ライフサイエンスコーパス: sea water

1 ronment of low Cbl bioavailability (~2 pm in sea water).

2 carapaces of M. alvisca and those in ambient sea water.

3 p microplastics from melting ice and ambient sea water.

4 blue" osmotic energy between river water and sea water.

5 dal variability in the formation of Labrador Sea Water.

6 ral complexity to naturally occurring DOM in sea water.

7 ubmersion time of at least 83 minutes in icy sea water.

8 origin and appear to be transmitted through sea water.

9 sequester 30-60% of the uranyl in synthetic sea water.

10 mnant Early Cretaceous North Atlantic (ECNA) sea water.

11 ian period by low sulphate concentrations in sea water.

12 ogen either from water at neutral pH or from sea water.

13 of magnitude greater than in overlying deep sea water.

14 ing and chemical exchange between basalt and sea water.

15 ith a thin strip of glass, I added a drop of sea water.

16 the mantle is remarkably similar to that of sea water.

17 n the possibility of osmium contamination by sea water.

18 or have only been grown to low densities in sea water.

19 endent biofilm development in model and true sea water.

20 flows minimizes the interaction of lava with sea water.

21 detected in picoplankton from Hawaiian deep sea water.

22 as well as in buffer, nanopure, tap or even sea water.

23 dissolved and particle-bound phases of Irish Sea water.

24 ized analysis at the source, e.g., river and sea waters.

25 directly on unconcentrated pond, river, and sea waters.

26 At the pH of sea water (8.0-8.3), the enzymatic activity with (GlcNAc

27 A companion reconstruction of delta(18)O of sea water-a sea surface salinity and hydrology indicator

28 Indeed, we found that sea water-activated spermatozoa are able to synthesize N

29 imental results suggest that ions present in sea water, also called smart water, have a significant i

30 per cent from widely available tap water and sea water and an STH efficiency of 6.2 per cent in a lar

31 d various hypotheses regarding the origin of sea water and concluded that the most likely hypothesis

32 ut 70 per mil, which is twice that of modern sea water and consistent with the nearly closed ECNA bas

33 Real samples studies were carried out in sea water and fish samples.

34 somal RNA genes that have been identified in sea water and has been found in nearly every pelagic mar

35 independent of both dissolved iron levels in sea water and iron content in Trichodesmium colonies.

36 xothermic serpentinization reactions between sea water and mantle rocks.

37 Interactions between heated sea water and molten basaltic lava could exert significa

38 ctinium-231 ((231)Pa), which are produced in sea water and removed by particle scavenging on timescal

39 e of the formation and spreading of Labrador Sea water, and future studies with similar instrumentati

40 water, extensive intrusion of current Baltic Sea water, and substantial temporal variability of chlor

41 to be capable of continuous desalination of sea water (approximately 99% salt rejection at 50% recov

42 aerosols is significantly lower than that of sea water (approximately four pH units, with pH being a

43 and inorganic) in natural systems (fresh and sea waters) as well as in wastewater treatment plants, w

44 s >95% of this flux and is highly soluble in sea water, as indicated by a significant increase in dis

45 n in isolated bag cell neurons in artificial sea water (ASW).

46 diatom Cyclotella meneghiniana in artificial sea-water (ASW) demonstrated higher growth response to i

47 diatom Cyclotella meneghiniana in artificial sea-water (ASW) demonstrated higher growth response to i

48 ulturable state of V. cholerae in artificial sea water at 4 degrees C, whereas the mutation of hapR l

49 alytic system operates in pure and untreated sea water at benign pH (2-8) and ambient temperature and

50 But it has been thought that heating sea water at pressures of several hundred bars cannot pr

51 rtant control on the chemical composition of sea water by serving as a major source or sink for a num

52 ficant advection of relatively warm Irminger Sea Water by the West Greenland Current since MIS 4.

53 SEA water captures much of the physics of explicit-solve

54 ta (measuring steric changes associated with sea water density).

55 ue to increases in ocean mass and changes in sea water density.

56 Changes in the amount of CO(2) in the sea water directly affect the oceanic carbon chemistry s

57 ace water picoplankton assemblages in a deep-sea water (DSW) mixing experiment.

58 es out drastic changes in the composition of sea water during the last 900 Myr.

59 nkton and eukaryotic fractions isolated from sea water either collected before sunrise or exposed to

60 SA, where trees experience different form of sea water exposure.

61 vealing zones of thermal cracking where cold sea water extracts heat from hot crustal rocks, as well

62 obial sulfate reduction, often accompanying (sea)water flooding during secondary oil recovery.

63 nstructions, which suggest weakened Labrador Sea Water formation and gyre strength with similar timin

64 ted in any other samples examined, including sea water, fresh water, sediment, terrestrial, extreme,

65 ants in a variety of environments, including sea water, fresh water, soil, and air.

66 PMCs endocytose sea water from the larval internal body cavity into a ne

67 zed the ice algaeMelosira arcticaand ambient sea water from three locations in the Fram Strait to ass

68 s that lead to this distribution of Labrador Sea water have, however, been difficult and therefore sc

69 theory for a random medium of ice floes in a sea water host.

70 from AIS expansion and local evaporation of sea water in concert with evaporite precipitation that c

71 e investigate the effect of additive ions of sea water in oil recovery by using acetic acid as a mode

72 In contrast, our study identifies ancient sea water in situ and provides a direct estimate of its

73 t moves between environments (e.g. fresh and sea water in the case of migratory fish).

