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Journal articles on the topic 'High-salinity'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

Linarić, M., M. Markić, and L. Sipos. "High salinity wastewater treatment." Water Science and Technology 68, no. 6 (September 1, 2013): 1400–1405. http://dx.doi.org/10.2166/wst.2013.376.

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The shock effect, survival and ability of activated sludge to acclimatize to wastewater containing different concentrations of NaCl and Na2SO4 were investigated under laboratory conditions. To accomplish this, the potential penetration of a sewage system by seawater as a consequence of storm surge flooding was simulated. The experiments were conducted using activated sludge taken from the aeration tank of a communal wastewater treatment plant and adding different concentrations up to 40 g/L of NaCl and 4.33 g/L of Na2SO4. The effects of salinity on the activated sludge were monitored for 5 weeks based on the values of pH, dissolved oxygen, total suspended solids, volatile suspended solids, sludge volume, sludge volume index, electrokinetic potential, respirometric measurements and enzymatic activity. The addition of salt sharply reduced or completely inhibited the microbial activity in activated sludge. When salt concentrations were below 10 g/L NaCl, microorganisms were able to acclimatize in several weeks and achieve the same initial activity as in raw sludge samples. When the salt concentration was above 30 g/L NaCl, the acclimatization process was very slow or impossible.

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2

Glass, Charles, and JoAnn Silverstein. "Denitrification of high-nitrate, high-salinity wastewater." Water Research 33, no. 1 (January 1999): 223–29. http://dx.doi.org/10.1016/s0043-1354(98)00177-8.

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3

Weller, Andreas, Zeyu Zhang, and Lee Slater. "High-salinity polarization of sandstones." GEOPHYSICS 80, no. 3 (May 2015): D309—D318. http://dx.doi.org/10.1190/geo2014-0483.1.

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4

Cai, Weiwei, Qiuying Chen, Jingyu Zhang, Yan Li, Wenwen Xie, and Jingwei Wang. "Effects of High Salinity on Alginate Fouling during Ultrafiltration of High-Salinity Organic Synthetic Wastewater." Membranes 11, no. 8 (July 31, 2021): 590. http://dx.doi.org/10.3390/membranes11080590.

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Ultrafiltration is widely employed in treating high-salinity organic wastewater for the purpose of retaining particulates, microbes and macromolecules etc. In general, high-salinity wastewater contains diverse types of saline ions at fairly high concentration, which may significantly change foulant properties and subsequent fouling propensity during ultrafiltration. This study filled a knowledge gap by investigating polysaccharide fouling formation affected by various high saline environments, where 2 mol/L Na+ and 0.5–1.0 mol/L Ca2+/Al3+ were employed and the synergistic influences of Na+-Ca2+ and Na+-Al3+ were further unveiled. The results demonstrated that the synergistic influence of Na+-Ca2+ strikingly enlarged the alginate size due to the bridging effects of Ca2+ via binding with carboxyl groups in alginate chains. As compared with pure alginate, the involvement of Na+ aggravated alginate fouling formation, while the subsequent addition of Ca2+ or Al3+ on the basis of Na+ mitigated fouling development. The coexistence of Na+-Ca2+ led to alginate fouling formed mostly in a loose and reversible pattern, accompanied by significant cracks appearing on the cake layer. In contrast, the fouling layer formed by alginate-Na+-Al3+ seemed to be much denser, leading to severer irreversible fouling formation. Notably, the membrane rejection under various high salinity conditions was seriously weakened. Consequently, the current study offered in-depth insights into the development of polysaccharide-associated fouling during ultrafiltration of high-salinity organic wastewater.

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5

Dudchenko, Alexander V., Timothy V. Bartholomew, and Meagan S. Mauter. "High-impact innovations for high-salinity membrane desalination." Proceedings of the National Academy of Sciences 118, no. 37 (September 7, 2021): e2022196118. http://dx.doi.org/10.1073/pnas.2022196118.

