ライフサイエンスコーパス: Waters

1 ude larger than what is found in the surface waters.

2 Cl(2) to occur above pH 7 in high-alkalinity waters.

3 tial fraction of the carbon cycled by inland waters.

4 a marked exception to phosphate-poor natural waters.

5 etreating where ice is exposed to warm ocean waters.

6 ent, chemicals and nutrients into over-lying waters.

7 hen modeling photobleaching rates in natural waters.

8 nts also suggests a source region in shallow waters.

9 des controls Fe availability in many natural waters.

10 ve strengths were produced in iron-deficient waters.

11 rd Nd isotope values more typical of Pacific waters.

12 cted to warm, deoxygenate, and acidify ocean waters.

13 highly dynamic accumulation in oxic surface waters.

14 undly impact the trophic status of temperate waters.

15 pecies sampled appeared restricted to Arctic waters.

16 ed NPP and standing stock observed in warmer waters.

17 rate floods and convert them into productive waters.

18 ed organic matter (DOM) isolates and natural waters.

19 ern waters and the opposite in cold northern waters.

20 he analysis of two spiked river and two lake waters.

21 roduction and bioaccumulation in high Arctic waters.

22 sk from enteric pathogens in sewage-impacted waters.

23 ss that will span several decades in natural waters.

24 to a significant buildup of sulfide in pore waters.

25 y contributing to carbon export from surface waters.

26 about the photoreactivity of Adirondack lake waters.

27 e life history strategies found in shallower waters.

28 stratification, and more stabilized surface waters.

29 e risk assessment of DA-contaminated natural waters.

30 r, wastewater, irrigation water, and surface waters.

31 erable species at kilometre scale in coastal waters.

32 as then applied to AFFF-contaminated surface waters.

33 ing accurate photobleaching rates in natural waters.

34 utrient and organic matter inputs to surface waters.

35 ounts, which do not affect the surface ocean waters.

36 o supply large quantities of Fe to overlying waters.

37 a model Fe INP, suspended in filtered field waters.

38 stance against dissolution in more corrosive waters.

39 tarctic soils and in the surrounding oceanic waters.

40 shallow coastal area within the Inner Danish waters.

41 s observed between NOM and IEX resin in real waters.

42 srupting characteristics of different source waters.

43 ature, sea level and salinity across coastal waters.

44 be a major pollutant source to urban surface waters.

45 norovirus (NoV) densities in ambient surface waters.

46 on the amended site can be low in turbulent waters.

47 creen lotions, rainwaters, and swimming pool waters.

48 of their transformation products in surface waters.

49 e estimates for northern mid-latitude bottom waters.

50 rivers could have been mineralized in inland waters.

51 s an important source of nitrogen to coastal waters.

52 monitoring of contaminants in environmental waters.

53 e inactivation of viral pathogens in surface waters.

54 lectivity for use in either blood or surface waters.

55 derstand the variability of AQY-M in natural waters.

56 hen magadiite precipitated in shallow saline waters.

57 to 20 times higher than that found in marine waters.

58 o anthropogenic copper inputs into protected waters.

59 ficient and faster than in areas with cooler waters.

60 abundances of species associated with warmer waters.

61 persistence of pollutants in sunlit surface waters.

62 icotinoids has led to their proliferation in waters.

63 lengths) were quantified in underlying bulk waters.

64 to increasing nutrient starvation of surface waters.

65 se osmosis, for the desalination of brackish waters.

66 reduction beneath suboxic, stagnant surface waters.

67 uction process in the cold Southeast Alaskan waters.

68 as also tested in the microchip with natural waters.

69 n in the stratification of shallow nearshore waters (0-200 m), that affects both the mixed layer dept

70 s direct interactions of the ion with nearby waters, 2) the packing free energy that is the work to p

71 imals have faster swimming speeds in clearer waters(4).

72 170-420 tonnes remain afloat in the surface waters, 49-63% ended up on coastlines, and 37-51% have s

73 th dolphins showing a preference for shallow waters (5-15 m) less than 2 km from the coast.

