ライフサイエンスコーパス: seawater

1 e dissolve (13)C-labeled calcites in natural seawater.

2 rtion, we isolated the colloidal fraction of seawater.

3 40 nm) was required for stable dispersion in seawater.

4 t only octocrylene was stable in chlorinated seawater.

5 nisms responsible for calcite dissolution in seawater.

6 s are dominating sources of (236)U in Danish seawater.

7 ajor sink of many elements and alkalinity in seawater.

8 does not contribute significantly to PFOS in seawater.

9 is formed rapidly when chlorine is added to seawater.

10 larval swimming patterns in control and DMS seawater.

11 levels of phytoplankton and bacteria in the seawater.

12 ice OCP burdens originate from both snow and seawater.

13 a surface microlayer (SSML) relative to bulk seawater.

14 ndwater were characterized and compared with seawater.

15 es in other environments, including soil and seawater.

16 in contact with divalent cations as found in seawater.

17 f carbohydrates in unsterilized, non-potable seawater.

18 The emitted CO2 increases the acidity of seawater.

19 e abundant in tropical and temperate coastal seawater.

20 cal behavior in contaminated tidal flats and seawater.

21 arse SSA, sea-surface microlayer or in fresh seawater.

22 rt materials for collecting uranium (U) from seawater.

23 luding synthetic hard water, pond water, and seawater.

24 (biofouling) on different solid surfaces in seawater.

25 ing of biological DMSO production in surface seawater.

26 c juvenile which migrates from freshwater to seawater.

27 w Ca and Sr relative to Mg and SO4 in modern seawater.

28 one pore-water salinity to be double that of seawater.

29 association with the elevated delta(18)O of seawater.

30 rough bubble bursting, analogous to SSA from seawater.

31 ce from controlled mixing of river water and seawater.

32 profile significantly different from that of seawater.

33 n nutrient-enriched and natural oligotrophic seawater.

34 is demonstrated with pH measurements in U.K. seawater.

35 xposed to low levels of H2O2 or incubated in seawater.

36 ng for the cycles of the major components of seawater.

37 experiments with river water and artificial seawater.

38 eir primary spines is in direct contact with seawater.

39 plying that (236)U behaves conservatively in seawater.

40 form of arsenic that has never been found in seawater.

41 raviolet absorbance spectra in lead-enriched seawater.

42 oherent with previously reported patterns in seawater.

43 ate-limiting step for calcite dissolution in seawater.

44 t on the flux of K between oceanic crust and seawater.

45 nd distal intestine of 67.3 g salmon kept in seawater (12-14 degrees C) and fed a commercial diet for

46 resence of 15 additional organoarsenicals in seawater, 14 of which had never been detected in marine

47 sting skeleton, separated from the overlying seawater [2].

48 Seawater (234)U/(238)U provides global-scale information

49 Here we report two seawater (234)U/(238)U records based on well-preserved d

50 3)C and a range of uplift proxies, including seawater (87)Sr/(86)Sr, which demonstrates how erosional

51 when low-seawater SO4 could help explain low seawater (87)Sr/(86)Sr.

52 Due to the high toxin levels found in seawater, a procedure for a rapid and efficient determin

53 chery with that of their full-siblings after seawater acclimatisation (SW) by a 16S rRNA (V3-V4) high

54 nd ammonia nitrogen, decrease P removal from seawater, activate the glyoxylate cycle, and reduce infe

55 aters, but it is unknown whether exposure to seawater after rainstorms increases rates of acute illne

56 , olivine weathering is expected to increase seawater alkalinity, thus resulting in additional CO2 up

57 work focuses on the occurrence of (236)U in seawater along Danish coasts, which is the sole water-ex

58 ction zone fluids via the composition of the seawater-altered oceanic lithosphere.

59 Future application of the new method for seawater analysis will shed new light on the biogeochemi

60 yrcene, delta3-carene, ocimene, limonene) in seawater and air during three cruises in the Arctic and

61 d from cellobiose and xylose in unsterilized seawater and algal-contaminated wastewater.

62 s were used to determine the salinity in the seawater and brackish water of the Baltic Sea.