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Reducing the cost of high-salinity (>75 g/L total dissolved solids) brine concentration technology would unlock the potential for vast inland water supplies and promote the safe management of concentrated aqueous waste streams. Impactful innovation will target component performance improvements and cost reductions that yield the highest impact on system costs, but the desalination community lacks methods for quantitatively evaluating the value of innovation or the robustness of technology platforms relative to competing technologies. This work proposes a suite of methods built on process-based cost optimization models that explicitly address the complexities of membrane-separation processes, namely that these processes comprise dozens of nonlinearly interacting components and that innovation can occur in more than one component at a time. We begin by demonstrating the merit of performing simple parametric sensitivity analysis on component performance and cost to guide the selection of materials and manufacturing methods that reduce system costs. A more rigorous implementation of this approach relates improvements in component performance to increases in component costs, helping to further discern high-impact innovation trajectories. The most advanced implementation includes a stochastic simulation of the value of innovation that accounts for both the expected impact of a component innovation on reducing system costs and the potential for improvements in other components. Finally, we apply these methods to identify innovations with the highest probability of substantially reducing the levelized cost of water from emerging membrane processes for high-salinity brine treatment.

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6

HEATH, M. R., E. W. HENDERSON, G. SLESSER, and E. M. S. WOODWARD. "High salinity in the North Sea." Nature 352, no. 6331 (July 1991): 116. http://dx.doi.org/10.1038/352116b0.

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7

Yale, Jaqueline, and Hans J. Bohnert. "Transcript Expression inSaccharomyces cerevisiaeat High Salinity." Journal of Biological Chemistry 276, no. 19 (February 14, 2001): 15996–6007. http://dx.doi.org/10.1074/jbc.m008209200.

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8

Safavi, Mohammadali, and Toraj Mohammadi. "High-salinity water desalination using VMD." Chemical Engineering Journal 149, no. 1-3 (July 1, 2009): 191–95. http://dx.doi.org/10.1016/j.cej.2008.10.021.

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9

Wu, Dihua, Aoran Gao, Hongting Zhao, and Xianshe Feng. "Pervaporative desalination of high-salinity water." Chemical Engineering Research and Design 136 (August 2018): 154–64. http://dx.doi.org/10.1016/j.cherd.2018.05.010.

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10

Alfazazi, Umar, Waleed AlAmeri, and Muhammad R. Hashmet. "Experimental investigation of polymer flooding with low-salinity preconditioning of high temperature–high-salinity carbonate reservoir." Journal of Petroleum Exploration and Production Technology 9, no. 2 (October 12, 2018): 1517–30. http://dx.doi.org/10.1007/s13202-018-0563-z.

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11

Grosso, Philippe, Marc Le Menn, Jean-Louis De Bougrenet De La Tocnaye, Zong Yan Wu, and Damien Malardé. "Practical versus absolute salinity measurements: New advances in high performance seawater salinity sensors." Deep Sea Research Part I: Oceanographic Research Papers 57, no. 1 (January 2010): 151–56. http://dx.doi.org/10.1016/j.dsr.2009.10.001.

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12

Logan, Bruce E., Jun Wu, and Richard F. Unz. "Biological Perchlorate Reduction in High-Salinity Solutions." Water Research 35, no. 12 (August 2001): 3034–38. http://dx.doi.org/10.1016/s0043-1354(01)00013-6.

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13

Kaplan, Lewis. "High salinity—Just what the intensivist ordered?*." Critical Care Medicine 40, no. 9 (September 2012): 2724–25. http://dx.doi.org/10.1097/ccm.0b013e31825bc810.

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14

Moulton, T. P., T. R. Sommer, M. A. Burford, and L. J. Borowitzka. "Competition between Dunaliella species at high salinity." Hydrobiologia 151-152, no. 1 (September 1987): 107–16. http://dx.doi.org/10.1007/bf00046115.

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15

Abu‐ghararah, Z. H., and J. H. Sherrard. "Biological nutrient removal in high salinity wastewaters." Journal of Environmental Science and Health . Part A: Environmental Science and Engineering and Toxicology 28, no. 3 (April 1993): 599–613. http://dx.doi.org/10.1080/10934529309375897.

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16

Zhang, Xiaodong, and Lianbo Hu. "Scattering by pure seawater at high salinity." Optics Express 17, no. 15 (July 20, 2009): 12685. http://dx.doi.org/10.1364/oe.17.012685.

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17

Grainger, E. H., and A. A. Mohammed. "High salinity tolerance in sea ice copepods." Ophelia 31, no. 3 (September 1, 1990): 177–85. http://dx.doi.org/10.1080/00785326.1990.10430860.

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18

Hoogakker, Babette A. A., Gary P. Klinkhammer, Harry Elderfield, Eelco J. Rohling, and Chris Hayward. "Mg/Ca paleothermometry in high salinity environments." Earth and Planetary Science Letters 284, no. 3-4 (July 2009): 583–89. http://dx.doi.org/10.1016/j.epsl.2009.05.027.

