ライフサイエンスコーパス: salinity

1 Mg C/ha for tidal forest (high elevation/low salinity).

2 on of deviations from the expected effect of salinity).

3 avorable condition (low temperature and high salinity).

4 in both Amazon river discharge and APR ocean salinity.

5 e navigation of salt gradients to avoid high salinity.

6 cantly impact regional water temperature and salinity.

7 sely associated with their performance under salinity.

8 rid 5, and BB 106) were the most tolerant to salinity.

9 t growth regime of low temperatures and high salinity.

10 n, and other factors such as temperature and salinity.

11 jor factor in eggplant yield associated with salinity.

12 ter of a different (i.e., desalinated water) salinity.

13 often subject to extremes in temperature and salinity.

14 t volatilization fluxes of PCBs and seawater salinity.

15 r staple crop and immensely affected by soil salinity.

16 mon e-fate models remain valid under varying salinity.

17 desalinate feedwater with a wide spectrum of salinity.

18 ore, can be seen as a mechanism to cope with salinity.

19 in poor soils, with little water and at high salinity.

20 ns over time, including temperature, pH, and salinity.

21 ormance under stress conditions such as high salinity.

22 .4 and SnRK2.10 acting mostly in response to salinity.

23 were already well-adapted to a wide range of salinities.

24 less river runoff, rainfall and higher ocean salinities.

25 th the sediments was of Na-Cl type with mild salinity (~0.1-0.5 mol/kg) and circumneutral pH.

26 esalination conditions (e.g., 3 g L(-1) feed salinity, 0.5 g L(-1) product water, 80% water recovery,

27 nsitivity and robustness for a wide range of salinity (10-37 per mille), temperature (0-25 degrees C)

28 lants cultivated with intermediate levels of salinity (110 and 200 mM) revealed better antioxidant st

29 2-14), and potentially ocean circulation and salinity(15-17), we anticipate that a pause in these tre

30 of the Mediterranean mussel to reduced water salinity (18 vs 37 ppt), caused a significant reduction

31 6% under one sun illumination and under high salinity (25 wt% NaCl), and water collecting rate of 1.7

32 esholds (soil temperature ~ 17 degrees C and salinity ~ 30 ppt), which dictated the regime transition

33 60 Mg C/ha for seagrass (low elevation/high salinity), 417 +/- 70 Mg C/ha for low marsh, 551 +/- 47

34 mental events in temperature (32 degrees C), salinity (45ppt), and pH (7.65 pH) on social behavior an

35 time of elevated temperature, sea level and salinity across coastal waters.

36 An induced drop in salinity allowed the virus to enter the nephrocomplex in

37 on, active analyte channels, variable pH and salinity, analyte breakdown and other confounding factor

38 hin 4 h), and robust with respect to varying salinities and composition of the water samples.

39 we probe the impact of water with variety of salinities and ion types on formation of water in oil mi

40 branes reject more than 99% of salts at high salinities and, in reverse osmosis, small-molecule organ

41 t hot temperatures, large pH gradients, high salinity and abundant divalent cations should preclude v

42 to evaluate the combined effects of elevated salinity and atmospheric CO(2) concentration (c(a) ) on

43 a related to depth, sea surface temperature, salinity and bed shear stress.

44 We find strong inverse correlations between salinity and concentrations of most PFAS, indicating tha

45 probably facilitated adaptation to the high salinity and drought stress in limestone karst.

46 Abiotic stresses, such as high salinity and drought, blunted immune responses in older

47 er inundation and, hence, combined stress by salinity and flooding.

48 eous environmental gradients of temperature, salinity and food availability across a 30 degrees latit

49 Interacting effects of salinity and food availability on mussel shell compositi

50 ies, especially for circumstances where high salinity and high temperature are involved.

51 ral P and organic amendments irrespective of salinity and irrigation.

52 al source of genes for tolerance to drought, salinity and low-temperature stresses.

