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951.
952.
基性麻粒岩产于大陆地壳深部,它的研究可以为大陆岩石圈的性质、组成、演化和深部动力学过程提供重要信息。南天山库米什榆树沟地区发育总厚达1000多米的基性麻粒岩构造岩片,走向南东,朝北东推覆。剖面上和石炭纪蛇绿混杂岩共存,并发生了石榴子石的旋转变形和强烈的石英-长石矿物相韧性变形。然而它们的变形条件至今尚未被研究。本文运用透射电镜(TEM)超微组构技术对榆树沟基性麻粒岩中石英和石榴子石进行了详细研究,结果表明,石英中存在着丰富的超显微变形构造,自由位错、亚颗粒和位错网非常发育,这表明研究区基性麻粒岩在折返抬升过程中曾遭受过较强的石英-长石相韧性变形作用;石榴子石中的超微变形构造则极为少见,只在其中发现几根自由位错,并在其颗粒边缘发现少量亚颗粒构造,说明该矿物主体属于脆性变形。这两种矿物变形性质的差异,反映了石榴子石的晶体结构在该条件下比石英更稳定,而且说明石榴子石的变质温度没有超过900℃,也就是说,本区麻粒岩的变质作用并非发生在极高温度的条件下。 相似文献
953.
基于中国静止气象卫星FY-2C的多光谱数据,研究了由热红外亮温和可见光反照率拟合反演白天地面像素级逐时雨强分布的方法.利用降雨概率判识矩阵区分了降雨云和非降雨云,技术得分为0.5073,比简单利用阈值划分方法显著提高了雨区判识精度.对逐时降水率的分析,允许误差为±20%内,正确率为52.19%.对降水等级的分析,经1200多个实测有雨样本的检验,其对小雨、中雨、大雨和暴雨的实测命中率达62.79%.若将降水率小于0.5mm/h的微雨这种临界状态作无雨处理,则有雨样本的降水强度判识准确率达到88.17%. 相似文献
954.
干旱区河流及湖泊变化是环境演变的最重要标志之一。本文根据实际调查、历史记载和遥感图像解译,论证了塔里木河河道变迁及水量变化与罗布泊的演化关系。魏晋及其以前,塔里木河与孔雀河合流从北面入罗布泊,当时上游农业规模小,入湖水量多,罗布泊水域面积达到5350km2。此后,孔雀河入塔里木河,从南面经喀拉和顺入罗布泊,由于绿洲面积扩大,引水增加,到了清末罗布泊水域明显缩小,但还没有干涸。1921~1952年塔里木河再度与孔雀河汇流,又从北面入罗布泊,湖面扩大到1900km2,代表了这一时期的罗布泊水域,因此罗布泊不是20世纪30年代末40年代初干涸。1952年塔里木河与孔雀河分流,孔雀河单独入湖,水量减少,使湖面缩小,但直至1959年中国科学院新疆综合考察队对罗布泊进行考察时仍有广阔的水面,1961年仍未干涸。孔雀河灌区为扩大灌溉面积,于1958年和1962年,分别在普惠和阿克苏甫修了拦河大坝和水库引起下游断流。因此,罗布泊应在1962年以后逐渐干涸,直到1972年美国第一颗地球资源卫星照片上才得到反映。同时,还根据塔里木盆地绿洲发展、水资源利用及水系关系,分析了罗布泊干涸的原因及与塔里木河开发有着必然联系,主要是人类活动改变了地表径流的地域分配,上中游引水过多,造成下游断流和尾闾湖干涸。 相似文献
955.
DUANSujuan HONGFan LIXinhua 《地球空间信息科学学报》2004,7(4):303-307
To meet the authorization administration requirements in a distributed computer network environment, this paper extends the role-based access control model with multiple application dimensions and establishes a new access control model ED-RBAC(Extended Role Based Access Control Model) for the distributed environment. We propose an extendable hierarchical authorization assignment framework and design effective role-registering, role-applying and role-assigning protocol with symmetric and asymmetric cryptographic systems. The model can be used to simplify authorization administration in a distributed environment with multiple applications. 相似文献
956.
