整周模糊度去相关的两种实现方法

整周模糊度搜索一直是GPS快速精确定位的关键问题。短时间的观测会导致观测方程和整周模糊度方差、协方差矩阵的高相关性，因而急剧增大整周模糊度的搜索空间，对整周模糊度未知数方差、协方差矩阵进行去相关性处理，可以有效地压缩搜索空间。本文对整周模糊度去相关的迭代法和联合变换法从原理上进行了阐述，并结合实际算倒进行了分析和比较。     

整周模糊度整数变换前后LAMBDA方法的执行结果比较

首先介绍了求取模糊度整数解的整数最小二乘方法的基本原理和LAMBDA方法，然后讨论了降相关的可容许整数变换对于LAMBDA方法求取双差模糊度整数解的影响。通过一个短基线的实例计算发现：对原始的双差模糊度进行降相关的可容许整数变换，不仅可提高模糊度整数解的准确性，而且还能提高模糊度的求取速度。     

单因素方差分析在煤层判分中的应用

针 对 多 煤 层矿 井 中 常 规地 质 方 法 对煤 层 判 分 的困 难 ,提 出 了 单 因 素方 差 分 析 的地 质 数 学 方法 。该 方 法对 煤层物 理 化 学 参数 进 行 量 化考 核 ,从而 将 煤 层 区分 出 来 ,既 考 虑 了 抽 样 观 测 中 的 随 机 误 差 ,又 考 虑 了 归 属 不 同 煤 层 的系统 误 差 ,为 煤 层 判 分提 供 了 一 种新 方 法 、新 思 路 。     

Compositional Distribution and Growth Mode of Garnet Porphyroblasts during Deformation and Metamorphism

Although porphyroblast microstructures play an important role in structural and metamorphic studies, there are still controversies in the interpretation. The focus is how porphyroblasts grow during deformation and metamorphism. In this paper, we introduce a new approach, the Synchrotron Radiation X-Ray Fluorescence, to a hemi-quantitative interpretation of the growth mode of porphyroblasts. The analysis was done at the Beijing Synchrotron Radiation Facility. The specimens were sampled from metapelite of the Baoyintu Group, northern Urad Middle Banner, Inner Mongolia. The new method is successful for determining the microscopic distribution of trace elements in porphybroblasts. The results support the theory of deformation partition, which has been brought forth by Bell and his colleagues, and demonstrate the existence of porphyroblast growth phases and the growth mode of porphyroblasts by hemi-quantitative mineral chemical analysis. The porphyroblast grows stage by stage in the manner of the distribution     

Partitioning of F between aqueous fluids and albite granite melt and its petrogenetic and metallogenetic significance

The fluid/melt partitioning experiments on fluorine were carried out in the system albite-H₂O-HF atP = 100 MPa, 770°C ≤T≤800°C: and wt = 2% −6% conditions. The concentrations of fluorine in quenched glasses (melt) were determined by electron microprobe and those of fluorine in the coexisting aqueous fluid were calculated by the method of mass balance. The result shows that the fluorine was concentrated in granitic melt relative to the coexisting fluid. The partition coefficient D_F(wt _F ^F1 /wt _F ^Mt ) ranges from 0.35 to 0.89. It increases with increasing fluorine content in the system. This means that there is not just one single value of partition coefficient for fluorine in the granitic melt-fluid system. The partitioning behavior of fluorine in this system depends critically on fluorine and proton (H⁺) concentrations. Our data suggest that F-rich granitic melts exist in nature and that fluorine may not be an important complexing agent of metal elements in F-bearing fluids. The project was financially supported by both the National Natural Science Foundation of China (No. 49603048) and the State Key Laboratory of Mineral Deposit Research, Nanjing University.     

钠长花岗岩—H2O—HF体系中流体／熔体间氟的分配实验研究

在ｐ＝１００Ｍｐａ,在７７０℃≤ｔ≤８００℃和ＷＦ＝２％－６％条件下进行了钠长花岗岩－Ｈ２Ｏ－ＨＦ体系液相线附近线体／熔体间氟的分配实验。对淬火玻璃的主要元素和氟含量进行了电子探针测定。用质量平衡法计算了流体中的氟含量,所获得的氟的流体／熔体分配系数ＤＦ均不盱１．０随体系氟含量的增加ＤＦ有所增大,表明在花岗岩岩浆一热液体系,氟优先进入熔体相,含氟花岗岗岩结晶晚期流体释放阶段残余熔体仍保保持富氟特征     

城市景观的三维抽象、描述与表达方法

提出了三维地理要素体系、三维空间描述粒度、建筑物立体剖分、城市景观三维模型库等概念与实现方法 ,实例证明了该方法的可行性     

一个新的GNSS模糊度估计类

介绍了一类新的GNSS模糊度估计。因为该类遵循移去一恢复原理，称之为整数等变估计类。本文将说明整数等变估计类较整数估计类和线性无偏估计类的范围要大，同时给出一个相当有用的整数等变估计类的表达式。这个表达式揭示了整数等变估计类的结构，并显示该表达式如何在浮点解的基础上实现整数等变估计。最后还提出最优整数估计。     

一种新颖的小波系数分类算法在图像无损编码中的应用

提出了一种新的小波系数分类算法，基于该分类算法，提出了一种更为合理的无损编码算法。实验结果显示，此方法优于其他基于小波的无损编码算法。     

Mechanistic roles of soil humus and minerals in the sorption of nonionic organic compounds from aqueous and organic solutions

Mechanistic roles of soil humus and soil minerals and their contributions to soil sorption of nonionic organic compounds from aqueous and organic solutions are illustrated. Parathion and lindane are used as model solutes on two soils that differ greatly in their humic and mineral contents. In aqueous systems, observed sorptive characteristics suggest that solute partitioning into the soil-humic phase is the primary mechanism of soil uptake. By contrast, data obtained from organic solutions on dehydrated soil partitioning into humic phase and adsorption by soil minerals is influenced by the soil-moisture content and by the solvent medium from which the solute is sorbed.