[1]魏康强,张元福,李 媛,等.利用水槽实验对不同流速下三角洲发育区别的探究[J].复杂油气藏,2017,(03):6.[doi:10.16181/j.cnki.fzyqc.2017.03.002]
 Wei Kangqiang,Zhang Yuanfu,Li Yuan,et al.Study on difference of delta development under different flow velocities by flume experiment[J].Complex Hydrocarbon Reservoirs,2017,(03):6.[doi:10.16181/j.cnki.fzyqc.2017.03.002]
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利用水槽实验对不同流速下三角洲发育区别的探究
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《复杂油气藏》[ISSN:1674-4667/CN:31-2019/TQ]

卷:
期数:
2017年03期
页码:
6
栏目:
油气勘探
出版日期:
2017-09-25

文章信息/Info

Title:
Study on difference of delta development under different flow velocities by flume experiment
作者:
魏康强张元福李 媛王 振白一鸣张博文
中国地质大学(北京)能源学院,北京 100083
Author(s):
Wei KangqiangZhang Yuanfu Li Yuan Wang Zhen Bai Yiming Zhang Bowen
School of Energy Resources,China University of Geosciences(Beijing), Beijing 100083, China
关键词:
水槽实验 流速 三角洲发育 分流河道 朵叶体
Keywords:
flume experiment flow velocity delta development distributary channel lobe
分类号:
P512.2
DOI:
10.16181/j.cnki.fzyqc.2017.03.002
文献标志码:
A
摘要:
实验借助自制的小型水槽,探究了中等流速和高流速下三角洲发育的区别,结果表明:流速对于三角洲发育的影响主要体现在时间和规模上。不同流速下的发育过程均可划分为高建设期和低建设期。中等流速下三角洲在低建设期横向发育和斜向发育交替进行,而高流速下三角洲在低建设期先横向发育再斜向发育,并且高流速下三角洲砂体发育的时间较长。对于河道和朵叶体来说,中等流速下两者的数量要比高流速下两者的数量多。同一种流速下,不同位置的河道和朵叶体的规模存在区别,一般来说,发育在正前方的河道和朵叶体规模比两侧的规模大,但数量比两侧的要少。
Abstract:
With the aid of a small homemade tank, it was carried out study on the differences of delta development at moderate and high flow rates. The experimental results showed that the influence of flow velocity on delta development is mainly reflected in time and scale. The developmental processes under different flow rates can be divided into high and low construction periods. At medium flow velocity, the delta was alternately developed on the transverse and the acclivous direction during low construction period. However, at high flow velocity, the delta was developed transversely and then obliquely during the same period, with a longer time of delta sand body development. For the channel and the leaf body, the number at moderate flow velocity is more than that at high flow velocity. At the same flow velocity, the scale of the channels and lobes is various at different position. Generally speaking, the channels and lobes in front are larger on scale, but smaller in number.

参考文献/References:

[1] 李敏,朱红涛,郭巧珍,等.沉积物理模拟技术进展及发展趋势[J].地质科技情报,2010,29(4):137-142.
[2] 曹耀华,赖志云,刘怀波,等.沉积模拟实验的历史现状及发展趋势[J].沉积学报,1990,8(1):143-147.
[3] 姜在兴.沉积学[M].北京:石油工业出版社,2009:186-187.
[4] 焦朝维,张元福,王倩茹,等.对湖平面下降的定量计算的水槽实验[J].科学技术与工程,2016,16(34):22-27.
[5] 王俊辉,姜在兴,张元福,等.三角洲沉积的物理模拟[J].石油与天然气地质,2013,34(6):758-764.
[6] 刘飞,张小峰,任实,等.窄浅水域三角洲堆积体形成规律的试验研究[J].水力发电学报,2014,33(2):138-139.
[7] 韩鹏,倪晋仁,李天宏.细沟发育过程中的溯源侵蚀与沟壁崩塌[J].应用基础与工程科学学报,2002,10(2):115-125.
[8] 刘忠保,施冬,谢锐杰.三角洲分流河道形成及演变模拟研究[J].矿物岩石,2000,20(3):53-58.
[9] Seybold HJ, Molnar p,Akca D,et al. Topography of inland deltas: Observations, modeling, and experiments[J]. Geophysical Resarch Letters,2010,37(8):1-5.
[10] Tesi T, Miserocchi S, Goi M A,et al. Influence of distributary channels on sediment and organic carbon supply in event-dominated coastal margins: the Po prodelta as a study case[J]. Biogeosciences Discussions,2011,81(8):7849-7902.
[11] 李明涛,于兴河,李顺利,等.环境敏感粒度组分在识别三角洲朵叶期次中的应用[J].中南大学学报(自然科学版),2014,45(11):3853-3865.

备注/Memo

备注/Memo:
收稿日期:2017-04-27; 改回日期:2017-06-02。 作者简介:魏康强(199—),硕士在读,主要从事沉积学与岩相古地理研究。E-mail:475635355@qq.com。 基金项目:受国家重大科技专项(2011ZX05009-002)资助。
更新日期/Last Update: 2017-09-25