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61.
湖南黄金洞金矿毒砂中Au赋存状态的电子探针研究   总被引:1,自引:0,他引:1  
本文利用JXA-8800M超大型电子探针,以湖南黄金洞金矿含金毒砂为研究对象。利用金特征X-射线扫描方法和微区含金含量,对不可见金赋存状态的研究方法和温试条件进行了探索,先观察背散射电子图像,排除金在含金矿物毒砂中呈显显微颗粒存在的可能性,继而用LiF晶体测定金L=88.76Lal峰位,然后逐渐放大倍数(x300,x1000,x5000,x30000,x200000)进行金特征,X-射线连续测量,,结果发现金元素总 是均匀分布在重砂中,从而证实了金呈品格金形式存在的推测。  相似文献   
62.
本文对辽宁宽甸碱性玄武岩中巨晶单斜辉石进行穆斯堡尔谱研究。应用晶体结构研究结果较合理地解释了单斜辉石的异常穆斯堡尔谱。结合XRD讨论了单斜辉石中Fe结构态的测定以及穆斯堡尔谱的可应用性。巨晶应结晶于相当氧化的环境。  相似文献   
63.
岩石所受的三向应力状态对其弹性波传播性质有一定的影响,此认识为所做的以泥质砂岩、泥岩和硅质胶结的坚硬砂岩为试样的实验所证实。实验结果表明,泥质砂岩和泥岩的vP/vS值几乎保持不变,硬质砂岩的vP/vS曲线却在应力达破坏荷载的90%左右出现下凹现象。经热处理后的硬质砂岩这一下凹现象则更突出  相似文献   
64.
The incidence of lung cancer in the Gejiu area of Yunnan Province ranks the first in the world.The radon level(indoor,soil) was measured in the Gejiu area by the SSNTD method from 1990 to 1996,The result indicates an extensive high-level of indoor radon in that area though U and Th are lower in local limestones,The indoor radon level of houses located in the geologic fault zone is 6 times high that 2km far from the fault zone.The reason probably is that the radon level of soil in the fault is 6-8 times high that 1 km far from the faults.our data indicate that a lower range of radon levels,0-100Bq.m^-3,exists in healthy families.However,a higher radon level,over 800 Bq.m^-3,is often found corresponding to that of cancer patients‘ homes(the house-owners are suffering from either lung cancer or leukaemia or liver cancer),Obviously,an increase in lung cancer incidence follows an increase in indoor radon level,The risk of cancer induced by indoor radon is no longer an inference,but a fact.  相似文献   
65.
The identifiability of model parameters of a steady state water quality model of the Biebrza River and the resulting variation in model results was examined by applying the Monte Carlo method which combines calibration, identifiability analysis, uncertainty analysis, and sensitivity analysis. The water quality model simulates the steady state concentration profiles of chloride, phosphate, ammonium, and nitrate as a function of distance along a river. The water quality model with the best combination of parameter values simulates the observed concentrations very well. However, the range of possible modelled concentrations obtained for other more or less equally eligible combinations of parameter values is rather wide. This range in model outcomes reflects possible errors in the model parameters. Discrepancies between the range in model outcomes and the validation data set are only caused by errors in model structure, or (measurement) errors in boundary conditions or input variables. In this sense the validation procedure is a test of model capability, where the effects of calibration errors are filtered out. It is concluded that, despite some slight deviations between model outcome and observations, the model is successful in simulating the spatial pattern of nutrient concentrations in the Biebrza River.  相似文献   
66.
The diagenetic mechanism and process of carbonate rocks, which is different to that of clastic rocks, decides the existence of different existing state organic matters in carbonate rocks. This has been verified by both the microscopic observation of organic petrology and the analysis of organic geochemistry of many samples. Based on the hydrous pyrolysis simulation experiment of the low-mature carbonate rocks, the contrasting study on the yield and their geochemistry characteristics of different existing state soluble organic matters of a series of various maturity samples shows that the different existing state organic matters make different contributions to hydrocarbon generation during every evolution state. So that, the hydrocarbon generation process of carbonate rocks can be summarized as the following three stages: the first is the direct degradation of biogenic bitumen macromolecules during the immature stage, the second is the thermal degradation of a large amount of kerogen at the mature stage, the last stage is the expulsion or release of inclusion organic matter owing to the increased thermal expansion pressure during the high evolution stage. Part of achievements of the Eighth Five-Year National Science-Technology Key-Task Project “85-102-02-07”.  相似文献   
67.
孕震系统中的1/f噪声行为   总被引:3,自引:1,他引:3       下载免费PDF全文
根据自组织临界现象理论,研究7海城、唐山等7个大地震前、后中小地震的活动特征,计算了不同孕震时期地震活动的功率谱特征.初步结果表明描述地震活动的谱幂律指数p值在大震发生前有明显的增高倾向.主震前一年及主震当年,p值一般落在闪变噪声的谱域,其他时间一般很小.最后讨论了地震孕育的物理过程及孕震系统的稳定性.  相似文献   
68.
王宁练  薄健辰 《冰川冻土》1997,19(2):167-172
探讨山谷冰川稳定状态时积累区面积比率,即AAR值的大小,认为冰川物质平衡高程分布,平面形态及坡面坡度沿程变化形式是影响山谷冰川稳定态AAR值的主要因素,并 山谷冰川稳定态AAR值与物质平衡高程分布及平面形态之间的定量关系。山谷冰川适合于应用AR值法来研究古冰川的零平衡线高程。  相似文献   
69.
A new complex modal analysis‐based method is developed in the frequency domain for efficient computation of the earthquake input energy to a highly damped linear elastic passive control structure. The input energy to the structure during an earthquake is an important measure of seismic demand. Because of generality and applicability to non‐linear structures, the earthquake input energy has usually been computed in the time domain. It is shown here that the formulation of the earthquake input energy in the frequency domain is essential for deriving a bound on the earthquake input energy for a class of ground motions and for understanding the robustness of passively controlled structures to disturbances with various frequency contents. From the viewpoint of computational efficiency, a modal analysis‐based method is developed. The importance of overdamped modes in the energy computation of specific non‐proportionally damped models is demonstrated by comparing the energy transfer functions and the displacement transfer functions. Through numerical examinations for four recorded ground motions, it is shown that the modal analysis‐based method in the frequency domain is very efficient in the computation of the earthquake input energy. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   
70.
王卫东  宋庆春 《华北地质》2004,27(3):144-148
新近系地下淡水是下辽河三角洲地区的盘锦市和辽河油田主要供水水源。地下水处于封闭到半封闭环境,包括明化镇组(Nm)和馆陶组(Ng)两个含水岩组。天然状态下,地下水位接近或高于地表;开采条件下,地下水位逐年下降,形成区域性降落漏斗,地下水流场均发生显著变化,形成汇向开采区的向心流场。开采明化镇组地下水为主的盘东水源地,开采初期水位下降速率为1.61~5.19m/a,至1996年降至0.63~1.03m/a;馆陶组地下水为主的各水源地,开采初期水位下降速率为2.10~4.21m/a,至1996年减至1.49~2.05m/a。这是由于地下水流场变化,导致明化镇成水体内侵和下移所致,该地地下水中Cl^-的不断增高也证明了这一点。至1998年。平面上,成水体每年增加3.18km^2,盘东水源南部,成水体内侵速率已达每年220m。垂向上成水体年下移速率一般每年0.5~1.67m。进行新近系地下水动态特征和演化趋势研究,将为合理开发利用宝贵的淡水资源提供科学依据。  相似文献   
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