Investigation of the Precipitation of Calcium Sulfate Scale during Low and High Salinity Water Injection in EOR Processes In carbonate and Sandstone Reservoirs

2013 ◽  
Author(s):  
Khaled Abd Elgawad ◽  
M. Mahmoud
Keyword(s):  
Calcium Sulfate ◽  
High Salinity ◽  
Water Injection ◽  
High Salinity Water ◽  
Calcium Sulfate Scale ◽  
Salinity Water ◽  
Eor Processes ◽  
Sandstone Reservoirs

scholarly journals Simulation of low and high salinity water injection method to determine the optimum salinity

2019 ◽  
Vol 4 (4) ◽  
pp. 348-353
Author(s):  
Seyed Mohammad Mehdi Nassabeh ◽  
Afshin Davarpanah ◽  
Joata Bayrami
Keyword(s):  
High Salinity ◽  
Water Injection ◽  
Injection Method ◽  
High Salinity Water ◽  
Salinity Water ◽  
Optimum Salinity

Monthly Water Exchange through the Ryukyu Islands Revealed by Salinity Structural Changes

2013 ◽  
Vol 864-867 ◽  
pp. 2335-2339
Author(s):  
Ya Pan Liu ◽  
Jian Cheng Kang ◽  
Jiong Zhu ◽  
Qin Chen Han
Keyword(s):  
Structural Changes ◽  
Water Exchange ◽  
High Salinity ◽  
World Ocean ◽  
Core Layer ◽  
Ryukyu Islands ◽  
High Salinity Water ◽  
The Ryukyu Islands ◽  
Salinity Water ◽  
World Ocean Atlas

Using salinity database of World Ocean Atlas 2009 (WOA09) issued by NOAA in 2010, refer the range of high-salinity tongue to indicate the strength about high-salinity water, from the perspective of structural changes of salinity; the water exchange through Ryukyu Islands upper 500 m have been analyzed, the results show that: due to Ryukyu Trough, currents on both sides of Ryukyu Islands occur exchange, for upper 500 m, high-salinity water in east of the Ryukyu Islands mainly invade the west waterthe Kuroshio in East China Sea; the intrusion strength is powerful from the depth of 100 m to 200 m, and the 150 m layer is the core layer of high-salinity water intrusion; the high-salinity water at the east of Ryukyu Islands invades the Kuroshio are stronger in March, May, June, September, October and November, are weaker in April and December.

scholarly journals Preliminary assessment of the potential for mangrove oyster cultivation in Piraquê-açu river estuary (Aracruz, ES)

2006 ◽  
Vol 49 (1) ◽  
pp. 163-169 ◽  
Author(s):  
Luciana Alvarenga ◽  
Rosebel Cunha Nalesso
Keyword(s):  
High Salinity ◽  
Shell Height ◽  
River Estuary ◽  
Oyster Shell ◽  
Preliminary Assessment ◽  
High Salinity Water ◽  
Salinity Water ◽  
High Predation ◽  
Fouling Organisms ◽  
Oyster Cultivation

At Piraquê-açu river estuary, Aracruz, ES, the technical viability of Crassostrea rhizophorae cultivation was determined through monthly measures in shell length and weight. Seeds of C. rhizophorae were put in cages and suspended in rafts. Increase in height and weight (flesh and dry) of the oysters was measured. During ten months (July/98 to May/99), oyster shell reached an average of 37.6 mm in shell height and 3.0 g in flesh weight (the whole animal). High mortality rates were registered and could be related to the high salinity water and to high predation observed, especially by flatworms Stylochophana divae and snails Cymatium parthenopeum, as well as fouling organisms such as barnacles, Serpulidae polychaetes and seed of the same species.

Effective removal of 60Co from high-salinity water by Ca–Mg phosphate sorbents

2018 ◽  
Vol 318 (3) ◽  
pp. 2341-2347 ◽  
Author(s):  
Andrei Ivanets ◽  
Natalja Kitikova ◽  
Irina Shashkova ◽  
Artem Radkevich ◽  
Lyudmila Shemet ◽  
...  
Keyword(s):  
High Salinity ◽  
High Salinity Water ◽  
Effective Removal ◽  
Salinity Water

Trace element determination in high-salinity water using an online ion imprinted helical tube demineralizer combined with ICP-MS

2020 ◽  
Vol 35 (7) ◽  
pp. 1306-1315
Author(s):  
Hongyan Li ◽  
Bei Zheng ◽  
Chunfu Li ◽  
Jiale Zheng ◽  
Yanfen Zhang
Keyword(s):  
High Salinity ◽  
Matrix Interference ◽  
Element Determination ◽  
High Salinity Water ◽  
Icp Ms ◽  
Ion Imprinted ◽  
Helical Tube ◽  
Trace Elements In Water ◽  
Salinity Water ◽  
P Matrix

Matrix interference is a common problem in the measurement of trace elements in water via ICP-MS.

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