冀中坳陷深县凹陷主伸展期的构造调节带及其对沉积环境的控制作用

深县凹陷沙河街组发育的构造调节带控制着沉积体系的迁移路径和平面展布。根据断层的组合特点与断距变化,可将构造调节带分同向、对向、背向及单线4大类。同向和单线调节带主要发育在北部何庄-兵曹-崔家庄一带,规模小,数量多; 对向调节带发育在榆科地区和赵家庄地区,规模较大,分布稀疏。背向调节带极不发育。伸展作用的不均一性以及地层力学性质差异是形成调节带的主要因素。单线调节带控制小规模的沉积体穿过断层进入汇水盆地,如衡水断层下降盘中的水下扇; 同向调节带控制何庄-西魏村、田家庄、东阳乡等辫状河三角洲的入湖路径和展布特征; 对向调节带控制深湖的形成,如赵家庄一带的深湖; 而背向调节带造成的正地形起到了阻隔物源作用。     

Urban Residential Land Value Analysis： Case Danyang, China

The research attempts to find out how the location of the CBD(central business district), the dis- tance to the main roads, the distribution of the public facilities, and the urban land-use pattern influence the urban residential land value variations. The study begins by identifying the influences into two categories: general circumstance and micro/neighboring circumstances. Benchmark price and market land value are tested to be the results influenced by general circumstance and both the influential range and the influential force of individual land-use are investigated and compared. At last explicit case comparisons are also taken for testing the result. The finding of the research is not only useful for understanding the spatial patterns of land values, but also beneficial for the policy-makers concerning land administration and urban planning.     

Continental- Margin Structure of Northeast China and Its Adjacent Areas

The continental margin of Northeast China and its adjacent areas is composed of two tectonic belts. The inner belt is a collage made up of fragments resulting from breakup of an old land with the north part related to the evolution of the Palaeo-Asian Ocean and the south part to the evolution of the Palaeo - Pacific Ocean. The outer belt is a Mesozoic terrane, which is a melange made up of fragments of the Late Palaeozoic to Early Mesozoic oceanic crust and the Late M esozoic trench accumulations.There existed another ocean-the Palaeo - Pacific Ocean during the period from the closing of the Palaeo-Asian Ocean to the opening of the modern Pacific Ocean or from the Devonian to Jurassic, and the ocean-floor spreading of the Palaeo - Pacific Ocean led to the formation of the above-mentioned tectonic belts. The development of the strike-slip fault system after the Late Jurassic and the formation of an epicontinental volcano -plutonic rock belt in the Late Cretaceous to Early Tertiary are attributed to the i     

Photosynthetic characteristics of spring ephemerals in the desert ecosystem of Dzungaria Basin,northwest China

Spring ephemerals have the highest photosynthetic rates in higher plants. Gas exchanges and related environmental factors of four typical spring ephemerals, Eremopyrum orientale, Malcolmia scorpioides, Tetracme quadricormis and Arnebia decumbens were measured in their natural environments in the Gurbantunggut Desert of the Dzungaria Basin, northwestern China. Diurnal variations in net photosynthetic rate (P _N), transpiration rate (E), stomatal conductance (gs), and water use efficiency (WUE) were analyzed at individual leaf level for these species. P _N of E. orientale and M. scorpioides showed a bimodal diurnal pattern, whereas that of T. quadricormis and A. decumbens showed a unimodal pattern, with the maximum value occurred at noon (around 12:00). E of all four species showed a unimodal pattern. Higher WUE in the morning was related to higher P _N and lower E. The maximum value of gs appeared in early morning, and then decreased gradually during the daytime. The highest photosynthetically active radiation (PAR) occurred at 14:00, but there was a 2 h lag between the highest temperatures of air and leaf and the highest PAR. The maximum net photosynthetic rate (P _Nmax) of the four spring ephemerals were 18.44, 32.03, 33.17, and 20.04 μmolCO₂ m⁻² s⁻¹, respectively. The present study revealed that the midday depression of photosynthesis of E. orientale and M. scorpioides was mainly due to non-stomatal limitation, whereas that of T. quadricormis and A. decumbens was mainly due to stomatal limitation during 14:00–16:00 followed by non-stomatal limitation after 16:00. Our results illustrated that the change of E was consistent with the diurnal fluctuation of air temperature, but the diurnal change of P _N was affected by the whole microclimate, i.e. temperature, relative humidity (RH), PAR, etc.     

