机载W波段毫米波辐射计扫描成像研究

通过机载试验 ,本文进行了W波段毫米波辐射计 (RADW92 )扫描成像研究 ,取得了黄河、渭河部分水域的微波辐射图像。试验结果表明 ,RADW92基本满足星载应用的要求。文中分析了影响图像质量的各种误差因素 ,并且提出了相应的解决方案。RADW92工作的中心频率为 92GHz ,带宽 2GHz ,积分时间 6 0ms ,系统灵敏度 0 6K ,线性度 0 999,天线为卡塞格伦 (Cassegrain)天线     

On the ore-forming conditions and ore-forming model of the superlarge multimetal deposit in Shizhuyuan

Eight favorable ore-forming conditions for the Shizhuyuan W-multimetal deposit are proposed. They are: (i) the geochemistry background special enriching the volatile and W and Sn ore-forming elements; (ii) the existence of melt-fluid system very rich in volatile and ore-forming elements; (iii) supply of sufficient ore-forming material and volatile multi-source; (iv) the infiltration and convection water source and driving force partly supplied by the Jurassic reservoir basin; (v) favorable tectonic conditions; (vi) ore-bearing greisen and vein superimposed in the pre-existing skarn rocks; (vii) favorable ore-transport and ore-concentration strata condition; (viii) there were a set of favorable ore-forming structures in Shizuyuan area; (ix) the orebody has good ore-reserve condition. Finally, ore-forming models are proposed. The paper is one of the achievements on the research related to the Climbing Project “The basic related to searching for the superlarge deposits supported by the State Science and Technology Commission. This research is also granted by the National Natural Science Foundation of China (Grant No. 49572134).     

The high-velocity molecular stream in W51B: a ring structure with compact H ii regions

We present ¹³ CO J  = 1 − 0 line observations of the H  ii region complex W51B located in the high-velocity (HV) stream. These observations reveal a filamentary and clumpy structure in the molecular gas. The mean local standard of rest (LSR) velocity ∼ + 65 km s⁻¹ of the molecular gas in this region is greater than the maximum velocities allowed by kinematic Galactic rotation curves. The size and mass of the molecular clouds are ∼ 48 × 17 pc² and ∼ 2.4 × 10⁵ M⊙ respectively. In a position–velocity diagram, molecular gas in the southern part comprises a redshifted ring structure with v _LSR=+ 60 to +73 km s⁻¹. The velocity gradient of this ring is ∼ 0.5 km s⁻¹ pc⁻¹, and the mass is ∼ 6.2 × 10⁴ M⊙. If we assume that the ring is expanding with a uniform velocity, the expansion velocity, radius and kinetic energy are ∼ 7 km s⁻¹, ∼ 13 pc and ∼ 3.0 × 10 ⁴⁹ erg respectively. The kinetic energy and mass spectrum of the ring could be explained by an expanding cylindrical cloud with a centrally condensed mass distribution. The locations of two compact H  ii regions, G49.0−0.3 and G48.9−0.3, coincide with the two molecular clumps in this ring. We discuss star formation, and the mechanism that produced the ring structure.     

A textbook case of bow shock entrainment in a YSO outflow

Near-infrared images in H₂ line emission and submillimetre maps in CO J  = 3–2 emission illustrate the remarkable association between a molecular bow shock and the redshifted molecular outflow lobe in W75N. The flow lobe fits perfectly into the wake of the bow, as one would expect if the lobe represented swept-up gas. Indeed, these observations strongly support the 'bow shock' entrainment scenario for molecular outflows driven by young stars.   The characteristics of the bow shock and CO outflow lobe are compared with those of numerical simulations of jet-driven flows. These models successfully reproduce the bulge and limb-brightening in the CO outflow, although the model H₂ bow exhibits more structure extending back along the flow axis. We also find that the size of the flow, the high mass fraction in the flow at low outflow velocities (low γ values) and the high CO/H₂ luminosity ratio indicate that the system is evolved. We also predict a correlation, in evolved systems, between outflow age and the CO/H₂ luminosity ratio.     

SN1996wHα线的初步分析

据观测到的ＳＮ１９９６的Ｈα谱线的初步计算结果表明,该超新星可能是由一颗晚Ｂ９型超新星爆发形成的,爆发时的气壳质量可达０．００３１Ｍ⊙,径向膨胀速度为１１７６０ｋｍ／ｓ。     

Meteorology and haze structure during AGASP-II,Part 2: Canadian Arctic flights, 13–16 April 1986

In April 1986, a well-instrumented NOAA WP-3D research aircraft conducted three flights in the Canadian Arctic tied to the Canadian Atmospheric Environment Service baseline station in Alert, Northwest Territories. Two of the flights were coordinated with the National Aeronautical Establishment of Canada Twin Otter and the University of Washington C-131 research aircraft. The haze observed in the Canadian Arctic was well-aged and mixed throughout the troposphere in concentrations well below those observed during the previous weeks in the Alaskan Arctic. Over the ice, beneath the surface temperature inversion, ozone was generally depleted to near zero. Over the coast at Alert, there is evidence that topography and downslope winds reduce the strength of the inversion, thus allowing lower tropospheric gases and aerosols to mix down to the surface. At the top of the troposphere, an aerosol-depleted region was observed. In the lower stratosphere, aerosol concentrations were elevated above those observed in the troposphere.     