63 ndicator dye suitable for pH measurements in seawater and conservative seawater-derived brines at sal

64 nvironments with frequent exposure to low pH seawater and consistent food.

65 lectricity from salinity differences between seawater and freshwater.

66 eratorPFAS ranged from 94 to 420 pg L(-1) in seawater and from 3.1 to 16 ng gdw(-1) in plankton.

67 FIB, MST markers, and pathogens measured in seawater and in gull, cat, and raccoon feces.

68 ntial removal of (65)Cu by iron oxides, left seawater and marine biomass depleted in (65)Cu but enric

69 f iodide-mediated ozone (O3) deposition over seawater and marine halogen chemistry accounted for in b

70 rations can increase by 100000 times between seawater and marine phytoplankton, but levels vary acros

71 not purely be driven by metal speciation in seawater and may be far more diverse than either single-

72 ter can affect the chemical exchange between seawater and oceanic basalt in hydrothermal systems at m

73 , are significantly more abundant in surface seawater and on shorelines than larger plastic particles

74 lthy sea lions, as well as those of adjacent seawater and other hosts.

75 could reach as high as 4.0 times that of the seawater and river water system, (2) the power density m

76 the initial stage, where both compartments (seawater and river water) have the same thickness and th

77 Microscopic examination of fixed seawater and sea ice samples revealed chytrids parasitiz

78 est concentrations of all analytes in Arctic seawater and sea-ice meltwater samples (224-253 and 34.7

79 The distribution profile between seawater and sea-ice showed a compound-dependency for Ar

80 ulfidic conditions, no fractionation between seawater and sediment should be observed if molybdate (M

81 mination of the dispersed radionuclides from seawater and soil, due to the huge amounts of coexisting

82 lumes of fine oil droplets in Gulf of Mexico seawater and successfully replicated the enrichment and

83 -time video multiple-corer to collect bottom seawater and surface sediments at vent sites.

84 concentrations and isotopic compositions in seawater and surface sediments from the Amundsen Sea con

85 a decrease in hydrothermal exchange between seawater and the ocean crust.

86 ass spectrometry to measure arsenobetaine in seawater, and apply the method to samples of seawater co

87 een natural and anthropogenic radionuclides, seawater, and diverse marine biota provide a unique wind

88 face snow, streams from melted snow, coastal seawater, and plankton samples were collected over a thr

89 Marine animals, seawater, and sediment near Fukushima, Japan have become

90 ased from 40 to 60 nm to >1 mm within 1 h in seawater, and the aggregates were highly polydispersed.

91 2) are causing ocean acidification, lowering seawater aragonite (CaCO3) saturation state (Omega arag)

92 ndicate that (236)U concentrations in Danish seawater are distributed within a relatively narrow rang

93 examples of these in freshwater and coastal seawater are fulvic and humic acids.

94 (236)U/(238)U atomic ratios in Danish seawater are more than 4 times higher than the estimated

95 at the colloids of NaEu(CO3)2.nH2O formed in seawater are taken up by A. cavernicola with no evidence

96 rom those of other mammals, dietary fish and seawater, are highly diverse and vary according to body

97 e groundwater was significantly favored over seawater as a feed source in terms of chemical compositi

98 PW injection volumes by 50% using brines and seawater as draw solutions (DS).

99 n contrast to previous studies that consider seawater as the most saline source to a coastal aquifer

100 aluated for its analytical performance using seawater as well lake water and groundwater spiked with

101 phate-enriched spring water mixing with cold seawater at the tufa-column-apex.

102 ies, desalination (the removal of salts from seawater) at high energy efficiency will likely become a

103 ical state of selected bacterial species and seawater bacterial community in comparison with four com

104 rentiation of ascidian symbionts compared to seawater bacterioplankton, and distinct microbial commun

105 h's oceans, critical to our understanding of seawater biogeochemistry, its long-timescale geologic hi

106 in over 100 environmental samples including seawater, bird eggs, fish, dolphin blubber, and in the b

107 ticipated feed streams are natural river and seawater, both of which contain not only monovalent ions

108 m chloride (NaCl), equivalent to salinity of seawater, brine at 50% and 75% water recovery, respectiv

109 ope compositions in saline solutions such as seawater, brines, and formation waters.