53 for example combined effects of temperature, salinity and nutrients on population survival and growth

54 arshes and determined their association with salinity and other soil physicochemical features by anal

55 Composite analysis of salinity and plankton biomass anomalies shows a strong a

56 er may leach Ra into groundwater by changing salinity and redox conditions in the subsurface rather t

57 racteristics to those that also incorporated salinity and sea surface height (proxies for primary pro

58 zing different spatiotemporal facets of soil salinity and sodicity variability over the past four dec

59 at temperatures of ~70 degrees C and require salinity and strongly alkaline conditions to self-assemb

60 ineages that differ based on the in-situ pH, salinity and temperature of the subsurface environment.

61 periments that altered nitrate availability, salinity and temperature to create stressed growth and t

62 sidered in inferring changes in global ocean salinity and the hydrological cycle from the surface and

63 pectinata Link) has a high tolerance to soil salinity and waterlogging, therefore, it can thrive on m

64 l circulation anomalies driven by changes in salinity and winds.

65 l stresses by increasing water temperatures, salinities, and heavy metal concentrations, as well as d

66 (combination of soil temperature, porewater salinity, and atmospheric pressure).

67 it tolerates extreme low temperatures, high salinity, and broad seasonal fluctuations in light condi

68 reme environmental conditions, such as heat, salinity, and decreased water availability, can have a d

69 ns and avoid high oxygen concentration, high salinity, and high density of algae.

70 tions, substrate quality, water-table level, salinity, and microbial community composition/activity.

71 under interacting gradients of temperature, salinity, and ocean acidification, then model growth rat

72 r global change factors, especially hypoxia, salinity, and ocean acidity, covary with temperature cha

73 of 2014 and they led to positive sea surface salinity anomalies in the central equatorial Pacific.

74 The positive sea surface salinity anomalies induced a westward displacement of th

75 the central equatorial Pacific conveyed the salinity anomalies of subtropical origin to the sea surf

76 n-contaminant stressors (e.g., sediment, low salinity, anoxia, and ocean acidification), offering an

77 We find that temperature and salinity are closely linked to larval growth and larval

78 lynya was hindered by relatively low surface salinity associated with the positive Southern Annular M

79 n water masses of different temperatures and salinities at boundaries.

80 del, respectively, with soil temperature and salinity being the most dominant controls.

81 to coastal aquifers can increase groundwater salinity beyond potable levels, endangering access to fr

82 The injection of low-salinity brine enhances oil recovery by altering the min

83 ing a parallel rise in the discharge of high-salinity brine into the ocean.

84 This study demonstrates ZLD of ultrahigh-salinity brines using temperature swing solvent extracti

85 thods for zero liquid discharge of ultrahigh-salinity brines.

86 depths (Delta c, typically reducing influent salinity by 10 mM or less).

87 ize and strength of the SPG, and they impact salinity by modulating the proportion of subpolar and su

88 Here, we examine global ocean salinity changes and ocean vertical salt fluxes over the

89 ommunities following fishing disruptions and salinity changes caused by a tropical cyclone.

90 ity measurements, previous studies of global salinity changes focused mostly on the surface and upper

91 For salinity changes in the relatively well-observed upper o

92 tially offset the carbon burial rates in low-salinity coastal wetlands, there is hitherto a paucity o

93 tic stress conditions such as drought, heat, salinity, cold and particularly their different combinat

94 olfactory receptor neurons encodes absolute salinity concentrations by detecting monovalent anions a

95 the most favorable (high temperature and low salinity) condition for CO(2) uptake, whereas the low re

96 The cells were cultured under different salinity conditions and sampled at four different time p

97 cessions outperformed D-genome cottons under salinity conditions.

98 tional charge transport under various pH and salinity conditions.