三轴压缩条件下三峡坝基岩石破裂的分形特征

根据分形理论,系统地研究了在三轴压缩条件下三峡坝基岩石破裂系和破损物的分形结构。结果表明,在三轴压缩条件下,岩石脆性破裂的破裂系和岩石破损物的粒度分布均有很好的统计自相似性。在不同的围压和应变率下,岩石脆性破裂的分维值各不相同,体现了岩石脆性断裂机制的差异性。分维可作为描述岩石脆性断裂的定量参数     

Flare morphologies and coronal field configurations

Chromospheric flares are the footpoints of closed coronal field lines. In this paper we present different flare morphologies from observations and examine the implied coronal field configurations above the flaring region. Flares are grouped according to the number of ribbons, from unresolved compact point-like flare to four-ribbon flares. Quiet region flares having characteristics all their own are also presented here.We find that compact, unresolved point-like flares have two distinct footpoints when viewed in offband H. The footpoints of some of the compact flares also show increased separation as a function of time.Unlike large two-ribbon flares, the ribbons of many small and/or short-lived two-ribbon flares usually have no measurable separation of ribbons.Multiple-ribbon (three or more ribbon) flares consist of two or more pairs of two-ribbons, or two or more sets of field lines. Parity of the ribbons in multiple-ribbon flares, or the lack of it, depends on the magnetic makeup of the locale of the ribbons.Flares in old quiet regions resulting from sudden filament eruptions show discrete small patches of emissions reflecting the spottiness of decayed and dispersed field of quiet region.     

Parametric uncertainty and sensitivity analysis of hydrodynamic processes for a large shallow freshwater lake

Abstract

A parametric uncertainty and sensitivity analysis of hydrodynamic processes was conducted for a large shallow freshwater lake, Lake Taihu, China. Ten commonly used parameters in five groups were considered including: air–water interface factor, water–sediment interface factor, surrounding terrain factor, turbulent diffusion parameters and turbulent intensity parameters. Latin hypercube sampling (LHS) was used for sampling the parametric combinations, which gave predictive uncertainty results directly without using surrogate models, and the impacts of different parametric distribution functions on the results were investigated. The results showed that the different parametric distribution functions (e.g. uniform, normal, lognormal and triangular) for sampling had very little impact on the uncertainty and sensitivity analysis of the lake hydrodynamic model. The air–water interface factor (wind drag coefficient) and surrounding terrain factor (wind shelter coefficient) had the greatest influence on the spatial distribution of lake hydrodynamic processes, especially in semi-closed bays and lake regions with complex topography, accounting for about 60–70% and 20%, respectively, of the uncertainty on the results. Vertically, velocity in the surface layer was also largely influenced by the two factors, followed by velocity in the bottom layer; the middle velocity had minimal impact. Likewise, the water–sediment interface factor (i.e. bottom roughness height) ranked third, contributing about 10% to the uncertainty of the hydrodynamic processes of the lake. In contrast, turbulent diffusion parameters and turbulent intensity parameters in the lake hydrodynamic model had little effect on the uncertainty of simulated results (less than 1% contribution). The findings were sufficiently significant to reduce the parameter uncertainties and calibration workload of the hydrodynamic model in large shallow lakes.

Editor Z. W. Kundzewicz; Associate editor S. Grimaldi     

高分辨率数值模式在风能资源评估中的应用初探

针对现有气象测站分布数量有限, 尤其是沿江沿海地带测站稀少的现状, 对数值模式在风能资源评估中的应用进行了尝试。首先利用TAPM数值模式对上海地区的风场作了数值模拟计算; 然后利用同步的气象站观测资料对风速模拟结果进行统计释用订正处理, 提高了模式计算结果的准确性和可靠性; 最后得到了分辨率为3 km的上海全年平均风速和风功率密度分布信息。这些结果为上海地区风能资源分析评估及风电场规划选址工作提供了科学依据, 同时也说明将统计释用的数值模拟结果应用到风能资源评估工作中是可行的。     

四川盆地的地震地质特征

四川盆地是我国具有代表性的中新生代沉积盆地,喜马拉雅运动使之发生褶皱变形。野外观察和深部探测资料表明,褶皱及与之相伴的断裂通常在3～5千米的深度上消失,为典型的浅层构造。上下层位构造形态的不协调现象是沿软弱层位发生滑脱作用的结果。盆地内的地震活动性比四川西部活动构造区明显减弱,仅有的几个中强地震震例表明,它们具有震源浅、震级低,烈度高且震中位置与背斜构造关系密切的特点。本文旨在通过盆地内盖层滑动及其与盖层沼皱、断裂的成因机制的讨论,探索导致盆地内地震活动特殊现象的原因。并预测盆地内未来地震的可能强度。     

供电线路勘测内外业一体化系统的开发和应用

供电线路勘测是属于普通工程测量,结合计算机技术制图技术和电子测绘仪器的特点,作者开发了一套适合市县一级的供电线路勘测系统,以AutoCad为绘图平台,VBA5.0为开发语言,符合测绘习惯,提高了工作效率。