Study of the development and evolution of seasonal thermocline and turbulent processes in the northern parts of Persian Gulf using numerical modeling

The Persian Gulf (PG) is a semi-enclosed shallow sea which is connected to open ocean through the Strait of Hormuz. Thermocline as a suddenly decrease of temperature in subsurface layer in water column leading to stratification happens in the PG seasonally. The forcing comprise tide, river inflow, solar radiation, evaporation, northwesterly wind and water exchange with the Oman Sea that influence on this process. In this research, analysis of the field data and a numerical (Princeton Ocean Model, POM) study on the summer thermocline development in the PG are presented. The Mt. Mitchell cruise 1992 salinity and temperature observations show that the thermocline is effectively removed due to strong wind mixing and lower solar radiation in winter but is gradually formed and developed during spring and summer; in fact as a result of an increase in vertical convection through the water in winter, vertical gradient of temperature is decreased and thermocline is effectively removed. Thermocline development that evolves from east to west is studied using numerical simulation and some existing observations. Results show that as the northwesterly wind in winter, at summer transition period, weakens the fresher inflow from Oman Sea, solar radiation increases in this time interval; such these factors have been caused the thermocline to be formed and developed from winter to summer even over the northwestern part of the PG. The model results show that for the more realistic monthly averaged wind experiments the thermocline develops as is indicated by summer observations. The formation of thermocline also seems to decrease the dissolved oxygen in water column due to lack of mixing as a result of induced stratification. Over most of PG the temperature difference between surface and subsurface increases exponentially from March until May. Similar variations for salinity differences are also predicted, although with smaller values than observed. Indeed thermocline development happens more rapidly in the Persian Gulf from spring to summer. Vertical difference of temperature increases to 9 centigrade degrees in some parts of the case study zone from surface to bottom in summer. Correlation coefficients of temperature and salinity between the model results and measurements have been obtained 0.85 and 0.8 respectively. The rate of thermcline development was found to be between 0.1 to 0.2 meter per day in the Persian Gulf during the 6 months from winter to early summer. Also it is resulted from the used model that turbulence kinetic energy increases in the northwestern part of the PG from winter to early summer that could be due to increase in internal waves activities and stability intensified through water column during this time.

The experimentally pathogenesis of Aeromonas hydrophila in Astacus leptodactylus with emphasis on temperature in bacterial pathogenesis

In this study, four hundred freshwater Crayfish (A. leptodactylus) with average weight of 25-40g were purchased from Aras dam reservoirs in west Azerbayjan province and transported to Iranian Artemia Research Center of Uromya province in September 2010. (One hundred crayfish extra purchased for probably mortality). Before implement of experiment the Crayfish were acclimated for ten days. These experiments was designed in four group treatments (Number, 1,2,3,4) and one control group (Number 5) in triplicate with 20 Crayfish in each repetition prepared of glass aquarium with size (50x40x30cm). Many of infected Crayfish were used for isolation of bacteria. Haemolymph sample had been gathered from infected Crayfish with cutting their antennules and transferred to TSA medium (tryptic soy agar) and then A. hydrophila were determined in order to biochemical test. The treatments and repetitions has exposed to A. hydrophila. The concentrations of the bacteria in 4 treatments were respectively 3 x 108 (T=10-15°C), 3x106 (T=25°C), 3 x 106 and 3 x 104 Cfu mL-1 (T=10- i5oc) (4, 2, 3 and 1) that were prepared in individual containers for exposure of treatments. The control (5) prepared without any bacteria and disinfected by oxytetracycline antibiotic with concentration 100 ppm for 24 hours. The hemolymph samples were withdrawn from abdominal second segments of Crayfish for measuring of THC and TPC in interval hours (2, 6, 12, 24, 48, 96, 144, 240 and 336). For histopatological studies the crayfish samples fixed in Davidson fixative. The results indicated that interval 2 hours after experiment the difference of THC value between treatment 4 with control and treatments 1,2, and 3 was significant (P< 0.05). After 48 hours of experiment the difference of THC value between control group with treatment 1 ,2 and 3 was significant (P< 0.05). The interval 336 hours after experiment also the difference of THC value between treatment 2 with treatments 1, 3 and 4 was significant (P< 0.05). The finding of TPP value showed that the last time after challenge (336 h) there was significant difference between treatment 2 with treatment 4 and control group (P< 0.05). In histopathology studying, in hepatopancreas observed hemocyte aggregated and necrosis withof peknosis nucleus that with increased concentration of bacteria and temperature, The value of hemocyte has increased. Gill revealed necrosis and cell death especially with increased concentration of bacteria and temperature. In lower concentration of bacteria in heart no difference observed, but with increased concentration of bacteria (3 x 108) the low aggregation of hemocyte observed in heart. In treatment 3 x 106 with high temperature also distributed of high hemocyte in heart was observed. In digestive system didn't appear any difference in treatments land 3 but in concentration of 3 x 108 Cfu m1-1 and 3 x 106 (T=25°C) in digestive system was revealed the low aggregation of hemocyte.