ライフサイエンスコーパス: sea water

1 ral complexity to naturally occurring DOM in sea water.

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

3 origin and appear to be transmitted through sea water.

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

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

6 ian period by low sulphate concentrations in sea water.

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

8 of magnitude greater than in overlying deep sea water.

9 ing and chemical exchange between basalt and sea water.

10 dal variability in the formation of Labrador Sea Water.

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

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

13 n the possibility of osmium contamination by sea water.

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

15 endent biofilm development in model and true sea water.

16 flows minimizes the interaction of lava with sea water.

17 detected in picoplankton from Hawaiian deep sea water.

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

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

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

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

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

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

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

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

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

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

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

29 xothermic serpentinization reactions between sea water and mantle rocks.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

57 00 mg l(-1)) in which a continuous stream of sea water is divided into desalted and concentrated stre

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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