ID Course Name Duration Start Date
BIOGEOCHEHICAL STUDIES ON THE MOLLUSK BIVALVE ANADARA DILUVII (LAHARCK, 1805) (PTERIOMORPHA ARCIDAE)
BIOGEOCHEMICAL STUDIES ON THE MOLLUSK BIVALVE AKADARA DILUVII (LAMARCK, 1805) (PTERIOMORPHA ARCIDAE)
CARBON, NITROGEN AND PHOSPHORUS CONTENT OF THE COPEPOD EUTERPINA ACgTIFRONS IN
COMPARATIVE ROLE OF EPIBIOTA AND PLANKTON PRIMARY AND SECONDARY PRODUCERS IN EGYPTIAN DELTA LAKES.
DESCRIPTIONS OF SOME THECATE HYDROIDS (CNIDARID-HYDROZOA) FROM THE EGYPTIAN MEDITERRANEAN WATERS.
DISTRIBUTION OF SOME ROTIFERS IN THE EGYPTIAN INLAND WATERS
ECOLOGY OF ROTIFERA IN WADI EL RAYAN, EGYPT
EFFECTS OF CHRONIC EXPOSURES TO COPPER ON PRODUCTIOlf AKD TOTAL RESIDES AKOlfG TILAPIA SPECIES.
EPPECT OF SALIMITY VARIATION OM HEMOLYMPH CALCIUM COHCEXTRATIOH DURIHG THE MOULT CYCLE OP THE PRAWH PEKAEUS JAPOHICUS (BATE)
EPPECT OP SODIUM, IRON IONS AXD TIME OP (STIRRING) ON THE CRYSTAL-LATTICE AXD MORPHOLOGY OF THE GYPSUM CRYSTALS.
EVALUATION OF THE SANITARY STATUS IN SOME BEACHES OF PORT-SAID BY USING THE INDICATOR ORGANISMS.
FECUNDITY OF THE SHRIMP HETAPEKAEUS ~TEBBIKGI JOBILI IX HE EGYPTIAN WATERS.
GEOCHEMISTRY OF SEDIHlNT CORES FROM THE SEA OF MARMARA, EASTERN TROUGH.
KUMERICAL INVESTIGATIOI OF M2-TIDE II THE MEDITERRANEAN SEA WITH ITS REAL BOUIDARIKS AID OF GRID SIZE 15’1 IS’ .
MINERALOGICAL AND CHEMICAL COMPOSITIONS AS CRITERIA FOR THE DIFFERENTIAL
NUMERICAL INVESTIGATION OF CO-OSCILLATING M2-TIDE IN THE MEDITERRANEAN WITH GRID SIZE 1″ X 1 0 •
NUMERICAL INVESTIGATION OF M2-TIDES IN THE MEDITERRANEAN, AS A CLOSED RECTANGULAR BASIN.
NUMERICAL INVESTIGATION OP M2-TID!8 1M THE MEDITERRANEAN AS ACLOSED BASIN.
PBYTOPWlTOI PRODOCTIOI, DIVERSIn AID CHLOROPHYLL-A 11 TBE SOEZ CARAL, EGYPT.
PHYTOPLANKTON STANDING CROP, DIVERSITY AND STATISTICAL MULTISPECIES ANALYSIS IN LAKE BUROLLUS, EGYPT.
POLYCULTURE OF SIX FISH SPECIES UNDER DIFFERENT MANAGEMENT SYSTEMS IN EGYPT.
STATISTICAL ANALYSIS OF DAILY SEA LEVEL IN ALEXANDRIA HARBOUR, EGYPT
STUDIES ON THE IONIC AND ALKALINE PHOSPHATASE CHANGES ASSOCIATED WITH THE MOULT
The present study aims to follow up the incorporation of both Na+ and Fe·· ions into the gypsum crystals. Time of stirring as controlling factor for the variation of crystal lattice and morphology of the gypsum crystals has been also investigated.