铅锌冶炼厂大气污染主要模式及防治   总被引：2，自引：0，他引：2  

赵桂久  于丽长 《地理科学》1989,9(2):158-162

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冀东花岗岩及迁西群中宇宙尘的发现及其特征     

康昱桂  陈克荣 《地质与勘探》1994,30(6):43-47,55

冀东的峪耳崖岩体、葫芦峪岩体、三道湾岩体及迁西群老基底变质岩中发现的强磁性铁质小球，经大量分析对比研究后，确认它们属同一种宇宙尘。这在迁西群变质岩中尚属首次。  相似文献   

用罗丹明B和2—噻吩甲酰三氟丙酮萃取荧光法测定铀     

长沼健  都筑智 《国外铀金地质》1991,(2):86-87

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震后土地使用计划对恢复重建至关重要     

陈英方  陈长林 《地震科技情报》1992,(6):1-3

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云南省煤层气资源勘探开发对外合作     

桂宝林  罗启亮  胡克宁  罗俊  司胜利  郭秀钦 《云南地质》2004,23(4):434-442

滇东地区有较丰富的煤炭和煤层气资源。中美合作项目"云南恩洪和老厂地区煤层气资源开采对外合作",属我国煤层气勘探开发对外合作项目之一。开展二年来,取得丰硕成果。本文介绍我省的煤层气资源,我国煤层气开发鼓励政策及相关法规,我国煤层气对外合作的基本原则和合作模式,我省煤层气勘探开发合作项目的进展及取得的成果。  相似文献   

带有差分GPS的多传感器无人直升机航测遥感系统   总被引：1，自引：0，他引：1  

陈天恩  长井正彦  柴崎亮介 《测绘科学》2012,(1):158-160,184

本文主要介绍作者在日本研制的一种基于无人直升机平台的多种传感器航测遥感系统,它直接采用GPS和IMU数据进行地理定位定向而不需要地面控制点。通过实飞数据对系统达到的几何精度进行了验证,结果表明该系统可用来测绘大比例尺地形图以及应用于其他相关领域。  相似文献   

临沂市地质灾害预警预报与指挥系统的设计与实现     

密长林  孙景广  安振  王祥 《国土资源信息化》2012,(4):40-43

本文结合国内外有关地质灾害预警预报的相关理论研究,论述了临沂市地质灾害预警预报与指挥系统的总体框架和功能设计,介绍了本系统的预警预报、应急指挥、态势标绘等功能。系统旨在逐步提高临沂市的地质灾害预警预报技术水平,为各级政府制定国民发展计划和城镇规划提供重要的科学依据,为减灾防灾提供技术支撑。  相似文献   

Eurasian Snow Cover Variability and Its Association with Summer Rainfall in China   总被引：13，自引：0，他引：13  

WU Bingyi  YANG Kun  ZHANG Renhe 《大气科学进展》2009,26(1):31-44

This study investigates the statistical linkage between summer rainfall in China and the preceding spring Eurasian snow water equivalent (SWE), using the datasets of summer rainfall observations from 513 stations, satellite-observed snow water equivalent, and atmospheric circulation variables in the NCEP/NCAR re-analysis during the period from 1979 to 2004. The first two coupled modes are identified by using the singular value decomposition (SVD) method. The leading SVD mode of the spring SWE variability shows a coherent negative anomaly in most of Eurasia with the opposite anomaly in some small areas of the Tibetan Plateau and East Asia. The mode displays strong interannual variability, superposed on an interdecadal variation that occurred in the late 1980s, with persistent negative phases in 1979--1987 and frequent positive phases afterwards. When the leading mode is in its positive phase, it corresponds to less SWE in spring throughout most of Eurasia. Meanwhile, excessive SWE in some small areas of the Tibetan Plateau and East Asia, summer rainfall in South and Southeast China tends to be increased, whereas it would be decreased in the up-reaches of the Yellow River. In recent two decades, the decreased spring SWE in Eurasia may be one of reasons for severe droughts in North and Northeast China and much more significant rainfall events in South and Southeast China. The second SVD mode of the spring SWE variability shows opposite spatial variations in western and eastern Eurasia, while most of the Tibetan Plateau and East Asia are in phase. This mode significantly correlates with the succeeding summer rainfall in North and Northeast China, that is, less spring SWE in western Eurasia and excessive SWE in eastern Eurasia and the Tibetan Plateau tend to be associated with decreased summer rainfall in North and Northeast China.  相似文献   

The time and frequency standard system for FAST receivers     

朱凯  范瑾  Kun Liang  Wei Tang  Zhi-Sheng Gao  Yan Zhu  Yi Feng  Wei-Wei Zhu  Lei Qian  You-Ling Yue  Jin-You Song  Xiang-Wei Shi  Xing-Yi Wang  Ming-Lei Guo  Hang Zhang  Heng-Qian Gan  Hong-Fei Liu  Cheng-Jin Jin  Peng Jiang 《天文和天体物理学研究(英文版)》2020,(5):148-154

This paper reports on the time and frequency standard system for the Five-hundred meter Aperture Spherical radio Telescope(FAST),including the system design,stability measurements and pulsar timing observations.The stability and drift rate of the frequency standard are calculated using 1-year monitoring data.The UTC-NIM Disciplined Oscillator(NIMDO)system improves the system time accuracy and stability to the level of 5 ns.Pulsar timing observations were carried out for several months.The weighted RMS of timing residuals reaches the level of less than 3.0μs.  相似文献   

神狐海域海底峡谷群脊部细粒浊积体分布范围及意义     

姜衡  苏明  雷新华  匡増桂  吴能友  刘丽华  杨睿 《海洋地质与第四纪地质》2018,(5)

利用广州海洋地质调查局在南海北部神狐钻探区采集的高分辨率地震数据,结合2007年第一次水合物钻探航次(GMGS01)获取的岩心资料,从宏观地震反射结构、微观岩心粒度特征两个方面对GMGS01区块内残留在峡谷群脊部的细粒浊积体进行特征识别和刻画。研究结果显示,似海底反射(bottom simulating reflectors,BSR)之上存在着2套特征不同的沉积单元,位于下部的沉积单元1表现为薄层杂乱透镜状的地震反射特征,对应于粒度C-M图版中与C=M基线近似平行的含水合物层段的样品,被解释为峡谷群脊部的细粒浊积体。选取穿过神狐海域峡谷群中第16条海底峡谷的8条测线为研究对象,能够揭示沉积单元1(细粒浊积体)自北向南的空间变化特征,从而进行分布范围的确定。神狐海域沉积过程分析表明,峡谷群脊部的细粒浊积体是北部小型水道侵蚀下伏沉积物并发生再搬运和再沉积的结果。利用区域性覆盖的二维地震资料,本次研究确定了小型水道的北部侵蚀边界。综合GMGS01区块细粒浊积体的地震反射特征、穿过神狐海域东部第16号海底峡谷自北向南的地震反射差异、研究区北部小型水道的侵蚀边界,本次研究利用两点确定一线和相似平行的方法,在整个神狐海域初步确定了峡谷群脊部细粒浊积体的分布范围。细粒浊积体沉积边界的识别,将为从深水沉积的角度探讨神狐海域水合物不均匀性分布提供依据,同时也能进一步揭示该区域峡谷群脊部水合物的成藏机制和富集规律。  相似文献