分层岸滩侧蚀坍塌过程及其水动力响应模拟          下载免费PDF全文

假冬冬  黑鹏飞  邵学军  张幸农 《水科学进展》2014,25(1):83-89

非均质岸滩广泛分布于冲积河流中,其侧蚀过程沿垂向具有分层特点。基于全三维水沙模型及河岸侧蚀坍塌力学模式,提出动态网格跟踪技术,构建了非均质岸滩侧蚀沿垂向差异的三维动力学模拟方法。以连续弯道概化水槽为例,模拟分析了非均质河岸侧蚀过程中三维水流结构的响应特征。研究结果表明:坡脚冲刷后,底部主流向凹岸偏移,在已有弯道环流的基础上,于坡脚处出现一反向次生流;上部粘性土层坍塌后,崩塌土体堆积于坡脚处,上部主流明显左偏,下部次生流消失;随着坡脚堆积体的冲刷搬运,下部主流进一步向凹岸偏移;如此循环,主流不断向凹岸偏移,致使岸坡持续崩退、河道摆动。  相似文献   

Classification and detection of dominant factors in geospatial patterns of traditional settlements in China     

Wu  Shaolin  Di  Baofeng  Ustin  Susan L.  Stamatopoulos  Constantine A.  Li  Jierui  Zuo  Qi  Wu  Xiao  Ai  Nanshan 《地理学报(英文版)》2022,32(5):873-891

Journal of Geographical Sciences - The geospatial distribution pattern in traditional Chinese settlements (TCSs) reflects the traditional harmony between humans and nature, which has been learned...  相似文献   

地理国情普查影像解译自动化方案研究     

任思思  张学之  张禹 《东北测绘》2014,(6):44-46

随着空天地一体化对地观测传感网的逐步完善,积累了大量的空间遥感影像。地理国情普查项目进一步地推动了遥感技术的发展和遥感影像的使用,使遥感影像更好地服务于经济社会的发展和生态文明的建设。传统的依靠人工的地物信息提取方式不能满足需求,本文尝试影像解译自动化方案替代完全依靠人工采集的方式,提高遥感信息提取的效率。  相似文献   

On the relation between the evolution of natural environment and human factors and the development of urban settlement—Take the Lanzhou Valley Basin as an examples     

Xiaowei Xian  Linyuan Zhang  Nanshan Ai  Wohlke Wihelm 《中国地理科学(英文版)》1991,1(1):42-53

Lanzhou Valley Basin is composed of two smaller diamond-shaped basins striking from NW to SE and including 6 river terraces. The lower terraces remaining even and smooth are main sites for city buildings. The main function of Lanzhou urban settlement is a ferry and transport centre. Lanzhou used to be an important crossing site and post on the “silk road”, and then became a transport and trade centre in Northwest China. In the middle part of the 17th century, Lanzhou became the capital of Gansu, a new province. The development process of Lanzhou urban settlement indicates that urban settlement is a system consisting of natural environment and human society based on the former.  相似文献   

Reversed-polarity structures of chromospheric magnetic field     

Wei Li  Guoxiang Ai  Hongqi Zhang 《Solar physics》1994,151(1):1-14

Reversed-polarity structures of chromospheric magnetic fields are magnetic gulfs and islands of opposite polarity relative to the underlying photospheric fields. In this paper data measured with the Solar Magnetic Field Telescope of the Huairou Solar Observing Station in Beijing were analyzed. From more than 300 pairs of photospheric magnetograms (in FeI λ5324.19 Å) and relevant chromospheric magnetograms (Hβ λ4861.34 Å), the reality of the reversed-polarity structures is demonstrated. According to an analysis of the fine structure of the magnetic field in the two layers of active regions, we found that there are probably four different types as follows: Type A: magnetic islands of opposite polarity corresponding to photospheric fields appear in the chromospheric magnetogram. Type B: magnetic gulfs of opposite polarity corresponding to photospheric fields appear in the chromospheric magnetogram. Type C is the reverse of type B. That is, a magnetic gulf of opposite polarity corresponding to the chromospheric field appears in the photospheric magnetogram. Type D is the reverse of type A.  相似文献   

加快信息产业化 促进社会经济持续发展     

吕鸣伦  鲁奇 《地球信息科学学报》1997,(1):9-11

以构建高效信息传输网络为代表的全球信息化浪潮正在蓬勃兴起。这是现代科学技术发展对人类社会的一次革命性变革,对人类社会生产方式、产业结构、价值观和行为规范都将产生深刻的影响。从世界范围看,信息产业从传统的第三产业中分离出来,成为一种独立的新兴产业的趋势已日益明显。信息产业可以成为中国跨世纪发展的支柱产业和具有持久效能的高效经济增长点。而将汽车工业作为全国2/3省区“九五”期间的支柱产业是不适宜的。加快发展信息产业,也是中国根据自身的国情,建立资源节约型的国民经济体系,实现“两个转变”和社会经济可持续发展目标的必然选择。  相似文献   

Geochronology, Eruption Sequence and Geochemistry of Mid–Late Jurassic Volcanics South of Manzhouli: Petrogenesis and Implications for Mesozoic Tectonic Regime Transformation     

BAI Yuling  WANG Tao  WANG Zongqi  YAN Jie  ZHANG Ai 《《地质学报》英文版》2023,97(4):1112-1131

