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71.
以实测的流体资料为基础,初步揭示了塔北地区油田水文地质和水文地球化学特征。塔北地区存在两股地下水流,南部生油区为压实水流,由南向北流动,北部为重力水流,由北向南流动,这两股水流交汇于雅克拉和轮南地区,向上封闭式内泄。无论重力水流或压实水流,皆为非海相成因、非浓缩成因溶滤水。表明:油气藏的形成绝大部分是寒武-奥陶纪生油层二次成油的结果。  相似文献   
72.
陈敏 《地质论评》1995,41(6):571-576
本文根据安太堡露天煤矿排土场基底黄土的粘土矿物组成的微结构及其在分级荷载下微结构变化的研究,论述了排土场基底黄土内弱层的形成机理,提出弱层是在上覆排土压力下由于黄土的微结构变化而形成的演化弱层。并指出弱层的形成是导致排土场失稳滑坡的主要控制因素,这种弱层在新排土场设计时期并不存在,极具隐蔽性,但在设计时必须考虑在排土增至一定高度后,弱层的形成对排土场稳定性的影响,否则必将会存在重大滑坡隐患。  相似文献   
73.
Dissolved (dialysis in situ) and total concentrations ofCu, Zn, Cd and Al in eight mining polluted rivers in the Røros area, central Norway, were determinedby atomic absorption spectrometry (flame and graphite furnace) and compared to pH, Caconcentration and alkalinity through seasonal variations in river discharge. Totalconcentrations of the metals were highest during early spring flood and during summer andautumn rain episodes. Dissolved concentrations also increased as the spring floodproceeded, but small discharge peaks within this 2 month period as well as a considerableautumn flood episode appeared to lower rather than to raise the dissolved metal concentrations.Consequently the dissolved fractions of Zn, Cd and Al showed a significant negative correlationwith river discharge, and were low at the discharge peaks. Possibly high sediment concentrationsoccurring at high flood conditions more than counteracted desorption induced by pHdecrease, and led to decreased dissolved fractions through adsorption. Cu speciationon the other hand seemed to be more closely linked to pH. Alkalinity and Ca concentration,both assumed to protect aquatic life from metal pollution, were significantly lowerduring episodes with high Cu and Al total concentrations.  相似文献   
74.
A comparative analysis has been performed of the channel-base current and light waveforms for four rocket-triggered lightning strokes. It has been found that the current and light signals at the bottom of the channel exhibit a linear relationship (direct proportionality) in their rising portions. However, just after the peaks the linearity disappears, and the light signals usually decrease faster than the currents during the next several microseconds. Later, this trend is reversed and in some cases the light signals show another rising trend, even when the currents continue to decrease. The linear light/current relationship for the rising portions of the waveforms appears to be the same for different strokes. The findings support the idea of evaluating the variation of return stroke current along the lightning return stroke channel using light signals, provided that evaluation is limited to the rising portions of those signals and assuming that the light/current relationship observed at the bottom of the channel holds at other heights.  相似文献   
75.
The Tianjiazhen reach of the middle Yangtze is about 8 km long, and characterized by a narrow river width of 650 m and local water depth of > 90 m in deep inner troughs, of which about 60 m is below the mean sea level. The troughs in the channel of such a large river are associated with regional tectonics and local lithology. The channel configuration plays a critical role in modifying the height and duration of river floods and erosion of the riverbed. The formation of the troughs in the bed of the Yangtze is considered to be controlled by sets of NW–SE-oriented neotectonic fault zones, in which some segments consist of highly folded thick Triassic limestone crossed by the Yangtze River. Several limestone hills, currently located next to the river channel, serve as nodes that create large vortices in the river, thereby accelerating downcutting on the riverbed composed of limestone highly susceptible to physical corrosion and chemical dissolution. Hydrological records indicate that the nodal hills and channel configuration at Tianjiazhen do not impact on normal flow discharges but discharges > 50,000 m3s− 1 are slowed down for 2–3 days. Catastrophic floods are held up for even longer periods. These inevitably result in elevated flood stages upstream of prolonged duration, affecting large cities such as Wuhan and a very large number of people.  相似文献   
76.
程先云  刘洪禄  郑凡东 《水文》2007,27(6):42-45
引入水箱模型进行城市地下排水设施降雨一侵入水的模拟,探讨了初期蓄流值对模拟结果的影响并提出了相应的解决办法;由于模型参数多、非线性,参数的率定采用通用优化分析计算平台PowerFit,并获得了满意的结果,表明:①水箱模型适用于地下排水设施雨洪模拟和预测,可为市政规划设计和城市灾害预报提供可靠依据;②PowerFit全局优化能力强、简单易用,可广泛应用于水利水电等工程领域中的优化计算。  相似文献   
77.
长江口九段沙下段冲淤演变水动力机制分析   总被引:5,自引:0,他引:5       下载免费PDF全文
概述了长江口深水航道整治一期工程及工程对九段沙下段地形冲淤的影响.根据已建立的σ坐标系下三维非线性水流数学模型,用新测水文资料对模型进行验证.利用所建立的模型,结合由现场测量得到一期工程前后九段沙下段近期地形演变,数值模拟了北槽区域流通量、底层欧拉余流和北槽中下段平面水流特征,以综合分析北槽水域水动力变化对九段沙下段地形冲淤变化的影响.  相似文献   
78.
Impacts on water resources caused by human activity, natural climate variation and long-term climate change are unclear in the US Great Lakes region. Improved understanding of the impact of atmospheric circulation on stream discharge variability into the Lakes is thus important. In this analysis, monthly surface and mid-tropospheric circulation patterns suggest that surface pressure variations over Missouri and Illinois are most strongly correlated to discharge. The mid-tropospheric patterns most directly related to discharge place the Great Lakes in a trough-to-ridge flow pattern. The analysis confirms that at this scale, lee shore advection resulting in ‘lake-effect’ precipitation is not very important to regional discharge, and neither are variations in the Pacific–North American teleconnection.  相似文献   
79.
贵州绝大多数煤矿井是以岩溶水充水为主,矿井排水量与大气降水密切,地面塌陷与淹井事故也屡见不鲜,因此矿井涌水量预测是个非常复杂的问题,作者根据在本地工作的多年工作经验,介绍了一种适用的简易的矿井涌水量与突水量计算方法。  相似文献   
80.
1 mTRonvcnox: moareS Aun CoxcmSAJluvial rivers have the pOtenhal to adjust their shaPe and dimensions to all flows that tranSPOrtsediment, but Inglis (l94l) suggested that, for rivers that are in regime, a single steady flow could beidenhfied which would Produce the same bankfll dimensions as the natural sequence of events. Hereferrd to this now as the dondnan discharge.Wolman and Mller (l960) idenhfied that the flow doing most bed material transPort over a period ofyears may be taken tO…  相似文献   
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