相山铀矿田邹家山矿床成矿流体特征   总被引：2，自引：0，他引：2  

郭建  李子颖  李秀珍  聂江涛  王健 《铀矿地质》2014,(5):263-270

通过流体包裹体的岩相学研究、显微测温和激光拉曼探针测试,探讨了邹家山铀矿床成矿流体特征、演化及矿质沉淀方式。研究结果表明,该矿床的成矿流体为中低温热液,碳氢化合物对铀的富集具有不可忽视的作用,流体持续的沸腾作用是矿质沉淀的主要因素。  相似文献   

How does afforestation affect the hydrology of a blanket peatland? A modelling study     

Ciaran Lewis  John Albertson  Tan Zi  Xianli Xu  Gerard Kiely 《水文研究》2013,27(25):3577-3588

Over the last century, afforestation in Ireland has increased from 1% of the land area to 10%, with most plantations on upland drained blanket peatlands. This land use change is considered to have altered the hydrological response and water balance of upland catchments with implications for water resources. Because of the difficulty of observing these long‐term changes in the field, the aim of this study was to utilize a hydrological model to simulate the rainfall runoff processes of an existing pristine blanket peatland and then to simulate the hydrology of the peatland if it were drained and afforested. The hydrological rainfall runoff model (GEOtop) was calibrated and validated for an existing small (76 ha) pristine blanket peatland in the southwest of Ireland for the 2‐year period, 2007–2008. The current hydrological response of the pristine blanket peatland catchment with regard to streamflow and water table (WT) levels was captured well in the simulations. Two land use change scenarios of afforestation were also examined, (A) a young 10‐year‐old and (B) a semi‐mature 15‐year‐old Sitka Spruce forest. Scenario A produced similar streamflow dynamics to the pristine peatland, whereas total annual streamflow from Scenario B was 20% lower. For Scenarios A and B, on an annual average basis, the WT was drawn down by 16 and 20 cm below that observed in the pristine peatland, respectively. The maximum WT draw down in Scenario B was 61 cm and occurred in the summer months, resulting in a significant decrease in summer streamflow. Occasionally in the winter (following rainfall), the WT for Scenario B was just 2 cm lower than the pristine peatland, which when coupled with the drainage networks associated with afforestation led to higher peak streamflows. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献   

Sediment Characteristics Studies on Slope Moving Fans of the Third Section of Shahejie Formation on the Southern Slope of Dongying Depression     

ZHOU Juan  LUO Rongtao 《《地质学报》英文版》2015,89(Z1):310-311

<正>From the beginning of lithological exploration in shengli oilfield,the research of turbidites of the third section of Shahejie formation on the southern slope of Dongying depression were fast maturity.Previos study holds that delta-turbidities depositional systems were widely developed in the middle third section of Shahejie formation in Dongying depression.And make the sands  相似文献   

基于时间序列雷达干涉测量的钱塘江海塘形变分析     

张云俊  万紫  谢酬  邵芸  袁名欢  陈武  王新 《遥感学报》2015,19(2):339-354

形变监测是海塘安全运行的重要组成部分。本文利用杭州地区2006年—2010年获取的31景EnvisatASAR影像,根据MTInSAR(Multi-Temporal In SAR)方法,综合提取PS(Persistent Scatterer)和DS(Distributed Scatterer)点,得到密集的钱塘江海塘形变的In SAR测量结果。与28个点的水准数据对比表明,两者的平均误差为0.436 mm,最大误差为5.016 mm,验证了In SAR技术毫米级的测量精度和准确性。通过这两种数据的时间序列分析发现,海塘的沉降在空间上具有连续性,其空间分布呈现为单峰下沉曲线;在时间上,则具有明显的线性变化规律,并伴随有短时间范围的小幅度波动。  相似文献   

近10年我国天体测量的发展   总被引：3，自引：0，他引：3  

金文敬  李东明  夏一飞  朱紫  陈力 《天文学进展》2004,22(2):115-121

简述天体测量学研究的内各以及与各相关学科之间的关系；描述近10年来国际天体测量研究的进展和前沿课题；叙述我国天体测量研究的历史背景和研究基础，以及近10年来在国家自然科学基金委员会和其他科学组织支持下取得的成果，并对今后10～20年我国天体测量的发展提出初步看法。  相似文献   

利用基本天体测量仪器开展天文测光研究(英)     

朱紫 《天文学进展》1997,(1)

讨论有关天体测量中的测光问题，介绍一些地面天体测量仪器和空间天体测量望远镜的测光研究。给出一种测光资料的处理方法，并建议利用DCMT开展天文测光课题研究。  相似文献   

依巴谷参考架惯性特征     

朱紫 《天文学进展》2001,19(2):302-306

通过分析和比较依巴谷自行系统与FK2．0自行系统之间的关系，研究了依巴谷系统的惯性问题，指出该系统可能然存在较大的非惯性剩余旋转。  相似文献   

Microplane constitutive model for porous isotropic rocks     

Zdenk P. Baant  Goangseup Zi 《国际地质力学数值与分析法杂志》2003,27(1):25-47

The paper deals with constitutive modelling of contiguous rock located between rock joints. A fully explicit kinematically constrained microplane‐type constitutive model for hardening and softening non‐linear triaxial behaviour of isotropic porous rock is developed. The microplane framework, in which the constitutive relation is expressed in terms of stress and strain vectors rather than tensors, makes it possible to model various microstructural physical mechanisms associated with oriented internal surfaces, such as cracking, slip, friction and splitting of a particular orientation. Formulation of the constitutive relation is facilitated by the fact that it is decoupled from the tensorial invariance restrictions, which are satisfied automatically. In its basic features, the present model is similar to the recently developed microplane model M4 for concrete, but there are significant improvements and modifications. They include a realistic simulation of (1) the effects of pore collapse on the volume changes during triaxial loading and on the reduction of frictional strength, (2) recovery of frictional strength during shearing, and (3) the shear‐enhanced compaction in triaxial tests, manifested by a deviation from the hydrostatic stress–strain curve. The model is calibrated by optimal fitting of extensive triaxial test data for Salem limestone, and good fits are demonstrated. Although these data do not cover the entire range of behaviour, credence in broad capabilities of the model is lend by its similarity to model M4 for concrete—an artificial rock. The model is intended for large explicit finite‐element programs. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

2020年前我国核能发展的策略和目标研究     

潘自强  沈文权 《铀矿地质》2004,20(5):257-259

本文提出了我国核电发展的 4项策略 ,明确了近中远兼顾的 3个层次的发展目标及相关的重点工程。  相似文献   

无限长土坡滑移变形模拟     

谢州  周成  刘焦  曾子 《山地学报》2012,(1):65-69

从建立土体应力平衡微分方程入手,在平面应变的假定下求解均质无限长土坡的应力平衡方程。通过拟定坡土的滑移速度和粘塑性应变率的关系式,以剑桥模型为依托,得出滑移变形速率的显式表达式,由此推出土坡滑动位移的计算式。因为模型计算值与实测值无论变形趋势还是大小都有不少误差,所以经修正粘滞性参数来改进模型的模拟精度。最后通过一个算例,将现场实测滑移数据和模型计算值进行比较,分析表明二者较为一致。  相似文献