基于新型超材料结构的高效率发射天线技术研究综述     

杨琬琛  车文荃  陈东旭  陈思 《南京气象学院学报》2017,9(1):54-63

近年来,超材料打破了传统材料或结构的物理极限,为高效率发射天线的发展开辟了崭新的研究空间,获得了愈来愈广泛的关注.首先介绍了超材料的理论和结构研究概况,然后针对几种新型超材料技术在提高平面天线单元效率的研究工作进行了详细介绍和分析,包括非周期超材料技术、超材料作为新型辐射元或低剖面反射板等方面.最后,针对无线能量收集系统对高效率天线阵列的需求,介绍了高次模激励技术和新型低损耗传输线技术,以此降低阵列馈电网络的损耗,从而提高系统的整体效率.  相似文献   

集成遥感数据的陆地净初级生产力估算模型研究综述     

洪长桥  金晓斌  陈昌春  王慎敏  杨绪红  项晓敏 《地理科学进展》2017,36(8):924-939

净初级生产力(NPP)是衡量碳循环、指导土地利用、评估生态安全、指示环境变化、反映粮食安全等的重要参量,其估算受模型构建机理和生态系统关键地表参数输入的影响。近年来,随着遥感数据的不断丰富和遥感处理技术的快速发展,集成遥感数据的NPP估算模型相较于仅采用气候、土壤等传统观测数据的非遥感模型,在分析时空异质性等方面的优势日益凸显。本文基于Web of Science和CNKI两大数据库,采用文献统计分析方法,系统回顾NPP研究概况及国内外集成遥感数据的NPP估算模型的近期进展;并将集成遥感数据进行NPP估算的模型分为统计模型、光能利用率模型、过程模型及耦合模型四类;重点阐述了各类遥感估算模型的机理、差异性、适宜性及局限性;最后,在分析NPP遥感估算面临困境和科学挑战的基础上,从机理与影响因素、数据基础、参数反演、时空尺度拓展、软硬件支撑等方面对未来研究进行了展望。  相似文献   

陆缘扩张型地洼盆地系及其形成机制探讨   总被引：9，自引：5，他引：4  

邹和平 《大地构造与成矿学》1995,19(4):303-313

本文提出“陆缘扩张型地洼盆地系”这一概念,以突出表述分布于东亚陆缘壳体之上,形成于地洼余动期的张性地洼盆地系列的壳体演化—动力环境。指出陆缘海中的裂陷盆地的成因难于与大洋板块俯冲导致弧后扩张的理论模式相联系,也不同于大西洋型盆地,而是大陆地壳演化到地洼余动期,并经历过华夏期地洼型造山运动之后拉伸裂陷的结果。论证了“岩石圈底层剥落、华夏期地洼造山带拉伸裂陷”是东亚陆缘扩张发生的一种重要机制,进而建立了由华夏期地洼型挤压造山带到盆岭型构造带和陆缘海盆地系的构造发展模式。  相似文献   

中国电子机械制造业产品内出口贸易空间布局     

李振发  贺灿飞 《地理研究》2021,40(1):119-137

电子机械制造业产品在中国对外贸易中占有重要地位,以产品内贸易视角研究其出口空间布局有助于剖析中国出口体系结构特征。在区分中间、最终产品,一般、加工贸易的前提下,本文观察了出口所在地和目的国两个维度中国电子机械制造业产品出口企业空间布局,并基于技术关联探讨了其动态演化的驱动因素。结果如下：① 在全国层面,除加工贸易最终产品外,一般贸易中间产品、加工贸易中间产品和一般贸易最终产品与某地产品结构的技术关联程度越高,对应的出口企业越可能到该地进行出口。在东部地区,上述关系在4类产品中均存在,而在中部和西部地区,其只存在于一般贸易产品。② 一般贸易产品与某国从中国进口的产品结构技术关联程度越高,对应企业越倾向于出口到该国。但依据收入水平将目的国分组后,这种促进关系在高收入国家中不存在。加工贸易产品出口企业目的国布局与对应技术关联程度无明显关系。  相似文献   