110 hange rates of selected OCPs between air and seawater, but are not expected to reverse their directio

111 f global warming, such deep recirculation of seawater can accelerate the melting of methane hydrates

112 is conserved, despite substantial changes in seawater carbonate chemistry between the modern and glac

113 thm for spectrophotometric determinations of seawater carbonate ion concentrations ([CO3(2-)]spec) de

114 marine olivine weathering and its effect on seawater-carbonate chemistry remain poorly understood.

115 vestigated the extent to which recirculating seawater carries fecal indicators, Enterococcus and bird

116 Acidification of seawater caused by anthropogenic carbon dioxide (CO2) is

117 The seawater chemistry effects can be expressed in terms of

118 In providing results from the first seawater chemistry manipulation experiment of a natural

119 seawater, and apply the method to samples of seawater collected at various depths from seven sites in

120 Seawater collected in 2013 and 2014 were analyzed for (2

121 Traditionally, both river water and seawater compartments have a fixed intermembrane distanc

122 compartments are compressed by expanding the seawater compartments.

123 ed surface layers containing minor inorganic seawater components such as magnesium and calcium.

124 ffect provides a modest negative feedback on seawater composition and (87)Sr/(86)Sr changes.

125 Based on our measured seawater concentrations and a global model simulation, w

126 day coral reefs are threatened by changes to seawater conditions associated with rapid anthropogenic

127 periments under nutrient-amended and natural seawater conditions, and show that it is not the concent

128 er competitive fertilisation success in both seawater conditions.

129 rbents following deployment in environmental seawater confirms V binding solely by the imide-dioximes

130 nd also indicates significant possibility of seawater contamination through subsurface conduit networ

131 Near-equilibrium calcite dissolution in seawater contributes significantly to the regulation of

132 ce snow (CSD/CSnow), snowmelt (CSD/CSM), and seawater (CSD/CSW) were close to 1 (from 0.44 to 1.4) fo

133 In this study we present new seawater data of (236)U and (238)U sampled in the North

134 Field studies on soil and seawater decontaminations in Fukushima gave satisfactory

135 and aquarium water, as well as dechloridized seawater) decreases the pH down to approximately 5.

136 The mid-Spathian shift in seawater delta(13)CDIC to typical thermocline values is

137 om the North Icelandic shelf, in relation to seawater density variability and demonstrate that solar

138 pH measurements in seawater and conservative seawater-derived brines at salinities (S) between 35 and

139 and Ordovician, hydrothermal fluids had more seawater-derived Sr and Ca, a prediction that is support

140 While seawater desalination brine is a seemingly attractive hi

141 Reverse osmosis (RO) seawater desalination is currently a widespread means of

142 alization potential for applications such as seawater desalination or industrial wastewater reuse may

143 ) membrane coupons used in the high recovery seawater desalination process.

144 y, rechargeable desalination cell for use in seawater desalination.

145 -coagulating fractions of 32 groundwater and seawater DOM samples along a salinity gradient from a sh

146 Compared with no exposure, exposure to seawater during dry weather increased incidence rates of

147 Fecal indicator bacteria measured in seawater (Enterococcus species, fecal coliforms, total c

148 st estimates of rates of acute illness after seawater exposure during both dry- and wet-weather perio

149 Urban coastal seawater exposure increases the incidence rates of many

150 he concentration levels occurring in coastal seawaters, Fe acts not as a toxic agent but as an essent

151 ed gilt-head bream (Sparus aurata) to AMI in seawater for 7 days at two concentrations (0.2 mug/L and

152 ementary sampling of air, snow, sea-ice, and seawater for a range of organochlorine pesticides (OCPs)

153 ce ocean decreases the buffering capacity of seawater for CO2, whilst photosynthetic carbon fixation

154 aracterization factors for metals in coastal seawater for use in life cycle assessment.

155 and hydroxypalytoxin) in both soft coral and seawater from a home marine aquarium involved in the poi

156 terile alginate particles to microcosms with seawater from coastal California, a habitat rich in algi

157 arge overpressures, capable of recirculating seawater from the seafloor to depth in the sediment laye

158 Estimated air-seawater fugacity ratios and fluxes indicate a current n

159 tion always increases pore-water salinity by seawater-groundwater mixing dynamics.

