Matches in SemOpenAlex for { <https://semopenalex.org/work/W3159081495> ?p ?o ?g. }
Showing items 1 to 91 of
91
with 100 items per page.
- W3159081495 abstract "The present study has been conducted to evaluate the pollution load that has been exerted on two of the major lakes in Egypt; Bardawil and Manzala lakes. Bardawil lake is mainly sea water subjected to evaporation while Manzala lake is a mixture of saline water and fresh water and receives drainage water and effluents of different wastes. The study involves both environmental isotopes ({sup 18}O and D), major ions, nitrate and phosphate analysis of about 75 water samples collected through horizontal and vertical profiles in the two lakes. Bardawil lake water (the average of TDS equals to 46,521 ppm) is dominated by Cl, Na and Mg salts. The distribution of the ions is controlled by the inflow from sea water, the concentration by evaporation, the precipitation due to supersaturation and the specific gravity variations. The hydrochemical composition of Manzala lake water (average of TDS equals to 2,554 ppm) is less homogenous than that of Bardawil lake water and reflects the effects of several factors and recharge sources; irrigation water/drainage water discharge, waste water load, sea water or groundwater inflow, bathometry and evaporation intensity. The concentrations of nitrate and phosphate acquire considerably high values in Manzala lake which indicate a high degree of pollution and eutrophication. The isotopic content of Bardawil lake water has average values of 3.69 per mille and 28.59 per mille for {delta} {sup 18}O and {delta} D, respectively. It has a relatively wide range of variation reflecting the effect of the different recharge sources (seawater, precipitation and seepage of groundwater) and the influence of the different hydrogeochemical conditions. The distribution of Bardawil lake water on {delta} {sup 18}O vs {delta} D conventional diagram, follows a linear pattern. {delta} D = 4.70 {delta} {sup 18}O +10.31 of lower slope (4.70) than the meteoric line (slope = 8). This reflects the effect of evaporation on the occurring surface water in the lake. The starting points of the samples line (evaporation line) lie very close to Mediterranean Sea water which represent the original sources of lake water. The relative position of the water samples on the evaporation line and their deviation from the original points is a function of evaporation intensity. The effect of evaporation on the isotopic composition of Bardawil lake water is also shown by the direct relationship between {sup 18}O and TDS. This figure shows that the correlation coefficient is low particularly in the deeper zones (bottom water) than that of surface zones (surface water). This can be related to salt precipitation after stages of supersaturation in the surface water due to excessive evaporation processes which reaches about 1.6 m/y. The isotopic content of Manzala lake water is characterized by average values of 5.07 per mille and 29.79 per mille for {delta} {sup 18}O and {delta} D, respectively. The frequency distribution of the isotopic values reflects the multiplicity of the recharge sources (precipitation, seawater, drainage, irrigation and groundwater). The relationship between {sup 18}O and deuterium for Manzala lake water is direct and follows a linear pattern of evaporation trend {delta} D = 4.76 {delta} {sup 18}O +7. The isotopic contents of Nile water, seawater and drainage water (the recharging sources of the lake) lie close to the starting points of the evaporation line. The scatter of the points around the regression line is relatively high due to the variant proportion of the recharge sources and the different evaporation intensity. The relationship between {sup 18}O and TDS, is very weak and the pattern is not easily defined. This can highlight on the great difference of salinity between the recharging sources (due to leaching, evaporation, dissolution etc.), while the isotopic content is not so variant." @default.
- W3159081495 created "2021-05-10" @default.
- W3159081495 creator A5007982410 @default.
- W3159081495 creator A5019301123 @default.
- W3159081495 creator A5049858914 @default.
- W3159081495 creator A5068609573 @default.
- W3159081495 date "2004-07-01" @default.
- W3159081495 modified "2023-09-27" @default.
- W3159081495 title "Environmental isotopes and hydrochemistry approach to evaluate the source of recharge and pollution load in Manzala and Bardawil Lakes, Egypt" @default.
- W3159081495 hasPublicationYear "2004" @default.
- W3159081495 type Work @default.
- W3159081495 sameAs 3159081495 @default.
- W3159081495 citedByCount "0" @default.
- W3159081495 crossrefType "journal-article" @default.
- W3159081495 hasAuthorship W3159081495A5007982410 @default.
- W3159081495 hasAuthorship W3159081495A5019301123 @default.
- W3159081495 hasAuthorship W3159081495A5049858914 @default.
- W3159081495 hasAuthorship W3159081495A5068609573 @default.
