英文原文Quarterly Journal of Engineering Geology and Hydrogeology-1986-Discussion-209-14[1]

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the descriptions of sabkhas referred to by Fookes et al. (1985). The area of the Industrial Complex, approximately 150 km 2, part of Jubail Industrial City, is generally low lying and consists of a large area of sabkha extending to the south, with sand dunes, some of which rise to more than 30 m to the north and west, and bounded to the east by a raised sandy coastal strip. At some points on the coast, rock outcrops on the beach and there is a small rock outcrop south-west of the quarry north-west of the site. The general elevation of the sabkha is about 3.0 to 4.0 m RCD (Royal Commission Datum). The coastal strip elevation varies, but rises to about 5 to 6 m RCD. The base geology of the area is shown on U.S G.S Map 1-208A 1958 to a scale of 1:50,000. The near surface materials consist of young, poorly consolidated, but occasionally cemented deposits of Quaternary age composed of mobile or relatively stable vegetated dunes, coastal deposits and sabkha. The older Hadrukh formation described by Powers et al. (1966), underlies the whole area and occasional small outcrops are found at the surface. The dunes, which form the hills surrounding the sabkha embayments, consist of either fine sand or graded fine to medium sand with only a small silt content. Generally, the grains are composed of rounded fragments of quartz with minor amounts of other minerals. Some of the dunes contain part of the Hadrukh formation extending upwards to within a few metres of their top surfaces. Granular gypsum, halite and fragments of sea shells may be present in areas close to the sea or in the surface layers of the sabkha. The coastal deposits consist of a mixture of weakly cemented or loose dune sands and beach sands. A surface layer of limestone or cemented sand known as 'caprock' occurs in some places on top of these deposits with measurable unconfined compressive strength, in one case greater than 5 MN/m 2. Sabkha covers about 40% of the area of the Industrial Complex. It has been assumed in previous studies (Fookes et al. 1985) that sabkha areas have been formed by the infilling of sea embayments with sand and subsequent evaporation of saline water to produce ground conditions varying from loose, fine and medium sands, with or without lenses and crystals of gypsum, halite and other salts, to very soft gypsiferous muds. Hard layers composed entirely of salts or cemented sands are found within the surface layers and at depth. It was observed at Jubail during the summer months when evaporation is high, that the water table dropped by about 0.5-1 m; the surface layers then became hard
Quarterly Journal of Engineering Geology and Hydrogeology
Discussion on 'The influence of ground and groundwater geochemistry on construction in the middle east' by P. G. Fookes, W. J. French & S. M. M. Rice
Discussion
Discussion on 'The influence of ground and groundwater geochemistry on construction in the middle east' by P. G. Fookes, W. J. French & S. M. M. Rice (Q. J. eng. Geol. London, 18, 101-27). Dr A. N. JAMES and Mr A. L. LITTLE write: Dr Fookes and his co-authors are to be congratulated on a valuable and interesting paper which is similar to work in Saudi Arabia for which the writers of this present discussion were responsible during 1977 and 1978. The present writers were concerned with geotechnical aspects of certain structures being designed for the Royal Commission of Jubail and Yanbu, under whose authority the very large Jubail Industrial Complex was being constructed. Many of the structures were to be situated on the sabkha areas near Jubail and A1 abd Allahand on the Arabian penninsula some 25 km north of the sabkha A1 Riyas which has been briefly described by Johnson et al. (1973). The present authors had access to extensive investigations of the Jubail sabkha area made by a number of different organizations including: A1-Muhandis Nizar Kurdi, Arabian Engineering Bureau, Sir Alexander Gibb & Partners, Dames and Moore & Basil Geotechnics, Binnie & Partners, Consulting Engineering Office Soilmafco, Pacific Consultants Inc. and Saudi Fugro Ltd. Information available from these investigations was used during the design stages of a variety of large and small structures with different load bearing and settlement requirements. During the review stages of the project it became apparent that effects of artesian water were an important consideration for all the foundation designs. This aspect of foundation design and construction on sabkha has received very little attention previously although it is mentioned briefly by Owles and Bowman (1981). The artesian pressures and corresponding upward flows of water in the sabkha areas required special provisions for the design and construction of many of the structures. The purpose of this discussion is to draw attention to the presence of artesian conditions associated with sabkha as experienced at Jubail. It is intended to submit a fuller description of this work for future publication in the Quarterly Journal of Engineering Geology to demonstrate the effects that it can have on various types of foundations and to describe some of the ways in which these effects were overcome. The sabkha at Jubail would appear to belong to the continental type as described by Akili & Torrance (1981) because it contains no lagoon areas or clear evidence of algal mats. In other respects it is typical of