160 ate that, relative to freshwater conditions, seawater halides can increase photodegradation rates of

161 er samples demonstrated that the presence of seawater halides increased quantum yields for microcysti

162 omputational kinetic modeling indicates that seawater halogen radical concentrations are two to three

163 rials can involve the direct ozone activated seawater halogenation of N-methylbipyrrole precursors.

164 nt was different from that of seawater while seawater harboured local bacterial assemblages in respon

165 Oil samples were spread over seawater in a jacketed beaker held at 27.0 degrees C and

166 boratory generated SSA produced from natural seawater in a marine aerosol reference tank.

167 transfer efficiency of basaltic Ca and Sr to seawater in hydrothermal systems, which varies by a fact

168 NPP) accident, the distribution of (90)Sr in seawater in the coast off Japan has received limited att

169 current elevated Fukushima (137)Cs levels in seawater in the eastern North Pacific are equivalent to

170 challenges in extracting potable water from seawater including salt accumulation and long-term evapo

171 tial to exacerbate carbon steel corrosion in seawater incubations with and without a hydrocarbon-degr

172 phobicity even after 30 days of immersion in seawater, indicating its good stability in marine enviro

173 stal aquifer system, thereby concluding that seawater infiltration always increases pore-water salini

174 nthesis of hydrocarbons during oceanic crust-seawater interactions.

175 ifers which penetrate beneath the freshwater-seawater interface.

176 aper documents the first and longest case of seawater intrusion in the WKP, and also indicates signif

177 creases in conductivity are directly tied to seawater intrusion moving inland and traveling 11 miles

178 ls of bromide (Br(-)) and iodide (I(-)) from seawater intrusion or high mineral content in the source

179 Recirculating seawater is an important component of submarine groundwa

180 an that of igneous rocks, so the addition of seawater K to oceanic crust would be expected to generat

181 on transport, even at salinities that exceed seawater levels, and their ion selectivity can be tuned

182 shallow marine environment, as indicated by seawater-like rare-earth element plus yttrium trace elem

183 bjected to rotational agitation in different seawater media for periods of days to months.

184 When cells were shifted from white light D2O-seawater medium to far-red light H2O-seawater medium, th

185 Chl f from H. hongdechloris grown in 50% D2O-seawater medium under different light conditions.

186 ght D2O-seawater medium to far-red light H2O-seawater medium, the observed deuteration in Chl f indic

187 asured fish eDNA shedding and decay rates in seawater mesocosms.

188 y 1.6 over the Phanerozoic, with minima when seawater Mg and SO4 are low.

189 clay formation, contributing to the rise in seawater Mg/Ca and decline in atmospheric CO2 over the p

190 responsible for global cooling and increased seawater Mg/Ca over the past 50 million years.

191 The seawater microalga Nannochloropsis gaditana is capable o

192 nea, and P. zorritensis (n = 5), and ambient seawater (n = 4), were collected in Wrightsville Beach,

193 nses to environmental variables (tidal flat, seawater, naphthalene, and pyruvate) and exhibited certa

194 hthalene (TF-N), tidal flat-pyruvate (TF-P), seawater-naphthalene (SW-N), and seawater-pyruvate (SW-P

195 and a mean residence time for dissolved V in seawater of about 130,000 y with respect to inputs from

196 The phototroph adapted to seawater oligotrophy by reducing its selective leakiness

197 eries measurements of (134)Cs and (137)Cs in seawater on Line P and on the CLIVAR-P16N 152 degrees W

198 s, suggesting a modulating effect of natural seawaters on Ag toxicity.

199 erage ANG abundance were found in either the seawater or sediment, which is consistent with the hypot

200 on of a variety of natural and anthropogenic seawater organics may be a significant process occurring

201 e volume that we simulate is equivalent to a seawater oxygen isotope signal of 0.52-0.66 per thousand

202 also increases significantly (by 4%) at low seawater pCO2 in one genotype.

