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Relevant bibliographies by topics / Nile River Delta (Egypt)

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Academic literature on the topic 'Nile River Delta (Egypt)'

Author: Grafiati

Published: 28 February 2023

Last updated: 1 March 2023

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Journal articles on the topic "Nile River Delta (Egypt)"

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Saleh, Amgad A., Kurt A. Zeller, Abou-Serie M. Ismael, Zeinab M. Fahmy, Elhamy M. El-Assiuty, and John F. Leslie. "Amplified Fragment Length Polymorphism Diversity in Cephalosporium maydis from Egypt." Phytopathology® 93, no. 7 (July 2003): 853–59. http://dx.doi.org/10.1094/phyto.2003.93.7.853.

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Cephalosporium maydis, the causal agent of late wilt of maize, was first described in Egypt in the 1960s, where it can cause yield losses of up to 40% in susceptible plantings. We characterized 866 isolates of C. maydis collected from 14 governates in Egypt, 7 in the Nile River Delta and 7 in southern (Middle and Upper) Egypt, with amplified fragment length polymorphism (AFLP) markers. The four AFLP primer-pair combinations generated 68 bands, 25 of which were polymorphic, resulting in 52 clonal haplotypes that clustered the 866 isolates into four phylogenetic lineages. Three lineages were found in both the Nile River Delta and southern Egypt. Lineage IV, the most diverse group (20 haplotypes), was recovered only from governates in the Nile River Delta. In some locations, one lineage dominated (up to 98% of the isolates recovered) and, from some fields, only a single haplotype was recovered. Under field conditions in Egypt, there is no evidence that C. maydis reproduces sexually. The nonuniform geographic distribution of the pathogen lineages within the country could be due to differences in climate or in the farming system, because host material differs in susceptibility and C. maydis lineages differ in pathogenicity.

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Mabrouk, M. B., A. Jonoski, D. Solomatine, and S. Uhlenbrook. "A review of seawater intrusion in the Nile Delta groundwater system – the basis for assessing impacts due to climate changes and water resources development." Hydrology and Earth System Sciences Discussions 10, no. 8 (August 19, 2013): 10873–911. http://dx.doi.org/10.5194/hessd-10-10873-2013.

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Abstract. Serious environmental problems are emerging in the River Nile basin and its groundwater resources. Recent years have brought scientific evidence of climate change and development-induced environmental impacts globally as well as over Egypt. Some impacts are subtle, like decline of the Nile River water levels, others are dramatic like the salinization of all coastal land in the Nile Delta – the agricultural engine of Egypt. These consequences have become a striking reality causing a set of interconnected groundwater management problems. Massive population increase that overwhelmed the Nile Delta region has amplified the problem. Many researchers have studied these problems from different perspectives using different methodologies, following different objectives and, consequently, arrived at different findings. However, they all confirmed that significant groundwater salinization has affected the Nile Delta and this is likely to become worse rapidly in the future. This article presents, categorizes and critically analyses and synthesizes the most relevant research regarding climate change and development challenges in relation to groundwater resources in the Nile Delta. It is shown that there is a gap in studies that focus on sustainable groundwater resources development and environmentally sound protection as an integrated regional process in Nile Delta. Moreover, there is also a knowledge gap related to the deterioration of groundwater quality. The article recommends further research that covers the groundwater resources and salinization in the whole Nile Delta based on integrated three-dimensional groundwater modelling of the Nile delta aquifer.

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Mączyńska, Agnieszka. "The Nile Delta as a Center of Cultural Interaction Between Upper Egypt and the Southern Levant in the 4th Millennium BC." Studies in Ancient Art and Civilisation 18 (December 30, 2014): 25–45. http://dx.doi.org/10.12797/saac.18.2014.18.03.