74 s of a global survey covering 196 dry inland waters across diverse ecosystem types and climate zones.

75 d larval fish (8.1-fold) than nearby ambient waters across our study region in Hawai'i.

76 Open Arctic waters also increase the source of moisture and increase

77 Lastly, species associated with cold waters also increased in abundances close to shore in so

78 d 113% (SD 15%) recovery for raw and potable waters and 52% (SD 13%) for sludge.

79 the surface water layer than in intermediate waters and a negligible intrusion into deep waters (>100

80 ogen Vibrio vulnificus inhabits warm coastal waters and asymptomatically colonizes seafood, most comm

81 waters fell within ranges reported for whole waters and DOM isolates from various sources, while Phi(

82 isotopes show promise for tracking formation waters and for understanding water-rock interaction unde

83 versity leaders were thrust into unchartered waters and forced them to make unprecedented decisions.

84 , and physical properties) measured in these waters and found that the profiles covaried with at most

85 ion of Al(3+) in real food samples, drinking waters and herbal teas, were employed.

86 hat is, macro- and megafauna) living in deep waters and in benthic habitats, whereas monitoring of ec

87 In the future, if warming ocean waters and increased surface meltwater trigger faster ic

88 is widespread in North Atlantic and adjacent waters and is one of the most abundant vertebrates on ea

89 ilder conditions than the frigid surrounding waters and it could be an ideal location for newly intro

90 n processes from hyperpolarized "structural" waters and labile side-chain protons; and the possibilit

91 thin ice moderates iron delivery to offshore waters and likely also affects the subsequent ocean iron

92 formed abiotically on the surface in shallow waters and on continents during the Archean eon in the a

93 Secondary Fe oxyhydroxides forming in inflow waters and on creek beds have V K-edge XANES spectra exh

94 mineral-related activities in international waters and protecting the marine environment from the ha

95 s and guiding threat assessments in offshore waters and represent an important initial step towards q

96 enarios of future nutrient loading to inland waters and show that enhanced eutrophication of lakes an

97 However, the pathways of REEs from waters and soils into freshwater food webs remain poorly

98 and revealed temperate and tropical surface waters and the Arctic as biodiversity hotspots and mecha

99 vely low DIC and high Omega in warm southern waters and the opposite in cold northern waters.

100 anged from Papua New Guinea to sub-Antarctic waters and to Western Australia, highlighting connectivi

101 mask detection of TBA metabolites in surface waters and treatment systems.

102 wo bacteriophages-MS2 and phiX174-in surface waters and waste stabilization ponds by integrating sola

103 inct from the communities of the surrounding waters, and a few plastic-degrading microorganisms have

104 II)phases is a key process in soils, surface waters, and the ocean.

105 Ce-NPs were ubiquitously detected in surface waters, and their presence was related to a high natural

106 No interferences were observed from surface waters, and there was no match between bitumen-influence

107 th freshwaters, Hg methylation in open ocean waters appears less restricted to anoxic environments.

108 changes in the North Atlantic region, whose waters are among the world's fastest warming.

109 Amazonian waters are classified into three biogeochemical categori

110 s when iron and nitrogen resupply to surface waters are diminished.

111 hy and the rate at which well-mixed boundary waters are exchanged with the stratified ocean interior.

112 Changes in carbon-14 age of intermediate waters are in phase with peaks in Cordilleran ice-rafted

113 Cable deployments in coastal waters are increasing worldwide, in capacity and number,

114 change-driven increases in SSTs for tropical waters are predicted to cause increased stratification,

115 the diffuse solar illumination of shallower waters-are conspicuous when illuminated by directed biol

116 st predator endemic to the temperate coastal waters around southern Australia.

