够为环境介质中高氯酸盐来源的识别、迁移转化过程的示踪及其污染的防治提供重要的分析工具。采用单因子试验系统研究了方法的裂解温度、样品质量和样品类型对高氯酸盐氧同位素测试精度的影响,并采用阴离子交换树脂法进行高氯酸盐环境样品的预处理,探讨测试方法的应用。实验结果表明,反应温度对方法测试精度的影响显著,反应温度必须严格控制在1325℃;样品质量对测试精度不产生显著影响,但最小样品量不低于0.25μmol ClO-4;测试方法适用于不同类型的高氯酸盐,测试精度均优于0.5‰。测试结果不同的校正方法表明,采用多种氧同位素标准的线性校正优于采用单一高氯酸盐氧同位素标准的校正,特别是在样品与标准的氧同位素组成差别较大时,单一标准的校正会产生较大的误差。基于A530E型双官能团阴离子交换树脂的富集与提取ClO-4的预处理方法,可实现高氯酸盐环境样品的氧同位素测定,测试精度优于0.3‰。  相似文献   

Study on the geological conditions of metallogenesis of the Shazi large-scale anatase deposit in Qinglong County,Guizhou Province     

Min Zhang  Aiguo Nie  Fei Xie  Zhuru Zhang 《中国地球化学学报》2014,33(4):450-458

The Shazi large-scale anatase deposit in Qinglong County, Guizhou Province, has been discovered recently and now is under exploration. Investigations show that the orebodies mostly occur at the top of the karst unconformity of the Middle Permian Maokou Formation strata and at the bottom of the Emeishan basalt. And the following three prerequisites should be satisfied for the formation of the deposit： 1） there must be the material source of anatase; 2） there must be weekly alkaline media and low-tempeature and low-pressure conditions; 3） there was no high-temperature and high-pressure environment subsequently for the transformation of anatase into rutile. In the Emeishan basalt of western Guizhou, the element Ti mostly entered the silicon-oxygen tetrahedra of picrite in heterovalent isomorphism （Ti4＋＋Al3＋→Mg2＋＋Si4＋）. When volcanic ejecta resultant from strong eruption of the Emeishan basalt magma fell into water, picrite was usually dissociated to chlorite. Thus, the element Ti4＋ in the picrite could be released from the silicon-oxygen tetrahedraa of picrite into water, and conbined with oxygen in the water to form TiO2. This paper has proved that this deposit, enriched in anatase, discovered recently at Shazi, Qinglong Country, Guizhou Province, is a residual-deluvial-type deposit. Its genesis can be explained as follows. Volcanic clastics formed at the early stage of strong eruption of the Emeishan basalt magma were chemically deposited to form anatase in the low-temperature, low-pressure and weekly alkaline waters in the karst depressions at the top of the Maokou Formation （limestone） strata. The anatase was then dissociated owing to weathering and leaching during the Quaternary and the anatase was further enriched to form the residual-deluvial-type anatase ore deposit.  相似文献   

重庆市岩溶泉发育特征与流量控制机制分析     

肖成芳  魏兴萍  张爱国  陈英 《地理科学进展》2022,41(4):693-706

为给岩溶山区的经济发展和居民的生产生活提供水资源保障,论文以重庆市为例,通过查明重庆岩溶泉及其流量的发育规律和控制机制,利用1∶200000区域水文地质图和水文地质普查报告,运用水文地质勘查、统计分析和ArcGIS的空间分析等手段,在分析岩溶发育特征的基础上,分析地形地貌、地层岩性、地质构造和地表水系等因素对岩溶泉发育、分布及其流量的影响。结果表明：地势起伏度范围在0~200 m时最有利于岩溶泉的发育,随着地势起伏度的增加,岩溶泉平均流量开始逐渐减少;碳酸盐岩与碎屑岩岩组岩溶泉发育密度最大,其次为灰岩与白云岩互层岩组、灰岩岩组、白云岩岩组;构造复合部位、背斜缓翼、向斜轴部、断裂构造等地质构造部位均有利于岩溶泉发育;以岩溶水水动力特征及其与当地侵蚀基准面的相互关系为依据,将重庆市的岩溶大泉划分为以下3种类型：河床型、河岸型、河源型,而岩溶大泉分布数量由多到少分别为河岸型>河源型>河床型。  相似文献   