99 , a high temperature oil reservoir of marine salinity contains a microbial population that is predomi

100 Rootstock's performance under salinity correlated highly with its leaf Na and Cl conce

101 ep of +0.3 [Formula: see text]C and +0.08 in salinity could be observed concomitant with a weak winte

102 HSSW salinity decreased between 1995 and 2014, consistent wit

103 nvestigated using new records of sea surface salinity (delta(18)Ow) and sea surface temperatures (SST

104 these phenomena: After accounting for known salinity-dependent electrode effects, the measured curre

105 The changes of the horizontally averaged salinity display a vertically layered structure, consist

106 Therefore, it is important to understand salinity distributions and compare defined bases of fres

107 nd compare defined bases of fresh water with salinity distributions and groundwater well depths.

108 Thus, it is paramount to understand how salinity drives both microbial community structures and

109 er into the assessment, there was no overall salinity effect on the dissipation rates of antibiotics,

110 Our results show that, by taking the vigor-salinity effect tradeoff into account, we can identify u

111 In polar, subpolar, and Baltic low-salinity environments, mussels produced thin shells with

112 models capable of making predictions of soil salinity (expressed as electrical conductivity of satura

113 various abiotic stresses, including drought, salinity, flooding, and temperature stress.

114 dicting whether a gene is responsive to high salinity for each cell type with machine learning).

115 common natural fibres, under three different salinities (freshwater, brackish water, saltwater).

116 nvestigates the 2014/15 failed El Nino using salinity from an ocean general circulation model.

117 ts were (1) an abrupt and marked decrease in salinity (from > 30ppt to < 5ppt) due to rainfall in the

118 in 24 h to 120 h forecasts for temperature (salinity) from sea surface to a depth of 1000 m.

119 d a westward displacement of the sea surface salinity front that represents the eastern boundary of t

120 rs with different salt concentrations (i.e., salinity gradient energy) can theoretically provide a su

121 electing electrode materials used to harvest salinity gradient energy.

122 than the deeper sections, indicating that a salinity gradient exists within the mats.

123 A salinity gradient propels a DNA molecule through a solid

124 effect into a mechanical force based on the salinity gradient.

125 the oscillatory motion of a liquid without a salinity gradient.

126 I), and tidal flat (TF, habitat IV) across a salinity gradient.

127 have the ability to navigate and thus detect salinity gradients and that this is achieved through pre

128 This work illustrates how salinity gradients can be used to power and operate a na

129 generate electrical current when alternating salinity gradients flow along its surface in a liquid fl

130 liquids, including sliding liquid droplets, salinity gradients in a flowing liquid, and in the oscil

131 One method for generating electricity from salinity gradients is to use electrode-based reactions i

132 ng along increasing elevation and decreasing salinity gradients.

133 h increase with the magnitude of the applied salinity gradients.

134 nificantly increased along the elevation and salinity gradients: 217 +/- 60 Mg C/ha for seagrass (low

135 uctural control on the lateral extent of low-salinity groundwater and potentially a control on where

136 m consists of one main, and two smaller, low salinity groundwater bodies.

137 While low-salinity groundwater is thought to be abundant, its dist

138 c coast and contains about 2800 km(3) of low-salinity groundwater.

139 Salinity had a secondary role in shaping prokaryotic com

140 presence of abiotic stressors, such as soil salinity, heat, and drought.

141 ecological mechanisms of selection (drought, salinity, herbivory, and burial) that together are suffi

142 marked effect on growth, which decreases for salinities higher than 110 mM.

143 ied by natal origin, dispersal age and adult salinity history.

144 dments in soils could efficiently ameliorate salinity impacts on soil properties and plant biomass pr

145 Salinity impairs seed germination and seedling establish

146 New research reveals how low levels of salinity in soil inhibit a plant's ability to respond to

147 suggesting some potential advantage of ocean salinity in the El Nino-Southern Oscillation prediction.

148 arable land predicted to be lost due to soil salinity in the next 30 years.