117 ere collected between 2006 and 2015 from the waters around the Lizard Island reef platform in Eastern

118 Diatoms are found universally in waters around the world.

119 f irrigation, recreation, and other types of waters, as well in watershed-scale microbial water quali

120 Fisheries species in tropical waters associate with a wide range of habitats, so asses

121 platforms for bacterial pathogens in ambient waters at the point of sample collection are urgently ne

122 Although CH(4) accumulation in oxic surface waters became apparent in recent years, the sources are

123 finding is important to OGW-impacted source waters because drinking water plants with high-bromide s

124 he glendonites of the Danish Basin formed in waters below 5 degrees C, at water depths of <300 m.

125 s of plastics in catchments and transitional waters both independently as a major transport routes to

126 w negative impacts of warmer and less saline waters, both outcomes of climate change.

127 encies can regularly flush reefs with cooler waters, buffering the thermal stress from rising sea-sur

128 c potential is present throughout the trench waters, but is less prominent below 8000 m, perhaps indi

129 ogeochemical cycling of iron in AMD-impacted waters, but its impact on dissolved organic matter (DOM)

130 freely living in Antarctic or sub-Antarctic waters, but no established populations have been reporte

131 -oxidizing archaea (AOA) are present in deep waters, but the mechanisms that determine ecotype format

132 al estimates of carbon emissions from inland waters by 6% (~0.12 Pg C y(-1)).

133 influences mercury retention in wetland pore waters by complexing Hg(II)(i) and decreasing the concen

134 For example, individuals could "test the waters" by first clustering for warmth (no cost), then c

135 ossess a similar chemistry to these proposed waters can be used to develop an understanding of the di

136 Mixing the two waters can precipitate HFFF-Ba and -Sr with AMD-SO(4), t

137 nd likely increasing component of the inland waters carbon cycle.

138 carbonate and the arrival of subpolar-origin waters close to carbonate undersaturation.

139 In oligotrophic waters, cnidarian hosts rely on symbiosis with their pho

140 , and hydroxyl radicals ((*)OH), for surface waters collected from 16 representative Adirondack lakes

141 Here, we show that Marcellus Shale produced waters contain some of the heaviest Ba (high (138)Ba/(13

142 Waters coproduced with hydrocarbons from unconventional

143 cleavable detergent, RapiGest SF Surfactant (Waters Corporation), we developed and optimized a nanopr

144 ar, and DOM processing in stratified surface waters could be attributed to photochemical transformati

145 In Australian and New Zealand waters, current knowledge on white shark (Carcharodon ca

146 very low concentrations of cobalt in marine waters, cyanobacteria in the genus Prochlorococcus retai

147 s may nucleate below the water table because waters depressurize as they flow from ridge to valley an

148 In surface waters, direct and indirect photochemical transformation

149 ne reuptake inhibitor, is present in surface waters downstream of wastewater treatment plants.

150 rophic Sargasso Sea to North America coastal waters, driven primarily by cyanobacterial diazotrophs.

151 In open and coastal waters, drivers were identified as a biological componen

152 a potential contaminant in flowback/produced waters due to the large volumes/types of chemicals injec

153 ined with the involvement of heated meteoric waters during their cooling in the crust.

154 shallow water (e.g., soil water) versus deep waters (e.g., groundwater), inducing primarily flushing

155 chemistry for the Utica Shale Play produced waters (e.g., total dissolved solids = 214-283 g/L) over

156 and iodide (I(-)) are common in many source waters, enhancing Br- and I-DBP formation.

157 plankton primarily when iron-rich subsurface waters enter the euphotic zone.

158 Many inland waters exhibit complete or partial desiccation, or have

159 Sinking into oxygen depleted waters explains the exceptional soft tissue preservation

160 ellular) until released into the surrounding waters (extracellular) during cell lysis.

161 Phi(app,(1)O(2)) for native Adirondack lake waters fell within ranges reported for whole waters and

162 cific ligands, were added weekly to mesocosm waters for 9 months.

163 est force fields and maintaining the crystal waters for accuracy.

