泥炭样品不同有机组分的~(14)C测年的初步研究

分别用ＮａＣｌＯ、ＮａＯＨ溶液、Ｎａ４Ｐ２Ｏ７和ＮａＯＨ混合溶液和有机溶剂对采自延庆盆地大王庄两个泥炭样品进行前处理，每个样品获得１０个不同有机组分，对这些有机组分的１４Ｃ年龄测定值进行对比。以探讨泥炭等样品不同有机组分１４Ｃ测年的可靠性     

Preliminary Study on Paleoearthquake Chronology on the Northern Liulengshan Piedmont Fault in Yangyuan, Hebei Province, China

The northern Liulengshan piedmont fault is located along the southern margin of the Yangyuan basin and represents a dip-slip normal fault,generally NEE-trending and NNW-dipping.Landforms offset by the fault are fairly developed and well preserved in the Dushanpu area of Yangyuan County,Hebei Province.Two trenches were excavated in front of a scarp of the northern Liulengshan piedmont fault at Dushanpu and two paleoseismic events were revealed in the trenches,from which several samples were collected for dating.The samples were dated using the IRSL dating technique.The preliminary result shows the possible ages of the two paleoseismic events.     

青藏—蒙古高原东缘构造过渡带的布格重力场特征及地壳上地幔结构

本文从青藏—蒙古高原东缘构造过渡带的布格重力场特征、地壳厚度和上地幔密度分布状态入手,就该带具有较统一的地球动力学背景的地球物理标志,壳-幔系统动力学模式及重力均衡调整等问题进行了讨论     

偶氮氯膦Ⅲ双波长分光光度法同时测定铀矿石中钍和铀

本文对偶氮氯膦Ⅲ与钍、铀的显色反应作了研究,提出了三烷基氧膦-G.D.X-301萃取色层分离、偶氮氯膦Ⅲ双波长分光光度法同时测定铀矿石中钍和铀的方法。方法简便,精密度、准确度良好。     

我国盐湖沉积物中的硫酸盐还原细菌及其地球化学作用(英文)

本文对我国某些盐湖和苦水湖沉积物中的硫酸盐还原细菌进行了分离和鉴定。讨论了它们所处的耐盐度、温度、pH等生态条件。从而探讨了它们对沉积物中有机质的富集和保存所起的作用。同时,由于它们在还原硫酸盐时产生大量的硫化氢,导致沉积物中的金属离子以硫化物形式大量地沉淀和富集,这对次生硫化矿沉积物的形成也起着较大的作用。     

Incremental Nonlinear Models

In this paper the incremental nonlinear models are generally discussed, the correlation of this sort of models with others and the difference between them are interpreted, and some basic concepts are clarified. We presented a nonlinear dilatant stress-strain model for soil, which is referred to as KKG model for the sake of simplicity. The experimental results of a sand sample are used to determine the moduli for the following models KKG, KG (the deformation model), and Eν (elastoplastic model) respectively. The comparison of the calculation values of these models with the associated experimental results shows good fittings and prediction of KKG model, and its good simulation of soil dilatant behaviour in particular. The predicted pore pressure and effective stress path have a reasonably good agreement with observed results as well.     

The effect of the electrical anisotropy on the response of helicopter-borne frequency-domain electromagnetic systems

Helicopter electromagnetic (HEM) systems are commonly used for conductivity mapping and the data are often interpreted using an isotropic horizontally layered earth model. However, in regions with distinct dipping stratification, it is useful to extend the model to a layered earth with general anisotropy by assigning each layer a symmetrical 3 × 3 resistivity tensor. The electromagnetic (EM) field is represented by two scalar potentials, which describe the poloidal and toroidal parts of the magnetic field. Via a 2D Fourier transform, we obtain two coupled ordinary differential equations in the vertical coordinate. To stabilize the numerical calculation, the wavenumber domain is divided into two parts associated with small and large wavenumbers. The EM field for small wavenumbers is continued from layer to layer with the continuity conditions. For large wavenumbers, the EM field behaves like a DC field and therefore cannot be sensed by airborne EM systems. Thus, the contribution from the large wavenumbers is simply ignored. The magnetic fields are calculated for the vertical coaxial (VCX), horizontal coplanar (HCP) and vertical coplanar (VCP) coil configurations for a helicopter EM system. The apparent resistivities defined from the VCX, VCP and HCP coil responses, when plotted in polar coordinates, clearly identify the principal anisotropic axes of an anisotropic earth. The field example from the Edwards Aquifer recharge area in Texas confirms that the polar plots of the apparent resistivities identify the principal anisotropic axes that coincide well with the direction of the underground structures.     

WebGIS的空间数据共享与互操作

WebGIS技术是目前实现空间数据共享的有效手段，但是，由于空间数据异构复杂性，空间数据共享与互操作的实现还存在大量的问题亟待解决。本文阐述了空间数据共享与互操作技术模式，介绍了地理标记语言GML及在WebGIS中应用的优势，提出了一种基于GML的WebGIS空间数据共享与互操作方案。     

太湖流域洪涝灾害评估模型

在地理信息系统支持下建立了太湖流域DEM模型,并建立了全流域12类共24种土地利用类型、2194个圩区、1012个乡镇和94个报汛站点的空间数据库及属性数据库。在此基础上,根据实时报汛资料,通过插值得到各乡汛期圩外水位和降雨量。圩区采用排涝计算圩内内涝水量再与DEM叠加,非圩区用乡最高水位与DEM叠加,可获得全流域淹没水深栅格数据。统计不同乡镇、不同土地类型、不同淹没水深的淹没面积,并根据当年的社会经济数据,建立了太湖流域洪涝灾害损失评估模型。对1999年太湖流域洪涝灾害评估结果表明,模型具有一定的精度,可为流域防洪减灾决策提供依据。     

3-D rheologic model of earthquake preparation (I) — Displacement field

Based on the three-dimensional ela stic inclusion model proposed by Dobrovolskii, we developed a three-dimensional rheologic inclusion model and theory to study the earthquake preparation process. By using correspondence principle in the theory of rheologic mechanics, we derived the analytic expression of the viscoelastic displacement at an arbitrary point (x, y, z) in three directions of x, y and z-axes (i.e., U(r, t), V*(r, t) and W(r, t)) produced by a three-dimension inclusion in the semi-infinite rheologic medium defined by the standard linear rheologic model. Foundation item: Chinese Joint Seismological Science Foundation (101105)