Hydrochemical and stable isotopic investigation of groundwater quality and its sustainability for irrigation in the Hammamet-Nabeul basin,northeastern Tunisia     

Amor Ben Moussa  Sarra Bel Haj Salem  Kamel Zouari  Faycel Jelassi 《Arabian Journal of Geosciences》2017,10(20):446

The major ion hydrochemistry, sodium absorption ratio (SAR), sodium percentage, and isotopic signatures of Hammamet-Nabeul groundwaters were used to identify the processes that control the mineralization, irrigation suitability, and origin of different water bodies. This investigation highlights that groundwater mineralization is mainly influenced by water-rock interaction and pollution by the return flow of irrigation water. The comparison of groundwater quality with irrigation suitability standards proves that most parts of groundwater are unacceptable for irrigation and this long-term practice may result in a significant increase of the salinity and alkalinity in the soils. Based on isotopic signatures, the shallow aquifer groundwater samples were classified into (i) waters with depleted δ¹⁸O and δ²H contents, highlighting recharge by modern precipitation, and (ii) waters with enriched stable isotope contents, reflecting the significance of recharge by contaminated water derived from the return flow of evaporated irrigation waters. The deep-aquifer groundwater samples were also classified into (i) waters with relatively enriched isotope contents derived from modern recharge and mixed with shallow-aquifer groundwater and (ii) waters with depleted stable isotope contents reflecting a paleoclimatic origin. Tritium data permit to identify three origins of recharge, i.e., contemporaneous, post-nuclear, and pre-nuclear. Carbon-14 activities demonstrate the existence of old paleoclimatic recharge related to the Holocene and Late Pleistocene humid periods.  相似文献   

Nitrogenous compounds changes in emersed oysters: Crassostrea gigas     

Sarra Rafrafi  Roger F. Uglow 《Estuarine, Coastal and Shelf Science》2009

The effects of emersing oysters (Crassostrea gigas) for up to 66 h at 4 °C under humid air and nitrogen atmospheres were studied. A significant, gradual body mass loss occurred under nitrogen (8.36 ± 0.85% final weight loss) but no significant loss occurred under humid air (4.92 ± 2.67% final weight loss). Emersion duration and the mantle cavity fluid (MCF) total ammonia (TA) concentration showed a positive, linear relationship (r² = 0.73 and 0.74 under humid air and N₂, respectively). The MCF TA and trimethylamine (TMA) contents were also positively related (r² = 0.64 and 0.69 under humid air and N₂, respectively).  相似文献   

Natural and artificial recharge investigation in the Zéroud Basin,Central Tunisia: impact of Sidi Saad Dam storage   总被引：1，自引：0，他引：1  

Sarra Bel Hadj Salem  Najiba Chkir  Kamel Zouari  Anne Laure Cognard-Plancq  Vincent Valles  Vincent Marc 《Environmental Earth Sciences》2012,66(4):1099-1110

Hydrochemical and isotopic data of waters from the Zéroud aquifer have been used to potentially provide a means for locating occurrences and to trace movements of a variety of natural and anthropogenic recharge waters in the Zéroud Basin, Central Tunisia. Geochemical data have been measured during the dam water release, from May to September 2005, with a sampling time step of 15 days. An implication of dam water has been demonstrated that is noticeable up along the main flow path to a distance of 10 km far from the injection site. Environmental isotopes ²H, ¹⁸O and ³H of water molecule were studied to investigate the effect of dam water on the hydrological system, and an isotope balance was established to compute the contribution of water storage component in groundwater. Based on isotopic mass balance, we assess that an average of 13% of total groundwater in the upper aquifer came from dam water storage. Three distinctive recharge waters in the aquifer can be determined. Water from local rainfall (pre-dam Zéroud River) that infiltrated into the boundaries of the Draa Affane Mountain was easily distinguished from the water influenced by anthropogenic recharge located in the Zéroud right rivulet. Distinguishable isotopic signatures of native wadi Zéroud recharge due to “recent lineal recharge” through the riverbed were also identified.  相似文献   

