Tidally averaged circulation in Puget Sound sub-basins: Comparison of historical data,analytical model,and numerical model

Through extensive field data collection and analysis efforts conducted since the 1950s, researchers have established an understanding of the characteristic features of circulation in Puget Sound. The pattern ranges from the classic fjordal behavior in some basins, with shallow brackish outflow and compensating inflow immediately below, to the typical two-layer flow observed in many partially mixed estuaries with saline inflow at depth. An attempt at reproducing this behavior by fitting an analytical formulation to past data is presented, followed by the application of a three-dimensional circulation and transport numerical model. The analytical treatment helped identify key physical processes and parameters, but quickly reconfirmed that response is complex and would require site-specific parameterization to include effects of sills and interconnected basins. The numerical model of Puget Sound, developed using unstructured-grid finite volume method, allowed resolution of the sub-basin geometric features, including presence of major islands, and site-specific strong advective vertical mixing created by bathymetry and multiple sills. The model was calibrated using available recent short-term oceanographic time series data sets from different parts of the Puget Sound basin. The results are compared against 1) recent velocity and salinity data collected in Puget Sound from 2006 and 2) a composite data set from previously analyzed historical records, mostly from the 1970s. The results highlight the ability of the model to reproduce velocity and salinity profile characteristics, their variations among Puget Sound sub-basins, and tidally averaged circulation. Sensitivity of residual circulation to variations in freshwater inflow and resulting salinity gradient in fjordal sub-basins of Puget Sound is examined.     

中国地质调查信息网格平台构建和地质图 数据服务的实现

对组成中国地质调查信息网格平台的结点计算池的构架、机制和组成结点计算池的资源聚合器、元服务、智能服务引擎的概念进行了阐述,提出了结点自治的方案;基于资源共享、虚拟化、Web服务等创建了基于元数据服务、栅格流服务、矢量地图服务、三维可视化服务等多模式的地质图数据服务。目前已初步构建了中国地质调查信息网格,连通10个结点 ,为地质图空间信息共享和应用提供一种全新的技术解决方案,取得了良好的实际运行效果。     

方格网布孔法注浆设计在底板改造中的应用

为了安全回采受底板承压水害威胁的采煤工作面,可采取注浆改造的防治水方法,而注浆改造设计是注浆改造的基础和前提。由于传统设计方法较为繁琐且效率较低,本次研究,首先对方格网布孔法的设计原理与基本思路进行了介绍,然后以新桥煤矿北二采区2207工作面为例,对根据工作面大小和底板水文地质情况设计方格网,输入基本参数,得出需要施工的钻孔参数,并根据物探资料及实际揭露的底板灰岩岩溶裂隙发育情况的变化,及时调整钻孔数量与位置进行了详细说明。应用效果表明,该方法具有设计简便,钻孔布置均匀,重点突出,清除了设计盲区,底板注浆改造效果好的特点,是一种操作简便、安全高效的注浆设计方法。     

基于CUBE算法的多波束测深数据自动处理研究

对CUBE算法自动处理多波束测深数据的模型建立、格网节点的多重估计和最优估值选取准则进行了详细介绍,深入分析了多重估计的实用性,并通过实测数据对该算法进行实现.利用了抗差Kalman滤波改进CUBE算法.通过模拟数据对改进的CUBE算法进行实验,验证了算法改进的必要性.     

球面格网系统特征分析及比较

球面格网系统是一种新型栅格数据模型。在全面检索和分析前人相关研究成果的基础上,将球面格网系统分成4种类型:基于经纬线划分的格网系统、基于正多面体划分的格网系统、基于Voronoi划分的格网系统和混合格网系统;并针对各种不同类型的格网,分析了同级格网单元的空间几何特征及不同级别格网之间的层次嵌套等特性。通过对比分析,给出不同格网系统的优缺点及其适用领域,认为不存在满足所有需求的通用的格网系统,相关应用只能针对具体情况,选用最适宜的格网系统。     

The impact of heterogeneity of land surface roughness length on estimation of turbulent flux in model