74 ich is the expected main pathway of Labrador Sea water in the thermohaline circulation.

75 lgae and from 1.4 to 4.5 x 10(3) MP m(-3) in sea water, indicating magnitude higher concentrations in

76 is in balance with its production in Arctic sea water, integrated depth profiles for all time interv

77 An energy-efficient approach to converting sea water into fresh water could be of substantial benef

78 Accumulation of authigenic molybdenum from sea water is already seen in shales by 2,650 Myr ago; ho

79 Labrador Sea water is characteristically cold and fresh, and it c

80 00 mg l(-1)) in which a continuous stream of sea water is divided into desalted and concentrated stre

81 We find that sea water is drawn into aquifers as the freshwater-saltw

82 ons if the dissolved silica concentration of sea water is estimated.

83 We find that the sea water is probably 100-145 million years old and that

84 media like serum, cytoplasm of the cell, and sea water is selectivity: the ability to determine the a

85 Labrador Sea Water (LSW), formed by open ocean convection in the

86 Dense Labrador Sea Water (LSW), formed by winter cooling of saline Nort

87 ce height are likely to lead to transport of sea water, marine particulates, and marine biofilms into

88 discharge of the dense Persian Gulf and Red Sea Water may contribute to the observed seasonality.

89 ly populated landscapes where freshwater and sea water meet.

90 luids mix with cold, alkaline and oxygenated sea water, minerals precipitate to form porous sulphide-

91 ambers to air pressure equal to 18 meters of sea water (msw) for 60 minutes or 30 msw for 35 minutes

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

93 contrary, and show that bubbles of vaporized sea water often rise through the base of lava flows and

94 Lava erupts into cold sea water on the ocean floor at mid-ocean ridges (at dep

95 Thus, the effect of sea water on the osmium systematics of abyssal peridotit

96 Clean water obtained by desalinating sea water or by purifying wastewater, constitutes a majo

97 ues to utilize the abundant solar energy and sea water or other unpurified water through water purifi

98 In 50% artificial sea water (or sucrose/Na+), [3H]Me-TCB accumulation atta

99 gest that it is likely that remnants of ECNA sea water persist in deep sediments at many locations al

100 nd one challenged with SAV as post-smolts in sea water (POP 2).

101 ustainable methods for capturing energy from sea water: pressure-retarded osmosis and reverse electro

102 tion of mercury onto sea ice and circumpolar sea water provides mercury for microbial methylation, an

103 pectral range of minimal light absorption in sea water, raising intriguing questions regarding their

104 hanges in the lithium-isotopic conditions of sea water, rather than by changes in the sedimentary alt

105 without pre-freezing holding in refrigerated sea water (RSW) were stored at -19 degrees C for ~12 mon

106 Here, we report a process for converting sea water (salinity approximately 500 mM or approximatel

107 In sea water samples, Marine Group II and III archaea and o

108 ecies, from both Caribbean and Pacific Coral Sea water samples, whose geographical patterns of divers

109 e successful detection of nitrite in tap and sea water samples.

110 y-constructed estuarine mesocosms containing sea water, sediment, sea grass, microbes, biofilms, snai

111 and from such environmental sources such as sea water, sediments, and shellfish.

112 Embryos cultured in 400 mM lithium chloride sea water showed marked delay to the cell cycle and a te

113 tran (FDx; 10,000 mol wt) from extracellular sea water (SW) was not detected by confocal microscopy.

114 water, wastewater, river water, well water, sea water, tea, cacao, nut, bitter chocolate, rice, leek

115 Sea water temperature affects all biological and ecologi

116 Using simulated changes in sea water temperature from three Earth system models, we

117 bottle-microcosms with eastern Mediterranean Sea water that were supplemented with mono and polysacch

118 f extreme tides increases vertical mixing of sea water, thereby causing episodic cooling near the sea

119 4H (Cp34H) in subzero brines and supercooled sea water through long-term incubations under eight cond

120 r shells to estimate the pH of surface-layer sea water throughout the past 60 million years, which ca

121 DNA from Antarctic snow, brine, sea ice and sea water to elucidate potential microbially mediated me

122 ay of calcium carbonate from calcium ions in sea water to mineral deposition and integration into the

123 that the introduction of low-salinity Bering Sea water to the Arctic Ocean by 3.3 Myr ago preconditio

124 of the SAR11 clade in northwestern Sargasso Sea waters to 3,000 m and in Oregon coastal surface wate

125 buffering capacity allows the Mediterranean Sea waters to remain over the saturation level of aragon

126 ese vacuolar networks are involved in direct sea water uptake.

127 ely 8 ka, with the establishment of Labrador Sea Water ventilation.

128 tural aquatic matrices (river, estuarine and sea waters) was modeled at very low concentrations (from

129 surface waters (lakes, rivers, and streams), sea water, wastewater treatment plants (influents and ef

130 een biofilms, sediments, plants, animals and sea water with a recovery of 84.4%.

131 ed to anomalous production of dense Labrador Sea Water with buoyancy forcing in the western subpolar

132 18)O(P) values and assuming equilibrium with sea water with delta(18)O = 0 per thousand range from 26

133 to cells involves nonspecific endocytosis of sea water with its calcium.