Water Quality Monitoring and Management 2019
DOI: 10.1016/b978-0-12-811330-1.00009-0
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Seawater Quality Detection

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Cited by 5 publications
(4 citation statements)
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“…However, if LC-coacervates were to have participated in primitive biochemistries on early Earth, they likely would have necessarily resided in oceanic environments due to the requirement of high salinities relative to freshwater environments and physiological conditions for assembly. The salinity of the modern ocean is roughly 35 g/L, which corresponds to ~600 mM NaCl (this assumes that most of the salt is NaCl, although there are a number of other species present at lower concentrations) [86], and appears to suggest that some LC-coacervate phases are compatible with an ocean environment in the absence of temperature modulations (Figure 1) [63]. However, upon modulation of temperature, plausibly caused by seasonal or diurnal changes, or salinity, less restrictive environmental conditions could allow for more LC-coacervate phases to assemble.…”
Section: Relevance Of Lc-coacervates To Prebiotic Oceansmentioning
confidence: 99%
“…However, if LC-coacervates were to have participated in primitive biochemistries on early Earth, they likely would have necessarily resided in oceanic environments due to the requirement of high salinities relative to freshwater environments and physiological conditions for assembly. The salinity of the modern ocean is roughly 35 g/L, which corresponds to ~600 mM NaCl (this assumes that most of the salt is NaCl, although there are a number of other species present at lower concentrations) [86], and appears to suggest that some LC-coacervate phases are compatible with an ocean environment in the absence of temperature modulations (Figure 1) [63]. However, upon modulation of temperature, plausibly caused by seasonal or diurnal changes, or salinity, less restrictive environmental conditions could allow for more LC-coacervate phases to assemble.…”
Section: Relevance Of Lc-coacervates To Prebiotic Oceansmentioning
confidence: 99%
“…Seawater in the world's oceans has a salinity average of about 3.5% (35 g/L, 599 mM) [27]. In general, seawater pH ranges between 7.5 and 8.4 [27,28].…”
Section: Methods and Setting Experimentsmentioning
confidence: 99%
“…Seawater in the world's oceans has a salinity average of about 3.5% (35 g/L, 599 mM) [27]. In general, seawater pH ranges between 7.5 and 8.4 [27,28]. Seawater salinity is not uniformly distributed throughout the world, whereas, the majority of seawater has a salinity of between 31 g/kg and 38 g/kg [29].…”
Section: Methods and Setting Experimentsmentioning
confidence: 99%
“…Seawater is an inexhaustible water resource, attributed to its extensive geographic coverage on Earth (i.e., about 97 percent of water reserves on the Earth are saline) [ 13 ]. Seawater has an average salinity of 3.5% (35 g/L) globally, where the dissolved salts are composed predominantly of sodium (Na + ) and chloride (Cl - ) ions [ 14 ]. The high availability of seawater offers tremendous benefits for the application of photocatalytic H 2 evolution reaction (HER), especially for areas where pure water is not accessible.…”
Section: Introductionmentioning
confidence: 99%