STUDIES ON WATER STAGE FLUCTUATION OF YAMZHO LAKE IN XIZANG

ＳＴＵＤＩＥＳＯＮＷＡＴＥＲＳＴＡＧＥＦＬＵＣＴＵＡＴＩＯＮＯＦＹＡＭＺＨＯＬＡＫＥＩＮＸＩＺＡＮＧＬｉｕＴｉａｎｃｈｏｕ（刘天仇）（ＴｉｂｅｔａｎＢｕｒｅａｕｏｆＷａｔｅｒＲｅｓｏｕｒｃｅａｎｄＨｙｄｒｏｌｏｇｉｃａｌＳｕｒｖｅｙ，Ｌｈａｓａ３５０...     

基于富钴结壳微地形采集头载荷波动性仿真研究

根据富钴结壳微地形的数字高程模型进行分类,得到某个特定高程差下9种地形模型。针对基于富钴结壳微地形的采集头切削过程,编制仿真程序进行模拟。仿真结果表明相同高程差地形模型(SS,MS,LS)、(SM,MM,LM)、(SL,ML,LL)的波动系数平均值对应为(0.35583,0.33142,0.32795)、(0.39355,0.41104,0.39326)、(0.48822,0.46608,0.50516),数据表明地形的高低对载荷波动性的影响不明显;不同类型地形模型(SS,SM,SL)、(MS,MM,ML)、(LS,LM,LL)的平均值对应为(0.35583,0.39355,0.48822)、(0.33142,0.411 04,0.466 08)(0.32795,0.39326,0.50516),数据表明地形起伏越大,对应的载荷波动系数也越大,采集头切削过程越不平稳。     

云南中甸纳帕海湖泊记录指示的57ka环境演化

根据沉积环境，总有机碳，氢指数，有机碳同位素，磁化率和粒度等替代性指标以及和陆地，深海气候记录的对比，重建了纳帕海57kaBP以来的湖面变化和主要气候演化阶段，57-32kaBP主要为低湖面和频繁的湖面波动，与气候的暖偏干/凉偏湿交替有关。32-15kaBP湖面大幅度上升，出现相对高湖面，气温下降，有效湿度增加，全新世湖盆的萎缩与持续的暖偏干气候有关，这种冷湿-暖干气候与滇西北特殊的地形地貌造成大气环流的独特性有关。     

潮汐作用下渤海温跃层波动与起伏的数值研究

研究了潮汐(四大分潮 M₂,S₂,K₁,O₁同时输入)作用下渤海温跃层起伏与波动的三维数值模型(将海洋分为3层,即上混和层、跃层和下混和层),揭示了整个海区温跃层上界面处跃层起伏(在文中指每个时刻跃层波高的周期平均值)的地理分布及叠加在起伏之上的潮周期波动的时空变化,模拟出跃层波动与实测基本一致.结果发现大振幅的跃层波动均发生在海峡及近海地形突变之处.一般界面波动的波高大于甚至远远大于同一位置的表层潮波.从位相以及周期来看,潮波和跃层上下界面波动相互之间,有些海域一致,有些地方则相差甚远.跃层上界深度及厚度的梯度,对跃层起伏分布有一定的影响.跃层起伏还可能与海岸海底摩擦有关.     

大亚湾冬季海流波动的分析

本文以实测资料为依据,利用时间序列功率谱的方法,分析大亚湾湾口冬季的海流波动特点,得出了本海域海流波动是以半日分潮潮流为主的半日分潮、全日分潮和浅海分潮潮流共存的波动形式,其振幅表层大于底层等结论。文中还指出了半日分潮、全日分潮和浅海分潮潮流波动振幅变化的特征。     

邵阳地震前后安乡井水位异常变化

通过对邵阳两次地震活动前后安乡井水位异常变化的总结,分析了其前兆反应的特征,认为该井在邵阳地震发生前是有短临前兆显示的．该井可能是区域应力场活动的一个＂敏感点＂．     

Application of Random Process in Soil Profile Modeling

When using the random process in soil profile modeling, the stationary and ergodicity of thesoil properties in the profile must be tested. This paper describes a procedure for stationary and ergodicity testing. Numerical examples were given for demonstration. A log-cosine function is suggested to simulate the correlation function, which has been proved to be good for soil profile modeling.     

Response of Coastal Groundwater Table to Offshore Storms

Large groundwater table fluctuations were observed in a coastal aquifer during an offshore storm. The storm induced significant changes of the mean shoreline elevation, characterized by a pulse-like oscillation. This pulse propagated in the aquifer, resulting in the water table fluctuations. A general analytical solution is derived to quantify this new mechanism of water table fluctuation. The solution is applied to field observations and is found to be able to predict reasonably well the observed storm-induced water table fluctuations. Based on the analytical solution, the damping characteristics and phase shift of the oscillation as it propagates inland are examined.     

Spatial correlation for transformation uncertainty and its applications

This paper shows that the transformation uncertainty varies in space and can be decomposed into (a) a slowly fluctuating component contributed by the systematic bias for a local site and (b) a rapidly fluctuating component partly contributed by the measurement error. Based on a piezocone database, the slowly fluctuating component is found to have a vertical scale of fluctuation (SOF) of 17–60 m, larger than the vertical SOFs for most soil properties and characteristic dimensions for many geotechnical structures. This paper provides an empirical basis to justify the assumption that the transformation uncertainty is fully correlated in space.