中国亚热带北界及其过渡带

本文根据亚热带热量指标构造了热量综合指数表达式,确定亚热带北界的具体位置、宽度和特征,分析过渡带内气候变量在时间上和空间上的内在联系。     

地理信息工程的多指标综合评价研究

介绍了多指标综合评价方法的概念、特性与分类，对地理信息工程中的评价对象和评价步骤进行了归纳，并阐述了实施评价时应着重考虑的关键问题。     

一种基于Bayesian准则和MRF模型的SAR图像滤波方法

提出了一种新的斑点噪声的滤波方法，该方法基于小波分解的框架，采用小波域隐MRF模型，计算图像中表征像素纹理特征的隐状态参数的后验概率，以此后验概率作为权重因子对传统GammaMAP滤波算法进行改进。该算法被用于模拟SAR图像和真实ERS-1图像的Speckle抑制。试验结果表明，与传统Gam—maMAP算法相比，本文提出的方法能更好地抑制Speckle，并保持图像细节。     

Subcrustal Low Velocity Layers in Central India and their Implications

A 2-D subcrustal velocity model for the central Indian continental lithosphere has been derived by travel time and relative amplitude modeling of a digitally normalized analog seismic record section of the Hirapur-Mandla DSS profile, using a ray-tracing technique. Some prominent wave groups with apparent velocities slightly higher than the Moho reflection phase (P_MP) are identified on the normalized record sections assembled with a reduction velocity of 6 km s⁻¹. We interpret these phases as the wide-angle reflections from subcrustal lithospheric boundaries. Comparison of synthetic seismograms with the observed record section shows that the observed phases cannot be explained either by multiples or by the P-to-S converted phase (P_MS) from the Moho. Subcrustal velocity models either with a velocity increase or with a single low velocity layer (LVL) also do not provide a satisfactory fit. We infer that a subcrustal velocity model with two alternate LVLs (velocity 7.2 km s⁻¹), separated by a 6-km thick high velocity layer (velocity 8.1 km s⁻¹), can satisfy both the observed travel times and amplitudes. The prominent reflection phases are modeled at depths of 49, 51, 57 and 60 km. It is inferred that the subcrustal lithosphere in the central Indian region has a lamellar structure with varying structural and mechanical properties. The alternating LVLs, occurring at relatively shallow depths below Moho, may be associated with the zones of weakness and lower viscosity suggesting continued mobility, with a possible thermal source in the upper mantle. This explains the source of observed high heat flow values in the central Indian region.     

模糊综合评判在旅游客源市场中的应用--以西藏为例

西藏旅游资源丰富,但客源不足。在公众调查和数据分析的基础上,引入模糊综合评判方法,分析西藏旅游客源不足的原因,并提出相关措施:加强交通建设;完善旅游产品;多种形式促销;形成良性循环。以便为西藏旅游业的发展提供参考。     

Map Drift算法在实时成像处理器中的应用

随着计算机技术的发展，实时成像处理器技术的成熟，不但处理数据量越来越大，而且对成像质量要求也越来越高，实时成像处理中需要有自动聚焦算法。但是由于实时成像处理器的特殊结构和实时性要求，需要算法的计算量不能太大、不能太不确定。因此并不是所有的算法都适合用于实时处理。 主要介绍Map Drift算法的原理和实现步骤以及在实时成像处理器中的应用。文中对适合于实时成像处理器中应用的公式进行了推导，得到频域二次相位误差系数和相关峰位置的线性关系，并利用该关系在频域进行相位补偿，有效缩减迭代次数。利用一种插值来计算相关峰位置的方法，消除了离散化计算相关峰位置所带来的量化误差的影响，并在迭代过程中改进二次相位误差系数和相关峰位置关系的系数，对减少迭代次数，提高估计精度有一定帮助。最后给出仿真结果，验证算法的正确性。     

子波整形提高合成地震记录质量

阐述合成地震记录的制作原理,利用测井数据计算出反射系数。根据地震波传播机制,通过三维地震数据统计得到子波,由此计算出原始合成记录。再根据过井剖面建立褶积模型,对子波进行整形,得到一个随时间变化的地震子波,最终得到与地震数据的波组特征相吻合的合成地震记录。为精细储层描述打下了坚实的基础。     

Synthetic Fluid Inclusions in the Systems NaCl-H2O and NaCl-CO2-H2O: Dissolution Temperatures of Halite

Abstract. This study examined the effect of CO₂ on NaCl solubility in hydrothermal fluid, with the synthetic fluid inclusion technique. Fluid inclusions of 30–40 wt% NaCl and 5 mol % CO₂ were synthesized, and their halite dissolution temperatures, T_m(halite), were measured. The solubilities of NaCl in CO₂-bearing aqueous fluid were obtained at 160–320C under vapor-saturated pressures. The T_m(halite) value in aqueous fluid with 5 mol % CO₂ obtained in this study agrees with that of Schmidt et al. (1995), showing that 5 mol % CO₂ reduces the solubility of NaCl by about 1 wt%.
Calculation of magnetite solubility suggests that 5–10 mol % CO2 decreases magnetite solubility by 4.5–8.9 % relative to the magnetite solubility in CO2-free solution. Therefore, an increase of CO2 content in ore-forming solutions may cause deposition of iron minerals and produce ore deposits.