203 ons, but varies significantly in response to seawater pCO2 in two genotypes of Porites lutea, whilst

204 Increasing seawater pCO2 leads to ocean acidification (OA) with a r

205 alaeoclimate reconstruction), cultured under seawater pCO2 reflecting modern, future (year 2100) and

206 Ca increases significantly (by 2-4%) at high seawater pCO2 relative to modern in both genotypes, and

207 des) under an ecologically relevant range of seawater pH (7.5 to 8.3 total scale).

208 Reduction in seawater pH due to rising levels of anthropogenic carbon

209 The biological impacts of seawater pH have additional, important implications for

210 cification, respiration, and spine repair on seawater pH suggests that foraminifera will likely be ch

211 We constrain seawater pH through time by accounting for the cycles of

212 l physiology is currently in flux, including seawater pH, pCO2, temperature, redox chemistry, irradia

213 re we present boron isotope data-a proxy for seawater pH-that show that the ocean surface pH was pers

214 low pH, thus appearing most sensitive to low seawater pH.

215 ast growth in nitrogen-deficient and aerobic seawater probably correlated with high expression of glu

216 Seawater produces mineralo-organic particles following s

217 is saline groundwater with salinity close to seawater, pumped from beach wells in coastal aquifers wh

218 ate (TF-P), seawater-naphthalene (SW-N), and seawater-pyruvate (SW-P).

219 of up to approximately 1,900 times above the seawater ratio of I(-)/Na(+), consistent with iodine act

220 the mid-Cretaceous, the low (87)Sr/(86)Sr of seawater requires either exceptionally large amounts of

221 d removal of organic compounds from a shared seawater reservoir.

222 etals was found in the LMEs with the longest seawater residence times.

223 nitude across LMEs, largely due to different seawater residence times.

224 oning, diffusion and separation on a typical seawater reverse osmosis (RO) membrane.

225 to the determination of Cu in tap, river and seawater, rice flour and black tea samples as well as ce

226 thropogenic salinity gradients (for example, seawater-river water and desalination brine-wastewater,

227 overcome some of the limitations inherent to seawater-river water.

228 omise for application to bacteria control in seawater RO.

229 matter (DOM) and halides, rather than other seawater salt constituents (e.g., carbonates) or photoac

230 even in troublesome sample matrixes, such as seawater, salt, and fruit juices, with relative recoveri

231 )U, and Pu isotopes ((239)Pu and (240)Pu) in seawater sampled during four different cruises performed

232 Seawater samples collected off the FDNPP in September 20

233 with parallel-factor analysis (PARAFAC) for seawater samples obtained from the northern Gulf of Mexi

234 ance using the lake water, ground water, and seawater samples spiked with known amounts of As(III).

235 d in standard solutions as well as simulated seawater samples to demonstrate their usefulness as sens

236 Most interestingly, when the seawater samples were analyzed, the nanocubes showed a s

237 Paired high-volume atmospheric and seawater samples were collected along a transect between

238 Seawater samples were collected onboard three cross-basi

239 ion of nitrite in aquarium and dechloridized seawater samples.

240 and correlations with FIB concentrations in seawater, sand, and eelgrass.

241 inundations, with less arsenic release from seawater scenarios than river water due to inhibition of

242 Mean concentrations in seawater, sea-ice and snow were generally greater at the

243 s revealed synthetic fibers are prevalent in seawater, sediments and biota.

244 ich source of energy and carbon are found in seawater, sediments, and shorelines from the tropics to

245 nt superoleophobic aerogel for efficient oil/seawater separation.

246 atographic separation of iodide in simulated seawater, showing a limit of detection (LOD) of 1.30 mum

247 ring data from measurements in air, sea ice, seawater, snow, frost flowers, and brine.

248 thermal systems in the Precambrian, when low-seawater SO4 could help explain low seawater (87)Sr/(86)

249 Using synthetic seawater solutions, we show that the increased photodegr

250 d chlorination experiments were conducted in seawater spiked with UV filters to investigate the react

251 e of Salmonella was found in pups exposed to seawater, suggesting that this may represent a source of

252 communities were separate from those in the seawater, suggesting the copepod gut hosts long-term, sp

253 tle is known about the fate of UV filters in seawater swimming pools disinfected with chlorine.

