伊拉克巴士拉南部Khor Al-Zubair港区Khor Al-Zubair海峡西岸海岸土工性质分析

W. Muttashar
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引用次数: 4

摘要

2009年7月,巴士拉国家建设中心与海洋科学中心/巴士拉大学合作,在Khor Al-Zubair海峡西岸钻了五个海上井眼,以及三个陆上井眼。已使用螺旋钻式钻孔机进行钻孔。在0.5米至2.0米的深度或地层发生变化的地方,以适当的间隔采集有代表性的土壤样本。陆上钻孔深度为距离自然地表19.0 ~ 20.5 m,而海上钻孔深度为距离地层7 ~ 16 m。钻探深度达到基岩,基岩足够坚硬,需要超过50次的n值打击。每2m深度进行标准侵彻试验(SPT)。测定了这些土壤的粒度分析、含水率和阿特伯格极限。结果表明,Khor Al-Zubair航道的海岸主要由两层组成。一种是浅粉质粘土或肥粘土,其厚度为18 m,由极软- m -硬逐渐转变为硬-v。它属于Hammar矿床。二是粉砂层,砂质土有两种类型,即:(1)外借来的回填层,为表层压实土,厚度为2.0 m;(2)井内和岸上的灰色硬粉质粘土与硬棕色粉质粘土之间的相互作用透镜层,属于底底坝组。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Some geotechnical soil properties of western bank of Khor Al-Zubair channel coast at Khor Al-Zubair Port location, southern Basrah, Iraq
Five Offshore Boreholes have been drilled by the National Construction Center at Basrah with cooperation the Marine Science Center/Basrah University, together with three Onshore Boreholes at the western bank of Khor Al-Zubair channel during July 2009. The drilling machine of Auger type has been used for drilling. Representative soil samples were taken at appropriate intervals ranged between 0.5 and 2.0 meters depth or where the stratum has been changed. Onshore boring depths ranged from 19.0 – 20.5 m, from natural ground surface, while, the offshore borings were from 7-16 m from the bed level. The depths of drilling reached the bedrock which is hard enough to require N-value of more than 50 blows. Standard Penetration Test (SPT) has been carried out for each 2m depths. Grain size analysis, moisture content, Atterberg limits of these soils were also determined.  The results show that there are two main strata making up the coast bank of the navigational channel of Khor Al-Zubair. First is Marly silty Clay or fat clay soil which has of a thickness18 m, and gradually changes from very soft- m.stiff to stiff-v.stiff which belongs to the Hammar deposits. The second is Silty Sand layer which has two types of sandy soil, these are: (1) borrowed Back filled layer as surficial compaction soil with of a thickness 2.0 m, and (2) are interacted lenses stratum between the gray stiff silty clay and the hard brown silty clay in the near and onshore Boreholes which belongs to the Dibdiba formation.    
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