149 e rate, magnitude and duration of the recent salinity increase are unusual in the context of the (spa

150 tigating climate change, sea-level rise, and salinity increase, soil organic carbon (SOC) sequestrati

151 bined with organic amendments mitigated soil salinity, increased organic matter content, available wa

152 orts to control nutrients are ongoing, rapid salinity increases are ushering in a new set of poorly d

153 ttrappc11/rog2 mutants are hypersensitive to salinity, indicating an undescribed role of TRAPPs in st

154 salinity should be monitored to account for salinity-induced differences in sampling recovery.

155 d (2) to evaluate possible mechanisms of low-salinity-induced wettability alteration, including rock/

156 River deltas are frequently facing salinity intrusion, thus challenging agricultural produc

157 Soil salinity is a global environmental challenge for crop pr

158 Salinity is a growing issue worldwide, with nearly 30% o

159 Salinity is a major abiotic constraint for rice farming.

160 Hyperosmotic stress caused by drought and salinity is a significant environmental threat that limi

161 to ameliorate A reductions due to increased salinity is also discussed using the aforementioned mode

162 Salinity is among the major factors limiting crop produc

163 Salinity is an environmental stress that causes decline

164 Salinity is an essential proxy for estimating the global

165 Salinity is detrimental to plant growth, crop production

166 Salinity is known to affect plant productivity by limiti

167 Because high salinity is lethal to offspring, correctly evaluating wa

168 Soil salinity is one of the most devastating factors threaten

169 powered cloth-based sensors to monitor sweat salinity is presented.

170 henotype of the mur4/hsr8 mutants under high salinity is rescued by exogenous Ara or gum arabic, a co

171 One adaption strategy to increasing salinity is shrimp production, which however, heavily re

172 For a given salinity level, increasing c(a) increased A linearly, bu

173 Salinity levels constrain the habitable environment of a

174 While the adverse effects of elevated salinity levels on leaf gas exchange in many crops are n

175 f crops that can be grown at increasing soil salinity levels.

176 urements collected for five irrigation water salinity levels.

177 patial and temporal coverage of the existing salinity measurements, previous studies of global salini

178 Increasing salinity negatively affects biodiversity, mobilizes sedi

179 ents to document temporal variability in the salinity of the Ross Sea High Salinity Shelf Water (HSSW

180 The high salinity of the subpolar North Atlantic is a prerequisit

181 f intra-basin circulation in determining the salinity of the subpolar North Atlantic.

182 luence of atmospheric CO(2), temperature and salinity on pH across scales.

183 not fully counteract the negative effects of salinity on soil microbial activities and productivity,

184 obiome and alleviate the negative impacts of salinity on soil properties.

185 rformed to evaluate the effect of increasing salinity on the dissipation rates of antibiotics in trop

186 under conditions of constant temperature or salinity or in flows with only small gradients of these

187 However, sample matrixes of high salinity or strong acidity/alkalinity often break the el

188 terial densities and macrofaunal abundances, salinity, or sediment organic carbon.

189 For each water type we evaluated 5 different salinity (osmotic) levels of -0.003 (control), -0.15, -0

190 due to rainfall in the catchments, with hypo-salinity persisting weeks to months, and (2) dermatitis

191 Salinity, pH, and redox states are fundamental propertie

192 Salinity, pH, coexisting estrogens, and water chemistry

193 t alternative sources such as seawater, high-salinity processed water, or underground reservoirs.

194 of ground and surface water quality by high-salinity produced water generated during well stimulatio

195 lless culture systems using low-intermediate salinities produces S. ramosissima plants fit for commer

196 s mossambicus) are fish that tolerate a wide salinity range from fresh water to > 3x seawater.

197 However, HSSW salinity rebounded sharply after 2014, with values in 20

198 dicating Ra in groundwater was influenced by salinity, redox, and pH.

199 queried to characterize the temperature and salinity regimes in each of the closed areas as a basis

200 Conversely, in temperate, higher salinity regimes, thicker, more calcified shells with a

201 dictates the interpretation of SPG strength-salinity relationship in the ENA.

202 nd are therefore best suited to describe SPG-salinity relationship in the ENA.

203 CREs identified based on the whole-root high-salinity response can predict cell-type responses as wel

204 pCREs predict complementary subsets of high-salinity response genes.

