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黄河中游水沙频率关系研究 被引量:6
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作者 金鑫 郝振纯 张金良 《泥沙研究》 CSCD 北大核心 2006年第3期6-13,共8页
扼要指出进行黄河中游水沙频率关系研究的必要性,并通过对黄河中游部分连续泥沙观测序列的独立同分布性的检验,验证了建立黄河中游泥沙频率曲线的可行性以及泥沙序列对P-Ⅲ型分布曲线的适应性。在此基础上建立了黄河中游水沙序列的理论... 扼要指出进行黄河中游水沙频率关系研究的必要性,并通过对黄河中游部分连续泥沙观测序列的独立同分布性的检验,验证了建立黄河中游泥沙频率曲线的可行性以及泥沙序列对P-Ⅲ型分布曲线的适应性。在此基础上建立了黄河中游水沙序列的理论频率曲线,分析了黄河中游的水沙频率之间的关系,给出了一定泥沙频率条件下所对应的洪水发生的频率范围,对年径流量和输沙量的频率组合进行了量化,对水沙丰枯组合进行了确定,最后提出了有待于进一步研究的问题。 展开更多
关键词 黄河中游 水沙频率关系 泥沙频率曲线
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松辽流域主要河流水沙规律分析 被引量:2
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作者 林沫 刘颖 +2 位作者 丛远飞 王宇轩 张羽 《东北水利水电》 2009年第12期40-42,共3页
本文基于统计理论的概念,从建立泥沙频率分布曲线入手,分析了松辽流域主要河流(松花江、辽河)水沙频率之间的关系。定量界定了水沙丰平枯组合类型,将年径流量和输沙量分别划分为丰、平、枯(大、中、少)3个等级,以频率作为实测年径流量... 本文基于统计理论的概念,从建立泥沙频率分布曲线入手,分析了松辽流域主要河流(松花江、辽河)水沙频率之间的关系。定量界定了水沙丰平枯组合类型,将年径流量和输沙量分别划分为丰、平、枯(大、中、少)3个等级,以频率作为实测年径流量和输沙量丰、平、枯(大、中、少)划分的标准,结合泥沙频率研究成果,对松辽流域主要河流的水沙分布规律进行了探讨,为进一步研究松辽流域人为活动对河流泥沙、水土流失问题的影响创造了条件。 展开更多
关键词 松辽流域 泥沙频率 水沙关系 分布 规律
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Grain-size Characteristics of Sediment in Daniugou Peatland in Changbai Mountains,Northeast China:Implications for Atmospheric Dust Deposition 被引量:5
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作者 BAO Kunshan JIA Lin +1 位作者 LU Xianguo WANG Guoping 《Chinese Geographical Science》 SCIE CSCD 2010年第6期498-505,共8页
The grain-size distribution characteristics and grain-size parameters of sediment in two vertical sections of Daniugou peatland in the Changbai Mountains were systematically investigated.A comparative analysis of the ... The grain-size distribution characteristics and grain-size parameters of sediment in two vertical sections of Daniugou peatland in the Changbai Mountains were systematically investigated.A comparative analysis of the sediment granularity using a discriminative function with Hongyuan peat,red clay,loess-paleosol,fluvial deposit as well as lacustrine deposit was also conducted.It turns out that the vertical section of Daniugou peat ash is primarily constituted by clay and silt particles,and the content of sand is relatively small.Grain-size frequency curves generally show a single-peak modality while a bimodal pattern is detected in the upper layer.The grain-size component and peak pattern of grain-size frequency curves also illustrate that peat ash materials were transported to the peatland by long-range aeolian dust during the deposition process,while there existed short-distance dust influence in peat deposition of the upper layer.Comparisons of grain-size parameters and the discriminative Y-value of Daniugou peat ash with those of typical aeolian sediments show close similarities,suggesting the possibility that atmospheric dust transport processes were involved in the accumulation of peat again.Moreover,the variations of grain-size distribution suggest the local environmental deterioration which is just the driving force of local dust elevation.Grain-size analysis of peatland sediment is demonstrated to be one effective method to extract information about regional and global environmental evolution,and more attention should be paid to current local ecological environment and to seeking a balance between economic development and environmental protection in Northeast China. 展开更多
关键词 GRAIN-SIZE PEATLAND aeolian sediment atmospheric dust deposition Changbai Mountains
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Characteristics of vibration liquefaction of saturated medium sandy soil with silt
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作者 HUANG Rui ZHANG Yanjun GONG Liliang 《Global Geology》 2010年第2期90-93,共4页
In order to understand and master the dynamic characteristics of sandy soil with different silt contents, the authors carried out many indoor dynamic triaxial tests for five groups of sandy with silt which took from P... In order to understand and master the dynamic characteristics of sandy soil with different silt contents, the authors carried out many indoor dynamic triaxial tests for five groups of sandy with silt which took from Panjin and Xiamen. Under the conditions of consolidation pressure of 100 kPa, 200 kPa, 300 kPa, stationary vibration frequency H=1 and cyclic loading, the authors found that the effective cohesion increases and the effective internal friction angle decreases with the increase of the silt contents. During the liquefied scope, the cementation and the strength have been increased with the increase of the silt contents. 展开更多
关键词 sandy soil dynamic characteristics vibration liquefaction
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