Geographical Impact and Ecological Restoration Modes of the Spatial Differentiation of Rural Social-Ecosystem Vulnerability: Evidence from Qingpu District in Shanghai     

REN Guoping  LIU Liming  LI Hongqing  SUN Qian  YIN Gang  WAN Beiqi 《资源与生态学报(英文版)》2021,12(6):849-868

Vulnerability research is the core issue and one of the research hotspots of sustainable development science. Vulnerability and its evaluation framework provide a new perspective for rural social-ecosystem studies. This paper introduced the ‘input-output’ efficiency theory and constructed the ‘SEE-PSR’ framework for the analysis of social-ecosystem vulnerability in the rural area in Qingpu District of Shanghai City. The DEA models, spatial autocorrelation model, multivariate logistic regression model, geographical detector and hierarchical cluster model were used to analyze the spatial differences of social-ecosystem vulnerability, and its geographical impact mechanisms and ecological restorations, in 184 administrative villages in this area. The results can be divided into three main points. (1) The results of the ‘input-output’ efficiency model of the EW-DEA based on entropy weight aggregation crossover was more reliable and accurate for the evaluation of rural social-ecosystem vulnerability. The vulnerability of the social-ecosystems in the administrative villages showed a trend of gradual decline from east to west, with an average value of vulnerability of 0.583, and the vulnerability of social systems had become an important factor in constraining the decrease of the vulnerability of the social-ecosystems in the region. (2) The distances from the center of Shanghai City, from Dianshan Lake, from the center of Qingpu District and from the water area were the four dominant geographical factors affecting the vulnerability of the social-ecosystem in this region. The geographical impacts exhibited the spatial differentiations of systemic structure, the substitution of typological attributes and the transformation level. (3) The geographical factors coupling the impact types of the social-ecosystem vulnerability were divided spatially into 10 types. The geographic multi-factor coupling impact types were dominant, which presented multi-cyclic spatial patterns and were dominated by the central multi-factor which was surrounded by the single factor types on both sides. According to the different types, some feasible ways of ecological restoration were proposed, which drew on the experiences of integrated territory consolidation to remediate the vulnerability of rural social-ecological systems. The results of this study can provide scientific reference for rural spatial reconstruction, regional ecological restoration and sustainable development for the regions characterized by conflict in the ‘strict protection of the ecological environment and vigorous development of the economy’.  相似文献   

Tectonic configuration of the Apuseni–Banat—Timok–Srednogorie belt, Balkans-South Carpathians, constrained by high precision Re–Os molybdenite ages     

Aaron Zimmerman  Holly J. Stein  Judith L. Hannah  Dejan Koželj  Kamen Bogdanov  Tudor Berza 《Mineralium Deposita》2008,43(1):1-21