Based on preliminary theoretical analysis and numerical experiment, it is found that land surface heterogeneity plays an important role in the models turbulent flux calculation. In nearly neutral atmosphere conditions, variation coefficient of sub-scale roughness length, cell-average roughness, and reference height are main factors affecting the calculation of grid turbulent fluxes. The first factor has a determinant role on calculation deviation. The relative error generated by roughness heterogeneity could be more than 40% in some cases in certain areas (e.g., in vegetation-climate transition belt). Selecting a specific reference height may improve the calculation of turbulent flux. In stable or unstable atmosphere conditions, with sensible heat flux as an example, analysis shows that the discrepancy is correlated to the sub-grid distributions of mean wind velocity, potential temperature gradient between land surface and reference levels, and atmosphere stability near surface layer caused by the heterogeneity of land surface roughness. The calculation of turbulent flux is the most sensitive to stability in the above three factors. The above analysis shows that it is necessary to make a further consideration for the calculation deviation of the turbulent fluxes brought from land surface heterogeneity in the present numerical models.     

Evaluation of coal longwall caving characteristics using an innovative UDEC Trigon approach

The paper presents an innovative numerical approach to simulate progressive caving of strata above a longwall coal mining panel. A proposed Trigon logic is incorporated within UDEC to successfully capture the progressive caving of strata which is characterized by fracture generation and subsequent propagation. A new damage index, D, is proposed that can quantify regions of both compressive shear and tensile failure within the modelled longwall. Many features of progressive caving are reproduced in the model and found to fit reasonably well with field observations taken from a case study in the Ruhr coalfield. The modelling study reveals that compressive shear failure, rather than tensile failure, is the dominant failure mechanism in the caved strata above the mined-out area. The immediate roof beds act like beams and can collapse in beam bending when vertical stress is dominant or in beam shear fracture when horizontal stress is dominant. The proposed numerical approach can be used to guide the design of longwall panel layout and rock support mechanisms.     

Decametric survey of discrete sources in the northern sky

This paper presents results and describes the improved data processing algorithm of the low frequency sky survey of discrete sources carried out with the UTR-2 radio telescope. The measurements were conducted within the frequency range 10 to25 MHz. Coordinates and flux densities of the sources detected were obtained. Identification with sources from the 4C survey has been done. The resulting catalogue contains parameter estimates for 483 sources on a set of frequencies within the UTR-2 range. This revised version was published online in July 2006 with corrections to the Cover Date. This revised version was published online in July 2006 with corrections to the Cover Date.     

Metamorphism of pelites in NKFMASH – a new petrogenetic grid with implications for the preservation of high-pressure mineral assemblages during exhumation

A petrogenetic grid for metapelites in the system NKFMASH is presented. The P–T range is investigated in three sections: (1) The high‐ and ultrahigh‐pressure range is discussed in the system NFMASH because phengite is the only stable potassic phase. (2) The transition region is characterised by four NKFMASH‐invariant points that separate high‐pressure glaucophane‐bearing from medium‐pressure biotite‐bearing metapelites. (3) The medium‐pressure range contains the fifth NKFMASH‐invariant point. The univariant reactions of this point terminate the stability range of paragonite, which breaks down to form staurolite or kyanite and plagioclase during decompression and/or heating. As the growth of albitic plagioclase by decomposition of paragonite via continuous reactions may be conspicuous already before these staurolite‐ or kyanite‐producing reactions are reached, such albite porphyroblast schists are typical indicators of a former high‐pressure metamorphic history. Considering the preservation of high‐pressure metapelitic assemblages, those crossing the NKFMASH‐transition region during exhumation commonly dehydrate and preservation is unlikely. Three types of metapelites have a fairly good survival potential: (1) low‐temperature metapelites (up to c. 540 °C) with an exhumation path back into the chlorite + albite stability field, (2) assemblages with chloritoid + glaucophane, and (3) the relatively high‐temperature glaucophane + kyanite and jadeite + kyanite bearing parageneses, that are relatively dry at the onset of exhumation. A comparison with data from the literature shows that these rock types are the most abundant in nature.     

Statistical probability distribution of snow depth at the model sub‐grid cell spatial scale

Comprehensive snow depth data, collected using georadar and hand probing, were used for statistical analyses of snow depths inside 1 km grid cells. The sub‐grid cell spatial scale was 100 m. Statistical distribution functions were found to have varying parameters, and an attempt was made to connect these statistical parameters to different terrain variables. The results showed that the two parameters mean and standard deviation of snow depth were significantly related to the sub‐grid terrain characteristics. Linear regression models could explain up to 50% of the variation for both of the snowcover parameters mentioned. Copyright © 2004 John Wiley & Sons, Ltd.