A Gradient Maintenance Technique for Seawater Solar Ponds

1997 ◽  
Vol 119 (1) ◽  
pp. 8-12 ◽  
Author(s):  
S. J. Kleis ◽  
Haoming Li ◽  
J. Shi

Seawater solar ponds are being evaluated as a means of reducing heat losses from thermal refuge areas in outdoor mariculture ponds during cold weather. The thermal refuge areas are intended to provide a reliable means of protecting fish crops from lethal cold water temperatures in the winter months. A continuous filling technique is demonstrated for use in gradient zone maintenance of the seawater solar ponds. The technique allows indefinite operation of the refuge areas with a minimal amount of fresh water.

1997 ◽  
Vol 119 (1) ◽  
pp. 2-7 ◽  
Author(s):  
J. Shi ◽  
R. A. Hart ◽  
S. J. Kleis ◽  
R. B. Bannerot

An experimental program has been conducted to examine the feasibility of using seawater solar ponds in mariculture operations along the Texas gulf coast to protect fish crops from the potentially lethal, cold temperatures experienced in outdoor ponds. Seawater solar ponds in the form of floating thermal refuge areas are proposed as a method for reducing the loss of heat from small sections of a pond. Gradient zone erosion under various ambient and operating conditions is examined. Comparisons with previous laboratory studies show a much lower entrainment rate in the natural environment. For conditions which are typical of those encountered in mariculture pond operation, the entrainment rate was found to depend only weakly on the Richardson number. For these conditions, a simple (linear) correlation of entrainment rate with wind speed was developed.


2021 ◽  
Vol 10 ◽  
Author(s):  
Hossein Ahangari ◽  
Haleh Forouhandeh ◽  
Tahereh Ebrahimi ◽  
Vida Ebrahimi ◽  
Soheila Montazersaheb ◽  
...  

Background: Sabalan (Savalan) Lake is a stable crater lake locating at the summit of Sabalan, an inactive stratovolcano and the third highest mountain of Iran. Because of cold weather conditions, the lake is frozen in most months of the year. The biodiversity of microbial flora in this area needs to be explored to find its similarity with the arctic regions’ biodiversity. Objective: The psychrophilic bacterial population of Sabalan (Savalan) Crater Lake was identified. The current research is the first report of aquatic bacterial strains isolation and characterization from Sabalan Lake. Methods: Water sample collections were cultured on four different media, then colonies were isolated by the plating method. The phylogenetic features of the isolates were scrutinized and finally, the phenotypic characteristics were investigated using specific culture methods. Results: The results of morphological tests indicated that most isolates were Gram-negative and rod shape, which were able to grow between ˗4 and +37 ºC.‎ According to the phylogenetic analysis the isolated strains belong to Pseudomonas, Yersinia, Kocuria, and Micrococcus genera and about 60% of the isolates belong to the various species of Pseudomonas as a ‎dominant genus with abounded frequency. ‎In addition, several isolates showed 99% similarity with bacteria, which were previously isolated from Antarctic regions such as Pseudomonas antarctica and Micrococcus antarctica. Conclusion: It can be concluded that the microbial populations of cold areas is the same across the geographical distances. In addition, these bacterial strains could be a primitive source of new enzymes for technological applications such as biosurfactant production.


Solar Energy ◽  
1987 ◽  
Vol 38 (2) ◽  
pp. 135-136 ◽  
Author(s):  
J. Srinivasan ◽  
Abhijit Guha

2013 ◽  
Vol 448-453 ◽  
pp. 1521-1524
Author(s):  
Chun Juan Gao ◽  
Qi Zhang ◽  
Hai Hong Wu ◽  
Liang Wang ◽  
Xi Ping Huang

The solar ponds with a surface of 0.3m2were filled with different concentration salt water and fresh water. The three layer’s structure of solar ponds was formed in the laboratory ponds by using the salinity redistribution. The performance and diffusion of salinity were xperimentally in the solar pond. The measurements were taken and recorded daily at various locations in the salt-gradient solar pond during a period of 30 days of experimentation. The experimental results showed that the salinity gradient layer can sustain a longer time when the lower convective zone is thicker, which is benefit to store solar energy. Therefore, properly increasing the height of LCZ is a good method to enhance the solar pond performance.


2014 ◽  
Vol 137 (1) ◽  
Author(s):  
Amin Mobarak

This work is an extension and modification of the novel thermal cycle reported in the study “Techno-Economic Evaluation of a Novel Thermal Cycle for Electricity Generation and Fresh Water Production From Solar Ponds.” For low temperature power generation, such as the case of solar ponds or a field of solar flat plate collectors (60–90 °C), it is a common practice to use an organic Rankine cycle. The novel cycle uses water vapor as a working medium under pressure values lower than atmospheric. This is achieved by a turbovapor generating unit, a conventional low-pressure steam turbine, and a condenser working in an open cycle. Such a plant has a low thermal efficiency which approaches 12%, because of the small temperature range between evaporator and condenser (80–30 °C). The ratio of fresh water to electric power is also fixed for a certain temperature range (e.g., 14 tons/MW h for temperatures of 80 °C evaporator and 30 °C condenser). To increase the thermal utilization of the available heat flux and to achieve a variable fresh water production, a conventional multistage flash evaporation plant (MSF plant) is incorporated between the evaporator and condenser. The thermodynamic analysis of the plant shows that the thermal utilization of the available energy may reach 90%, while the amount of fresh water could be raised from 14 tons/MW h to 300 tons/MW h, for the same temperature range. This system has the advantage of being self-sufficient, yielding a net electric power after having supplied its own needs of pumping power.