CCD astronomical applications for X-ray temporal studies     

P. F. Sarra  G. F. Bignami 《Experimental Astronomy》1992,2(6):357-375

Charge coupled devices (CCDs) are under active investigation as imaging detectors in future X-ray astronomy satellites. The exploitation of such detectors holds great promise because of their capability to perform simultaneous imaging and spectroscopy. Unfortunately, standard readout techniques give a temporal resolution insufficient to study X-ray sources showing variability on timescales less than few seconds. In this paper alternative, non-imaging readout modes are investigated, in order to achieve millisecond temporal resolution for point-like sources. Simulation results are presented for the EPIC camera, the focal plane instrument for ESA's mission XMM, showing that the required temporal capabilities can be reached without loss of energy resolution.Work performed in part at the IFC/CNR, Milan, supported by a special EPIC grant from LABEN S.p.A.  相似文献   

Effect of surface albedo, water vapour, and atmospheric aerosols on the cloud-free shortwave radiative budget in the Arctic     

C. Di Biagio  A. di Sarra  P. Eriksen  S. E. Ascanius  G. Muscari  B. Holben 《Climate Dynamics》2012,39(3-4):953-969

This study is based on ground-based measurements of downward surface shortwave irradiance (SW), columnar water vapour (wv), and aerosol optical depth (τ) obtained at Thule Air Base (Greenland) in 2007–2010, together with MODIS observations of the surface shortwave albedo (A). Radiative transfer model calculations are used in combination with measurements to separate the radiative effect of A (ΔSW_A), wv (ΔSW_wv), and aerosols (ΔSW_τ) in modulating SW in cloud-free conditions. The shortwave radiation at the surface is mainly affected by water vapour absorption, which produces a reduction of SW as low as ?100 Wm^?2 (?18%). The seasonal change of A produces an increase of SW by up to +25 Wm^?2 (+4.5%). The annual mean radiative effect is estimated to be ?(21–22) Wm^?2 for wv, and +(2–3) Wm^?2 for A. An increase by +0.065 cm in the annual mean wv, to which corresponds an absolute increase in ΔSW_wv by 0.93 Wm^?2 (4.3%), has been observed to occur between 2007 and 2010. In the same period, the annual mean A has decreased by ?0.027, with a corresponding decrease in ΔSW_A by 0.41 Wm^?2 (?14.9%). Atmospheric aerosols produce a reduction of SW as low as ?32 Wm^?2 (?6.7%). The instantaneous aerosol radiative forcing (RF_τ) reaches values of ?28 Wm^?2 and shows a strong dependency on surface albedo. The derived radiative forcing efficiency (FE_τ) for solar zenith angles between 55° and 70° is estimated to be (?120.6 ± 4.3) for 0.1 < A < 0.2, and (?41.2 ± 1.6) Wm^?2 for 0.5 < A < 0.6.  相似文献   

Estimation Of Atmospheric Water Vapour Flux Profiles In The Nocturnal Unstable Urban Boundary Layer With Doppler Sodar And Raman Lidar     

M.P. Rao  S. Casadio  G. Fiocco  M. Cacciani  A. Di Sarra  D. Fuá  P. Castracane 《Boundary-Layer Meteorology》2002,102(1):39-62

The vertical wind profiles determined by Doppler sodar and the water vapourmixing ratio profiles obtained by Raman lidar are used to estimate the atmosphericwater vapour flux profiles in the nocturnal urban boundary layer under unstableconditions. The experiment was conducted for several nights in the central areaof Rome under a variety of moisture conditions and different urban boundary-layerflow regimes. Despite some scatter in the profiles, the latent heat flux is found tobe positive throughout the depth of the nocturnal urban boundary-layer. Thelayer-averaged flux shows a variation between -4 to +40 W m^-2, whileindividual values of flux in excess of +150 W m^-2 pertain to a case offree convection during cold air advection caused by the sea breeze. The qualityof flux estimates is found to be highly limited by the low sampling rates employedin the experiment resulting in errors to the order of 60%. Therefore, the results mustbe viewed as estimates rather than precise measurements. The skewness profiles ofthe turbulent fluctuations of vertical velocity and water vapour mixing ratio are alsopositive.  相似文献   

Convective characteristics of the nocturnal urban boundary layer as observed with Doppler sodar and Raman lidar     

