首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 140 毫秒
1.
介绍一种天线口面温度定标的方法,当用这个方法对目标源进行温度定标时,由于定标源讯号和目标源讯号均由天线口面同路输入,因此波导和微波器件的传输损耗在定标的过程中被自动消除,因而这种温度定标方法能大大地提高观测资料的精度。目前天线口面温度定标方法除了在射电天和微波天线测量中应用外,还广泛应用于雷达和无线电技术测量及微波遥感控制等。  相似文献   

2.
本文主要介绍天体辐射天线温度的两种定标形式,即天线后端温度定标和天线口面温度定标.还介绍用于天线口面温度定标和天体辐射温度定标的微波黑体噪声源的辐射特性及其应用等.  相似文献   

3.
以新月时月亮的射电辐射为温度基准和准口面温度定标的方法,在22GHz频率上于1993年7月~3月测量了13.7m射电望远镜抛物面天线的增益。根据测量的增益值(67.10─±0.07db)定标了太阳射电流量,流量测量的系统差为±5.8%,偶然差为±2.7%,测量的宁静太阳亮温度(非源区)为10100±300K。除此之外,还推导和计算了不同源模型下的天线方向图改正因子Ks,并计算了太阳射电源的流量密度。  相似文献   

4.
以新月时月亮的射电辐射为温度基准和准口面温度定标的方法,在22GHz频率上于1993年7月 ̄8月测量了13.7m射电望远镜抛物面天线的增益,根据测量的增益值(67.10±0.07db)定标了太阳射电流量。流量测量的系统差为±5.8%,偶然差为±2.7%,测量的宁静太阳亮温度(非源区)为10100±300K。除此之外,还推导和计算了不同源模型下的天线方向图改正因子Ks,并计算了太阳射电源的流量密度。  相似文献   

5.
韩溥  吕静 《天文学报》1994,35(2):209-214
1992年1月,在紫金山天文台13.7米毫米波望远镜上进行了用射电全息术的相位恢复方法测量天线表面精度的尝试。利用望远镜的22GHz系统,用强水脉泽源ORION-KL作为信号源测量了天线的聚焦和偏焦方向图,采用Misell算法获得了天线口面上的相位分布,由此得到的天线表面相对于理想抛物面偏差的均方根值与1989年用经典的经纬仪带尺方法测量的结果基本相符。  相似文献   

6.
本文报导由全功率辐射计、作为初级噪声校准源的室温和低温微波黑体、作为次级噪声校准源的同轴固态噪声源、集录和处理数据的微机等设备以及从空间注入校准噪声的准光校准技术组成的测量天线电参数的射电天文方法。用此方法测量了一具口径20米的卫星通讯天线的天线噪声温度、天线口面效率、天线方向图半功率点宽度等参数。测量结果表明这套方法简易可行,精度较高并有推广价值。  相似文献   

7.
由天线成像原理可知,通过密云50 m天线、“嫦娥一号”卫星(CE-1)和“嫦娥二号”卫星(CE-2)所搭载微波探测仪获取的月球亮温度图是微波天线方向图与真实亮温度图的卷积,所以想清晰准确地还原亮温度图,就必须采取反卷积方法.在处理过程中引入最大熵方法,选择基于Bonavito提出的直接迭代法求解方式,并论证了其作为反卷积方法的可行性,通过一系列的模拟仿真验证其反卷积的有效性.仿真结果理想,对后期处理真实数据(密云50 m天线观测数据,微波探测仪观测数据)打下坚实的基础.  相似文献   

8.
厘米波段背景噪声电平的测量方法及数据分析   总被引:2,自引:0,他引:2  
论述了厘米波段天线背景噪声电平测量的重要作用、基本条件和要求。介绍了其测量系统灵敏度的估值方法,及在工程上用定标的技术参数计算灵敏度的公式。测量结果表明理论计算和测量数据处理结果符合得很好,证明该测量系统的灵敏度估算、工程计算方法及实施的测量方法是科学的、严密的,测量的数据是真实的、准确的。同时给出系统测量原理方框图,定标的技术参数和技术路线等,并对测量结果进行了分析和讨论。  相似文献   

9.
中国频谱日像仪(Chinese Spectral Radioheliograph,CSRH)一期工程包括40面天线(400 MHz ~2 GHz)组成的天线阵,二期工程包括60面天线(2~15 GHz).天线统一控制包括天线指向调整、目标源跟踪、射电定标等.无论何种情况,所有的天线均需统一协调工作.对CSRH天线阵列整体控制进行了研究,提出了一种基于以太网的CSRH天线阵控制方案,并对可能遇到的关键问题进行分析.  相似文献   