钨的迁移形式成矿机理新探

通过对钨羰基络合物及钨合金氢化物的物理化学性质、钨矿床矿物流体包裹体的化学组成、钨矿物的化学成分、主要共生伴生矿物组合的研讨,结合钨成矿的地质背景和环境,认为钨羰基络合物及钨合金氢化物是钨的主要迁移形式。它们形成于地球深部高压、富氢、富CO的强还原环境,随着岩浆、热液、热气迁移至地壳浅部,由于压力、温度下降,氧逸度大增,H2、CO逃逸、氧化,钨羰基络合物、钨合金氢化物分解,氧化形成钨矿物,沉淀富集形成钨矿床。     

基于SLOPE／W的汾离高速公路靳家庄1^#滑坡研究

汾(阳)-离(石)高速公路是青岛至银川国道主干线在山西境内的重要路段。文章以汾离高速公路靳家庄1#滑坡为研究对象,从岩性条件、地质构造及地下水等方面详细分析了滑坡的成因。应用基于刚体极限平衡理论的SLOPE/W程序,对滑坡的稳定性进行分析与计算。结果表明:该滑坡在天然状态下,整体处于稳定状态;在工程状态下,受水动力条件的变化以及人为活动的影响,易发生复活。为设计人员提供了参考。     

Numerical model simulations of continental shelf flows off northern California

The three-dimensional circulation on the continental shelf off northern California in the wind events and shelf transport (WEST) experiment region during summer 2001 is studied using the primitive equation regional ocean modeling system (ROMS). The simulations are performed with realistic topography and initial stratification in a limited-area domain with a high-resolution grid. Forcing consists of measured wind-stress and heat flux values obtained from a WEST surface buoy. The general response shows a southward coastal upwelling jet of up to and a weakening or reversal of currents inshore of the jet when upwelling winds relax. Model results are compared to WEST moored velocity and temperature measurements at five locations, to CODAR surface current observations between Pt. Reyes and Bodega Bay, and to hydrographic measurements along shipboard survey lines. The model performs reasonably well, with the highest depth-averaged velocity correlation (0.81) at the inshore mooring (40 m water depth) and lowest correlation (0.68) at the mid-depth mooring (90 m depth). The model shows generally stronger velocities than those observed, especially at the inshore moorings, and a lack in complete reversal of southward velocities observed when upwelling winds relax. The comparison of surface velocities with CODAR measurements shows good agreement of the mean and the dominant mode of variability. The hydrography compares closely at the southern and northern edges of the survey region (correlation coefficients between 0.90 and 0.97), with weaker correlations at the three interior survey lines (correlation coefficients between 0.44 and 0.76). Mean model fields over the summer upwelling period show slight coastal jet separation off Pt. Arena and significant separation off Pt. Reyes. The cape regions also experience relatively strong bottom velocities and nonlinearity in the surface flow. Across-shelf velocity sections examined along the shelf reveal a double jet structure that appears just north of Bodega Bay and shows the offshore jet strengthening to the south. We examine the dynamics during an upwelling and subsequent relaxation event in May 2001 in which the WEST measurements show evidence of a strong flow response. The alongshelf variability in the upwelling and relaxation response introduced by Pt. Reyes is evident. Analysis of term balances from the depth-averaged momentum equations helps to clarify the event dynamics in different regions over the shelf. A clear pattern in the nonlinear advection term is due to the spatial acceleration of the southward jet around the capes of Pt. Arena and Pt. Reyes during upwelling. Results from a three-dimensional Lagrangian analysis of water parcel displacement show significant southward displacement in the coastal jet region, including a strong signal from the double jet. Alongshelf variability in parcel displacements and upwelling source waters due to the presence of Pt. Arena and Pt. Reyes is also apparent from the Lagrangian fields. A cyclonic eddy-like recirculation feature offshore of Pt. Arena prior to the upwelling event causes large patches of onshore-displaced parcels. Additionally, across-shelf variability in the response of water parcels along the D line includes decreased vertical displacement and increased alongshelf displacement in the offshore direction.     

中国碱蓬属植物修订

本文对《中国植物志》藜科(Chenopodiaceae)碱蓬属(Suaeda Forsk. ex Scop.)长期存在的分类错误进行了纠正。将其中的高碱蓬S. altissima (L.) Pall.合并入碱蓬S. glauca (Bunge) Bunge,纵翅碱蓬S. pterantha (Kar. et Kir.) Bunge合并入刺毛碱蓬S. acuminata (C.A. Mey.) Moq.,同时增加了垦利碱蓬(新种)S. kenliensis J. W. Xing sp. nov。由此将中国碱蓬属(Suaeda)植物从原来的20种,变更为19种。并重新修订了中国碱蓬属(Suaeda)植物的分种检索表,使中国碱蓬属(Suaeda)植物的系统分类更趋于完善,为《中国植物志》的修订和碱蓬属(Suaeda)植物分类及其深入研究与开发利用提供了依据。