Solar Energy ◽  
2015 ◽  
Vol 122 ◽  
pp. 1425-1428 ◽  
Author(s):  
Morteza Khalilian ◽  
Mina Shahrooz ◽  
Morteza Abbaszadeh

1996 ◽  
Vol 37 (3) ◽  
pp. 199
Author(s):  
I. Sezai ◽  
E. Tasdemiroglu
Keyword(s):  

1971 ◽  
Vol 11 (04) ◽  
pp. 351-355 ◽  
Author(s):  
M.M. El-Saleh ◽  
S.M. Farouq Ali

Abstract Results of an experimental study of oil recovery by a steam slug driven by a cold waterflood in a linear porous medium are described. The model included simulation of heat losses to the adjacent formations. Steam displacements were conducted, using a number of hydrocarbons and various steam-slug sizes, with the core initially containing a residual oil or irreducible water saturation. It was found that the steam-slug displacement is more efficient in the case of light oils than for the heavier ones. The injection of cold water following steam resulted in almost total condensation of the steam present in the porous medium, with the process degenerating into a hot waterflood. The oil process degenerating into a hot waterflood. The oil recovery efficiency of the process depends on whether an oil bank is formed during the steam-injection phase and whether the oil responds favorably to a hot phase and whether the oil responds favorably to a hot waterflood Introduction Steam injection has been shown to be an effective oil recovery method both by field and laboratory tests. However, the method has the inherent disadvantages of a high cost of operation and excessive heat losses. The modification discussed here consists in the injection of cold water after a slug of steam, which helps to offset the above disadvantages partly at the expense of oil recovery. The injected water serves to propel the oil bank formed ahead of the steam-invaded zone and transports the heat contained in the steam-swept zone farther downstream, thus leading to more complete utilization of the heat injected. EXPERIMENTAL APPARATUS AND PROCEDURE Fig. 1 depicts a schematic diagram of the apparatus employed. It consisted of a 4-ft-long core composed of a steel tube having a rectangular cross-section (see Table 1 for dimensions and other information) packed with glass beads (mesh size 200 to 270, corresponding to 0.0021 to 0.0029 in.) and fitted with 15 iron-constantan thermocouples and eight pressure gauges. The two ends of the core were fitted with sintered bronze plates to ensure strictly linear fluid flow. In order to simulate the underlying formations, the core was placed upon a sand-filled wooden box having a depth placed upon a sand-filled wooden box having a depth of 2.5 ft and a length and width equal to those of the core. An identical box was placed in contact with the top surface of the core to simulate the overlying formations. The sand packs simulated infinitely thick formations, since the temperatures at the upper and lower extremities remained undisturbed during a run. The sides of the two boxes were fitted with thermometers and insulated, together with the exposed surface of the core; the top and bottom surfaces of the core were in contact with sand. An electrical system was designed for temperature measurement at the 15 points; the core inlet and outlet were fitted with thermocouples. A technique was devised for pressure measurement virtually without disturbing the flow. A positive-displacement pump, in conjunction with a coil immersed in a high-temperature oil bath, was used for conducting hot waterfloods as well as for preparing the core for a run (Fig. 1). Steam, having a quality of 95 percent was supplied by an electric boiler capable of delivering up to 69 lb/hr at pressures up m 250 psig. The core effluent was passed though a suitable condenser provided with passed though a suitable condenser provided with a backpressure regulator used to control the steam injection rate. The average steam (as condensate) injection rate for a run was estimated by dividing the total effluent volume minus the volume of the water needed to fill up the core at the end of steam injection, by the steam injection time. The properties of the fluids used are listed in Table 1. The hydrocarbon mixtures were chosen to study the steam distillation effects. Drakeol 15 and 33 at 80 deg. F are high-boiling mineral oils having viscosities of 515 and 100.0 cp, respectively. Viscosity-temperature behavior for the hydrocarbons used is shown in Fig. 2. The core was saturated with distilled water and then saturated with the oil to be tested by displacement (terminal WOR 1:100). If desired, the core was waterflooded prior to steam injection (terminal WOR 100:1). SPEJ P. 351


2020 ◽  
Vol 12 (17) ◽  
pp. 2689
Author(s):  
Yan-Lun Wu ◽  
Ming-An Lee ◽  
Lu-Chi Chen ◽  
Jui-Wen Chan ◽  
Kuo-Wei Lan

Despite numerous studies on the effect of a cold weather disaster on fisheries in 2008, no operational systems have been developed to monitor the threat of such an event to mariculturists in the Penghu Islands (PHI) region of Taiwan. The present study employed a suitable aquaculture site selection map of the inner bay of the PHI to reduce aquaculture losses and mortality rates of cobia (Rachycentron canadum) during extreme events. Daily marine environmental data, including sea surface temperature (SST), chlorophyll-a concentration (chl-a), and wind speed in the winter, were collected. An extreme event was defined as a period of over 11 days in a month of strong winds (>6 m/s). Four parameters in the PHI inner bay, including SST, cold-water intrusion days, chl-a, and offshore distance to the PHI coastline, were used to evaluate suitable aquaculture sites for cobia culture. The results indicated that La Niña events could not be used as a factor to detect cold-water intrusion events and select suitable aquaculture sites in the PHI. The evaluated suitable aquaculture site selection map, obtained using an arithmetic mean model and a geometric mean model, revealed that the avoidance sites during extreme events were concentrated in the northern and northwestern PHI. Suitable areas were concentrated in the southeastern areas. We further suggested that commercial cobia aquaculture operations in the PHI inner bay could be moved to the suitable sites in southeastern PHI during extreme events.


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