S. Casadio  A. Di Sarra  G. Fiocco  D. Fuà  F. Lena  M. P. Rao 《Boundary-Layer Meteorology》1996,79(4):375-391

Convective plume patterns, characteristic of clear sky and light wind daytime boundary layers over land, were observed for two nights with a tri-axial Doppler sodar operated in the central area of Rome during the summer of 1994. An urban heat island effect, combined with a continuation of a breeze from the sea late into night during both days, is believed to be responsible for the observed nocturnal convection. Estimates of the surface heat flux and the vertical velocity scaling parameter are obtained from profiles of vertical velocity variance, and the Raman lidar water vapor measurements are used to obtain the humidity scaling parameter. Convective scaling results for vertical wind and humidity fairly agree with the results of other experiments and models. On the basis of available measurements, it appears that mixed-layer similarity formulations used to characterize the daytime convective boundary layer over horizontally homogeneous surfaces can also be applied to the nocturnal urban boundary layer during periods of reasonable convective activity.  相似文献   

Investigation of groundwater mineralization in the Hammamet–Nabeul unconfined aquifer,north-eastern Tunisia: geochemical and isotopic approach     

Amor Ben Moussa  Sarra Bel Haj Salem  Kamel Zouari  Vincent Marc  Fayçal Jlassi 《Environmental Earth Sciences》2011,62(6):1287-1300

Detailed hydrogeochemical and isotopic data of groundwaters from the Hammamet–Nabeul unconfined aquifer are used to provide a better understanding of the natural and anthropogenic processes that control the groundwater mineralization as well as the sources of different groundwater bodies. It has been demonstrated that groundwaters, which show Na–Cl and Ca–SO₄–Cl water facies, are mainly influenced by the dissolution of evaporates, the dedolomitization and the cation-exchange process; and supplementary by anthropogenic process in relation with return flow of irrigation waters. The isotopic signatures permit to classify the studied groundwaters into two different groups. Non-evaporated groundwaters that are characterized by depleted δ ¹⁸O and δ ²H contents highlighting the importance of modern recharge at higher altitude. Evaporated groundwaters with enriched contents reflecting the significance infiltration of return flow irrigation waters. Tritium data in the studied groundwaters lend support to the existence of pre-1950 and post-1960 recharge. Carbon-14 activities in shallow wells that provide evidence to the large contamination by organic ¹⁴C corroborate the recent origin of the groundwaters in the study area.  相似文献   

Apport de la gravimétrie à l’étude des structures effondrées du Nord-Est de la Tunisie: implications hydrogéologiques     

Sarra Ouerghi  Noamen Rebai  Hakim Gabtni  Boutheina Farhat  Samir Bouaziz 《水文科学杂志》2013,58(6):1361-1373

Résumé

Cette étude basée sur l’analyse des données gravimétriques a pour but d’améliorer la connaissance des structures effondrées du Nord-Est de la Tunisie. La carte de l’anomalie résiduelle a d’abord été calculée à partir de la carte de l’anomalie de Bouguer en enlevant un gradient régional. La résiduelle calculée fournit des informations sur la variation de la densité dans les bassins sédimentaires de l’Oued Chafrou-Khlidia, de Mornag et de Grombalia. Afin de mettre en évidence les différentes structures géologiques (failles, bassins, etc.) dans le secteur d’étude, différentes techniques (gradient vertical, gradient horizontal, prolongement vers le haut, déconvolution d’Euler) ont été appliquées à la carte gravimétrique des structures effondrées du Nord-Est de la Tunisie. Les résultats obtenus ont permis de dresser une carte structurale présentant le système de failles responsable de la structuration de la zone d’étude. Cette carte constitue un document très utile pour orienter les recherches hydrogéologiques futures qui seront menées dans ces plaines.

Editeur Z.W. Kundzewicz

Citation Ouerghi, S., Rebai, N., Gabtni, H., Farhat, B., et Bouaziz, S., 2013. Apport de la gravimétrie à l’étude des structures effondrées du Nord-Est de la Tunisie: implications hydrogéologiques. Hydrological Sciences Journal, 58 (6), 1361–1373.  相似文献