含硼氯化镁饱和卤水的冷冻实验     

高世扬  赵金福 《盐湖研究》1998,6(1):1-10

对含胡浓缩盐卤在冷冻析出一般盐类进行研究结果表明,在从－１０℃至－２０℃范围内,析出高水合硫酸镁和氯化镁盐。尤其是硼酸镁盐。经化学分析,热分析粉晶衍射结果表明,从室温到－２０．５℃范围内,不同时间放量析出同一种硼酸镁－三方硼镁石。  相似文献   

第四纪孢粉分析的时间序列与空间模型   总被引：4，自引：0，他引：4  

郑卓 《地球科学进展》1998,13(3):300-305

论述了第四纪孢粉时间序列和孢粉空间模型在不同尺度上的时空代表性,同时介绍了一些相关的研究方法和主要成果。利用数理统计方法来定量恢复古气候已成为目前第四纪孢粉时间序列研究的一个发展趋势。各种尺度的第四纪孢粉空间模型图可以反映植被对第四纪气候变化的响应。根据孢粉数据与气候变量之间的函数关系还可换算成古气候图。此外,在全球气候模拟和植被模拟中,孢粉数据成为必不可少的诊断工具。  相似文献   

岩体声发射监测在马步坎高边坡岩体稳定研究中的应用   总被引：1，自引：0，他引：1  

严明  苗放 《地质灾害与环境保护》1998,9(1):29-33

简要阐述岩体声发身监测的基本原理,监测仪器与技术,及其在金沙江向家坝水电站马步坎高边坡岩体稳定研究中的应用情况,认为岩体声发射监测是研究边坡岩体稳定性的一种有效手段。  相似文献   

Brine transport in porous media: On the use of Von Mises and similarity transformations     

C.J. van Duijn  R.J. Schotting 《Computational Geosciences》1998,2(2):125-149

In this paper we use a Von Mises transformation to study brine transport in porous media. The model involves mass balance equations for fluid and salt, Darcy's law and an equation of state, relating the salt mass fraction to the fluid density. Application of the Von Mises transformation recasts the model equations into a single nonlinear diffusion equation. A further reduction is possible if the problem admits similarity. This yields a formulation in terms of a boundary value problem for an ordinary differential equation which can be treated by semi‐analytical means. Three specific similarity problems are considered in detail: (i) one‐dimensional, stable displacement of fresh water and brine in a porous column, (ii) flow of fresh water along the surface of a salt rock, (iii) mixing of parallel layers of brine and fresh water. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

胜利海上埕岛油田下古生界潜山高产因素分析   总被引：1，自引：0，他引：1  

高喜龙  杨鹏飞 《海相油气地质》1998,3(4):51-56

埕岛油田是我国浅海－极海海域发现的第一个大型整流油气田,四周环凹,油源条件十分优越,全区可划分为西排山,中排山,东排山三个潜山带构造单元,油气运移通道主要是断裂和风化壳不整合面,区域盖层发育良好,储集条件是油气富集高产控制因素,纵向上潜山带储层主要集中在潜山的风化壳;平面上主要沿断层分布,沿断层发育的奥陶系在潜山是本区古生办潜山勘探的最有利目标。  相似文献   

中国东北冬季极端低温的年代际变化及其成因     

闵锦忠  粘新悦  孙玉婷  李岩 《气象科学》2022,42(6):711-720

利用JRA-55再分析资料和中国824站日最低气温数据,分析了1961—2013年冬季中国东北地区极端低温的年代际变化及其动力成因。结果表明:东北冬季极端低温1980s中期前频发,1980s后期到2000s初少发,2000s后恢复多发。这与贝加尔湖阻塞高压频次偏多—偏少—偏多的同步年代际变化直接相关,与北极涛动(Arctic Oscillation,AO)和准定常行星波活动的年代际振荡相联系。相比于1980s中期前,1988—1999年期间行星波沿极地波导向平流层的传播减弱,引起高纬度平流层下层E-P通量辐合变弱;而行星波沿低纬波导往副热带对流层上层的传播增强,造成副热带对流层中上层E-P通量辐合增强。行星波E-P通量散度的异常由于波—流相互作用,分别导致了极夜急流加强、副热带急流减弱,因而AO增强,不利于贝湖阻高建立和环流经向型发展,极端低温减少。2000—2013年,行星波活动相反,导致AO减弱,贝湖阻高多发,极端低温恢复增多。  相似文献   

盐卤对接井溶腔计算方法探讨     

秦沛  齐如明  李斌 《城市地质》2008,3(1):11-13

盐卤井对接施工中,能否成功对接（中靶）,一方面取决于定向井的定向精度,另一方面决定于直井溶腔的建立（通称“建槽”）是否达到设计要求。建槽未能严格按要求进行会导致溶腔与计算不符,造成对接失败或重复工作。而溶腔的设计计算,与目的（盐）层厚度、倾角及采卤方式有关。  相似文献   

