Using Natural Stable Hydrogen and Oxygen Isotopes for Studying the Conditions of Ground Ice Formation

The isotopic composition of ground ice in lacustrine deposits of different age in the Taimyr Peninsula is discussed. It is shown that the combined use of two isotopic indicators (²H and ¹⁸O) provides additional information (unavailable when any of the isotopes is used alone) about the conditions of formation of segregated ground ice.     

Probabilistic Microzonation of Urban Territories: A Case of Tashkent City

—?The problem of accounting for local soil effect on earthquake ground motion is especially urgent when assessing seismic hazard – recent needs of earthquake engineering require local site effects to be included into hazard maps. However, most recent works do not consider the variety of soil conditions or are performed for generalized site categories, such as “hard rock,”“soft soil” or “alluvium.” A technique of seismic hazard calculations on the basis of the Fourier Amplitude Spectra recently developed by the authors allows us to create hazard maps involving the influence of local soil conditions using soil/bedrock spectral ratios. Probabilistic microzoning maps may be constructed showing macroseismic intensity, peak ground acceleration, response and design spectra for various return periods (probability of exceedance), that allow optimization of engineering decisions. An application of this approach is presented which focused on the probabilistic microzoning of the Tashkent City.     

古吉黑造山带拼接带地球物理特征线

吉黑造山带拼接带的地球物理特征线，在重磁图上为伊通-吉昌-桦甸、贤儒-安图-开山屯一线。它分割了两种截然不同的地球物理场区，与两侧中元古宙-早三叠世不同的地质发育历史相呼应；和石炭-二叠系安哥拉与华夏植物地球区系的界线相一致。这是有别于前人而为更多新的地质资料所支持的新认识。     

安徽巢湖—滁州地区中生代构造变形特征

安徽巢湖—滁州地区位于张八岭冲断带的南东侧 ,中生代构造活动十分强烈。早印支期 ,区内以北东—北北东向褶皱和逆冲推覆构造变形为特征 ,形成区内主体构造格架 ,为下扬子构造带的组成部分 ;晚印支期以近南北向挤压作用为主 ,形成北西西—近东西向叠加褶皱构造。燕山期 ,受郯庐断裂构造活动的影响 ,区内断裂活动加剧 ,形成多期不同性质的脆性断裂及其所控制的沉积盆地 (拗陷 )。     

小兴安岭黑大公路沿线多年冻土分布及退化状态

黑大公路沿线多年土主要分布于黑河－北安段，属小兴安岭岛状多年冻土区，该区存在的多年冻土是晚全新世寒冷时期的产物，现处于欧亚多年冰土南界边缘，多年冻土发育在低洼、地表积水、塔头草生长茂密、草炭和泥炭发育的沼泽化湿地当中，沼泽湿地独特的热交换特性决定了其中发育的多年冻土处于退化的最晚阶段，冻土的退化在自然条件下可能依赖于由于至上的地下热流。多年冻土的地温剖面表现为零梯度曲且冰土温度接近于0℃，由此决定了多年冻土对人为活动干扰的敏感性。     

快速法固结试验经验修正系数的探讨

实践证明，常规固定试验（压缩试验）可以采用快速法替代现行规范的慢速法。本文在大量统计对比和相应理论分析基础上提出上海地区经验修正系数K值，以利快速法的推行。     

裂缝性边水油气藏水侵量计算方法

水侵量求取一直是困扰油藏工程师的一个问题，其中,裂缝性边水水侵量的计算还没有一个公开的有效方法。本文试根据不稳定渗流模型，提出裂缝性边水水侵量的新计算方法。     

羟基磷灰石吸附剂去除铬黄工业废水中铅离子的研究

羟基磷灰石吸附剂对铬黄废水中Pb^2 吸附的间歇实验结果表明：当每吨废水中吸附剂用量为200～400g时，常温搅拌60min后，在弱酸性或中性废水中，铅离子质量浓度由2.74mg/L降至0.5mg/L以下，完全符合GB8978-1996工业废水排放标准1.0mg/L。     

叠前正演模拟与偏移的网络并行计算

在叠前深度偏移和非零炮检距声波方程正演计算过程中包含了大量的可并行计算的成分。作者在本文中提出叠前正演模拟与偏移的网络并行计算算法，并基于TCP／IP协议，将该算法设计成网络并行处理程序，极大地提高了计算效率。实际运算结果证明，本文提出的并行算法和技术路线是切实可行的。     

The Dynamics of Spring Ice Drifts and Jams in the Northern Dvina and Pechora Mouths

The dynamic type of ice drift development is found to dominate in the mouth zones of the Northern Dvina and Pechora rivers in the period of spring ice break. The ice drift is accompanied by the formation of ice jams in the mouth, the most common among them being jams of arched and wedge type. The jams are a common cause of flooding of towns and settlements in the region. The particular features of ice breaking in the mouths of northern rivers are discussed along with the regularities of ice jam formation during ice drift. The formation of jams is shown to be associated with stable retardation of ice in the sites of river channels that have specific morphological characteristics or to be caused by drifting ice mass running into solid ice fields in lower parts of river delta arms.