164 isotherms in warm and relatively undisturbed waters (for example, the Central Pacific Basin) or in co

165 Preventing and remedying fresh waters from chemical pollution is a fundamental societal

166 ncentrations of trace elements in subglacial waters from the Greenland Ice Sheet (GrIS) and the Antar

167 d microbial community beta-diversity whereas waters from the most impacted nearshore reefs in the Flo

168 waters and a negligible intrusion into deep waters (>1000 m).

169 ollution in rivers, lakes, and other surface waters has exceeded $1.9 trillion since 1960, and has al

170 Trophic downgrading in coastal waters has occurred globally during recent decades.

171 H(4)) accumulation in oxic marine and limnic waters has redefined the role of aquatic environments in

172 Shallow, coastal waters identified here should be considered priority are

173 oalkyl substances (PFAS) in foams on surface waters impacted by aqueous film-forming foam (AFFF).

174 ations significantly before entering coastal waters in Chandler Fjord.

175 here highlight an essential role of solvated waters in driving zinc coordination dynamics and transme

176 sociated with PCB-contaminated sediments and waters in protecting vulnerable fish and shellfish speci

177 Summer thermally stratified surface waters in southwestern regions have historically been we

178 rea influenced by highly productive upwelled waters in the California Current System.

179 Inland waters, including streams and rivers, are active compone

180 In the HS-rich surface Arctic waters, including the Fe-rich Transpolar Drift (TPD), we

181 otein fragments were found in the processing waters, indicating heat- induced modifications.

182 conversion of warm, salty, shallow Atlantic waters into colder, fresher, deep waters that move south

183 tion but an eventual incursion of sub-Arctic waters into the North Sea re-established density-driven

184 ticide contamination in agricultural surface waters is a common phenomenon, large-scale studies deali

185 ng presence of contaminants in environmental waters is an alarming issue, not only because of their h

186 Po(2+) occurrence in low-to-neutral-pH waters is attenuated by adsorption.

187 the environment, their occurrence in surface waters is largely unknown.

188 distribution of sperm whales in New Zealand waters is mainly known from whaling records or opportuni

189 the toxic potential of fluoxetine in surface waters is markedly influenced by its own metabolism in a

190 ing, acidification and deoxygenation of deep waters, leading to decreased food availability at the se

191 mes along a gradient of oxygenated to anoxic waters (<0.02 mumol/l O(2) ) in the Eastern Tropical Sou

192 persistent organic pollutants, reaching open waters mainly via atmospheric deposition.

193 For example, in warmer waters, mangroves and seagrasses are in decline and bent

194 Suwannee River Fulvic Acid (SRFA) and marine waters (Marine DOM) were used as a test bed for the new

195 g that pharmacophore-driven sorption in real waters may be diminished.

196 Oxygen depletion in coastal waters may lead to release of toxic sulfide from sedimen

197 inking water plants with high-bromide source waters may switch to chloramination to meet DBP regulati

198 ggest that episodic acidification of coastal waters might limit the ability of pueruli to locate sett

199 re uptake genes were more abundant in low-Fe waters, mirroring paradigms of low-Fe adaptation in diat

200 We found that in international waters, more than one-third of vessels had no Automatic

201 ntrations of aerosol components across ocean waters next to the Antarctic Peninsula, South Orkney Isl

202 ional boundaries and entered the territorial waters of Cuba and/or Mexico.

203 n of (234)U enrichment within the subglacial waters of East Antarctica recorded the ice sheet's respo

204 between white sharks and large squids in the waters of Guadalupe Island, Mexico.

205 y described snakehead fish from subterranean waters of Kerala in South India.

206 statewide study on OMP occurrence in surface waters of New York lakes.

207 (Dendrophylliidae), in the northern Red Sea waters of Saudi Arabia at a depth of about 640 m.

208 Nevertheless, in the cold coastal waters of the Antarctic, these degraders seem to be abse

209 highest (6.3 degrees C) compared to the cold waters of the CAA (0.7 degrees C) that were associated w

210 the upstream closure are likely in adjacent waters of the Canadian continental shelf.

