ライフサイエンスコーパス: water layer

1 d guest, can then be manipulated back into a water layer.

2 the lipid membranes are separated by a thin water layer.

3 influence, and testing for the presence of a water layer.

4 and only considers their propagation in the water layer.

5 binding led to the ordering of the adjacent water layer.

6 ree OD' transition found only in the topmost water layer.

7 with the typical hysteresis indicative of a water layer.

8 gap has closed to sterically permit a single water layer.

9 s frictional coupling across an interstitial water layer.

10 idity imposed by residues and by the surface water layer.

11 in an ice shell, possibly overlying a liquid water layer.

12 enough heat to maintain a subsurface liquid water layer.

13 in beyond the bilayer, and the intermembrane water layer.

14 's elastic modulus and height of an adsorbed water layer.

15 ing the fluidic flow in a wick-free confined water layer.

16 tion of such interfaces into two distinctive water layers.

17 an worlds to steam worlds with supercritical water layers.

18 fluencing the H-bond topologies in the first water layers.

19 of the adsorbed water film is more than two water layers.

20 y and hydrogen-bonding properties in central water layers.

21 are separated from the surface by one or two water layers.

22 logical strategies associated with different water layers.

23 ioavailable dissolved Fe(II) in sunlit upper water layers.

24 For the saturated water layer ((2)/(3) ML) we find a stable structure with

25 The 3470 cm(-1) feature comes from the top water layer adjacent to the hydrophilic headgroup of DMP

26 Results show that a tightly bound water layer adjacent to the OEG-SAMs is mainly responsib

27 Understanding the influence of water layers adjacent to interfaces is fundamental in or

28 on mechanism is dictated by the existence of water layers adjacent to the solid and orientational ord

29 First, a < 100 nm water layer adsorbed on the NaCl cubes and caused sharp

30 verage 0.86 +/- 0.27 pmol L(-1) in the upper water layer and 1.02 +/- 0.12 pmol L(-1) in intermediate

31 domain with charged surfaces separated by a water layer and a hydrophobic tunneling domain with atom

32 ll, two apposed monolayers merged across the water layer and developed into an hourglass structure co

33 h excellent resistance to the formation of a water layer and no interference caused by light, O2, and

34 tron conductor suppresses the formation of a water layer and results in an electrode-to-electrode sta

35 Both washout from the upper water layer and the physical resistance of the mucus lay

36 controls the thickness of the inflowing warm water layer and the rate of basal melting.

37 before the entropy increase of releasing the water layers and the short-range van der Waals attractio

38 served as a defect in a partially structured water layer, and favored relaxed, weakly helical, coiled

39 ral Arctic Basin (PML, intermediate Atlantic Water Layer, and the Arctic Deep Water Layer) are 158 +/

40 kilometers, which is equivalent to a global water layer approximately 11 meters thick.

41 Triple emulsion drops with an ultrathin water layer are developed to achieve high encapsulation

42 rested in phenomena in which nanometer-sized water layers are involved.

43 not the protein itself but ordered ice-like water layers are responsible for the recognition and bin

44 te Atlantic Water Layer, and the Arctic Deep Water Layer) are 158 +/- 77 kg, 6320 +/- 235 kg and 3080

45 ination of interfacial polymerization by the water layer around each hydrophilic nanoparticle.

46 The extent of an external water layer around moss tissue influences CO(2) assimila

47 ion of water within ~10 A of, i.e., up to ~3 water layers around the spin probes located on hydrophil

48 5 billion years ago) had a global equivalent water layer at least 137 meters deep.

49 entually, this results in the formation of a water layer at the interface to the underlying electron

50 rst, we find that zwitterions act to disrupt water layering at interfaces, leading to smoothed intera

51 layers, followed by the properties of liquid water layers at metal surfaces.

52 clear evidence for the presence of ice-like water layers at the ice-binding site of the protein in a

53 ined in a "pseudo-adsorption" state at a few water layers away from the active site and respond to th

54 the outer limit of the first cosolvent (not water) layer; B(i) mainly counts the solvent near the ma

55 e, facilitating the formation of an ice-like water layer between the Li(+) cations and the surface.

56 tive electrodes (ISEs) with an unintentional water layer between the sensing membrane and underlying

57 e packing limit, corresponding to only a few water layers between adjacent proteins.

58 This water layer, between the tip and specimen, could act as

59 the appearance and the evaporation of a thin water layer cannot enhance the charge diffusion.

60 ds prefer to be localized in the interfacial water layers close to the TiO2 surface where they are st

61 bstituents showed modulations of the surface water layers coating the protein-bound inhibitors.

62 in the TransFEr chamber reduced the stagnant water layers compared to theoretical predictions.