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19

Xie, Quan, Patrick V. Brady, Ehsan Pooryousefy, Daiyu Zhou, Yongbing Liu, and Ali Saeedi. "The low salinity effect at high temperatures." Fuel 200 (July 2017): 419–26. http://dx.doi.org/10.1016/j.fuel.2017.03.088.

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20

Laverty, Gary, and Erik Skadhauge. "Adaptation of teleosts to very high salinity." Comparative Biochemistry and Physiology Part A: Molecular & Integrative Physiology 163, no. 1 (September 2012): 1–6. http://dx.doi.org/10.1016/j.cbpa.2012.05.203.

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21

Juwarno, Juwarno, Tata Brata Suparjana, and Muachiroh Abbas. "Mahameru Soybean (Glycine max) Cultivar, High Salinity Tolerant." Biosaintifika: Journal of Biology & Biology Education 10, no. 1 (April 2, 2018): 23–31. http://dx.doi.org/10.15294/biosaintifika.v10i1.11870.

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Mahameru cultivar is high salinity tolerant cultivar. The previous study result showed Mahameru cultivar could tolerate 140mM NaCl, but Cilacap Coast salinity levels often reaching 200mM NaCl. A research of salinity stress on Mahameru cultivar at 200 mM NaCl have not conducted yet. Therefore to conduct the research of Mahameru at high salinity stress to obtained high salinity tolerant soybean cultivar. The observed variables are anatomy (epidermis thickness, the density of stomata and trichomes, palisade thickness) physiology (the dry weight of roots and canopy, the content of chlorophyll a and b) Production (whole pod, total filled pod, total empty pod, weight per one-hundred beans). The salinity treatment was 0, 50,100, 150, 200 mM NaCl given at three days before planting and twenty-one days after planting. The data of anatomy and physiology was taken at forty-five days after planting. The production data was taken when soybean plants turned brown. The result indicates that salinity affects anatomy characteristic of leaf, higher the salinity increasing epidermis thickness and the density of stomata and trichomes. Salinity affected the content of chlorophyll a and b. Higher the salinity increased the content of chlorophyll a and b. Salinity did not affect soybean production. Based on this study Mahameru cultivar is resistant to salinity up to 200 mM NaCl. The benefit of this research help to enhance national soybean production with utilization coastal land for soybean planting Mahameru cultivar.

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22

Puerto, Maura, George J. Hirasaki, Clarence A. Miller, and Julian R. Barnes. "Surfactant Systems for EOR in High-Temperature, High-Salinity Environments." SPE Journal 17, no. 01 (October 25, 2011): 11–19. http://dx.doi.org/10.2118/129675-pa.

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Summary A systematic study was made of phase behavior of alkoxyglycidylether sulfonates (AGESs). These surfactants were screened with either NaCl-only brines or NaCl-only brines and n-octane at water/ oil ratio (WOR) ~1 for temperatures between approximately 85 and 120°C. All test cases were free of alcohols and other cosolvents. Classical Winsor phase behavior was observed in most scans, with optimal salinities ranging from less than 1% NaCl to more than 20% NaCl for AGESs with suitable combinations of hydrophobe and alkoxy chain type [ethylene oxide (EO) or propylene oxide (PO)] and chain length. Oil solubilization was high, indicating that ultralow interfacial tensions existed near optimal conditions. The test results for 120°C at WOR~1 have been summarized in a map, which might provide a useful guide for initial selection of such surfactants for EOR processes. Saline solutions of AGESs separate at elevated temperatures into two liquid phases (the cloud-point phenomenon), which may be problematic when they are injected into high-temperature reservoirs. An example is provided that indicates that this situation can be alleviated by blending suitable AGES and internal olefin sulfonate (IOS) surfactants. Synergy between the two types of surfactant resulted in transparent, single-phase aqueous solutions for some blends, but not for the individual surfactants, over a range of conditions including in synthetic seawater. Such blends are promising because both AGES and IOS surfactants have structural features that can be adjusted during manufacture to give a range of properties to suit reservoir conditions (temperature, salinity, and crude-oil type).

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23

Sharma, Gaurav, and Kishore K. Mohanty. "Wettability Alteration in High-Temperature and High-Salinity Carbonate Reservoirs." SPE Journal 18, no. 04 (April 22, 2013): 646–55. http://dx.doi.org/10.2118/147306-pa.