205 y modulate Ca(2+) and Na(+) fluxes in cotton salinity responses.

206 opy of an osmoresponsive element, osmolality/salinity-responsive enhancer 1 (OSRE1).

207 I systems-in addition to using the same feed salinity, salt removal, water recovery, and productivity

208 anographic factors (e.g., ocean temperature, salinity, sea surface height) and seabed characteristics

209 of acidity and alkalinity (pH 2-14) and high-salinity seawater (up to 330 g kg(-1) ).

210 diatoms and dinoflagellates dominated higher salinity sections of the estuary.

211 Salinity severely reduces plant growth and limits agricu

212 ability in the salinity of the Ross Sea High Salinity Shelf Water (HSSW), a precursor to RSBW.

213 across river-estuarine or similar transects salinity should be monitored to account for salinity-ind

214 Although the net changes in soil salinity/sodicity and the total area of salt-affected so

215 ds used for tracking the variability of soil salinity/sodicity are extensively localized, making pred

216 evaluate their potential for growth in high salinity soils and as a basis for engineering varieties

217 dilute solution and to more than 50% in high-salinity solution even in the presence of very high conc

218 ure method and were extremely stable in high-salinity solutions and across a wide pH range.

219 the underlying role of sustained CEF in high-salinity stress acclimation.

220 xpression in rice provides tolerance against salinity stress and cause upregulation of SOS1 pathway g

221 in the promoters of genes responsive to high-salinity stress in six Arabidopsis (Arabidopsis thaliana

222 INDING TRANSCRIPTION ACTIVATOR 6 (CAMTA6) in salinity stress responses during early germination.

223 Expression analyses of 23 genes involved in salinity stress revealed that the expression differences

224 ular CO(2) concentration (c(i) ) modified by salinity stress to estimate g(m) was proposed.

225 itself need not be associated with increased salinity stress tolerance and provide information for us

226 igh salinity tolerance based on growth under salinity stress.

227 sitive role in regulating cotton response to salinity stress.

228 b elevates Na(+) efflux in Arabidopsis under salinity stress.

229 reater proportional decline in biomass under salinity stress.

230 ssypium spp.) suffers severe yield losses to salinity stresses, largely due to being grown on saline-

231 Low-salinity submarine groundwater contained within continen

232 etic variation and surface chlorophyll-a and salinity, suggesting an important role for hydrographic

233 was significantly enriched in the cold, low-salinity surface water exiting the Arctic compared to wa

234 During a field experiment, temperature/salinity (T/S) profiles from a set of underwater gliders

235 380,000 underway measurements of sea surface salinity, temperature, and carbon dioxide (CO(2)) in the

236 o depend on geography, oxygen concentration, salinity, temperature, and other environmental variables

237 s are known to tolerate wide fluctuations in salinity, temperature, pH, and oxygen.

238 e. high temperature, high pressure, and high salinity) that exist in the subsurface that far exceed t

239 Results showed that with increased salinity, the estimated g(m) and maximum photosynthetic

240 With increasing salinity, the model captures different transpiration pat

241 ol into the vacuole plays a critical role in salinity tissue tolerance, but another, often neglected

242 We attribute along-shelf variability in salinity to permeability heterogeneity due to permeable

243 The results provide evidence that salinity tolerance and associated physiological traits a

244 LA1449, and LA1403 showed particularly high salinity tolerance based on growth under salinity stress

245 -overexpressing lines also showed increased salinity tolerance due to reduced salinity uptake and di

246 nt a valuable genetic resource for improving salinity tolerance in commercial tomatoes.

247 To identify genetic determinants conferring salinity tolerance in cotton, we deployed a functional g

248 ions), they provide an avenue for increasing salinity tolerance in high-performing sunflower genotype

249 hat Na(+) and Cl(-) exclusion is crucial for salinity tolerance in Prunus.

250 and be used as a resource for increasing the salinity tolerance of commercial tomatoes.

