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一个片流过程控制的冲积扇——太原盆地风峪沟冲积扇 被引量:16
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作者 李新坡 莫多闻 +2 位作者 朱忠礼 马元旭 刘运明 《北京大学学报(自然科学版)》 EI CAS CSCD 北大核心 2007年第4期560-566,共7页
风峪沟冲积扇位于太原盆地西北侧,面积较大,平面形态十分开阔。野外考察表明,在该冲积扇顶部出露了典型的、具平行层理结构的沉积物剖面。说明该冲积扇主要由高流态的片流过程形成的。片流沉积物由厚度小、侧向延伸长的中、细砾石坝沉... 风峪沟冲积扇位于太原盆地西北侧,面积较大,平面形态十分开阔。野外考察表明,在该冲积扇顶部出露了典型的、具平行层理结构的沉积物剖面。说明该冲积扇主要由高流态的片流过程形成的。片流沉积物由厚度小、侧向延伸长的中、细砾石坝沉积物和相对粒度较细的坝间沉积物所组成。风峪沟冲积扇流域的地质地貌特征表明,由于该段吕梁山地较大幅度的抬升给冲积扇的发育提供了充分的可容空间,这可能是风峪沟冲积扇上片流沉积物发育的主要原因。 展开更多
关键词 冲积扇 片流沉积 太原盆地
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冲积扇背景下的砂体沉积类型及优势储集砂体 被引量:2
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作者 孟祥超 李小华 +1 位作者 施强 杨西娟 《大庆石油地质与开发》 CAS CSCD 北大核心 2009年第3期19-22,共4页
依据测井、岩心资料,对准噶尔盆地西北缘乌尔禾油田百口泉组进行了砂体沉积类型划分。在冲积扇相-扇中、扇缘亚相背景下,研究区沉积物类型主要为筛状沉积、辫状河道沉积、片流沉积、泥石流沉积4种。辫状河道沉积呈明显的正韵律,具板... 依据测井、岩心资料,对准噶尔盆地西北缘乌尔禾油田百口泉组进行了砂体沉积类型划分。在冲积扇相-扇中、扇缘亚相背景下,研究区沉积物类型主要为筛状沉积、辫状河道沉积、片流沉积、泥石流沉积4种。辫状河道沉积呈明显的正韵律,具板状、槽状交错层理,富含油;筛状沉积呈微弱的反韵律,层理构造不发育,多为块状构造,含油级别较辫状河道低。在此认识基础上,明确了乌尔禾油田百口泉组地层储集砂体厚度分布特征,对优势储集砂体通过实例剖面进行了量化认定,最终确定优势储集砂体类型,优势储层为辫状河道砂体,筛状沉积为次要储层,泥石流沉积仅局部发育在东部WU7井一带,未见油气显示。在此优势储集砂体分布规律指导下部署钻探的13口评价井均在T1b^2、T1b^3段见到了良好的油气显示,有效指导了油田现场勘探开发。 展开更多
关键词 筛状沉积 辫状河道沉积 片流沉积 泥石沉积
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Effects of submerged sheet pile vanes on mobile river beds
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作者 Maria Antonietta BONIFORTI Roberto GUERCIO Roberto MAGINI 《Journal of Zhejiang University-Science A(Applied Physics & Engineering)》 SCIE EI CAS CSCD 2015年第3期182-193,共12页
Submerged vanes are low-height flow-training structures emerging from the riverbed with a suitable angle of attack to the incoming flow. These structures redirect the stream flow and modify erosion and depositional ra... Submerged vanes are low-height flow-training structures emerging from the riverbed with a suitable angle of attack to the incoming flow. These structures redirect the stream flow and modify erosion and depositional rates in the bottom and in the banks of a river as a result of the secondary currents generated by their installation. For this reason they have many applica- tions in river hydraulics for controlling river bed morphology. An experimental investigation is carried out to compare the effi- ciency of sheet-piling vanes versus thin plane ones in controlling sediment redistribution in the channel bed. In particular, exper- imental tests were carried out within a straight water channel, in conditions of bed load motion. The morphology of the river bed both in the area close to the structure and in the far field was examined at different angles of attack of the vane to the incoming flow and at different values of the submergence parameter, which is the ratio between the height of the water above the structure and the water level. The experimental results show that both the shape of the vanes as well as the angle of attack affect their per- formance in terms of the effects on the bed morphology, especially for greater submergence parameters. Specifically, plane and sheet-piling vanes produce comparable remodelings of the channel bed in the downstream region, but when the attack angle is increased, the thin plane vane causes deeper scour holes close to the structure. This last effect is probably due to the increased erosive capacity of the horseshoe vortex associated with the plane vane, while the uneven surface of the sheet-piling vane miti- gates the erosive strength of that vortex. 展开更多
关键词 Vanes SEDIMENT SCOUR River hydraulics Experimental hydraulics
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