63 omic force microscopy, that we can visualize water layers containing alkali metal cations on a charge

64 t chain recoil by adhesion to the structured water layer covering the surface.

65 rom the moon's silicate interior by a liquid water layer, delayed or prevented from freezing by tidal

66 nd endowing it with a charged character, the water layers ensure the peptide feels the effect of the

67 The water layer grew to several hundred nanometers with incr

68 is a test for the presence of an undesirable water layer, if the conditions for this test are not sel

69 fectively prove the presence or absence of a water layer in a short time period.

70 shoaling of the intermediate-depth Atlantic Water layer in the eastern Eurasian Basin have increased

71 omaly was explained through the formation of water layers inside CNTs.

72 namics, with fastest dynamics at the surface water layer, intermediate dynamics within the flexible c

73 1) to count only the waters within the first water layer is a poor approximation; 3) when determining

74 of the surface water reveal that the topmost water layer is affected structurally at high concentrati

75 de films reaches a maximum when one complete water layer is intercalated between the graphitic planes

76 A drag of water flow at the first water layer is revealed, which is conjugate to sharp inc

77 of hydrophobic molecules across hydrophilic water layers, just as membrane carriers catalyze the tra

78 cations that the presence of such an ordered water layer may have for imaging of biological samples a

79 /quasifree water molecules and surface-bound water layer (minimum binding energy of 1-2 kcal/mol).

80 Our results show that while a water layer mitigates protein damage, the noise generate

81 s within the sediment and anoxic hypolimnion water layer of five humic lakes in WI, USA.

82 2 +/- 2 cm/s, close to the permeability of a water layer of the same thickness.

83 veal an inert, densely hydrogen-bonded first water layer on the (104) facet that favors interparticle

84 , respectively, suggesting the presence of a water layer on the cell surface created by NG-MUC1.

85 The presence of a water layer on the surface of muscovite mica under ambie

86 Since water layers on Pt are important in many catalytic proce

87 d to the physical properties of interstitial water layers present between the nanoparticles and the p

88 r, which shelters the chemistry of life, the water layer protects other water molecules and allows fo

89 ed stratification between the mixed and deep water layers reduced entrainment, particularly at Easter

90 ized the height and contact angle of ordered water layer(s) formed by wetting and de-wetting processe

91 depends directly on the shape of the frozen water layer set by the support foil.

92 limited delivery of AEA through an unstirred water layer surrounding the cells (1).

93 Water layer test, reversibility, and selectivity for chl

94 ed higher PFAS concentrations in the surface water layer than in intermediate waters and a negligible

95 as a model for passage across the unstirred water layer that lines the small intestine.

96 ed by forming a hydrogel network within this water layer that serves as a physical barrier.

97 ese disadvantageous effects due to the thick water layer, the effects of radiation damage on the orie

98 e biofilter in the seasonally euxinic bottom water layer, the methane-filtering potential was much lo

99 The model water layer thickness along with the fraction of wet sur

100 Here, we investigate the impact of water layer thickness and radiation damage on orientatio

101 o-dimensional lamellar structures with known water layer thickness as well as well-defined monodisper

102 The water layer thickness between the bilayer planes in the

103 tuations with no net particle dissolution or water layer thickness change.

104 he resultant internal dimensions (d-spacing, water layer thickness, average lipid length, and headgro

105 ing applied in the model based on equivalent water layer thickness, while transmission and reflection

106 howing the effects of changing dose-rate and water-layer thickness are presented.

107 panned up to 24 orders of magnitude from the water layer to the bilayer center, due primarily to its

108 s have neglected the effect of the unstirred water layer (UWL).

109 ctly at the cell surface across an unstirred water layer, via a hydrophobic channel in the receptor,

110 The polymer was isolated in the water layer when cells were extracted by phenol/water an

111 ells distinguished by numbers of intervening water layers, which reach a minimum when aligned.

112 apposed leaflets becomes coupled across the water layer, while the "outer" leaflets remain unaffecte

113 geable, creating stable channels, one to two water layers wide, that exhibit robust and tuneable ion

114 nanotubes, this feature also results from a water layer with "free" OH (dangling) bonds facing the n

115 d applicability by integrating this confined water layer with a recently developed contactless solar

116 tential between the sensing membrane and the water layer with its uncontrolled ionic composition.

117 molecules more loosely bonded to the topmost water layer with oxygen toward the interface, and thus e

118 a significant source of dPb, particularly in water layers with relatively higher dPb concentrations (

119 We hypothesised that descriptors of deep-water layers would better predict the deep-diving cetace

120 ing the use of variables describing the deep-water layers would provide a better understanding of the