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Summary The goal of this work was to change the wettability of a carbonate rock from mixed-wet toward water-wet at high temperature and high salinity. Three types of surfactants in dilute concentrations (<0.2 wt%) were used. Initial surfactant screening was performed on the basis of aqueous stability at these harsh conditions. Contact-angle experiments on aged calcite plates were conducted to narrow the list of surfactants, and spontaneous-imbibition experiments were conducted on field cores for promising surfactants. Secondary waterflooding was carried out in cores with and without the wettability-altering surfactants. It was observed that most but not all surfactants were aqueous-unstable by themselves at these harsh conditions. Dual-surfactant systems, mixtures of a nonionic and a cationic surfactant, increased the aqueous stability. Some of the dual-surfactant systems proved effective for wettability alteration and could recover could recover 70 to 80% OOIP (original oil in place) during spontaneous imbibition. Secondary waterflooding with the wettability-altering surfactant increased the oil recovery over the waterflooding without the surfactants (from 29 to 40% of OOIP).

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24

Carić, Marina, Nenad Jasprica, Marijeta Čalić, and Mirna Batistić. "Phytoplankton response to high salinity and nutrient limitation in the eastern Adriatic marine lakes." Scientia Marina 75, no. 3 (April 26, 2011): 493–505. http://dx.doi.org/10.3989/scimar.2011.75n3493.

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25

Nassabeh, Seyed Mohammad Mehdi, Afshin Davarpanah, and Joata Bayrami. "Simulation of low and high salinity water injection method to determine the optimum salinity." Petroleum Research 4, no. 4 (December 2019): 348–53. http://dx.doi.org/10.1016/j.ptlrs.2019.07.003.

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26

Held, Mirjam B. E., and Christopher D. G. Harley. "Responses to low salinity by the sea starPisaster ochraceusfrom high- and low-salinity populations." Invertebrate Biology 128, no. 4 (November 2009): 381–90. http://dx.doi.org/10.1111/j.1744-7410.2009.00175.x.

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27

Zhang, Yuhong, Yan Du, W. N. D. S. Jayarathna, Qiwei Sun, Ying Zhang, Fengchao Yao, and Ming Feng. "A Prolonged High-Salinity Event in the Northern Arabian Sea during 2014–17." Journal of Physical Oceanography 50, no. 4 (April 2020): 849–65. http://dx.doi.org/10.1175/jpo-d-19-0220.1.

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AbstractA prolonged high-salinity event in the northern Arabian Sea, to the east of the Gulf of Oman, during 2014–17 was identified based on Argo datasets. The prolonged event was manifested as enhanced spreading of the surface Arabian Sea high-salinity water and the intermediate Persian Gulf water. We used satellite altimetric data and geostrophic current data to understand the oceanic processes and the salt budget associated with the high-salinity event. The results indicated that the strengthened high-salinity advection from the Gulf of Oman was one of the main causes of the salinity increase in the northern Arabian Sea. The changes of the seasonally dependent eddies near the mouth of the Gulf of Oman dominated the strengthened high-salinity advection during the event as compared with the previous 4-yr period: the westward shifted cyclonic eddy during early winter stretched to the remote western Gulf of Oman, which carried the higher-salinity water to the northern Arabian Sea along the south coast of the Gulf. An anomalous eddy dipole during early summer intensified the eastward Ras Al Hadd Jet and its high-salinity advection into the northern Arabian Sea. In addition, the weakened low-salinity advection by coastal currents along the Omani coast caused by the weakened southwest monsoon contributed to the maintenance of the high-salinity event. This prolonged high-salinity event reflects the upper-ocean responses to the monsoon change and may affect the regional hydrography and biogeochemistry extensively.

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28

Etherington, J. R., H. Leith, and A. A. Al Masoon. "Towards the Rational Use of High Salinity Tolerant Plants, Vol. 1. Deliberations about High Salinity Tolerant Plants and Ecosystems." Journal of Ecology 81, no. 4 (December 1993): 832. http://dx.doi.org/10.2307/2261687.

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29

Wang, Hao. "Preliminary Study on Tracer of High Temperature and High Salinity Resistant." Advanced Materials Research 868 (December 2013): 473–76. http://dx.doi.org/10.4028/www.scientific.net/amr.868.473.