Aspect control of water movement on hillslopes near the rain–snow transition of the Colorado Front Range          下载免费PDF全文

Eve‐Lyn S. Hinckley  Brian A. Ebel  Rebecca T. Barnes  Robert S. Anderson  Mark W. Williams  Suzanne P. Anderson 《水文研究》2014,28(1):74-85

In the Colorado Front Range, forested catchments near the rain–snow transition are likely to experience changes in snowmelt delivery and subsurface water transport with climate warming and associated shifts in precipitation patterns. Snowpack dynamics are strongly affected by aspect: Lodgepole pine forested north‐facing slopes develop a seasonal snowpack, whereas Ponderosa pine‐dotted south‐facing slopes experience intermittent snow accumulation throughout winter and spring. We tested the degree to which these contrasting water input patterns cause different near‐surface hydrologic response on north‐facing and south‐facing hillslopes during the snowmelt period. During spring snowmelt, we applied lithium bromide (LiBr) tracer to instrumented plots along a north–south catchment transect. Bromide broke through immediately at 10‐ and 30‐cm depths on the north‐facing slope and was transported out of soil waters within 40 days. On the south‐facing slope, Br^? was transported to significant depths only during spring storms and remained above the detection limit throughout the study. Modelling of unsaturated zone hydrologic response using Hydrus‐1D corroborated these aspect‐driven differences in subsurface transport. Our multiple lines of evidence suggest that north‐facing slopes are dominated by connected flow through the soil matrix, whereas south‐facing slope soils experience brief periods of rapid vertical transport following snowmelt events and are drier overall than north‐facing slopes. These differences in hydrologic response were largely a function of energy‐driven differences in water supply, emphasizing the importance of aspect and climate forcing when considering contributions of water and solutes to streamflow in catchments near the snow line. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献   

Middle Permian high Sr/Y monzogranites in central Inner Mongolia: reworking of the juvenile lower crust of Bainaimiao arc belt during slab break-off of the Palaeo-Asian oceanic lithosphere     

《International Geology Review》2012,54(17):2083-2099

ABSTRACT

The high Sr/Y geochemical feature of granitoids can be attributed to various mechanisms, and elucidating genesis of high Sr/Y granitoids provides insights into the material recycling and magmatic processes at depth. In southeastern Central Asian Orogenic Belt (CAOB), many Middle Permian granitoids exhibit high Sr/Y ratios, but their origins remain unclear, inhibiting a comprehensive understanding of the magmatic response to the final closure of the Palaeo-Asian ocean. Here we present new zircon U-Pb ages, Lu-Hf isotopes and whole-rock geochemical data for the Middle Permian high Sr/Y monzogranites from central Inner Mongolia, southeastern CAOB. LA-ICP-MS zircon U-Pb data shows that these high Sr/Y rocks were emplaced during 273–261 Ma. They are calc-alkaline, sodium-rich and metaluminous to weakly peraluminous, with enriched large-ion lithophile elements (Rb, Th, K and Pb) and depleted high field strength elements (Nb, Ta, P and Ti), suggesting a mafic lower crustal source rather than evolved potassic crustal materials. Their relatively low (Gd/Yb)_N (1.1–2.0), (Dy/Yb)_N (1.0–1.3), Nb/Ta (7.9–10.9) ratios and flat heavy rare earth element patterns are characteristics of derivation from a relatively shallow depth with amphibolite as dominant residue. They also have highly variable ε_Hf(t) values (?8.2 to +10.0) and T_DMC (1814 to 649 Ma), similar to those of the Early Palaeozoic high Sr/Y intrusions along the Bainaimiao arc belt. Combined with data from literatures, we suggest that the high Sr/Y monzogranites in this study were probably generated by reworking of the newly underplated juvenile high Sr/Y lower crust of the Bainaimiao arc belt. Moreover, taking into account the regional investigations, the sublinear distributed Middle Permian magmatic rocks in the southeastern CAOB were likely associated with the incipient slab break-off of the Palaeo-Asian oceanic lithosphere following initial collision between the North China craton and the South Mongolia terranes.  相似文献   

采空区探测高密度电阻率法的应用     

李远强 《城市地质》2012,7(1):51-54

高密度电阻率法由常规电法演化而来,其电极排列类型多,应用范围广。本文以北京地区的地下采空勘查探测为例,论述了高密度电阻率法的测线布置、电极排列,到数据处理、图像解释等技术方法。通过实地钻孔验证,说明探测结果准确,为采空区评价提供了可信的基础数据。  相似文献