排序方式： 共有39条查询结果，搜索用时 390 毫秒
21.
Ben Kahla-Nakbi A Besbes A Chaieb K Rouabhia M Bakhrouf A 《Marine environmental research》2007,64(4):469-478
The aim of this study was to evaluate the survival responses of four strains of Vibrio alginolyticus in seawater under starvation conditions. We used microcosms containing sterilised seawater and incubated at ambient temperature (22-25 degrees C). V. alginolyticus maintained its culturability for at least nine months. Long-term-starved cells showed an absence or a decrease in their enzymatic activities. Resuscitation assays of viable but non-culturable (VBNC) cells were conducted and the recovery of these cells was achieved after the addition of nutrients. Amplified 16S ribosomal DNA (rDNA) restriction analysis (ARDRA) was used to confirm that the same strain of V. alginolyticus persisted in all microcosms during a long period of time. Starved cells maintained their infectivity for gilt head sea bream (Sparus aurata) and sea bass (Dicentrachus labrax) as determined by intraperitoneal challenges. 相似文献
22.
Alireza Farrokhnia Saied Pirasteh Biswajeet Pradhan Mohamad Pourkermani Mehrdad Arian 《Arabian Journal of Geosciences》2011,4(7-8):1337-1349
Mass movements or mass wasting is being considered as one of the severe forms of natural disasters. Iran is geographically located in the Alps–Himalaya seismicity belt. It has a high potential to mass wasting. This seismic phenomenon creates landslides and rock falls in the high mountains of Alborz and Zagros. These mass movements and various types of slides can be systematically assessed and mapped through traditional mapping frameworks using geo-information technologies. The geo-information-based technology offers the earth scientist to study and map various types of mass movement and stability of slopes. In this study, we used field data coupling with the tectonic-related factors to provide a solution for slope-related hazards. Firstly, various geological and geomorphological factors such as lineaments and faults, vegetation, lithology, slope, drainage, land use/land cover, seismicity and roads network were extracted and compiled using geo-information technology. This is because the factors mentioned above play important role in the instability of the region. Then, the study area was divided into four regions based on the rate of mass wasting and its degree of vulnerability. The results of this study showed that the erosion in Karaj formation is severe. Additionally, this research also reveals that the hydrothermal solutions caused by the erosional activities have influenced the glassy element of tuffs and subsequently changed into the clays. This change has caused the tuffs to be relatively unstable. Further, it is evident that the chemical and physical weathering has had a big impact on it whilst most of the mass wasting has occurred within the unstable tuffs of Karaj formation. Finally, the paper concluded that the recent construction of the new roads in the region has increased the potential danger for generating the mass wastes and thus makes the region more unstable. 相似文献
23.
In Algeria, the climate change in recent decades has a negative impact on water resources. The goal of this study is to determine the influence of these hazards on surface water resources in the basin of Macta (Northwest of Algeria). The study of climatic pulsations is implemented from the climate coefficient changes and its moving averages over 3 years. Variations of this coefficient based on years, for the period 1949–1973, show an alternation of wet and dry years. Starting from 1973, a very dry period of more than 20 years was installed in the basin, with deficits ranging from 22% to 72%. The consequences of the surface water deficit can damage the environmental balance and consequently affect the various human activities that are directly or indirectly related to the use of these resources. 相似文献
24.
Abderrahmane Bendaoud Amel Derridj Khadidja Ouzegane Jean-Robert Kienast 《Journal of African Earth Sciences》2004,39(3-5):187
In the Laouni terrane, which belongs to the polycyclic Central Hoggar domain, various areas contain outcrops of formations showing granulite-facies parageneses. This high-temperature metamorphism was accompanied by migmatization and the emplacement of two types of magmatic suite, one of continental affinity (garnet pyroxenites and granulites with orthoferrossilite–fayalite–quartz), and the other of arc affinity (layered metanorites). Paragenetic, thermobarometric and fluid-inclusion studies of the migmatitic metapelites and metabasites make it possible to reconstruct the P–T–aH2O path undergone by these formations. This path is clockwise in the three studied areas, being characterized by a major decompression (Tamanrasset: 10.5 kbar at 825 °C to 6 kbar at 700 °C; Tidjenouine: 7.5 kbar at 875 °C; to 3.5 kbar at 700 °C; Tin Begane: 13.5 kbar at 850 °C; to 5 kbar at 720 °C), followed by amphibolitization that corresponds to a fall of temperature (from 700 to 600 °C) and an increase in water activity (from 0.2–0.4 to almost 1).The main observed features are in favour of petrogenesis and exhumation related to the Eburnean orogeny. However, the lacks of good-quality dating work and a comparison with juvenile Pan-African formations having undergone high-pressure metamorphism, in some cases reaching the eclogite facies, do not rule out the possibility that high-temperature parageneses are locally due to Pan-African events. 相似文献
25.
