世界时化地球力学时经验公式的改进

针对计算△TE(由世界时化算至地球力学时的改正值)的经验公式所存在的问题,利用1983年~1998年中国天文年历上登载的△TE数据,建立了新的计算△TE的经验公式;并用其后推算至1980年和前推算至2001年的计算结果,分析了该经验公式的推算精度;最后提出了确保推算精度的措施。     

Improved ENSO simulation in regional coupled GCM using regressive correction method

A regressive correction method is presented with the primary goal of improving ENSO simulation in regional coupled GCM. It focuses on the correction of ocean-atmosphere exchanged fluxes. On the basis of numerical experiments and analysis, the method can be described as follows: first, driving the ocean model with heat and momentum flux computed from a long-term observation data set; the pro-duced SST is then applied to force the AGCM as its boundary condition; after that the AGCM’s simula-tion and the corresponding observation can be correlated by a linear regressive formula. Thus the re-gressive correction coefficients for the simulation with spatial and temporal variation could be obtained by linear fitting. Finally the coefficients are applied to redressing the variables used for the calculation of the exchanged air-sea flux in the coupled model when it starts integration. This method together with the anomaly coupling method is tested in a regional coupled model, which is composed of a global grid-point atmospheric general circulation model and a high-resolution tropical Pacific Ocean model. The comparison of the results shows that it is superior to the anomaly coupling both in reducing the coupled model ‘climate drift’ and in improving the ENSO simulation in the tropical Pacific Ocean.     

大地主题解算方法综述

大地主题解算是大地测量中的重要问题,由于椭球的复杂性,随之产生的解算方法也是多种多样。本文分析了大地主题解算的一般方法及其公式的适用范围,指出了它们的特点和不足,讨论了现今常用解算方法存在的问题和进一步的研究方向。     

论工程岩体完整性的评价方法

目前国内外对工程岩体完整性的评价方法很多,均从某一侧面间接反映了岩体的完整程度,缺乏科学性.结合工程勘察实践及相关学科的研究,对岩体完整性评价,建立了KY、RID新公式,提高了工程岩体完整程度评价方法的科学性.     

滇西重力断层运动时间分布特征的初步研究

地表观测的重复重力数据综合反映了地表观测点的位置变化、地壳内部密度变化和地壳内部构造变形，通过反演这些数据得到的断层位错运动的时间变化综合反映了地壳内部形变和密度变化的耦合运动。为此，利用滇西1985年以来的重复重力观测数据，结合地质调查和地球物理推断结果确定断层运动模型作为约束，并考虑到观测数据和模型粗差，反演获得了滇西主要活动断裂运动的时间变化分布。结果表明，滇西1985－2001年断层运动的时间变化表现出断层往复运动特征，较好地反映了区内Ms≥6.0地震（如1996年丽江Ms7.0地震、1998年宁蒗Ms6.2地震和2000年姚安Ms6.5地震等）的孕育过程。指出强震孕育过程遵循地壳内部密度和地壳形变耦合运动模式（简称DD耦合运动模式），并给出了断层位错DD耦合运动模式的基本图像。     

A Local Least-Squares Modification of Stokes’ Formula

The combination of Stokes formula and an Earth Gravity Model (EGM) for geoid determination has become a standard procedure. However, the way of modifying Stokes formula vary from author to author, and numerous methods of modification exist. Most methods are deterministic, with the primary goal of reducing the truncation bias committed by limiting the area of Stokes integration around the computation point, but there are also some stochastic methods with the explicit goal to reduce the global mean square error of the geoid height estimator stemming from the truncation bias as well as the random errors of the EGM and the gravity data. The latter estimators are thus, at least from a theoretical point of view, optimal in a global mean sense, but in a local sense they may be far from optimality.Here we take advantage of the error variance-covariance matrices of the EGM and the terrestrial gravity data to derive the modification parameters of Stokes kernel in a local least-squares sense. The solution is given for the unbiased type of modification of Stokes formula of Sjöberg (1991).     

T-a曲线法求承压含水层参数

针对承压含水层抽水试验数据,本文提出一种新方法求含水层水文地质参数.并附上有关计算程序.     

用偏硼酸锂熔样ICP-AES法测定岩石中Si、Zr等12个元素

本方法采用偏硼酸锂分解样品，电感耦合等离子体发射光谱法测量，在同一份溶液中可以测定硅、钠、铝、钙、镁、铁、钛、锰、钡、锶、钒、锆等元素。通过对国家标准物质测定，其准确度、精密度能满足岩石样品中定量分析要求。