In this work, four methods are introduced to analyse the unevenly sampled data. The four methods are power spectral density, auto-correlation function, structure function and Jurkevich method. Some interesting mathematical links are derived amongst the four methods. These links show that the four methods have the same performance. For the Jurkevich method, the effect of the width of bins is apparent. If the width is half the time scale, the method has better performance. 相似文献
957.
Ying-Xi Zuo Yang Li Ji-Xian Sun Ji Yang Jing-Jing Li Ye Xu Deng-Yun He Qin-Hong Fan Sheng-Hong Fan 《Chinese Astronomy and Astrophysics》2011,35(4):439-446
Based on digital photogrammetric measurements, the antenna panels of the Delingha 13.7m radio telescope are adjusted to make the main dish have an optimal paraboloidal surface at the elevation of 52°, thus the overall antenna efficiency is optimized for different observing elevations. Observations indicate that the aperture efficiency of the telescope has been improved approximately twice in comparison with the antenna panels adjusted on the basis of theodolite measurements. According to the results of the measurements at different elevations, the models of antenna gravity deformation are built, including the displacement and tilt angle of the subreflector, as well as the focal length and surface error of the main reflector, as functions of elevation angle. In the process of modeling the gravity deformation of the main dish, instead of the direct calculation method, the least square fitting on the measured surface errors at different elevation angles is adopted, in order to reduce the effect of measurement errors on the accuracy of the model. 相似文献
958.
959.
Improving the estimate of wind energy input into the Ekman layer within the Antarctic Circumpolar Current 总被引:2,自引:2,他引:0
ZHANG Yuming WU Kejian ZHANG Xiaoshuang BI Fan SONG Zhaoyang LIU Shouhua 《海洋学报(英文版)》2013,32(3):19-27
Based on the data and method offered by Liu et al. (2009), the direct wind and Stokes drift-induced energy inputs into the Ekman layer within the Antarctic Circumpolar Current (ACC) area are reestimated since the results of the former have been proved to be underestimated. And the result shows that the total rate of energy input into the Ekman-Stokes layer within the ACC area is 852.41 GW, including 649.75 GW of direct wind energy input (76%) and 202.66 GW of Stoke drift-induced energy input (24%). Total increased energy input, due to wave-induced Coriolis-Stokes forcing added to the classical Ekman model, is 52.05 GW, accounting for 6.5% of the wind energy input into the classical Ekman layer. The long-term variability of direct wind and Stokes drift-induced energy inputs into the Ekman layer within the ACC is also investigated, and the result shows that the Stokes drift hinders the decadal increasing trend of direct wind energy input. Meanwhile, there is a period of 4-5 a in the energy spectrums, as same as the Antarctic circumpolar wave. 相似文献
960.
The role of mindanao dome in the variability of the Pacific North equatorial current bifurcation 总被引:2,自引:0,他引:2
The Mindanao Dome (MD) features prominent oceanic variability and is located geographically close to the bifurcation latitude Y b of the Pacific North Equatorial Current. In this study, the role of the MD in the variability of Y b is examined with 20 years of satellite altimetric sea surface height (SSH) data and a 1.5-layer linear Rossby wave model. It is shown that the seasonal variations of surface Y b are related to not only the SSH fluctuations near the bifurcation point (bifurcation box; 125°–130°E, 12°–15°N) but also those outstanding in the MD region (MD box; 127°–132°E, 6°–9°N). The impact of the MD SSH changes is significant when the bifurcation point stays at southerly latitudes during February–September, which hinders (delays) the southward leap (northward retreat) of Y b in April–May (July–August) and thus leads to the asymmetry of the mean Y b seasonal cycle (with a positive skewness of γ = +0.64). Such asymmetry also shows year-to-year variations depending on yearly mean Y b value. A southerly yearly mean Y b involves larger contribution of the MD and thus causes larger asymmetry of Y b seasonal cycle. At interannual and longer timescales, the MD acts to amplify the fluctuations of the bifurcation. It is responsible for about 20 % of the total low-frequency Y b variances and plays an important role in the 0.12° year?1 southward trend of Y b in the past two decades. The impact of the MD on Y b changes is becoming increasingly significant at various timescales such as the bifurcation point migrating southward in recent years. 相似文献