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The societies occupying the Nile Delta in the 4th millennium BC were not cut off from the neighboring regions of Upper Egypt and the Southern Levant. The Nile River, which served as a transport route between southern and northern Egypt, and the geographical proximity of the Southern Levant to the Nile Delta were probably both factors that allowed contact to occur between the regions. Whilst a significant number of Southern Levantine and Upper Egyptian imports have been found at Lower Egyptian cultural sites, the quantity of Lower Egyptian items from the same period found in the Southern Levant and in southern Egypt is more limited. This state of affairs did not occur by chance, which suggests that the scarcity of northern Egyptian finds outside Lower Egypt can probably be attributed to the nature of trade and the position of the Nile Delta in this period.Although our knowledge of the contact of the Delta with Upper Egypt and the Southern Levant is constantly expanding, many issues still remain unclear, including that of trading patterns. Archeological research currently being conducted in northern Egypt (mainly at Tell el-Farkha, Tell el-Iswid, Sais and Buto) has provided us with new material that adds to our understanding of the field. From the most recent excavation results, it would appear that from the very beginnings of its existence, the Tell el-Farkha site in the eastern Delta was as an important exchange center where the influence of the east and the south came together.The aim of this paper is to portray the interaction occurring between the Delta, Upper Egypt and the Southern Levant in the 4th millennium BC on the basis of material found at the excavation site of Tell el-Farkha in the eastern Nile Delta and to explain the role of the Nile Delta in political and cultural relations between these regions.

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Proussakov, Dmitry. "From the delta to the Delta: Natural Conditions and Settlers on the Main Nile in the Fifth Millennium BC. Part II." Oriental Courier, no. 3 (2022): 66. http://dx.doi.org/10.18254/s268684310023759-2.

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The primordial neolithization on the banks of the Nile River is associated with the archaeological culture of the Early Khartoum, or Khartoum Mesolithic. The bulk of its monuments date back to the 7th–6th millennia BC and is located on a long stretch of the river valley from the Gezira at the confluence of the White and Blue Nile to the 2nd cataract of the Main Nile at the current border of Sudan and Egypt. Khartoum Mesolithic shows a tendency of enlarging its sites southwards probably connected with a progress of settled way of life of the early Neolithic population of this stretch approaching to the Gezira. The latter at that time was dissected by the paleochannels of the inner Blue Nile delta that discharged into the White Nile and was a swampy fertile alluvial plain, very similar to the Egyptian Delta that was formed two or three millennia later. Favorable climatic conditions of the African Humid Period (about 14.8 — 5.5 cal. yr BP) did not favor the mass migration of the inhabitants of the blooming Sahara to the Nile, as evidenced by numerous sites of the Saharo-Sudanese Neolithic in the Western Desert. According to recent paleoclimatic reconstruction by S. Kröpelin, a large-scale demographic shift from the Desert to the River, caused by abrupt desiccation of the North Africa and resulted in the epoch-making progress of the Neolithic communities on the Nile, including Egypt, took place starting from 5300 BC. This model, however, contradicts the available scientifical data and has no archaeological confirmation. An absolute majority of studies at the junction of archeology and paleoecology show that cooling and aridization that could have caused a mass migration of people from the Sahara to the banks of the Nile, developed only with the completion of the Holocene Atlantic optimum and, in general, the African Humid Period in the 4th millennium BC having reached the extremum at about 4500 uncal. yr BP ≈ 3221 BC. All earlier manifestations of neolithization on the Nile from the natural point of view should be obviously explained primarily by the attractiveness for people of the Nile Valley itself or of its individual parts and basins, such as the delta of the Gezira.

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Dessouki, Sami, Mohamed Deyab, and Jelan Mofeed. "PHYCOLOGICAL ASSESSMENT OF WATER QUALITY OF RIVER NILE DELTA - EGYPT." Egyptian Journal of Phycology 5, no. 1 (December 28, 2004): 19–34. http://dx.doi.org/10.21608/egyjs.2004.113980.

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Ullmann, Tobias, Leon Nill, Robert Schiestl, Julian Trappe, Eva Lange-Athinodorou, Roland Baumhauer, and Julia Meister. "Mapping buried paleogeographical features of the Nile Delta (Egypt) using the Landsat archive." E&G Quaternary Science Journal 69, no. 2 (December 9, 2020): 225–45. http://dx.doi.org/10.5194/egqsj-69-225-2020.