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Five kinds of new tracers of high temperature and high salinity resistant were screened in order to meet tracer monitoring requirements in Tarapoa block at Dorine oilfield, these tracers were evaluated according to the tracer selection criteria, the optimal detection method was also studied in this paper. It showed that new tracers can adapt to high temperature, high salinity of the formation conditions, so as to meet adjacent multi-well groups monitoring requirements. Tracer monitoring can provide basis for the next step implementation of the program and the adjustment of measures, of a bright application future.

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30

Shen, Hui, Li Li, Jianlong Li, Zhiguo He, and Yuezhang Xia. "The Seasonal Variation of the Anomalously High Salinity at Subsurface Salinity Maximum in Northern South China Sea from Argo Data." Journal of Marine Science and Engineering 9, no. 2 (February 20, 2021): 227. http://dx.doi.org/10.3390/jmse9020227.

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The large variations in salinity at the salinity maximum in the northern South China Sea (NSCS), as an indicator for the changes in the Kuroshio intrusion (KI), play an important role in the hydrological cycle. The high salinity here is more than 34.65 at the salinity maximum and is intriguing. In the past, the salinity was difficult to trace in the entire NSCS over long periods due to a lack of high-quality observations. However, due to the availability of accumulated temperature and salinity (T-S) profiles from the Argo program, it is now possible to capture subsurface-maximum data on a large spatiotemporal scale. In this study, the salinity maximum distributed in the subsurface of 80 to 200 m at a density of 23.0–25.5 σθ was extracted from decades of Argo data (on the different pressure surfaces, 2006–2019). We then further studied the spatial distribution and seasonal variation of the salinity maximum and its anomalously high salinity. The results suggest that a high salinity (salinity > 34.65, most of which is located at the shallow depths < 100 m) at the subsurface salinity-maximum layer often occurs in the NSCS, especially near the Luzon Strait, which accounts for about 23% of the total salinity maximum. In winter, the anomalously high salinity at the shallow subsurface salinity maximum can extend to the south of 17° N, while it rarely reaches 18° N and tends to locate at deeper waters in summer. The T-S values of the anomalously high-salinity water are between the mean T-S values in the NSCS and north Pacific subsurface water, implying that the outer sea water gradually mixes with the South China Sea water after passing through the Luzon Strait. Finally, our results show that the factors play an important role in the appearance and distribution of the anomalously high salinity at the subsurface salinity maximum, including the strength of the Kuroshio intrusion, the local wind stress curl and the anticyclonic eddy shedding from the loop current.

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31

Hoffmann, Tamara, Alexandra Schütz, Margot Brosius, Andrea Völker, Uwe Völker, and Erhard Bremer. "High-Salinity-Induced Iron Limitation in Bacillus subtilis." Journal of Bacteriology 184, no. 3 (February 1, 2002): 718–27. http://dx.doi.org/10.1128/jb.184.3.718-727.2002.

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ABSTRACT Proteome analysis of Bacillus subtilis cells grown at low and high salinity revealed the induction of 16 protein spots and the repression of 2 protein spots, respectively. Most of these protein spots were identified by mass spectrometry. Four of the 16 high-salinity-induced proteins corresponded to DhbA, DhbB, DhbC, and DhbE, enzymes that are involved in the synthesis of 2,3-dihydroxybenzoate (DHB) and its modification and esterification to the iron siderophore bacillibactin. These proteins are encoded by the dhbACEBF operon, which is negatively controlled by the central iron regulatory protein Fur and is derepressed upon iron limitation. We found that iron limitation and high salinity derepressed dhb expression to a similar extent and that both led to the accumulation of comparable amounts of DHB in the culture supernatant. DHB production increased linearly with the degree of salinity of the growth medium but could still be reduced by an excess of iron. Such an excess of iron also partially reversed the growth defect exhibited by salt-stressed B. subtilis cultures. Taken together, these findings strongly suggest that B. subtilis cells grown at high salinity experience iron limitation. In support of this notion, we found that the expression of several genes and operons encoding putative iron uptake systems was increased upon salt stress. The unexpected finding that high-salinity stress has an iron limitation component might be of special ecophysiological importance for the growth of B. subtilis in natural settings, in which bioavailable iron is usually scarce.

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32

Chow, WS, MC Ball, and JM Anderson. "Growth and Photosynthetic Responses of Spinach to Salinity: Implications of K+ Nutrition for Salt Tolerance." Functional Plant Biology 17, no. 5 (1990): 563. http://dx.doi.org/10.1071/pp9900563.