Amel Chakroun Dalila Zaghbib-Turki Mohamed Moncef Turki 《Arabian Journal of Geosciences》2016,9(4):327
Detailed observation of the Upper Pleistocene deposits of Rafraf (Bizerte, Northeastern Tunisia) provides new data about the significant variations in facies, thickness, and faunal assemblages. This work reports, for the first time, the occurrence of a Persististrombus latus level in the Rafraf sea coast. Facies analyses added to the recorded sedimentary features were carried in order to recognize stratigraphy, paleontology, and sea level highstands. They revealed complex succession of various Upper Pleistocene environments ranging from coastal dunes to inner platforms with scatter builds by Vermetus triquetrus and P. latus. The marine Upper Pleistocene deposits rich in the Senegalese fauna P. latus draw scale steps outcropping at diverse altitudes varying between 1 and 14 m. Serial sections along the border of the Rafraf beach show the action of many faults trending EW and NW-SE. Even though these faults got low values of vertical throw, their cumulative throw values led to these different altitudes of strata containing P. latus. These altitude variations are mainly the result of the inherited geomorphology, the environmental distribution, the sea level fluctuations and the tectonic activities. 相似文献
26.
J. Schumacher E. Luedeling J. Gebauer A. Saied K. El-Siddig A. Buerkert 《Journal of Arid Environments》2009,73(4-5):399-406
Urban agriculture (UA) in Khartoum, Sudan, contributes to meeting the increasing food demand of the city's rapidly growing population, but its spatial extent, development over time and resource consumption are unknown. To fill this knowledge gap, we analyzed scenes captured by Landsat satellites in 1972, 1987 and 2000. For each dataset, we calculated the Normalized Difference Vegetation Index (NDVI) and classified all grid cells with NDVI values higher than one standard deviation above the mean as vegetated land. We also quantified agricultural vegetation on aerial photographs taken in 1958 and on a recent Google Earth image. The built-up area of the city was estimated for each point in time. Based on these spatial estimates, we computed water consumption by UA based on geographic, temporal and climatic datasets and official data on the cropping patterns of Khartoum State, using the Penman–Monteith equation to estimate crop water demands, and assuming a water use efficiency of 0.56.Urban agriculture increased from 8751 ha in 1972 to 13,249 ha today. In the municipal core zone, UA decreased from 4799 ha in 1958 to 2869 ha today. Along the Nile, UA persisted through time, whereas many urban irrigation schemes have been pushed into the periphery. The built-up area increased strongly and today exceeds the UA area 5.5-fold. Estimated crop water demand on UA land increased from 241 to 365 million m3 year?1 between 1972 and today. 相似文献
27.
