共查询到20条相似文献，搜索用时 31 毫秒
1.
Karst Hazard Assessment of Eastern Saudi Arabia 总被引：1，自引：0，他引：1
Karst phenomena exist in areas in the eastern part of Saudi Arabia, forming solution features such as sinkholes, collapsed dolines and solution caverns, as a result of the chemical leaching of the carbonate and evaporite formations by percolating water. The instability of these karst phenomena could produce land subsidence problems. This paper reviews the geology of documented karstic rock units in Saudi Arabia and proposes a simple engineering classification of the solution features characteristic of limestone. Two case histories in the Dhahran area, eastern Saudi Arabia, will be used as examples for the application of a modified engineering classification. 相似文献
2.
Sami S. A. Al-Amiri Ph.D. 《GeoJournal》1986,13(2):143-151
The landform of Saudi Arabia in general and the Riyadh area in particular have their own potentiality for scenic and recreational purposes. The higher lands or features which have well cemented material in some areas of Riyadh have been recommended for scenic use, while lower lands like wide natural lakes, sand dunes and others can be mostly used for recreational purposes. Such features and purposes found here may be extrapolated into other similar areas within Saudi Arabia and may be compared with other areas elsewhere in the world. 相似文献
3.
Overview of some geological hazards in the Saudi Arabia 总被引：2，自引：1，他引：1
The Saudi Arabia has harsh environmental conditions which enhance some geomorphologic/geological processes more than in other areas. These processes create different geological hazards. The general physiography of the Saudi Arabia is characterized by the Red Sea coastal plains and the escarpment foothills called Tihama, followed by the Arabian Shield Mountains, the Arabian Shelf plateau and finally the Arabian Gulf coastal plains. These types of geological hazards can be categorized into sand accumulations, earth subsidence and fissures, flash floods, problematic soils, slope stability problems, and karst problems. The current study gives an overview of all these hazards with examples, as well as develops a geo-hazard map for the Saudi Arabia. Our findings indicate that the desert environment needs much concern and care. National and international agencies have to join together with other people to keep the system balanced and to reduce the resulting geological hazards. Also, remedial measures should be proposed to avoid and reduce these natural hazards. 相似文献
4.
A classification approach has been implemented in the present work by integrating traditional water sample analysis methods
and Geographic Information System (GIS) capabilities in order to classify zones with acceptable groundwater quality for drinking.
GIS extrapolation capabilities with their multi-conditional layering facilities were integrated together in order to assess
in the determination of areas suitable for drinking purposes. This technique was implemented in Wadi Rabigh, Western Saudi
Arabia, due to its significance as one of the most promising areas in the Western Province in the Kingdom of Saudi Arabia,
owing to the establishment of King Abdullah Commercial City and King Abdullah University for Science and Technology (KAUST)
nearby. Results show that only a limited area in the aquifer can be used for domestic purposes. This area is located in two
separate patches in the upstream part of the aquifer while most of the aquifer water is categorized as brackish which might
be used for agriculture purposes to a certain extent. The downstream area of the aquifer is very saline due to sea water intrusion
effect. 相似文献
5.
The occurrence of land subsidence in the Kingdom Saudi Arabia is either natural or man-made. Natural land subsidence occurs due to the development of subterranean voids by a solution of host rocks in carbonate and evaporite terrains, over many areas of Saudi Arabia. Man-induced land subsidence is either due to the removal of groundwater in the agricultural areas or to wetting of unstable soils. Therefore, earth fissures and a lowering of the ground surface in unconsolidated sediments took place in alluvial plains and volcanic vent terrains. Unstable soils include Sabkha soils and loess sediments. These types of soils occur in coastal plains, desert areas and volcanic terrains. When this soil is wetted either during agricultural activities, waste disposal or even during a rain storm, subsidence takes place due to either the removal of salts from the Sabkha soil or the rearrangement of soil particles in loess sediments. 相似文献
6.
Saad A. Aiban 《Engineering Geology》1995,39(3-4):203-215
The increasing number of construction projects and the lack of good quality soil for use in these projects in eastern Saudi Arabia necessitate the use of available marginal soils. Most, if not all, engineering projects use the fine-grained calcareous sediments, known locally as marl, either as a foundation material or as a fill material. The lack of published information on their engineering characteristics and behavior under ambient conditions has resulted in many construction and post-construction problems. This investigation is one of a series to evaluate the geotechnical properties of selected marl soils obtained from different areas in eastern Saudi Arabia. Marl samples, obtained from Abqaiq, were prepared in the laboratory under controlled conditions and subjected to different tests including CBR (soaked and unsoaked), triaxial compression, unconfined compression and one-dimensional compression tests. Samples were prepared at different moisture contents on both the wet and dry sides of optimum. X-ray diffraction analysis indicates that this marl contains high percentages of dolomite and calcite, in addition to other materials. The molding water content significantly affects the engineering properties of this material. Compaction on the dry side of optimum resulted in samples that have some swelling potential and highly compressible characteristics when subjected to a load after inundation. 相似文献
7.