10.
本叙述了上海天台25米射电望远镜天线电性能参数,即天线效率、天线噪声温度(天线指向偏离观测源时的天线等效噪声温度)及天线主瓣半功率宽度等的测量原理、方法和结果。  相似文献   

11.
本文介绍了用四种定标基准ΔTc=(T0-TL),(TH-T0),(T0-TANz)和(T0-THNz),并用射电源作为校准测量微波天线增益的基本原理和方法。并对四种不同类型的天线增益进行了测量,测量结果表明,以ΔTc=(T0-THNz)和总功率辐射计所组成的测量系统可实施增益的高精度测量。测量设备可以和接收系统兼容,不需专用测量设备,因此该技术可在工程中广泛使用。  相似文献   

12.
就上海佘山25 m抛物面天线上进行的相位相关法微波全息测量及其测量结果做了一定阐述。文章首先简要提到了微波全息测量技术在国内外的发展情况以及理论依据,其次介绍了我们所建立的测量系统的组成,重点讨论了基于窄带信号测量工作的有效性和准确性,采用自校准的数据处理手段,对测量误差做了估计和实际测试。当前我们已经取得了0.14 mm的测量精度(极限误差为0.2 mm),并分析了影响测量精度的各项因素。  相似文献   

13.
Defining the solar brightness temperature accurately at millimeter wavelengths has always been challenging. One of the main reasons has been the lack of a proper calibration source. New Moon was used earlier as a calibration source. We carried out a new extensive set of observations at 8 mm using the New Moon for calibration. The solar and Moon observations were made using the 14-meter radiotelescope operated by the Aalto University Metsähovi Radio Observatory in Finland. In this article, we present our method for defining the brightness temperature of the quiet-Sun level (QSL). Based on these observations, we found \(8100~\mbox{K} \pm 300~\mbox{K}\) to be the mean value for the QSL temperature. This value is between the values that were reported in earlier studies.  相似文献   

14.
J. Priese 《Solar physics》1969,9(1):235-240
In the frequency range from 1 to 2 GHz discrepancies exist between the values of the solar flux density observed at several stations. In order to clarify the situation a new absolute calibration has been carried out by the HHI at 1470 MHz. The equipment used for this purpose consists of an electromagnetic horn with calculated gain and of a receiver, the temperature scale of which has been calibrated by comparison with the noise of a heated absorber. The noise temperatures of the absorber have been identified with the mean thermodynamic temperatures of the absorbing material. The calibration procedure of the receiver and the observation method of the sun's radiation are described. An error analysis is given in detail, including impedance mismatches of the microwave components as well as impedance variations of the heated absorber. A maximum uncertainty of about ± 1.7% is calculated.  相似文献   

15.
The main aim of this paper is to estimate, from multispectral observations, the plasma parameters in a microwave burst source which was also the site of spike emission. This information is essential for the determination of the spike emission process. By analyzing one-dimensional source distributions observed with the SSRT at 5.7 GHz and correlating them with Yohkoh X-ray and Nobeyama 17 GHz images, we have concluded that the microwave emitting region was larger than the soft X-ray loop-top source, and that the origin of the burst could be explained by gyrosynchrotron emission of non-thermal electrons in a magnetic field of approximately 100 G. It has been shown that the source of 5.7 GHz spikes observed during the burst was located close to an SXR-emitting loop with high density and temperature and a relatively low magnetic field. Thus, plasma emission is the most favourable radiation mechanism for the generation of the sub-arc-second microwave pulses.  相似文献   

16.
接收机是射电天文中用于探测微弱射电信号的重要接收设备.接收机的强度校准就是将接收机对射电源的响应转换为天文意义上的流量密度.常规方法就是使用经典的冷热负载法,将接收机自身的强度响应转换为一个等效的温度值,之后再据此对射电源做进一步标定.通过搭建基于斩波轮技术的K波段接收机强度校准平台,使用斩波轮法测试K波段常温接收机的噪声温度,并与传统冷热负载法的测试结果进行比对.结果显示,在晴好天气条件下,斩波轮法在30°、90°仰角下噪声温度的最大测试误差为7.5%和8.4%,可以很好地应用于实际噪声温度测试中;但在5°仰角测试中,由于过低仰角引入了地面噪声,使得斩波轮法的测试误差上升至20%–30%之间而无法使用.希望在此基础上进一步开展K波段天空亮温度的理论计算与实测,从而完善斩波轮技术的应用,使之可以满足在不同气象条件下的噪声校准测试需求.  相似文献   