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Abstract. The contribution highlights the use of Landsat spectral-temporal metrics (STMs) for the detection of surface anomalies that are potentially related to buried near-surface paleogeomorphological deposits in the Nile Delta (Egypt), in particular for a buried river branch close to Buto. The processing was completed in the Google Earth Engine (GEE) for the entire Nile Delta and for selected seasons of the year (summer/winter) using Landsat data from 1985 to 2019. We derived the STMs of the tasseled cap transformation (TC), the Normalized Difference Wetness Index (NDWI), and the Normalized Difference Vegetation Index (NDVI). These features were compared to historical topographic maps of the Survey of Egypt, CORONA imagery, the digital elevation model of the TanDEM-X mission, and modern high-resolution satellite imagery. The results suggest that the extent of channels is best revealed when differencing the median NDWI between summer (July/August) and winter (January/February) seasons (ΔNDWI). The observed difference is likely due to lower soil/plant moisture during summer, which is potentially caused by coarser-grained deposits and the morphology of the former levee. Similar anomalies were found in the immediate surroundings of several Pleistocene sand hills (“geziras”) and settlement mounds (“tells”) of the eastern delta, which allowed some mapping of the potential near-surface continuation. Such anomalies were not observed for the surroundings of tells of the western Nile Delta. Additional linear and meandering ΔNDWI anomalies were found in the eastern Nile Delta in the immediate surroundings of the ancient site of Bubastis (Tell Basta), as well as several kilometers north of Zagazig. These anomalies might indicate former courses of Nile river branches. However, the ΔNDWI does not provide an unambiguous delineation.

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Mahrous, Mohamed Alsaid, Ali Radwan, Tharwat Abd El-Hafez, Salah Mahmoud, Mahmoud Gomaa, and Mahmoud Zayed. "The Current State of Deformation Parameters in the Nile Delta, Egypt, Using GNSS and Seismological Data." Iraqi Geological Journal 55, no. 2A (July 31, 2022): 19–28. http://dx.doi.org/10.46717/igj.55.2a.2ms-2022-07-18.

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Nile Delta region in northern Egypt and the Nile River separates it into two branches in the west, at Rosetta, and in the east, at Damietta, before draining into the Mediterranean Sea. Nile Delta is the most valuable commercial, agricultural, and industrial supply as well as over 70% of the country’s industrial and economic operations. More than half of Egypt 100 million population live there. Due to the vital value of the Nile Delta, the crustal deformation study in the Nile Delta has become one of the most essential researche. Using precise and accurate geodetic data, such as the Global Navigation Satellite System has been applied in the current work to evaluate the rates of crustal movements, including regional and local velocities, as well as the assessment of deformation characteristics, such as rates of dilatation, maximum shear and principal strain component analysis. Bernese 5.2 software was used to process data between 2013 and 2020 for fourteen Global Navigation Satellite System permanent sites. The result shows that the Delta has different geodynamic behaviors related to its structural properties as well assuffering from heterogeneous crustal movement. The northeastern side of the Nile Delta may suffer from sinking under the Mediterranean Sea more than the northwestern side because of its high subsidence rates, Crustal movements and deformation parameters Show; VN average values: 0.56 mm/yr, VE average values: 0.62 mm/yr for local velocities and average values -4.60 mm/yr for vertical subsidence. Also, the area is characterized by medium shear strain, indicating that the risk of an earthquake is low.

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Kheir, Ahmed Mohammed Saad, Aly Abdelaal, Gerrit Hoogenboom, and Senthold Asseng. "Experimental and simulated wheat data from across a temperature gradient along the River Nile in Egypt." Open Data Journal for Agricultural Research 6 (June 4, 2020): 19–20. http://dx.doi.org/10.18174/odjar.v6i0.16318.

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The dataset includes detailed field experiments from four locations across a temperature gradient along the River Nile. The data covering four contrasting environments from North (low temperature) to South (high temperature), includes Sakha (North delta, lower Egypt), Menofya (Middle delta), Benisuef (Middle Egypt) and Aswan (upper Egypt). Measurements included plant density, aboveground biomass, anthesis and maturity dates, grain yield, grains m-2, kernel weight and N content in grains as well as daily weather data (solar radiation, maximum and minimum temperature, precipitation, surface wind, relative humidity, dew point and vapor pressure) and soil characteristics and crop management. Wheat was sown under full irrigation and fertilization with two planting dates. Simulations include three DSSAT-Wheat models (CERES, NWHEAT and CROPSIM).

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Elewa, Hossam Hamdy. "Potentialities of Water Resources Pollution of the Nile River Delta, Egypt." Open Hydrology Journal 4, no. 1 (January 31, 2013): 1–13. http://dx.doi.org/10.2174/1874378101004010001.

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Proussakov, Dmitry. "From the Delta to the Delta: Natural Conditions and Settlers on the Main Nile in the Fifth Millennium BC. Part I (Introductory)." Oriental Courier, no. 2 (2022): 99. http://dx.doi.org/10.18254/s268684310021599-6.