The Apuseni–Banat–Timok–Srednogorie magmatic–metallogenic belt (ABTS belt), forms a substantial metallogenic province in the Balkan-South Carpathian system in southeastern Europe. The belt hosts porphyry, skarn, and epithermal deposits mined since pre-Roman times. Generally, the deposits, prospects, and occurrences within the belt are linked to magmatic centers of calc-alkaline affinity. Fifty-one rhenium-osmium (Re–Os) ages and Re concentration data for molybdenites define systematic geochronologic trends and constrain the geochemical-metallogenic evolution of the belt in space and time. From these data and additional existing geologic-geochemical data, a general tectonic history for the belt is proposed. Mineralization ages in Apuseni-Banat, Timok, and Panagyurishte (the central district of the larger E–W Srednogorie Zone) range from 72–83, 81–88, and 87–92 Ma, respectively, and clearly document increasing age from the northwestern districts to the southeastern districts. Further, Re–Os ages suggest rapidly migrating pulses of Late Cretaceous magmatic–hydrothermal activity with construction of deposits in ~1 m.y., districts in ~10 m.y., and the entire 1,500 km belt in ~20 m.y. Ages in both Timok and Panagyurishte show systematic younging, while deposit ages in Banat and Apuseni are less systematic reflecting a restricted evolution of the tectonic system. Systematic differences are also observed for molybdenite Re concentrations on the belt scale. Re concentrations generally range from hundreds to thousands of parts per million, typical of subduction-related Cu–Au–Mo–(PGE) porphyry systems associated with the generation of juvenile crust. The geochronologic and geochemical trends are compatible with proposed steepening of subducting oceanic slab and relaxation of upper continental plate compression. Resulting influx of sub-continental mantle lithosphere (SCML) and asthenosphere provide a fertile metal source and heat, while the subducting slab contributes connate and mineral dehydration fluids, which facilitate partial melting and metal leaching of SCML and asthenosphere. Cu–Au–Mo–(PGE) porphyry deposits may develop where melts are trapped at shallow crustal levels, often with associated volcanism and epithermal-style deposits (South Banat, Timok, and Panagyurishte). Mo–Fe–Pb–Zn skarn deposits may develop where felsic melts are trapped adjacent to Mesozoic limestones at moderate crustal levels (North Banat and Apuseni). Systematic spatial variations in deposit style, commodity enrichment, Re–Os ages, and Re concentrations support specific tectonic processes that led to ore formation. In a post-collisional setting, subduction of Vardar oceanic crust may have stalled, causing slab steepening and rollback. The slab rollback relaxes compression, facilitating and enhancing orogenic collapse of previously thickened Balkan-South Carpathian crust. The progression of coupled rollback-orogenic collapse is evidenced by the width of Late Cretaceous extensional basins and northward younging of Re–Os ages, from Panagyurishte (~60 km; 92–87 Ma) to Timok (~20 km; 88–81 Ma) to Apuseni-Banat (~5 km; 83–72 Ma). Generation of a well-endowed mineral belt, such as the ABTS, requires a temporally and spatially restricted window of magmatic–hydrothermal activity. This window is quickly opened as upper plate compression relaxes, thereby inducing melt generation and ingress of melt to higher crustal levels. The window is just as quickly closed as upper plate compression is reinstated. The transient tectonic state responsible for economic mineralization in the ABTS belt may be a paleo-analogue to transient intervals in the present subduction tectonics of SE Asia where much mineral wealth has been created in the last few million years.  相似文献   

Gypsum-karst problems in constructing dams in the USA     

Kenneth S. Johnson 《Environmental Geology》2008,53(5):945-950

Gypsum is a highly soluble rock and is dissolved readily to form caves, sinkholes, disappearing streams, and other karst features that typically are also present in limestones and dolomites. Gypsum karst is widespread in the USA and has caused problems at several sites where dams were built, or where dam construction was considered. Gypsum karst is present (at least locally) in most areas where gypsum crops out, or is less than 30–60 m below the land surface. These karst features can compromise on the ability of a dam to hold water in a reservoir, and can even cause collapse of a dam. Gypsum karst in the abutments or foundation of a dam can allow water to pass through, around, or under a dam, and solution channels can enlarge quickly, once water starts flowing through such a karst system. The common procedure for controlling gypsum karst beneath the dam is a deep cut-off trench, backfilled with impermeable material, or a close-spaced grout curtain that hopefully will fill all cavities. In Oklahoma, the proposed Upper Mangum Dam was abandoned before construction, because of extensive gypsum karst in the abutments and impoundment area. Catastrophic failure of the Quail Creek Dike in southwest Utah in 1989 was due to flow of water through an undetected karstified gypsum unit beneath the earth-fill embankment. The dike was rebuilt, at a cost of US $12 million, with construction of a cut-off trench 600 m long and 25 m deep. Other dams in the USA with severe gypsum-karst leakage problems in recent years are Horsetooth and Carter Lake Dams, in Colorado, and Anchor Dam, in Wyoming.  相似文献   