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To compare the effects of K+ under high and low salinity, spinach plants (Spinacia oleracea) were grown in nutrient solutions containing either 50 mM NaCl (low salinity) or 250 mM NaCl (high salinity), with a diurnal regime of 10 h light (~300 μmol photons m-2 s-1, 23°C) and 14 h dark (15°C). At each level of salinity, the nutrient KCl concentration was 0.01, 0.1, 1 or 10 mM. The plant and shoot biomass was greater at low salinity than high salinity and increased with the logarithmic increase in nominal K+ concentrations supplied to the roots. Plant and shoot growth were related to the K+ uptake into the leaves, with leaves having a higher K+ content under low salinity than high salinity. Variation of the K+ content in the leaves, induced by the combinations of nutrient KCl concentrations with high or low salinity, were accompanied by changes in the photosynthetic capacity at light- and CO2-saturation per unit leaf area; there was a greater decrease in photosynthetic capacity with decreasing K+ supply to the roots under high salinity than under low salinity. The photosynthetic capacity was in turn highly correlated with the contents of cytochrome f and ATP synthase per unit leaf area. Under conditions of high salinity and low K+ supply, a reduction in the quantum yield of oxygen evolution also occurred, due to malfunction of photosystem II and, apparently, an increased proportion of light absorbed by non-photosynthetic tissue. The decreases in photosynthetic capacity and quantum yield partly account for the lower plant and shoot biomass at high salinity and low nutrient KCl concentrations. Our results suggest strongly that there are higher K+ requirements for shoot growth under high than low salinity conditions, and that high concentrations of Na+ in the leaves may help to maintain turgor, but cannot substitute for adequate K+ levels in the leaves, presumably because K+ is specifically required for protein synthesis. Increasing the K+ supply at the roots can ameliorate reductions in plant and shoot biomass imposed by an increase in salinity.

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33

Haruna, Maje Alhaji, and Dongsheng Wen. "Stabilization of Polymer Nanocomposites in High-Temperature and High-Salinity Brines." ACS Omega 4, no. 7 (July 5, 2019): 11631–41. http://dx.doi.org/10.1021/acsomega.9b00963.

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34

Kamal, Muhammad Shahzad, Syed M. Shakil Hussain, Lionel Talley Fogang, and Izhar A. Malik. "Development of Polyoxyethylene Zwitterionic Surfactants for High‐Salinity High‐Temperature Reservoirs." Journal of Surfactants and Detergents 22, no. 4 (March 21, 2019): 795–806. http://dx.doi.org/10.1002/jsde.12278.

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35

Gao, Bo, Qi Yan Feng, and Xiang Dong Li. "Clarification of High-Salinity Mine Water with Plants." Advanced Materials Research 610-613 (December 2012): 1398–401. http://dx.doi.org/10.4028/www.scientific.net/amr.610-613.1398.

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High-salinity mine water has been often treating with electrodialysis, multi-effect. But there are still some problems. So we study high-salinity mine water treatment for 24 days with different plants and salinity. The sample was selected from Zhang Xiao Lou coal in Xuzhou. The resultes show that: Cress is able to adapt the water with high salinity and absorb the contamination. When the dosage of NaCl is 1 g/L and 2 g/L, TDS removal efficiency can reach 69.36% and 56.47%. With the increase of NaCl from 0 to 1 g/L, the treatment capacity of the plant increased gradually, and the treatment capacity would decline if the dosage sustained increase. TDS removal efficiency was best, when the dosage of NaCl is 1 g/L, respectively: 56.47%, 50.21% and 44.00% with different plants, and the plants also has a good effect on the removal of COD and nutrient element when the dosage of NaCl is 1 g/L.

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36

Min, Jin-Hong, Joong-Chun Kwon, Donghyuk Choi, and Taedong Kim. "The Wastewater Treatment Process for High Salinity Wastewater." Journal of the Korean Society of Urban Environment 18, no. 1 (March 31, 2018): 35–39. http://dx.doi.org/10.33768/ksue.2018.18.1.35.

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37

Lippi, G., G. Serra, P. Vernieri, and F. Tognoni. "RESPONSE OF POTTED CALLISTEMON SPECIES TO HIGH SALINITY." Acta Horticulturae, no. 609 (May 2003): 247–50. http://dx.doi.org/10.17660/actahortic.2003.609.36.