The status of medical facilities and personnel in the Kingdom of Saudi Arabia, at the end of the fourth five-year plan (1985–1990)
was reviewed and analyzed regarding the standards of services and workload of health personnel for the different regions and
urban/rural areas in the Kingdom. Innovative indices for the quantitative analysis of medical facilities were developed. The
analysis of health facilities in Saudi Arabia shows that the Kingdom enjoys a high standard of medical facilities. However,
there are maldistribution of clinical resources and personnel between regions and between urban/rural areas. Utilization of
these indices for the reallocation of medical facilities and personnel to ensure even distribution of services for all inhabitants
of the Kingdom was illustrated. In addition, indices give a guideline for the future planning and the rate of increase of
these facilities that keeps the standard of medical services in the proper class desired with minimum resources wastage. 相似文献
8.
Mohammed Abdullah Al-Saleh Dr. 《GeoJournal》1991,24(4):421-426
Conclusion This study represents a step forward in understanding the geomorphology of Wadi Al-Khanagah basin, especially the relationship between depositional landforms and drainage basin morphometry. Besides it has drawn the attention to the importance of establishing the relationships between landforms for rapid applied hydrogeomorphological studies in areas lacking systematic data base. To conclude, the established relationships between alluvium thickness and stream order in Wadi Al-Khanagah basin would give an adequate mean of predicting thickness of wadi alluvium and consequently the capacity of potential alluvium aquifers in the shield area of the Al-Quwayiyah region, in Central Saudi Arabia. 相似文献
9.
Ahmed M. Youssef Hasan M. Al-Harbi Francisco Gutiérrez Yasser A. Zabramwi Ali B. Bulkhi Saeed A. Zahrani Alaa M. Bahamil Ahmed J. Zahrani Zaam A. Otaibi Bosy A. El-Haddad 《Hydrogeology Journal》2016,24(3):625-644
Approximately 60 % of the 2,150,000 km2 area of Saudi Arabia is underlain by soluble sediments (carbonate and evaporite rock formations, salt diapirs, sabkha deposits). Despite its hyper-arid climate, a wide variety of recent sinkholes have been reported in numerous areas, involving significant property losses. Human activities, most notably groundwater extraction, have induced unstable conditions on pre-existing cavities. This work provides an overview of the sinkhole hazard in Saudi Arabia, a scarcely explored topic. It identifies the main karst formations and the distribution of the most problematic sinkhole areas, illustrated through several case studies covering the wide spectrum of subsidence mechanisms. Some of the main investigation methods are presented through selected examples, including remote sensing, trenching and geophysics. Based on the available data, the main causal factors are identified and further actions that should be undertaken to better assess and manage the risk are discussed. 相似文献
10.
11.
During the Early Paleozoic, transgressions and the distribution of sedimentary facies on the northern Gondwana margin were controlled by a regional NNW-SSE to almost north-south striking structural relief. In Early Silurian times, a eustatic highstand enabled the sea to reach its maximum southward extent.The counterclockwise rotation of Gondwana during the Cambrian and Early Ordovician caused the northern Gondwana margin to shift from intertropical to southern polar latitudes in Ordovician times. Glacial and periglacial deposits are reported from many localities in Morocco, Algeria, Niger, Libya, Chad, Sudan, Jordan and Saudi Arabia. The Late Ordovician glaciation phase was followed by a period of a major glacioeustatic sea-level rise in the Early Silurian due to the retreat of the ice-cap. As a consequence of the decreasing water circulation in the basin centers (Central Arabia, Murzuk- and Ghadames basins), highly bituminous euxinic shales were deposited. These shales are considered to be the main source rock of Paleozoic oil and gas deposits in parts of Saudi Arabia, Libya and Algeria.The following regression in the southern parts of the Early Silurian sea was probably caused by a second glacial advance, which was mainly restricted to areas in Chad, Sudan and Niger. Evidence for glacial activity and fluvioglacial sedimentation is available from rocks overlying the basal Silurian shale in north-east Chad and north-west Sudan. The Early Silurian ice advance is considered to be responsible for the termination of euxinic shale deposition in the basin centers. 相似文献
12.