- W3159081495 hasConcept C107054158 @default.
- W3159081495 hasConcept C107872376 @default.
- W3159081495 hasConcept C111368507 @default.
- W3159081495 hasConcept C127313418 @default.
- W3159081495 hasConcept C142796444 @default.
- W3159081495 hasConcept C153294291 @default.
- W3159081495 hasConcept C161382645 @default.
- W3159081495 hasConcept C174091901 @default.
- W3159081495 hasConcept C185592680 @default.
- W3159081495 hasConcept C186699998 @default.
- W3159081495 hasConcept C187320778 @default.
- W3159081495 hasConcept C18903297 @default.
- W3159081495 hasConcept C197248824 @default.
- W3159081495 hasConcept C205649164 @default.
- W3159081495 hasConcept C2776384668 @default.
- W3159081495 hasConcept C39432304 @default.
- W3159081495 hasConcept C521259446 @default.
- W3159081495 hasConcept C75622301 @default.
- W3159081495 hasConcept C76177295 @default.
- W3159081495 hasConcept C76886044 @default.
- W3159081495 hasConcept C8625798 @default.
- W3159081495 hasConcept C86803240 @default.
- W3159081495 hasConcept C87717796 @default.
- W3159081495 hasConceptScore W3159081495C107054158 @default.
- W3159081495 hasConceptScore W3159081495C107872376 @default.
- W3159081495 hasConceptScore W3159081495C111368507 @default.
- W3159081495 hasConceptScore W3159081495C127313418 @default.
- W3159081495 hasConceptScore W3159081495C142796444 @default.
- W3159081495 hasConceptScore W3159081495C153294291 @default.
- W3159081495 hasConceptScore W3159081495C161382645 @default.
- W3159081495 hasConceptScore W3159081495C174091901 @default.
- W3159081495 hasConceptScore W3159081495C185592680 @default.
- W3159081495 hasConceptScore W3159081495C186699998 @default.
- W3159081495 hasConceptScore W3159081495C187320778 @default.
- W3159081495 hasConceptScore W3159081495C18903297 @default.
- W3159081495 hasConceptScore W3159081495C197248824 @default.
- W3159081495 hasConceptScore W3159081495C205649164 @default.
- W3159081495 hasConceptScore W3159081495C2776384668 @default.
- W3159081495 hasConceptScore W3159081495C39432304 @default.
- W3159081495 hasConceptScore W3159081495C521259446 @default.
- W3159081495 hasConceptScore W3159081495C75622301 @default.
- W3159081495 hasConceptScore W3159081495C76177295 @default.
- W3159081495 hasConceptScore W3159081495C76886044 @default.
- W3159081495 hasConceptScore W3159081495C8625798 @default.
- W3159081495 hasConceptScore W3159081495C86803240 @default.
- W3159081495 hasConceptScore W3159081495C87717796 @default.
- W3159081495 hasLocation W31590814951 @default.
- W3159081495 hasOpenAccess W3159081495 @default.
- W3159081495 hasPrimaryLocation W31590814951 @default.
- W3159081495 hasRelatedWork W1989557140 @default.
- W3159081495 hasRelatedWork W2027609836 @default.
- W3159081495 hasRelatedWork W2060249561 @default.
- W3159081495 hasRelatedWork W2087746654 @default.
- W3159081495 hasRelatedWork W2119285819 @default.
- W3159081495 hasRelatedWork W2336714510 @default.
- W3159081495 hasRelatedWork W2348386813 @default.
- W3159081495 hasRelatedWork W2362531744 @default.
- W3159081495 hasRelatedWork W2388308219 @default.
- W3159081495 hasRelatedWork W2412656772 @default.
- W3159081495 hasRelatedWork W2552277106 @default.
- W3159081495 hasRelatedWork W2912332563 @default.
- W3159081495 hasRelatedWork W2970401086 @default.
- W3159081495 hasRelatedWork W2978837527 @default.
- W3159081495 hasRelatedWork W2981488526 @default.
- W3159081495 hasRelatedWork W3013226996 @default.
- W3159081495 hasRelatedWork W3080291666 @default.
- W3159081495 hasRelatedWork W3084712097 @default.
- W3159081495 hasRelatedWork W3170802572 @default.
- W3159081495 hasRelatedWork W3186261062 @default.
- W3159081495 isParatext "false" @default.
- W3159081495 isRetracted "false" @default.
- W3159081495 magId "3159081495" @default.
- W3159081495 workType "article" @default.