1) turbidity current
浊流
1.
The sediment field can be judged the turbidity current s origin based on its related characters,regional distribution and material composition,which initiated at 1.
2Ma左右转移至台湾南部,造成台湾南部的物理剥蚀、乃至向毗邻深水的碎屑供应急剧增加,改变了深水沉积动力学状态,浊流活动的强度和频率极大加强,从而开始了该波域的起动和发育。
2.
The part can be divided into five types: debris flow, grain flow,fluidify sediment flows,turbidity current and slump.
这个连续部分可以分为五类:泥石流、颗粒流、流体化沉积物流、浊流和滑塌。
3.
The analysis result suggests that there are different geo-hazard factors during different periods of development of the Yellow River delta:(1)In the present estuarine area,the submergence of the high silt concentration forms the unique phenomenon of turbidity current in the Yellow River mouth.
利用浅地层剖面、旁扫声纳剖面及测深资料对现代黄河水下三角洲的地质灾害现象进行了研究,发现三角洲不同的形成时期对应发育不同的地质灾害现象:①在现行河口地区,高浓度泥沙下潜海底形成了黄河口独特的浊流现象,河口泥沙的快速堆积和欠固结导致河口三角洲叶瓣以台阶状滑塌陡坎的形式向海尖灭;②由于河口物源断绝和受到冬季北风或偏北风作用,海底滑坡、冲蚀构造等大型地质灾害现象在老河口废弃三角洲叶瓣北侧大量发育;③埕北地区与孤东地区情况较为相似,经过长时间改造之后多种灾害地质现象大量分布,且在水深5~10 m的三角洲陡坡上最为发育。
2) turbidity currents
浊流
1.
Experimental study on the incipient plunging point of stratified flow of turbidity currents and debris flows;
浊流和泥石流的异重流初期潜入点的实验研究
3) turbid flow
浊流;乱流
4) separate discharge of clear wastewater and turbid wastewater
清浊分流
1.
The method of separate discharge of clear wastewater and turbid wastewater, which meant anaerobic treatment(UASB) and catalytic oxydation secondary biochemical treatment were practiced on high concentration organic wastewater, could result in wastewater discharge at national standard with lower expenditure and easier operation.
结合啤酒企业的实际情况 ,对啤酒工业废水的治理现状进行探讨 ,提出一条合理的治理途径 ,即实行“清浊分流” ,对高浓度有机废水进行厌氧(UASB) +接触氧化二级生化处理 ,可实现啤酒废水的达标排放 ,且费用低 ,操作管理方便。
5) turbidite deposit
浊流沉积
1.
By applying OBMI imaging logging technique to a sedimentary study in Block S,the stratigraphic occurence,the provenance direction and the water energy are determined,and it is concluded that the regional sedimentary system mainly consist of deep-water mudstones and turbidite deposits with various sizes.
利用OBMI成像测井技术在S区块开展了沉积研究,确定了地层产状、物源方向及水体能量大小,明确了区域沉积体系主要为深水泥岩沉积及不同规模的浊流沉积;结合弹性波反演砂体平面分布及连井剖面对比,分析了A构造浊流沉积水道物源供给的方向及所形成的朵叶复合体展布特征,为该区有利目标评价提供了依据。
6) turbidity deposit
浊流沉积
1.
64 Bouma sequences of the turbidity deposit are divided within the whole thickness of 20 meters along the eastern margin.
在露头剖面上连续发育的厚约２０ｍ的浊流沉积可划分为６４个鲍玛层序，既广泛发育有代表浊流沉积特征的递交砂和多种底痕构造，又有Ｔａ—Ｔｅ都发育的典型层序，在层序组合上呈周期性变化。
补充资料：浊流
①浑浊的水流。比喻品格卑污的人。②一种含有大量泥、砂的高密度底流。密度比周围的水体(清水)大，能靠自重的作用在水下沿一定的坡度向下流动。可发育于水库、湖泊和海洋中。强烈的地震、构造运动或海啸等原因能形成海洋中的浊流。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条