DAVID J. GRAINGER 《Geology Today》1992,8(6):215-219
Wadi Fatima, east of jiddah on the Red Sea coast of Saudi Arabia, is a microcosm of the geology of the jiddah area. Rocks ranging in age from 800-million-year-old metamorphic rocks to Tertiary lava flows are exposed, and illustrate the geological richness of western Saudi Arabia. The valley is a major south-west-trending fault zone that has been active since Precambrian times. A major Tertiary dyke swarm in the vicinity of Wadi Fatima is related to the opening of the Red Sea as the African-Arabian landmass split apart. 相似文献
13.
《Sedimentology》2018,65(3):851-876
The Sarah Formation is a glaciogenic sedimentary unit deposited along the Gondwana margin during the latest Ordovician ice age and represents a major hydrocarbon reservoir in northern Saudi Arabia. Large‐scale glacial palaeo‐valleys cut into the Qasim Formation and were infilled by the Sarah Formation. Post‐glacial transgression in the earliest Silurian resulted in the deposition of the Qusaiba Shale Member and associated organic‐rich basal source rocks, which cap the Sarah Formation infilled palaeo‐valleys. This unique setting makes the Sarah Formation an important emerging exploration target in Saudi Arabia. This study focuses on the facies and depositional architecture in seismic‐scale outcrops of the Sarah Formation in north‐western Saudi Arabia. The Rahal Dhab palaeo‐valley provides a 100 km long dip‐oriented cross‐section which has been covered by 24 vertical sections, sedimentary architectural analyses at metre to kilometre scale and by three cored shallow boreholes. In the Rahal Dhab palaeo‐valley, the Sarah Formation was deposited in a proglacial setting that ranged from marginal marine to offshore prodelta and is made up of three units: (i) the Sarah Sandstone; (ii) the Sarah Shale; and (iii) the Uqlah Member. This study shows the relationships between these three units and architectural controls on reservoir quality in this system. This paper contributes to the regional understanding of the Sarah Formation, and the new depositional model of the Rahal Dhab palaeo‐valley provides an outcrop‐reservoir analogue for hydrocarbon exploration in adjacent areas. 相似文献
14.
15.
Randolf Rausch Theo Simon Hussain Al Ajmi Heiko Dirks 《Arabian Journal of Geosciences》2014,7(6):2437-2450
In central Saudi Arabia, the combination of rock types and sedimentary bedding created a unique scarp landscape. The escarpments were formed during Late Miocene through Early Quaternary times. At present, cuesta formation and migration are restricted to the actual escarpments as a consequence of negligible sediment removal. The plains between the escarpments are sealed through periodically active fluvial processes and through eolian sedimentation. In this publication, the major escarpments of central Saudi Arabia are described. The interactions between tectonics, climate, and morphogenesis which created this unique landscape are reviewed. 相似文献
16.
Sand and dust storms are causing hazards and problems in aviation as well as the dangers and distresses they cause on living things. The low meteorological visibility, the presence of strong winds with gust, and the transport of dust and sand particles by the wind are dangerous on landing and departure of aircrafts, and even on planes that are parked. The main aim of the study is to examine the meteorological conditions causing the dust storm that took place in the Arabian Peninsula on February 28, 2009, and to determine the source of dust caused dust storm, sand storm, blown sand, and blown dust at the airports. Within the scope of the study, aviation routine weather report (METAR) and aviation selected special weather report (SPECI) reports have been assessed at many airports over Arabian Peninsula (AP), the northern part of the AP and North Africa. As model outputs; NCEP–DOE Reanalysis 2 data, BSC–DREAM8B, and HYSPLIT model were used. In the satellite images; METEOSAT MSG dust RGB images, MODIS, and Kalpana-1 data were used. According to obtained results, dust storms were detected in Bahrain, Kuwait, Saudi Arabia, and United Arab Emirates (UAE). At Al-Ahsa Airport in Saudi Arabia, the lowest visibility measured on February 28, 2009, dropping to 200 m, which was dominated by blowing sand. The source region of the dust observed at Dubai Airport in UAE is the eastern regions of the Rub’al Khali Desert located between Saudi Arabia, Oman, and UAE. 相似文献
17.