Résumé La variabilité du climat, une gestion non optimale de la ressource en eau et l'intensification des activités anthropiques pourraient être les trois facteurs majeurs menaçant les écoulements et l'état de la ressource en eau dans les sous-bassins algériens. C'est le cas du bassin de la Tafna dans la partie occidentale de l'Algérie. Ce bassin est situé dans une région au climat semi-aride. Outre l'influence des précipitations, nous examinerons dans cet article la contribution possible d'autres facteurs (géologiques, topographiques et anthropiques) à la variabilité des écoulements dans le bassin de la Tafna. Pour cela, en plus de l'analyse du régime pluviométrique et des débits, nous avons choisi d'analyser le baseflow index ou BFI et les débits de base. Cinq sous-bassins de la Tafna, où des données journalières de pluie et de débit étaient disponibles sur la période 1976–2006 ont été étudiés. L'analyse, qui a distingué deux sous-régions déterminées par la topographie: les bassins d'altitude et ceux de plaine, montre que, selon leur contexte géologique, les sous-bassins ont des comportements différents en terme d'écoulement. Les zones en altitude présentant un écoulement de base et un BFI plus importants que les bassins de plaine. Ceci peut être relié à la nature lithologique des formations, les bassins d'altitude présentant une composante karstique importante. Les analyses de tendance/rupture sur les précipitations annuelles ne montrent aucune tendance significative sur la période 1976–2006. On note une baisse des débits moyens annuels uniquement sur deux stations en altitude (significatives aux seuils 1 et 10% respectivement). Une tendance à une diminution significative des débits de base est obtenue sur deux bassins d'altitude et un bassin de plaine (au seuil 1 ou 5%). La baisse du BFI est significative au seuil 1% pour seulement une station d'altitude. Ceci serait le signe d'une baisse du stock dans les bassins d'altitude. La modification des écoulements de base sur certains sous-bassins de la Tafna serait donc imputable à des causes, notamment de nature anthropique, ne relevant pas d'une diminution de la pluviométrie. Editeur Z.W. Kundzewicz; Editeur associé M. Lang Citation Bakreti, A., Braud, I., Leblois, E., et Benali, A. 2013. Analyse conjointe des régimes pluviométriques et hydrologiques dans le bassin de la Tafna (Algérie Occidentale). Hydrological Sciences Journal, 58 (1), 1–19. 相似文献
28.
Bourhane-Eddine Belabed Xavier Laffray Amel Dhib Mouna Fertouna-Belakhal Souad Turki Lotfi Aleya 《Marine pollution bulletin》2013
This paper presents the results of a seasonal survey of heavy metals accumulated in sediments and in the soft parts of the body of the mussel Perna perna at four stations in the Gulf of Annaba (Algeria). Pooled soft tissues from 10 mussels representing the entire range of sizes were digested in nitric acid. Statistical analysis reveals a significant seasonal effect on all the measured metals, the highest values being recorded in winter. With the exception of Cr, the levels for all metals were significantly higher in the east, at the outlet of the Seybouse River, than at all other monitoring stations. The study also shows that north-western waters are subject to a significantly lower degree of heavy metal pollution than elsewhere in the gulf. Levels were nevertheless within the limits of public health standards. 相似文献
29.
Mohamed SOUA Dalila ZAGHBIB-TURKI Hela BEN JEMIA Jalel SMAOUI Amel BOUKADI 《《地质学报》英文版》2011,85(6):1310-1335
In Tunisia, five Bahloul spaced sections, Bargou, Jerisa, Guern Halfaya, Kherij and Gafsa were analyzed for biostratigraphy (foraminifera and radiolarians) and major and trace elements. This high-resolution biostratigraphic and chemostratigraphic integrated analyses for the Late Cenomanian–Early Turonian Bahloul Formation provide new insight into the palaeoceanographic evolution of the southern Tethyan margin. Relative low abundance of related terrigenous Ti/Al and K/Al ratios and enrichment of some productivity proxies such as Ba, Cu, and Ni (organic matter related trace elements) suggests that the Bahloul, deposited during a relatively short period (0.5 Ma), was of relatively elevated primary productivity and minimal detrital input. While higher D* values concurrent with lower Ti/Al ratios are interpreted as caused by enhanced fluvial material contribution, due to more humid climate during the OAE-2. Enhanced humidity triggered probably fluvial influxes, resulted in a sluggish water circulation and consequent anoxic/euxinic conditions favoring the preservation of organic matter at the bottom. Enrichments in redox-sensitive trace metals U, V, and Mo in the Bahloul Formation deposits and redox indices, such as V/(V+Ni), U/Th, V/Cr, and Ni/Co, indicate that oxygen-restricted conditions prevailed during the Late Cenomanian to earliest Turonian times and correlate well with relative abundances of some foraminiferal and radiolarian paleo-environmental relevant indicators. High Baxs values and Uauth may indicate anoxic conditions at least at the water–sediment interface during the Bahloul Formation deposition and provide information about low to moderate sulfate-reduction reactions. 相似文献
30.
Gaur Shishir Mishra Aryan Gupta Anurag Jain Arihant Dave Apurve Eslamian Saied Dwivedi S. B. Graillot Didier 《Water Resources》2021,48(4):565-575
Water Resources - Predicting the Suspended Sediment Load (SSL) of the river is a very significant and challenging task. Being a non-linearity in the SSL data, it requires a non-linear method to get... 相似文献