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111.
112.
云南春季强低温的诊断分析 总被引:5,自引:2,他引:5
运用北半球500hPa格点资料,分析了3月倒春寒天气发生的同期、前期500hPa环流特征。云南春季倒春寒天气的发生与同期500hPa上乌拉尔山脊的建立、新西伯利亚附近横槽转竖有关,孟加拉湾南支槽的影响使倒春寒天气更易发生。 相似文献
113.
巴州春季气温趋势分类及预报 总被引:1,自引:0,他引:1
祝学范 《沙漠与绿洲气象(新疆气象)》2001,24(2):3-8
提出一种对春季气温趋势分类的方法,用чeσbцшeB多项式和EOF展开方法,求出一组系数,并根据这些系数把春季气温趋势分为5类,用上述方法明确地描述春季气温趋势的特征,更进一步从冬季500hPa平均图中选取预报因子,对春季气温趋势作出预测。 相似文献
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115.
We established the relationships between water chemistry changes in a pool fed by a permanent spring and seasonal variations in trace-element contents (Sr & Mg) in the shells of the ostracod species Herpetocypris intermedia, based on monthly collections of ostracod and water samples. The water chemistry of the investigated pool (Maïques, Valëncia, Spain) was dominated by calcium and bicarbonate, and showed marked seasonal variation in alkalinity, Ca2+ content, Sr/Ca and Mg/Ca ratios. Although the variability in the water chemistry was relatively low (~10% relative standard deviation over the entire period), the trace-element contents in the ostracod shells tracked the seasonal change in the water chemistry of Maïques pool. Moreover, due to the rapid renewal of H. intermedia population, this species is able torecord in its shells the evolution of the water chemistry at a monthly time scale. Our results also showed that, in the Maïques pool system, ostracod Sr/Ca and Mg/Ca ratios increased with the decrease in water salinity.To our knowledge, this is the first geochemical study of ostracods dwelling in spring environments. The results of this study may be applied to paleohydrological reconstruction using ostracods preserved in sediments deposited around springs (i.e. travertine and tufa deposits). 相似文献
116.
临汾龙子祠泉岩溶水系统水文地质特征及开发利用前景 总被引:1,自引:1,他引:1
在讨论了龙子祠泉岩溶水系统岩叶下水水文地质特征的基础上,岩溶地下水对开发利用前景进行了初步探讨。 相似文献
117.
Based on grey set, grey numbers and their operation properties, the grey numerical model of groundwater seepage system was
set up for the first time, the whole grey solving method of the model was given and it was proved that the common solving
method of the model was only a special case of the grey solving methods. At the same time, the grey solving method was compared
widely with common solving method, classical numerical method. The study shows that the grey solving method is better in depicting
the procedure of transporting grey data of groundwater system. On the basis of the theoretical study, two basic kinds of cases
about groundwater seepage were selected: the prediction of pit yield and the evaluation of groundwater resources on a groundwater
basin. In the cases, systematical analyses were made for generalization and greylization of the hydrogeologic conditions,
setting up of the grey model, identification and correction of the model as well as its prediction and evaluation. It was
pointed out that when the grey numerical model is used to predict pit yield, the upper limit of the “grey band” of groundwater
level cannot be higher than planed safe groundwater level, when evaluating the groundwater resource, the lower limit of the
“grey band” of groundwater level cannot be lower than controlled level of groundwater. 相似文献
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119.
Kurt O. Konhauser Vernon R. Phoenix Simon H. Bottrell David G. Adams & Ian M. Head 《Sedimentology》2001,48(2):415-433
Silicified deposits, such as sinters, occur in several modern geothermal environments, but the mechanisms of silicification (and crucially the role of microorganisms in their construction) are still largely unresolved. Detailed examination of siliceous sinter, in particular sections of microstromatolites growing at the Krisuvik hot spring, Iceland, reveals that biomineralization contributes a major component to the overall structure, with approximately half the sinter thickness attributed to silicified microorganisms. Almost all microorganisms observed under the scanning electron microscope (SEM) are mineralized, with epicellular silica ranging in thickness from < 5 μm coatings on individual cells, to regions where entire colonies are cemented together in an amorphous silica matrix tens of micrometres thick. Within the overall profile, there appears to be two very distinct types of laminae that alternate repeatedly throughout the microstromatolite: ‘microbial’ layers are predominantly consisting of filamentous, intact, vertically aligned, biomineralized cyanobacteria, identified as Calothrix and Fischerella sp.; and weakly laminated silica layers which appear to be devoid of any microbial component. The microbial layers commonly have a sharply defined base, overlying the weakly laminated silica, and a gradational upper surface merging into the weakly laminated silica. These cyclic laminations are probably explained by variations in microbial activity. Active growth during spring/summer allows the microorganisms to keep pace with silicification, with the cell surfaces facilitating silicification, while during their natural slow growth phase in the dark autumn/winter months silicification exceeds the bacteria’s ability to compensate (i.e. grow upwards). At this stage, the microbial colony is probably not essential to microstromatolite formation, with silicification presumably occurring abiogenically. When conditions once again become favourable for growth, recolonization of the solid silica surface by free‐living bacteria occurs: cell motility is not responsible for the laminations. We have also observed that microbial populations within the microstromatolite, some several mm in depth, appear viable, i.e. they still have their pigmentation, the trichomes are not collapsed, cell walls are unbroken, cytoplasm is still present and they proved culturable. This suggests that the bulk of silicification occurred rapidly, probably while the cells were still alive. Surprisingly, however, measurements of light transmittance through sections of the microstromatolite revealed that photosynthetically active light (PAL) only transmitted through the uppermost 2 mm. Therefore the ‘deeper’ microbial populations must have either: (i) altered their metabolic pathways; (ii) become metabolically inactive; or (iii) the deeper populations may be dominated by different microbial assemblages from that of the surface. From these collective observations, it now seems unequivocal that microstromatolite formation is intimately linked to microbial activity and that the sinter fabric results from a combination of biomineralization, cell growth and recolonization. Furthermore, the similarities in morphology and microbial component to some Precambrian stromatolites, preserved in primary chert, suggests that we may be witnessing contemporaneous biomineralization processes and growth patterns analogous to those of the early Earth. 相似文献
120.
本文首次弄清了毛垭温泉测点的局部地质环境,确定了测泉的水文地质性质和类型,弥补了建点基础资料之不足。采用常规的调查追踪方法对该前兆观测点近期出现的特大异常进行了较为详细地落实,并简要分析了调查结果。 相似文献