Q. Y. Tarawneh M. El Alfy 《International Journal of Environmental Science and Technology》2017,14(6):1267-1276
Saudi Arabia is a huge area with diverse climatic and topographical features. This diversity in climate is augmented by seasonal weather variations. The study discusses solar irradiance and sunshine duration in terms of seasonal weather systems. Sunshine duration and solar irradiance maps show that the East Mediterranean weather systems (such as Cyprus low) in winter affect the majority of the geographical regions in Saudi Arabia. In spring and autumn, Sudan low becomes more active than Cyprus low, especially in the west and central regions. Sunshine duration in April is 47% compared to 50% in January. Sunshine duration in the southwest region is affected by the rainy and wet summer monsoon which reduces sunshine duration to 33% in summer (July), while it is 43% in winter (January). In addition, the study uses the Angstrom equation to estimate solar irradiance. The absolute relative error between estimated and observed solar irradiance ranges between 2 and 10% in the majority of cases, with a few cases exceeding 13%. 相似文献
18.
A. S. El-Sharif Ph.D. 《GeoJournal》1986,13(2):119-127
A parametric crop yield model YIELD, which was developed by Prof. W. Terjung and his team at UCLA, was applied to calculate yield and water consumption for corn in Saudi Arabia. The model employs climatic and environmental data in order to simulate yield for several crops in different places all over the world. A network of 22 stations provided climatic data averaged over a period of 17 years (1967–1983). The nonclimatic data was derived from the FAO soil map of the world and the writer's personal experience. The main objectives of this paper are: [1] to determine suitable places and times for planting corn, under rainfed and irrigated conditions in Saudi Arabia; [2] to contrast irrigation water for corn in each province; and [3] to assess the potential yield for corn in the country in a year. This study concluded that highest yields of corn under fully-irrigated conditions (primary growing season) occurred in the mountainous region in SW Saudi Arabia (about 12,000 kg/ha, and more than 18,000 in Nimas) while lowest yields occurred in Tabuk and Al-Khawsh (about 4,000 kg/ha). Yields in most of the other stations were (5,000–8,000 kg/ha). Under rainfed conditions crop failed in all regions except in the SW region in which yields range between 2,000 kg/ha in Al-Khawsh and — 6,000 kg/ha as in Nimas. According to the findings of this study, the most suitable months for corn sowing in Saudi Arabia are December and January. 相似文献
19.
Ardiansyah Koeshidayatullah Khalid Al‐Ramadan Geraint Wyn Hughes 《Geological Journal》2016,51(5):704-721
The Al‐Jawf area of northern Saudi Arabia provides spectacular outcrops of Early Devonian carbonate bioherms in the Wadi Murayr and Dumat Al‐Jandal areas. These carbonate bioherms belong to the Qasr Member of the Late Pragian–Early Emsian Jauf Formation (~405 Ma) and are surrounded by a bioclastic carbonate succession. The Qasr Member is the first major carbonate unit of the Palaeozoic succession in Saudi Arabia that mainly consists of microbialite carbonates and metazoan reefs exhibiting distinct mound features. These bioherm complexes and their associated carbonate facies are pervasively dolomitized. Stratigraphic, petrographic and geochemical analyses were conducted to determine the facies distribution and interpret their depositional and diagenetic processes. A total of 11 facies are identified from a range of depositional environments within a carbonate platform system, ranging from tidal flats, lagoon, shoal, patch reefs to reef front. The main diagenetic processes are carbonate cementation and dolomitization. Dolomitization occurred as both fabric preserved (mostly in grain‐dominated facies) and fabric destructive (mud‐dominated facies). The microbialites and coralline sponges facies show poor reservoir with visual porosity less than 5%, but this succession may have a potential to serve as a good source for the underlying and overlying facies. Ooid and peloidal grainstone facies show fair to good visual porosity that locally exceeds 10% with intergranular porosity as the dominant type. However, in the most studied samples, vuggy and intraparticle porosities are observed as the dominant type. Copyright © 2015 John Wiley & Sons, Ltd. 相似文献
20.
Georg Glasze 《GeoJournal》2006,66(1-2):83-88
In discussions on the “fragmented city” and the boom of private and guarded neighbourhoods, several authors have stressed the importance of a growing differentiation of lifestyles and “cultural” orientations for this trend. The compounds for western foreigners in Saudi Arabia are explicitly based on the idea of a spatial seclusion of social groups with different “cultural” backgrounds. This study presents an overview of the development of these western enclaves. Narrative interviews with former expatriates provide insights into their daily life, their social relations within the compound, and to the Saudi Arabia behind the gates. 相似文献