211 ompleted a 4-y expedition into the uncharted waters of the Food and Drug Administration (FDA) new-dru

212 The dense overflow waters of the Nordic Seas are an integral link and impor

213 meters of molten lava into the nutrient-poor waters of the North Pacific Subtropical Gyre.

214 t event (i.e., a marine heatwave) in coastal waters of the northern Gulf of Mexico resulted from comp

215 sels operating in national and international waters of the Southern Ocean.

216 ged on prey isotopically consistent with the waters of the Subtropical Convergence, Polar Front and M

217 in four demersal sharks species found in the waters of the United Kingdom and investigate whether bod

218 e most likely mechanism that generated flood waters of this magnitude on a planet whose present-day a

219 Geothermal waters often are enriched in trace metal(loid)s, such as

220 that the impact of acidification of natural waters on Fe availability will be much more pronounced w

221 hioanions such as mixing with non-geothermal waters or H(2)S degassing and oxidation with increasing

222 We show that CH(4) accumulation in surface waters originates from a highly dynamic interplay betwee

223 crystal structure containing two persistent waters predicted most of the changes in receptor affinit

224 vide was observed, with Fe deficient surface waters present beyond the shelf break, much further east

225 he dynamic range enhancement (DRE) lens of a Waters Q-IM-TOF, or the exit lens of a transfer multipol

226 Heme b concentrations in surface waters ranged from 0.10 to 33.7 pmol L(-1) (median = 1.4

227 tion, leading to unique assemblages in polar waters, rather than being entirely derived from southerl

228 g the proportion of subpolar and subtropical waters reaching the ENA.

229 ons of nitrite are present (e.g., in surface waters receiving reverse osmosis concentrate from potabl

230 We hypothesized that only waters recently contaminated by methane still exhibit hi

231 ) microbial respiration in soils as meteoric waters recharge into the subsurface and 2) the coupled c

232 nd storage, (3) filters often clog in turbid waters, reducing the eDNA captured, and (4) grab samples

233 ults indicate that emissions from dry inland waters represent a significant and likely increasing com

234 dustrial revolution with wetlands and inland waters representing the largest source of methane to the

235 d dissolved organic matter (CDOM) in surface waters results in the formation of photochemically produ

236 Inland waters (rivers, lakes and ponds) are important conduits

237 ep during drinking water production, all tap waters samples, and two surface waters used for drinking

238 red among seals along North-European coastal waters, significantly impacting seal populations.

239 e of upwelled hydrothermally influenced deep waters stimulating massive phytoplankton blooms in the S

240 ample, the Central Pacific Basin) or in cold waters subject to high human pressures (for example, the

241 on, Florida over the years 2003-2015 and the waters surrounding Charleston, South Carolina over 2003-

242 ach additional ppm in atmospheric pCO(2) the waters surrounding CWC communities lose carbonate at a r

243 gurations, namely, an Agilent 6560 IMQToF, a Waters Synapt G2 possessing a TWIMS cell and a modified

244 able low temperature conditions of Antarctic waters than soils, and the fact that maximum in situ tem

245 's small protrusions in structurally ordered waters that are characteristic of the so-called "small-m

246 to its natural upwelling of carbon-enriched waters that generate corrosive conditions for local ecos

247 w Atlantic waters into colder, fresher, deep waters that move southward in the Irminger and Iceland b

248 ral sensitivity for the brightly lit surface waters that this species inhabits during its marine phas

249 1-3.0 Gya) likely resulted in saline surface waters that were rich in sulfur species.

250 In nitrogen-limited waters, the atmosphere can contribute significantly to e

251 y-state concentrations of (1)O(2) in surface waters, the environmental half-life of DA due to singlet

252 eorient while sinking from surface turbulent waters to a more stable environment (i.e., under the sea

253 e Carlo simulation allows highly coordinated waters to be placed on the surface of a protein while si

254 e vessels move from high-copper-contaminated waters to coastal regions with low concentrations of cop

255 carbon are annually transported from inland waters to coastal systems making rivers a critical link

256 us dissolved organic matter (DOM) in surface waters to greenhouse gases.