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The 5th millennium BC is marked by the transition to agriculture in the Egyptian Nile valley, rather late for the Fertile Crescent. This was preceded by the Quaternary epic of discovery of the Nile banks by hominids, from the Olduvian Pithecanthropus of the lower Palaeolithic to the Neolithic settlers of the Predynastic period, who laid the socio-economic foundation of the Pharaonic civilization. In the Pleistocene geological epoch, the Main Nile underwent a complex evolutionary transformation from palaeo-rivers with such powerful watercourses as the Prenile to the much inferior in volume Neonile on which, at the 2nd marine isotope stage (27.8–14.7 ka) when the Sahara was a hyperarid desert, comparatively frequent Paleolithic sites of gatherers, fishermen and hunters arose in Upper Egypt and Lower Nubia (the archaeological cultures Halfa, Fakhuri, Qadan, Ballana, Silsila, Afia, Makhadma et al.). Warming and humidification of the climate with the onset of the 1st marine isotope stage was accompanied by an “abrupt return” of the summer monsoon rains to East Africa and an episode of the “Wild Nile” with the incision of the River, which probably made its Egyptian valley unsuitable for settlement by the beginning of the Holocene (11700 ± 99 ka); thus, the Epipalaeolithic is represented here by rare industries of Elkab in Upper Egypt and Karun in the Fayum oasis. At the same time, from the 9th millennium BC there was an increase in the population of the Sahara, where during the African humid period of the early Holocene grassy and woody savannahs were spreading. The Nile Delta with its “historical” network of branches had not yet formed and represented a barren sandy plain which (as well as the Valley) was unsuitable for life and the establishment of the food-producing economy. Simultaneously in Sudan, in the Gezira region at the confluence of the White and Blue Nile, an inner delta was formed, which may have been the cause of the later Neolithization of the lower reaches of the Main Nile.

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Dissertations / Theses on the topic "Nile River Delta (Egypt)"

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Oczkowski, Autumn Jean. "Fertilizing the land, lagoons, and sea : a first look at human impacts on the Nile Delta fishery, Egypt /." View online ; access limited to URI, 2009. http://digitalcommons.uri.edu/dissertations/AAI3368003.

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Hibbs, Vivian A. "The Mendes maze a libation table for the inundation of the Nile (II-III A.D.) /." New York : Garland, 1985. http://catalog.hathitrust.org/api/volumes/oclc/12216064.html.

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Aly, Mohamed Hassan. "Radar interferometry for monitoring land subsidence and coastal change in the Nile Delta, Egypt." [College Station, Tex. : Texas A&M University, 2006. http://hdl.handle.net/1969.1/ETD-TAMU-1022.

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Cagle, Anthony J. "The spatial structure of Kom el-Hisn : an Old Kingdom town in the western Nile Delta, Egypt /." Thesis, Connect to this title online; UW restricted, 2001. http://hdl.handle.net/1773/6478.

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Echtaie, Rawad S. "An investigation into land-use change in two contrasting areas in the Nile Delta, Egypt." Thesis, University of Plymouth, 2008. http://hdl.handle.net/10026.1/386.