251 In this study, we investigated salinity tolerance of two species of wild tomato endemic

252 oving WUE, drought avoidance or attenuation, salinity tolerance, and for crassulacean acid metabolism

253 Salinity tolerance, survival and initial growth in seawa

254 tify unique traits and genes associated with salinity tolerance.

255 various transporters with known functions in salinity tolerance.

256 alophytes and glycophytes, in the context of salinity tolerance.

257 0 mm NaCl) and high (100 mm NaCl) hydroponic salinity treatments.

258 Abiotic stresses, including drought and salinity, trigger a complex osmotic-stress and abscisic

259 increased salinity tolerance due to reduced salinity uptake and dilution of internal Na(+) and Cl(-)

260 c stresses, nitrogen deficiency, drought and salinity, using HEB-YIELD, a selected subset of the wild

261 were largely responsible for the sea surface salinity variability but had less impacts on sea surface

262 At larger temperature or salinity variations, the changes in the index of refract

263 phase-behavior viscosity map-a plot of added salinity vs. soap fraction combining phase behavior and

264 Salinity was negatively correlated with CH(4) emissions

265 Salinity was the best predictor of within-region differe

266 gator abundance across tributaries; instead, salinity was the primary driver.

267 table indicators of the effectiveness of low-salinity water and (2) to evaluate possible mechanisms o

268 dynamic transport and mixing between the low salinity water and the formation brine (high salinity wa

269 is important to know i) how the injected low salinity water displaces and mixes with the high salinit

270 ation for the profitability of so-called low salinity water flooding, an enhanced oil recovery method

271 Hence, it would be favorable to inject low salinity water from the beginning of waterflooding to av

272 xiting the Arctic compared to warmer, higher-salinity water from the North Atlantic entering the Arct

273 of crude oils and the oils' response to low-salinity water in a spontaneous imbibition test, aiming

274 ta potential for the rock and the oil in low-salinity water is found to be an insufficient condition

275 For the first time, the effectiveness of low-salinity water is found to positively correlate with the

276 water and potentially a control on where low-salinity water rises into the seafloor.

277 To induce the wettability alteration, low salinity water should be transported to come in contact

278 However, the reported effectiveness of low-salinity water varies significantly in the literature, a

279 The numerical simulations show that when low salinity water was injected, the formation brine (high s

280 salinity water and the formation brine (high salinity water) in wettability alteration.

281 ater was injected, the formation brine (high salinity water) was swept out from the flowing regions b

282 nity water displaces and mixes with the high salinity water, ii) how continuous wettability alteratio

283 ity alteration of a rock by injection of low salinity water, it is important to know i) how the injec

284 hallenges such as low ion rejection for high salinity water, low water flux, and low stability over t

285 are of particular interest for treating high salinity water, since conventional methods such as rever

286 regions was diffused very slowly to the low salinity water.

287 are found to respond more positively to low-salinity water.

288 late with the oil interfacial tension in low-salinity water.

289 size was reduced under tertiary mode of low salinity waterflooding compared to the high salinity wat

290 Low salinity waterflooding has proven to accelerate oil prod

291 salinity waterflooding compared to the high salinity waterflooding.

292 ed as one of the most notable effects of low salinity waterflooding.

293 separate study on varietal tolerance to soil salinity were analyzed for plant viral sequences.

294 artificial reef, while daily photoperiod and salinity were not important.

295 xcessive rainfall from storms rapidly lowers salinity, which can destroy coastal foundation species a

296 urface temperatures (SSTs) and a decrease in salinity, which can lead to an intensification in the st

297 to a combination of high temperature and low salinity, while the wintertime F(CH4) was negligible.

298 as tidal inundation and increased porewater salinity will likely decrease ecosystem carbon stocks in

299 phic" to "eutrophic" for the mesohaline (MH) salinity zone of the bay.

300 ic" for oligohaline (OH) and polyhaline (PH) salinity zones, and from "hypertrophic" to "eutrophic" f