257 would have to rely on dilution by receiving waters to not exceed any EQS.

258 show that rates of nutrient supply from deep waters to the photic zone have dramatically increased si

259 water and is the first part of rising tidal waters to traverse intertidal and upper tidal surfaces.

260 s were tested under five types of irrigation waters to understand the genetic, physiological, and bio

261 tracking of OSPW plumes in surface receiving waters, together with the potential for confirmation of

262 ude that intense recreational use of running waters transiently increases the anthropogenic DOM load

263 and outflow takes place), the North Atlantic Waters transport most of the ocean heat, but also nutrie

264 ntified groundwater inputs to Arctic coastal waters under contemporary conditions.

265 We simulate the eutrophication of lentic waters under scenarios of future nutrient loading to inl

266 Microplastic abundance in surface waters underlying ice floes (0-18 particles m(-3)) were

267 nd composition in sea ice cores (n = 25) and waters underlying ice floes (n = 22) were assessed in th

268 ance of de facto reuse conditions in surface waters used for drinking water abstraction.

269 ion, all tap waters samples, and two surface waters used for drinking water production.

270 s (A, AF, AP, C, BP, G, M, and Z) from river waters using polymer nano- and microfibers followed by H

271 radation of triclosan in near-surface sunlit waters was relatively fast (t(1/2) < 5 h).

272 modified Synapt G2-S QTOF mass spectrometer (Waters), we investigated the influence of relevant input

273 -covered season, MeHg concentrations in lake waters were approximately ten-fold greater than in summe

274 ormation rates of micropollutants in surface waters were examined using photochemical model calculati

275 assurance samples of OSPW diluted in surface waters were positively identified to their corresponding

276 lignocellulose enrichment samples in coastal waters were traced and statistically analysed.

277 children and adults when they are in surface waters where foam is present.

278 rocess for CDOM absorption in sunlit natural waters, where it can regulate the biota's exposure to su

279 ing increased in deeper, colder, more saline waters, which are sites with increased primary productiv

280 In anoxic waters, which composed most of the Paleoproterozoic and

281 anic carbon is eventually exported to inland waters, which is equal to 14% of the simulated net carbo

282 n the anoxic zone were lower than in surface waters, which parallels the low microbial diversity seen

283 d cavity is occupied by a cluster of ordered waters whose positions overlap the polar groups of the s

284 xyhydroxides on the acidification of natural waters will also have implications to the fate of other

285 ts support the hypothesis that warming ocean waters will restrict the habitat range of the narwhal, f

286 energy contained in the controlled mixing of waters with different salt concentrations (i.e., salinit

287 most amplified in shallow, sluggishly mixed waters with high rates of photosynthesis, and provides a

288 Heme b concentrations typically decline in waters with low iron concentrations but due to lack of f

289 e Pacific coast, upwelling brings subsurface waters with low Omega and pH to the surface where net bi

290 ed sewer overflows can contaminate receiving waters with micropollutants.

291 ies is limited to narrow and shallow flowing waters with rapids and boulders.

292 mparison of delta(13)C(TIC) of the oxic lake waters with the delta(13)C in the top microbial mat laye

293 relevant fraction of organic contaminants in waters, with high spatial and temporal resolutions at lo

294 higher concentrations, a toxicant in natural waters, with the relative rates of transformation betwee

295 a from the SUP05 clade often dominate anoxic waters within marine oxygen minimum zones (OMZs) where t

296 in a substantive reduction of the number of waters within the first hydration shell of Cl(-) while i

297 od submerged in saline and oxygenated marine waters worldwide is efficiently degraded by crustaceans

298 els, we project that the mean TTE in coastal waters would decrease from 7.7% to 7.2% between 2010 and

299 is a potential source of uranium to natural waters, yet evidence is lacking.

300 rol temperature and productivity in tropical waters, yet potential interactions with low frequency cl