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38

AbdelRazek, A. Y., and R. K. Rowe. "Performance of GCLs in high salinity impoundment applications." Geosynthetics International 26, no. 6 (December 2019): 611–28. http://dx.doi.org/10.1680/jgein.19.00043.

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39

Chou, S. I., and J. H. Bae. "Phase-Behavior Correlation for High- Salinity Surfactant Formulations." SPE Reservoir Engineering 3, no. 03 (August 1, 1988): 778–90. http://dx.doi.org/10.2118/14913-pa.

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40

Algharaib, M., A. Alajmi, and R. Gharbi. "Improving polymer flood performance in high salinity reservoirs." Journal of Petroleum Science and Engineering 115 (March 2014): 17–23. http://dx.doi.org/10.1016/j.petrol.2014.02.003.

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41

Bryan, Frank. "High-latitude salinity effects and interhemispheric thermohaline circulations." Nature 323, no. 6086 (September 1986): 301–4. http://dx.doi.org/10.1038/323301a0.

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PAPADOPOULOS, I. "SOIL SALINITY AS AFFECTED BY HIGH-SULFATE WATER." Soil Science 140, no. 5 (November 1985): 376–81. http://dx.doi.org/10.1097/00010694-198511000-00009.

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Black, Michael J., Mahmood Alhusseini, and Mohamed Nabil Noui-Mehidi. "High Salinity Permittivity Models for Water Cut Sensing." IEEE Transactions on Instrumentation and Measurement 62, no. 10 (October 2013): 2805–11. http://dx.doi.org/10.1109/tim.2013.2263912.

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Malardé, D., Z. Y. Wu, P. Grosso, J.-L. de Bougrenet de la Tocnaye, and M. Le Menn. "High-resolution and compact refractometer for salinity measurements." Measurement Science and Technology 20, no. 1 (December 8, 2008): 015204. http://dx.doi.org/10.1088/0957-0233/20/1/015204.

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Saner, Salih, M. Namik Cagatay, and Mahamadu Sumani. "Electrical resistivity behavior of high salinity brine suspensions." Powder Technology 93, no. 3 (October 1997): 275–82. http://dx.doi.org/10.1016/s0032-5910(97)03284-1.

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Guzman-Sepulveda, Jose Rafael, Victor Ivan Ruiz-Perez, Miguel Torres-Cisneros, Jose Javier Sanchez-Mondragon, and Daniel Alberto May-Arrioja. "Fiber Optic Sensor for High-Sensitivity Salinity Measurement." IEEE Photonics Technology Letters 25, no. 23 (December 2013): 2323–26. http://dx.doi.org/10.1109/lpt.2013.2286132.

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Koutinas, G. "High salinity fluid handling in Milos geothermal field." Geothermics 18, no. 1-2 (January 1989): 175–82. http://dx.doi.org/10.1016/0375-6505(89)90025-4.

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Liu, Chunshuang, Chaocheng Zhao, Aijie Wang, Yadong Guo, and Duu-Jong Lee. "Denitrifying sulfide removal process on high-salinity wastewaters." Applied Microbiology and Biotechnology 99, no. 15 (March 17, 2015): 6463–69. http://dx.doi.org/10.1007/s00253-015-6505-5.

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余, 欢. "Summary of Mine Water Treatment with High Salinity." Advances in Environmental Protection 11, no. 02 (2021): 299–303. http://dx.doi.org/10.12677/aep.2021.112031.

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Liu, Jianwei, Wei Zhang, Shujie Long, and Chunzhao Zhao. "Maintenance of Cell Wall Integrity under High Salinity." International Journal of Molecular Sciences 22, no. 6 (March 23, 2021): 3260. http://dx.doi.org/10.3390/ijms22063260.

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Abstract:

Cell wall biosynthesis is a complex biological process in plants. In the rapidly growing cells or in the plants that encounter a variety of environmental stresses, the compositions and the structure of cell wall can be dynamically changed. To constantly monitor cell wall status, plants have evolved cell wall integrity (CWI) maintenance system, which allows rapid cell growth and improved adaptation of plants to adverse environmental conditions without the perturbation of cell wall organization. Salt stress is one of the abiotic stresses that can severely disrupt CWI, and studies have shown that the ability of plants to sense and maintain CWI is important for salt tolerance. In this review, we highlight the roles of CWI in salt tolerance and the mechanisms underlying the maintenance of CWI under salt stress. The unsolved questions regarding the association between the CWI and salt tolerance are discussed.

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