254 xycinnamate, and octocrylene, in chlorinated seawater swimming pools.

255 MOB = -0.65 +/- 1.1 per thousand, 1 SD), and seawaters (synthetic and natural).

256 serum, by the spike and recovery trials with seawater, tap water, mineral water, and alcoholic bevera

257 ins were subjected to interactive effects of seawater temperature (27 degrees C to 31 degrees C) and

258 bonate shells can be combined to reconstruct seawater temperature and delta (18)O (delta (18)OSW).

259 Here, we use Mg/Ca-derived seawater temperature and salinity estimates determined f

260 The relationship between seawater temperature and the average Mg/Ca ratios in pla

261 Increases in seawater temperature are expected to have negative conse

262 The variability of seawater temperature through time is a critical measure

263 se from 400 to 900 ppm by year 2100, causing seawater temperature to increase by 1-4 degrees C and pH

264 portant for a coral's resistance to elevated seawater temperature, but there is no information on how

265 sponse to climate change parameters, such as seawater temperature, pteropod shells (Heliconoides infl

266 how environmental factors such as anomalous seawater temperatures and consequent coral bleaching and

267 p abundance showed no direct relationship to seawater temperatures over the decade and were also unre

268 strains, fresh-water Chlorella vulgaris and seawater Tetraselmis chuii, were selected.

269 of dissolved organic carbon was leached into seawater than the corresponding dark controls.

270 ide and methanethiol) in euxinic or H2S-rich seawaters that were widespread in Proterozoic continenta

271 eference sensor that is immersed directly in seawater, the system is capable of operating for years a

272 </= 308.15 K and 20 </= S </= 40 in natural seawater, thereby allowing high quality pHT measurements

273 e transport of fecal indicators suspended in seawater through medium-grained beach sand under transie

274 At ocean spreading ridges, circulation of seawater through rock at elevated temperatures alters th

275 sistent with the general ease of movement of seawater through the sand patties as shown with a (35)SO

276 otoxins produced by microalgae directly from seawater, thus providing useful information for monitori

277 sand type, the contribution of recirculating seawater to surf zone contamination is likely to be mini

278 edulis) or blue mussels (Mytilus edulis) in seawater to two different densities (2.5 or 25 mug L(-1)

279 l need to convert nonpotable sources such as seawater to water suitable for human use.

280 concentrations ranged from levels below bulk seawater up to approximately 120 nM, some of the highest

281 been developed for the selective recovery of seawater uranium for more than six decades, with a renew

282 als developed from 2000-2016 for recovery of seawater uranium, in particular including recent develop

283 feedwater for desalination in comparison to seawater using fieldwork and laboratory approaches.

284 liquid droplets, gas bubbles, and entrained seawater, using 279 simulated chemical components, for a

285 ulnerability highest when exposure to low pH seawater was decoupled from high food availability, or i

286 Moreover, the (41)K/(39)K of seawater was recently found to be significantly higher t

287 and efficient determination of palytoxin in seawater was setup.

288 following two days of dark incubations, once seawater was supplemented with organic carbon substrate

289 nd dissolution of CdSe quantum dots (QDs) in seawater were investigated.

290 Their sedimentation rates in seawater were measured to be 4-10 mm/day.

291 sulfamethoxazole in a complex matrix such as seawater, where according to the literature sulfonamides

292 e larger supermicrometer particles from bulk seawater, which comprises largely salts and water-solubl

293 surface sediment was different from that of seawater while seawater harboured local bacterial assemb

294 es that scavenge surface-active species from seawater, while further enrichment in fine SSA likely de

295 a significant increase in alkalinity of the seawater with a consequent DIC increase due to CO2 invas

296 ment stage larvae from reef fish species for seawater with DMS.

297 d to result in rising average temperature of seawater with more extreme thermal events, and frequent

298 nd to reduce dissolution of nanoparticles in seawater with up to 3.3 times lower concentrations of si

299 device also exhibits long-term stability in seawater without salt accumulation as well as high perfo

300 O) represents a major sink of DMS in surface seawater, yet the underlying molecular mechanisms and ke