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991.
沈冠军 《中国地球化学学报》1996,15(4):303-313
Calculations,according to some open-system models,point out that while a statistically significant discrepancy between the results of two U-series methods,^230Th/^234U and ^227Th/^220Th(or ^231Pa/^235U),attests a relatively recent and important uranium migration,concordant dates cannot guarantee closes-system behavior of sample.The results of 20 fossil bones from 10 Chinese sites,19 of which are determined by two U-series methods,are given,Judging from independent age controls,8 out of the 11 concordant age sets are unacceptable,The results in this paper suggest that uranium may cycle into or out of fossil bones,such geochemical events may take place at any time and no known preserving condition may securely protect them from being affected.So for the sitew we have studied,the U-series dating of fossil bones is of limited reliability. 相似文献
992.
993.
994.
考虑入渗和蒸发影响的土坡稳定性分析方法 总被引:47,自引:7,他引:47
本研究建议的一种分析方法假定斜坡非饱和土体的水分运动参数及剪强度参数与饱和度的依赖关系均可根据实验或经验确定。通过数值计算方法妥任意给定的入渗和蒸发边界条件下斜坡土体的瞬态含水率分布及与其相对应的瞬态抗剪强度参数分布。在此基础上瞬态斜坡安全因数即可通过常规的稳定性分析方法求得。 相似文献
995.
介绍了利用隧道施工的位移量测信息来选择计算模型的原理和方法。应用实例表明,本文所提出的方法有较好的应用前景。 相似文献
996.
Peter K. Kitanidis 《Mathematical Geology》1997,29(3):335-348
This article discusses the issue of whether to use a variable mean and describes a test that can be used to evaluate whether
it is justified to add terms to the drift (deterministic part) of a geostatistical model. The basic model could be the intrinsic
one, where the deterministic part is a constant, and the alternate model could be any model that includes a constant term
in the expression for the drift. Also, differences between constant- and variable-mean models are discussed. 相似文献
997.
在岩溶地区,地下水的超强度开采与工业“三废”及生活废弃物不合理的排放,造成了地下水较严重的污染。用动态系统方法建立的地下水污染时间序列递推预测模型,在岩溶地下水环境质量预测与管理方面都具有指导意义。 相似文献
998.
中国古大陆及其边缘早古生代层序地层及海平面变化的基本特征 总被引:4,自引:0,他引:4
着重总结了我国古大陆及其边缘早古生代大层序(megasequence,一级层序)和中层序(mesosequence,二级层序),以及一级、二级海平面变化的基本特征,并与国外早古生代海平面变化进行对比.我国3大古陆(华北陆块、扬子陆块、塔里木陆块)及其边缘早古生代大层序可划分为两个(MG-1,MG-2).中层序划分为5个(MS-1,MS-2,MS-3,MS-4,MS-5).MG-1包括MS-1,MS-2和MS-3,时限为94~112Ma(寒武纪和早奥陶世),底以巨大不整合为界,顶以著名巨大沉没不整合为限,沉积了我国显生宙大部分的碳酸盐岩,赋存着丰富的油气和各种金属及非金属矿产.MG-2包括MS-4和MS-5,时限为58~68Ma(中、晚奥陶世和志留纪),底界以巨大沉没不整合为界,为硅质碎屑-碳酸盐岩组合.海平面变化的级别划分对应于层序.中国3大古陆及其边缘早古生代海平面变化的总貌:MGSC-1初期普遍发生快速海进,海平面升高,尔后海平面下降,其间有多期次的小幅度海进和海退变化.MGSC-2则普遍海平面升高,上升幅度大于MGSC-1,尔后逐渐下降. 相似文献
999.
K. S. Voudouris N. J. Lambrakis G. Papatheothorou P. Daskalaki 《Mathematical Geology》1997,29(1):43-59
R- andQ-mode factor analysis is applied to 51 groundwater samples collected from wells drilled in the Plio-Pleistocene aquifers of
NW Achaia, Greece. The purpose ofR- andQ-mode factor analysis application is to identify (i) the regional groundwater flow pattern, and (ii) the deterioration of
groundwater quality. Sixteen hydrogeological parameters are used in order to examine their importance and to provide significant
insight into their correlations. In theR-mode factor analysis, a six-factor model is suggested which can explain more than 77.5% of the total variance. The contribution
of each factor at every site (factor scores) also is computed. Maps are constructed showing the geographical distribution
of the factor scores. From these maps, the high salinity areas are delineated (seawater intrusion, possible appearance of
halite layers) and the areas with elevated contribution of karastic-water are defined. Using theQ-mode correspondence analysis the meaning of the electrical conductivity as the most important variable in groundwater quality
characterization is demonstrated. 相似文献
1000.
The Bengal basin, Bangladesh, represents one of the most densely populated recent floodplains of the world. The sediment
flux through the basin is one of the highest on a global scale. A significant portion of this sediment load find its sink
in the basin itself because of its lower elevation and frequent flooding. The textural, mineralogical and chemical nature
of the sediments thus have an important bearing on the environmental quality of the basin as well as for the Bay of Bengal.
The sediment load of the Ganges-Brahmaputra-Meghna (GBM) river system consists exclusively of fine sand, silt and clay at
their lower reaches within the Bengal basin, Bangladesh, and is deposited under uniformly fluctuating, unidirectional energy
conditions. The sediments have a close simitarity in grain size with the sediments of the surrounding floodplain. The mineral
assemblage is dominated by quartz and feldspars. Illite and kaolinite are the major clay minerals, and occur in almost equal
proportion in bed sediments. The heavy mineral assemblage is dominated by unstable minerals which are mostly derived from
high-rank metamorphic rocks. The characteristic smaller grain-size, i.e. having large surface-to-mass ratios, and the mineralogy
of sediments suggests that they are susceptible to large chemical adsorptive reactions and thus could serve as a potential
trap for contaminants. However, the sediments of the GBM river system in the Bengal basin, Bangladesh, shows lower concentration
of Pb, Hg and As, and a marginally higher value for Cd as compared to that of standard shale. Considering population density
and extensive agricultural practice in the basin, the sediments can in the long run become contaminated.
Received: 9 November 1994 · Accepted: 18 June 1996 相似文献