力觉临场感遥操作机器人(2):操作者的输入输出特性建模     

宋爱国  柯欣  潘礼正 《南京气象学院学报》2013,5(2):97-105

力觉临场感遥操作机器人系统是一个典型的人在回路(Human-in-Loop)的人机交互系统,操作者作为整个系统的一个重要单元是完成机器人控制的顶层控制环节.操作者需要接受力觉、触觉、视觉和运动信息反馈后,才能作出决策,远程操纵机器人执行任务,因此操作者是一个基于多输入单输出的复杂系统,而且具有非线性和时变性,需要建立一套相应的控制模型.文章通过分析操作者在力觉临场感遥操作系统中的感知、决策与动作的特性,建立了一种操作者的输入输出模型,并给出了模型的等效二端口网络形式,为力觉临场感遥操作机器人系统的分析提供了基础.  相似文献   

The flux profile of a blowing sand cloud: a wind tunnel investigation   总被引：11，自引：0，他引：11  

Zhibao Dong  Xiaoping Liu  Hongtao Wang  Aiguo Zhao  Xunming Wang 《Geomorphology》2003,49(3-4):219-230

The flux profile of a blowing sand cloud, or the variation of blown sand flux with height, is the reflection of blown sand particles that move in different trajectories, and also the basis for checking drifting sand. Here we report the wind tunnel results of systematic tests of the flux profiles of different sized sands at different free-stream wind velocities. The results reveal that within the 60-cm near-surface layer, the decay of blown sand flux with height can be expressed by an exponential function: q_h=aexp(−h/b), where, q_h is the blown sand transport rate at height h, a and b are parameters that vary with wind velocity and sand size. The significance of coefficient a and b in the function is defined: a represents the transport rate in true creep and b implies the relative decay rate with height of the blown sand transport rate. The true creep fraction, the ratio of the sand transported on the surface (h=0) to the total transport varies widely, decreasing with both sand size and wind speed. The flux profiles are converted to straight lines by plotting sand transport rate, q_h, on a log-scale. The slope of the straight lines that represents the relative decay rate with height of sand transport rate decreases with an increase in free-stream wind velocity and sand grain size, implying that relatively more of the blown sand is transported to greater heights as grain size and wind speed increase. The average saltating height represented by the height where 50% of the cumulative flux percentage occurs increases with both wind speed and grain size, implying that saltation becomes more intense as grain size and/or wind velocity increase.  相似文献   

东北地块群:构造演化与古大陆重建   总被引：7，自引：0，他引：7  

周建波  石爱国  景妍 《吉林大学学报(地球科学版)》2016,46(4):1042-1055

东北地区位于西伯利亚板块、华北板块和太平洋板块之间,为"中亚造山带"的东段和太平洋构造域的叠加部位,因此东北地块群构造属性和背景的研究对深入探讨二大构造域的叠加与转化背景具有重要的理论意义。东北地块群从东到西可细分佳木斯兴凯、松辽、兴安和额尔古纳四大地块,这些地块具有相同的新元古代泛非期变质基底,而古生代沉积岩也存在一定的可比性,表明这些地块存在相同或者相似的构造演化背景。分割这些地块的构造边界特征为:1）额尔古纳与兴安地块的缝合带为早古生代头道桥-新林缝合带,而非中生代德尔布干断裂;2）兴安地块与松辽地块之间的贺根山黑河缝合带形成时代为晚石炭世（330~300 Ma）,而非最近报道的中生代;3）古亚洲洋分布在东北陆块群与华北板块之间,沿西拉木伦-长春缝合带闭合,时代为三叠纪;4）佳木斯兴凯地块与松辽地块之间的吉黑高压带形成于古亚洲构造域与环太平洋构造域转换的关键时期（210~180 Ma）;5）那丹哈达增生杂岩为中国境内古太平洋板块俯冲增生的唯一直接证据,并记录了晚三叠早白垩世古太平洋板块向欧亚大陆俯冲增生的过程。在此基础上,分析了东北地块群发育的典型古生物和年代学标志,重建了东北地块群从Gondwana 大陆到Pangea大陆的位置与模型。  相似文献   