To the south of Manzhouli, Hulunbuir, Inner Mongolia, experienced a tectonic regime transformation from compression to extension in the mid-Mesozoic. Based on systematic research of the volcanics, petrology, volcanic facies, chronology and geochemistry of rocks in the Buridun area, two stages of volcanics are identified. The first stage named the trachyte series was formed in the late Middle Jurassic (167–163 Ma), its eruption rhythm is pyroxene trachyandesite–trachyandesite–trachyte, and its origin rock is basic volcanics from thickened lower crust, with a tectonic setting in the collision orogeny after the closure of the Mongolia Okhotsk Ocean (MOO). The second stage is a bimodal volcanic rock, formed in the early Late Jurassic (163–160 Ma). The eruption rhythm of basic volcanics in this stage is basaltic andesite–basalt–olivine basalt, which comes from the metasomatized lithospheric mantle, the acidic volcanics of which being characterized by the eruption rhythm of sedimentary-explosive-overflow facies, which came from the partial melting of newly formed lower crust, and this shows the characteristics of A-type granite; the tectonic setting is extension of the lithosphere after collision and closure of the MOO. The changes in the formation age and tectonic setting of the two stages of volcanics demonstrate that the transition time from the compressive system to the extensional system south of Manzhouli is about 163 Ma.  相似文献   

川东北元坝西部须家河组二段优质储层展布特征研究          下载免费PDF全文

黄彦庆  肖开华  王爱  林恬  王濡岳 《沉积与特提斯地质》2023,43(3):489-500

川东北元坝地区须家河组二段致密砂岩气资源潜力巨大,但储量探明率低、测试效果差异大,主要原因之一是致密砂岩储层非均质性强、优质储层分布规律不清。本文充分利用测录井、岩心及相关分析化验等资料,在分砂组刻画沉积微相展布的基础上,开展了须二段沉积演化过程、储层特征及其分布研究。结果表明：（1）元坝西部须二段经历了辫状河三角洲-滨浅湖-辫状河三角洲演化过程,沉积控制了砂体规模、粒度和矿物成分的空间变化;（2）须二段砂岩类型多样,整体致密,为低孔、低渗储层;储层物性与砂岩粒度,长石、石英和方解石胶结物含量等因素密切相关,这些因素主要受沉积和后期成岩作用控制;（3）须二段发育块状中粒长石岩屑砂岩和交错层理中粒石英砂岩两类有利岩石相,前者自西北向东南逐渐减薄、呈条带状展布,后者呈不连续土豆状,主体分布于西南部地区。  相似文献   

利用X射线粉晶衍射和电感耦合等离子体质谱法研究江西西华山钨矿床中黑钨矿的矿物学特征及指示意义     

鲁麟  梁婷  陈郑辉  王勇  黑欢  谢星 《岩矿测试》2015,34(1):150-160

目前针对江西大型黑钨矿石英脉型钨矿床西华山的黑钨矿矿物学特征及指示意义研究较少。本文利用X射线粉晶衍射分析和电感耦合等离子体质谱分析技术对黑钨矿晶体结构、化学成分特征及空间变化规律开展研究。获得黑钨矿晶胞参数为a0=0.477 nm,b0=0.573 nm,c0=0.498 nm,β=90°21',属于锰钨铁矿,与前人得出的黑钨矿晶胞参数略有不同,代表不同元素对铁锰的类质同象替代。主要化学成分WO3、Fe O、Mn O的含量在空间上具有一定的变化规律,反映了成矿物质的运移特征。微量元素Sc、Y、Nb、Ta在垂向含量变化大,说明矿液运移具有复杂性。稀土总量ΣREEs较高(397.16×10-6~1071.11×10-6),具有强烈的Eu负异常,具重稀土富集左倾的"躺椅式"球粒陨石标准化配分模式。将西华山、盘古山、淘锡坑、大吉山4个典型矿床的黑钨矿稀土元素特征进行对比,反映产在花岗岩内接触带的黑钨矿的稀土总量(ΣREEs)相对最高,分馏最明显;产在花岗岩内及其外接触带的黑钨矿的稀土总量(ΣREEs)相对较低,分馏程度最不明显;而产在花岗岩外接触带的黑钨矿的稀土总量(ΣREEs)有高有低,分馏程度有强有弱。因此,黑钨矿的化学成分变化特征,可以有效地指示成矿物质空间运移特征、物质来源和矿床成因。  相似文献   

透岩浆流体作用与矿田构造   总被引：1，自引：1，他引：0  

黑慧欣  罗照华  Vikentyev I V  郭晶 《地质力学学报》2015,21(1):1-12

从透岩浆流体成矿理论的角度对矿田构造进行了重新认识,提出矿田构造系统是一种复杂性动力系统的观点。根据这个模型,矿田构造是近场应力场与远场应力场强烈相互作用的产物。近场应力场由岩浆成矿系统而不是远场应力场派生,因而不能由矿田构造反演区域构造,但可以从区域构造限定矿田构造。矿田构造常有岩脉和热液脉充填,因而是可识别的。利用构造统计学方法,可以根据岩脉和/或热液脉的分布密度图(或等值线图)预测找矿靶区。  相似文献