17.
A passive and multi-channel microwave sounder onboard the Chang’e-2orbiter has successfully acquired microwave observations of the lunar surface and subsurface structure. Compared with the Chang’e-1 orbiter, the Chang’e-2 orbiter obtained more accurate and comprehensive microwave brightness temperature data,which are helpful for further research. Since there is a close relationship between microwave brightness temperature data and some related properties of the lunar regolith,such as the thickness, temperature and dielectric constant, precise and high resolution brightness temperature data are necessary for such research. However, through the detection mechanism of the microwave sounder, the brightness temperature data acquired from the microwave sounder are weighted by the antenna radiation pattern, so the data are the convolution of the antenna radiation pattern with the lunar brightness temperature. In order to obtain the real lunar brightness temperature, a deconvolution method is needed. The aim of this paper is to solve the problem associated with performing deconvolution of the lunar brightness temperature. In this study, we introduce the maximum entropy method(MEM) to process the brightness temperature data and achieve excellent results. The paper mainly includes the following aspects: first, we introduce the principle of the MEM; second, through a series of simulations, the MEM has been verified as an efficient deconvolution method; and third, the MEM is used to process the Chang’e-2 microwave data and the results are significant.  相似文献   

18.
Wenzhe Fa 《Icarus》2010,207(2):605-615
In China’s first lunar exploration project, Chang-E 1 (CE-1), a multi-channel microwave radiometer was aboard the satellite, with the purpose of measuring microwave brightness temperature (Tb) from lunar surface and surveying the global distribution of lunar regolith layer thickness. In this paper, the primary 621 tracks of swath data measured by CE-1 microwave radiometer from November 2007 to February 2008 are collected and analyzed. Using the nearest neighbor interpolation to collect the Tb data under the same Sun illumination, global distributions of microwave brightness temperature from lunar surface at lunar daytime and nighttime are constructed. Based on the three-layer media modeling (the top dust-soil, regolith and underlying rock media) for microwave thermal emission of lunar surface, the CE-1 measured Tb and its dependence upon latitude, frequency and FeO + TiO2 content, etc. are discussed. The CE-1 Tb data at Apollo landing sites are especially chosen for validation and calibration on the basis of available ground measurements. Using the empirical dependence of physical temperature upon the latitude verified by the CE-1 multi-channel Tb data at Apollo landing sites, the global distribution of regolith layer thickness is further inverted from the CE-1 brightness temperature data at 3 GHz channel. Those inversions at Apollo landing sites and the characteristics of regolith layer thickness for lunar maria are well compared with the Apollo in situ measurements and the regolith thickness derived from the Earth-based radar data. Finally, the statistical distribution of regolith thickness is analyzed and discussed.  相似文献   

19.
E. Fürst 《Solar physics》1972,25(1):178-187
The heating of the solar plasma of those layers is considered where the microwave bursts are emitted. In a first step, we restrict ourselves to phenomena correlated with the so-called type II m bursts. Bursts of this kind are excited by shock-waves initiated near the optical flare region. These shock-waves spread out into the higher corona, and if the shock strength is sufficiently high, the microwave region is heated to 107 K. But this temperature is too low to explain the burst radiation. In this paper, it is shown that at plasma temperatures about 107 K a fairly high number of electrons is accelerated by Alfvén waves to equivalent kinetic temperatures of about 108 K. We assume that the Alfvén waves are generated near the sunspots, and, therefore, the accelerated electrons run along the magnetic-field lines into the microwave source lying between the two spots of an assumed dipole field. Within this source, the considered electrons thermalize and, after a short time, the source reaches temperatures of 5 × 107 K to 108 K.A plasma of this temperature with an electron density about 5 × 109 cm–3 and a magnetic induction of 300 G is optically thick even at frequencies about 10 GHz, because the gyromagnetic absorption is very high.  相似文献   

20.
In this paper, a new method of estimating the spatial directivity (in the form of center-to-limb variation) of microwave burst emission is proposed and derived. Estimations of radioemission directivity values vs observation frequency are obtained. Results are compared to the radio source model using an inhomogeneous magnetic field, source size and particle density, and show a high degree of agreement. Values of model parameters from earlier estimations are confirmed.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号