羌塘盆地中生界海相黑色泥页岩特征及页岩气远景区预测   总被引：1，自引：0，他引：1  

王丽波  苏爱国  郑有业  李超  久凯 《地学前缘》2012,19(3):264-279

青藏高原羌塘盆地中生界发育上三叠统肖茶卡组（T3x）、中侏罗统布曲组（J2b）和上侏罗统索瓦组（J3s）3套海相黑色泥页岩,形成于有机质比较丰富且易于保存的营养型还原性沉积环境,以台地相为主,其次为盆地相和三角洲相;厚度在41～474 m范围内,有机碳（TOC）含量平均值为0.25%～8.34%,有机质类型主要为Ⅱ型干酪根,镜质体反射率（Ro）平均值为1.21%～3.0%,处于高-过成熟生气阶段,脆性矿物以石英、长石为主,含量为65%～70%,页岩孔隙度约2%。与美国主要盆地产气页岩各项指标相比较,羌塘盆地中生界海相黑色泥页岩具有厚度大、有机质丰度低、热演化熟度高、脆性矿物种类多、石英含量较低、长石和粘土矿物含量较高及孔隙度低的特征,具备了形成页岩气基本地质条件,是我国海相页岩气勘探的沉积盆地之一,综合评价预测的页岩气远景区以上三叠统肖茶卡组（T3x）分布范围大,其次是布曲组（J2b）和索瓦组（J3s）。  相似文献   

排桩冻结法深基坑施工监测与反馈分析   总被引：5，自引：0，他引：5  

袁宝远  赵燕容  朱旭芬  陈艳国  李爱国 《工程地质学报》2005,13(4):533-537

对于润扬大桥南锚碇排桩冻结法深大基坑,冻结作用使基坑的受力过程变得更为复杂,根据排桩冻结法基坑结构和场地工程地质条件,建立了大型安全监测系统。本文介绍了润扬大桥南锚碇场地工程地质条件、排桩冻结法基坑的结构和南锚碇基坑监测方案、分析了南锚排桩冻结法深基坑各项监测数据的变化规律,包括侧向土压力、内支撑轴力、排桩钢筋应力和排桩水平位移随时间变化规律,并基于施工监测进行了反馈分析,保障了南锚碇排桩冻结法深基坑的安全与稳定。监测结果分析表明,排桩冻结法是基坑工程的一种可行的施工工法,润扬大桥南锚碇排桩冻结法深大基坑的成功实践为今后类似工程的建设积累了宝贵经验。  相似文献   

Preliminary Study on the Water Drag of Schlegel＇s Black Rockfish Sebastes schlegeli     

LIWentao ZHANGXiumei GAOTianxiang JINGAiguo 《中国海洋大学学报(英文版)》2004,3(1):70-74

Drag forces acting on Schlegel‘s black rockfish Sebastes schlegeli were studied. A new drag force transducer was designed and used to measure the water drag on Schlegel‘s black rockfish in a vertical recirculating flume tank. Fourteen individuals were investigated, yielding two mean drag coefficients referred to the cross-sectional area and volume^2/3 respectively at water velocities ranging from 0.3 to 1.0 ms^-1 The drag coefficients can be used for estimating the drag forces acting on Sebastes schlegeli in water.  相似文献