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Understanding land-use change in developing countries, particularly those situated in environmentally vulnerable and and semi-arid zones, is crucial given the considerable pressures arising due to rapid population growth, climate change and desertification. The purpose of this research was to investigate the main drivers affecting land-use change in the eastern part of the Nile Delta, Egypt in the last two decades. Two contrasting cities in the region were selected for detailed analysis. Almansourah is an ancient settlement relatively close to the Damietta branch of the Nile whereas Alzaqazig is a recent development and the surrounding area was reclaimed from the desert. The DPSIR (driving forces, pressures, state, impacts and responses) model was adopted as the conceptual framework for organising and categorising the factors affecting landuse change in these two areas. It is a linear, `formulaic' approach, based on the concept of causality chains which connect human activities with environmental information. The case study approach was used as the main methodology, although both qualitative and quantitative techniques were employed throughout. A range of sources were consulted throughout the investigation to ensure that the evidence was internally consistent: remote sensing data, questionnaire data, interviews, participant observation and census data. More than 180 farmers were interviewed in the two study areas and the majority of these (71%) farmed less than 2ha. Using remote sensing data it was found that crop patterns had changed considerably in the two areas both with regard to their geographical distribution and extent. In the Almansourah study area, the key changes during the past two decades were the increase of cotton area and the decrease in rice, maize and other crops. In contrast, the Alzagazig study area experienced an increase in cotton and rice area with minor increase in maize fields. There was also an expansion of urban and rural-urban settlements into agricultural land in both the study areas.One of the critical physical factors for land-use change was found to be the need for irrigation water. Regarding the two study areas, Almansourah currently enjoys greater availability of irrigation water because of its proximity to the Nile compared to Alzagazig which facilitated land-use change in Almansourah. On a more general level the aridity of the Nile Delta region makes water a limiting factor in agricultural production. Analysis of the driving forces showed that land-use change was highly dependent on economic factors such as transportation availability and cost as well as the contribution of women. Land-use change was significantly influenced by transportation availability in Almansourah but not in Alzaqazig possibly because of the greater need to transport agricultural produce to market. Social drivers were also found to be significant. One significant pressure was caused by population growth; in Almansourah the lack of alternative sources of land led to the expansion of urban and rural urban settlements onto fertile agricultural fields. The study confirmed that a farmer's educational level plays an important role in agricultural production. Almost 25% of farmers in Almansourah and 30% in Alzaqaziq had no formal education and this difference led to variations in land-use change between the areas. Education level was found to have a considerable influence on crop rotation and manure use in the Almansourah study area. Conversely, subsidies from private financial sources and rural women's contribution to agricultural production were among the key drivers for land-use change in the Alzaqazig study area. One of the innovative aspects of this study was the application of the DPSIR framework. Although it has been used to advantage in the developed world, it has not been applied to study land-use change in an arid, developing country. The study confirmed that the framework worked well in such a context. Notable strengths included its comprehensive nature, ability to deal with uncertainty and handle different types of data. A further advantage was that it could incorporate sub-models to investigate individual driving forces, for example, the need for irrigation water. Overall the use of DPSIR was flexible enough to highlight the major causative drivers affecting land-use and also to take account of the action of more subtle and complex factors.

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Kaiser, Mona Fouad Mohamed. "Monitoring and modelling the impact of engineering structures on the coastline change, Nile Delta, Egypt." Thesis, University of Reading, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.402628.

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Elmetwalli, Adel M. H. "Remote sensing as a precision farming tool in the Nile Valley, Egypt." Thesis, University of Stirling, 2008. http://hdl.handle.net/1893/844.

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Detecting stress in plants resulting from different stressors including nitrogen deficiency, salinity, moisture, contamination and diseases, is crucial in crop production. In the Nile Valley, crop production is hindered perhaps more fundamentally by issues of water supply and salinity. Predicting stress in crops by conventional methods is tedious, laborious and costly and is perhaps unreliable in providing a spatial context of stress patterns. Accurate and quick monitoring techniques for crop status to detect stress in crops at early growth stages are needed to maximize crop productivity. In this context, remotely sensed data may provide a useful tool in precision farming. This research aims to evaluate the role of in situ hyperspectral and high spatial resolution satellite remote sensing data to detect stress in wheat and maize crops and assess whether moisture induced stress can be distinguished from salinity induced stress spectrally. A series of five greenhouse based experiments on wheat and maize were undertaken subjecting both crops to a range of salinity and moisture stress levels. Spectroradiometry measurements were collected at different growth stages of each crop to assess the relationship between crop biophysical and biochemical properties and reflectance measurements from plant canopies. Additionally, high spatial resolution satellite images including two QuickBird, one ASTER and two SPOT HRV were acquired in south-west Alexandria, Egypt to assess the potential of high spectral and spatial resolution satellite imagery to detect stress in wheat and maize at local and regional scales. Two field work visits were conducted in Egypt to collect ground reference data and coupled with Hyperion imagery acquisition, during winter and summer seasons of 2007 in March (8-30: wheat) and July (12-17: maize). Despite efforts, Hyperion imagery was not acquired due to factors out with the control of this research. Strong significant correlations between crop properties and different vegetation indices derived from both ground based and satellite platforms were observed. RDVI showed a sensitive index to different wheat properties (r > 0.90 with different biophysical properties). In maize, GNDVIbr and Cgreen had strong significant correlations with maize biophysical properties (r > 0.80). PCA showed the possibility to distinguish between moisture and salinity induced stress at the grain filling stages. The results further showed that a combined approach of high (2-5 m) and moderate (15-20) spatial resolution satellite imagery can provide a better mechanistic interpretation of the distribution and sources of stress, despite the typical small size of fields (20-50 m scale). QuickBird imagery successfully detects stress within field and local scales, whereas SPOT HRV imagery is useful in detecting stress at a regional scale, and therefore, can be a robust tool in identifying issues of crop management at a regional scale. Due to the limited spectral capabilities of high spatial resolution images, distinguishing different sources of stress is not directly possible, and therefore, hyperspectral satellite imagery (e.g. Hyperion or HyspIRI) is required to distinguish between moisture and salinity induced stress. It is evident from the results that remotely sensed data acquired by both in situ hyperspectral and high spatial resolution satellite remote sensing can be used as a useful tool in precision farming in the Nile Valley, Egypt. A combined approach of using reliable high spatial and spectral satellite remote sensing data could provide better insight about stress at local and regional scales. Using this technique as a precision farming and management tool will lead to improved crop productivity by limiting stress and consequently provide a valuable tool in combating issues of food supply at a time of rapid population growth.