碎石土潜水含水层成井工艺研究     

柯柏林 《地下水》2008,30(1):92-94

从北京市丰台地区第四系潜水含水层的地层岩性结构入手,分析了传统供水管井成井工艺存在的问题,详细研究介绍了孔壁坍塌填砾法成井工艺在实际水井工程项目中的成功应用,取得了较好的增加水井出水量的效果。  相似文献   

Late orogenic collapse and thermal doming in the northern Gondwana margin incorporated in the Variscan Chain: A case study from the Ozieri Metamorphic Complex, northern Sardinia, Italy     

Leonardo Casini  Giacomo Oggiano   《Gondwana Research》2008,13(3):396-406

A branch of the South European Variscan chain is noticeably exposed in Sardinia. The early stage of collision between the Northern Gondwana margin and the Armorica Terrane Assemblage (ATA) generated syn-metamorphic folding and thrusting. The evidences of such deformation are well preserved in the nappe zone, a structural domain characterized by stacking of different tectonic units under metamorphism of Barrovian greenschist facies. A late, post-nappe, shortening, under retrograde metamorphic conditions, gave rise to wide, upright, N120–N160 trending antiforms that control the trend of the chain. The structural analysis of the Ozieri Metamorphic Complex (OMC) shows evidence of an important phase of late-Variscan extensional tectonics. Deformation results in, the formation of oppositely dipping, normal shear zones, which developed at upper and middle structural level along the limbs of major regional antiforms causing fabric reactivation, crustal thinning, and exhumation of the OMC core. Within the OMC, the activity of the shear zones was coeval with HT-LP metamorphism as suggests the occurrence of syn-kinematic cordierite + andalusite ± sillimanite + biotite. Whereas syntectonic dykes and a tonalite body in the deeper part of the OMC indicate that early emplacement of melt along shear zones and/or in the antiform hinges possibly supplied the heat for the anomalous thermal gradient and triggered the exhumation of a core complex-like structure.  相似文献   

秦岭及周边地区夏季降水的主模态分析   总被引：3，自引：0，他引：3       下载免费PDF全文

潘留杰  张宏芳  陈小婷  邹涛  张科翔 《大气科学学报》2018,41(3):377-387

基于秦岭及周边地区394站气象观测资料、欧洲中期数值预报中心(ECMWF)再分析ERA-Interim数据,利用小波和回归等分析方法,讨论了秦岭及周边地区夏季降水年际变化的主模态以及与其相联系的大气环流异常。结果表明:1)在年际变化的时间尺度上,秦岭及周边地区夏季降水主要表现为秦岭南北降水的气候差异性变化(EOF1)、黄土高原第二地形抬升带与其两侧降水的反位相振荡(EOF2)、秦岭西南部降水正异常和其东北部降水负异常变化(EOF3)和关中平原的地形降水贡献(EOF4)4个模态,其解释方差总贡献为73%,并且具有显著的2~4 a周期,其中EOF3和EOF4还具有4~8 a左右的年际变化周期。2)回归分析表明,EOF1正位相环流特征表现为200 hPa急流偏弱,中纬度槽填塞,西太平洋副热带高压强度偏弱,有来源于东海的水汽输送,使得秦岭北部降水偏多;EOF2和EOF3分别具有显著的蒙古低压和东北冷涡环流特征;EOF4的500 hPa环流异常不显著。3)根据新定义的秦岭季风指数回归分析表明,回归场的季风指数和降水模态的时间系数显著相关,秦岭北部降水偏多(少),南部降水偏少(多),反映了强(弱)季风年的年际转换。反之则具有多态性,不同年份强(弱)秦岭回归季风指数的环流形势存在较大的差异,可能触发多种降水模态和位相振荡。  相似文献