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Buck, Paul E. "Structure and content of Old Kingdom archaeological deposits in the western Nile delta, Egypt : a geoarchaeological example /." Thesis, Connect to this title online; UW restricted, 1990. http://hdl.handle.net/1773/6543.

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Shacks, Vincent. "Habitat vulnerability for the Nile crocodile (Crocodylus niloticus) in the Okavango Delta, Botswana." Thesis, Link to the online version, 2006. http://hdl.handle.net/10019/1651.

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Belal, Abdelaziz Belal Abdel Elmontalbe. "Precision farming in the small farmland in the eastern Nile Delta Egypt using remote sensing and GIS." [S.l.] : [s.n.], 2006. http://deposit.ddb.de/cgi-bin/dokserv?idn=980583543.

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Books on the topic "Nile River Delta (Egypt)"

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The Nile River. Tarrytown, NY: Marshall Cavendish Benchmark, 2008.

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McGuire, Margit E. Ancient Egypt: Life in the Nile River Valley. Chicago, IL: Everyday Learning Corp., 1999.

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Aloian, Molly. The Nile: River in the sand. New York: Crabtree Pub. Co., 2009.

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1946-, Nomachi Kazuyoshi, ed. The Nile. London: Barrie & Jenkins, 1989.

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Guindy, S. El. Research on water management of rice fields in the Nile Delta, Egypt. Wageningen, The Netherlands: International Institute for Land Reclamation and Improvement, 1987.

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Erlich, Hagai. The cross and the river: Ethiopia, Egypt, and the Nile. London: L. Rienner, 2002.

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Erlikh, Ḥagai. The cross and the river: Ethiopia, Egypt, and the Nile. Boulder, Colo: L. Rienner, 2002.

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Down the Nile. New York: Little, Brown and Company, 2007.

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Pye-Smith, Charlie. The other Nile. Harmondsworth, Middlesex, England: Penguin, 1987.

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The other Nile. Harmondsworth, Middlesex, England: Viking, 1986.

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Book chapters on the topic "Nile River Delta (Egypt)"

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Negm, Abdelazim, Mohamed Elsahabi, Neama Abd El-Basset, Reham El-Sayed, Shenouda Ghaly, and Kamal Ali. "Investigating the Morphological Changes of the Nile River from Aswan High Dam to Delta Barrages, (Egypt) Using RS/GIS." In Recent Advances in Environmental Science from the Euro-Mediterranean and Surrounding Regions, 1771–73. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-70548-4_514.

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Badawy, Wael, Octavian G. Duliu, Marina V. Frontasyeva, and Hussien El-Samman. "Distribution of Major and Trace Elements in Soil and Sediments Along the Nile River and Delta—(Egypt): A Case Study." In Petrogenesis and Exploration of the Earth’s Interior, 93–95. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01575-6_22.

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Fishar, Mohamed Reda. "Nile Delta (Egypt)." In The Wetland Book, 1–10. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_216-1.

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Fishar, Mohamed Reda. "Nile Delta (Egypt)." In The Wetland Book, 1251–60. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_216.

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Sherif, M. "Nile Delta Aquifer in Egypt." In Seawater Intrusion in Coastal Aquifers — Concepts, Methods and Practices, 559–90. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-017-2969-7_17.

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Satoh, M., T. El Gamal, T. Taniguchi, X. Yuan, A. Ishii, and W. H. Abou El Hassan. "Water Management in the Nile Delta." In Irrigated Agriculture in Egypt, 187–224. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-30216-4_8.

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Youssef, Ahmed Mohamed Ali, Sawsan Moselhy Mohamed Ibrahem, and Rasha Abdallah Hussien. "Groundwater Ocurrences in West Nile Delta, Egypt." In Springer Water, 41–77. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-77622-0_3.

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Sharaky, Abbas M., Adel S. El Hasanein, Samir A. Atta, and Karima M. Khallaf. "Nile and Groundwater Interaction in the Western Nile Delta, Egypt." In The Handbook of Environmental Chemistry, 33–62. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/698_2016_127.

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El-Kilani, R. M. M., and M. Sugita. "Irrigation Methods and Water Requirements in the Nile Delta." In Irrigated Agriculture in Egypt, 125–51. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-30216-4_6.

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Kubota, A., B. Zayed, H. Fujimaki, T. Higashi, S. Yoshida, M. M. A. Mahmoud, Y. Kitamura, and W. H. Abou El Hassan. "Water and Salt Movement in Soils of the Nile Delta." In Irrigated Agriculture in Egypt, 153–86. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-30216-4_7.

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Conference papers on the topic "Nile River Delta (Egypt)"

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Shabana, M., K. Abdelaziz, M. Abdelaty, S. Sonika, A. Salem, F. Ibrahim, E. Fouad, E. Shady, and Mehmet C. Tanis. "Egypt Nile Delta — Processing/Reprocessing Case History." In Istanbul 2012 - International Geophysical Conference and Oil & Gas Exhibition. Society of Exploration Geophysicists and The Chamber of Geophysical Engineers of Turkey, 2012. http://dx.doi.org/10.1190/ist092012-001.8.

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Hynes, L., and A. Saber. "Operational Geomechanics - A Case Study, Nile Delta Egypt." In First EAGE Workshop on Pore Pressure Prediction. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700059.

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Khedr, Sherine, Fady El-dabi, Mohamed Nashaat, Ghulam Mohiuldin, Alaa Galal, Teddy Slim, Andrea Hughes, et al. "West Nile Delta Campaign Delivering Energy to Egypt." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 2019. http://dx.doi.org/10.2118/195809-ms.

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Mueller, M. C., L. A. Thomsen, and B. Chmela. "Dual Dipole Arrivals in Neogene Pay Zones, Nile Delta, Egypt." In 59th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.131.gen1997_p015.

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Samuel, A., A. Sharp, A. Sitta, J. Millington, and T. Worku. "Deep Water Slope Channel Reservoirs from the Nile Delta, Egypt." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406025.

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Shabana, Mahmoud. "Revealing the true subsurface image of Nile delta, offshore Egypt." In International Conference and Exhibition, Barcelona, Spain, 3-6 April 2016. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2016. http://dx.doi.org/10.1190/ice2016-6375045.1.

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Saleh, Gebril, Amr Talaat, Karim Ali, Ramy Eid, Sugandha Tewari, Hosny Diab, Mohamed Radwan, and Mohamed Helal. "Reinvigorating exploration in the Nile Delta and East Mediterranean, Egypt." In Second International Meeting for Applied Geoscience & Energy. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2022. http://dx.doi.org/10.1190/image2022-3751276.1.

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Huebner, N. "2D Cross-section Restoration in the Onshore Nile Delta, Egypt." In 78th EAGE Conference and Exhibition 2016. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201601184.

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Sharp, A., A. Samuel, and F. Federici. "Geophysical Characterisation of the Simian Discovery, West Delta Deep Marine Concession, Nile Delta, Egypt." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406026.

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Metwaly, M., G. El-Qady, A. El-Galladi, and K. Ushijima. "Evaluation of Peat Layer Using Geoelectrical Methods at Nile Delta– Egypt." In Near Surface 2005 - 11th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.13.p017.

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Reports on the topic "Nile River Delta (Egypt)"

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Ghazouani, W., F. Molle, A. Swelam, E. Rap, and A. Abdo. Understanding farmers’ adaptation to water scarcity: a case study from the western Nile Delta, Egypt. International Water Management Institute (IWMI)., 2014. http://dx.doi.org/10.5337/2015.200.

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