ライフサイエンスコーパス: on ice

1 matrigel for protection and stored in medium on ice.

2 tase (trxB) null mutant following incubation on ice.

3 of susceptibility to neuraminidase trimming on ice.

4 function compared with conventional storage on ice.

5 ns of an atomically smooth substrate sliding on ice.

6 excited state chemistry of mercuric bromides on ice.

7 d by a CD4-mimetic compound or by incubation on ice.

8 ure when it is followed by a 30-min chilling on ice.

9 n lipid and protein oxidation during storage on ice.

10 th Dome A, 24% of the base by area is frozen-on ice.

11 mug/ml), both of which were stored for 24 hr on ice.

12 tionally inactivated by prolonged incubation on ice.

13 it substantially slower vibrational dynamics on ice.

14 stant to overnight digestion in chymotrypsin on ice.

15 no staining was observed at 23 degrees C or on ice.

16 r preservation involves cooling of the organ on ice (0-4 degrees C).

17 is unusual import of Mtf1p was also observed on ice (3 degrees C).

18 Storage (SCS), which is static cold storage on ice (about + 4 degrees C) in a specialized media such

19 established the importance of this feedback on ice age AIS evolution.

20 direct and indirect impacts of glacier algae on ice albedo, with a significant negative relationship

21 where ice retreat has no significant impact on ice-algae peak timing, suggesting that changes in pel

22 ition to keeping any solution of free DiTags on ice, an analysis of the GC content should be performe

23 f ozone-depleting substances (ODSs) adsorbed on ice, an analytical equation is derived to give atmosp

24 hundreds of per cent, depending sensitively on ice and cloud cover as well as seasonal variations.

25 ng no reducing agents was essentially stable on ice and had a half-life of approximately 90 min at 37

26 EPS effects on ice and pore microstructure improve sea ice habitabil

27 sphere and reduces the albedo when deposited on ice and snow; accurate knowledge of past emissions is

28 as effective as simple postmortem treatment on ice and therefore not essential.

29 The [3H]2ME binds avidly to tubulin even on ice, and it is readily displaced by other colchicine

30 ed over a polar seasonal cycle, with a focus on ice-associated (sympagic) algae.

31 of experimentation, the animals were stored on ice at 4 degrees C for 0, 7, 14, and 21days.

32 ATP or Mg(2+) to otherwise complete mixtures on ice, ATP-initiated excision and final error correctio

33 Sliding speed depends on ice/bed coupling, dictated by the configuration and p

34 lenges to the field and various perspectives on ICE biology.

35 n food rotation and inadequate refrigeration on ice-chilled salad bars may have facilitated growth of

36 ht the importance of heterogeneous chemistry on ice clouds, and imply an additional Bry source from t

37 at hydrogen sulfide (H(2)S) can be converted on ice-coated interstellar grains in cold molecular clou

38 Based on ice core observations, laboratory measurements and ch

39 We applied the preconcentration method on ice core samples from the high-alpine Fiescherhorn gl

40 in the SU during the period 1935-1991 based on ice-core concentration records from Belukha glacier i

41 sion history for the Andean Altiplano, based on ice-core records from Illimani glacier in Bolivia, pr

42 Twenty years ago, measurements on ice cores showed that the concentration of carbon dio

43 long been a challenge to apply (81)Kr dating on ice cores where sample size is limited.

44 hether blood was kept at room temperature or on ice could be predicted based on inosine levels.

45 g considered proxies for possible life forms on ice-covered extraterrestrial bodies.

46 d (HOB), and roasted (ROB) peanut oil bodies on ice cream preparation.

47 an exoplanets; estimate thermodynamic limits on ice crust thickness and final ocean depth (of the cen

48 ver the regulatory effect of cryoprotectants on ice crystal growth and use this property to realize s

49 on, we found that survival is less dependent on ice-crystal formation than expected.

50 gs lead us to conclude that AFP accumulation on ice crystals, which are smaller than 100 mum in radiu

51 erved that placing blood samples immediately on ice decreased the serum levels of several cytokines,

52 s a clear influence of ocean thermal forcing on ice discharge.

53 mmertime lake drainage has little net effect on ice discharge.

54 should be collected, kept at 4 degrees C or on ice during transportation, and extracted ideally with

55 hape of the bed exerts a fundamental control on ice dynamics as well as the position of the grounding

56 find that frontal ablation is not dependent on ice dynamics, nor reduced by glacier surface freeze-u

57 n kinase activity of Mos was lost within 6 h on ice even though the Mos protein was not degraded and

58 t that the much-discussed quasi-liquid layer on ice evolves subtly above the melting point into a qua

59 at Ca(2+) uptake was sensitive to incubation on ice, extremely labile in the absence of protease inhi

60 r system that may exert an important control on ice flow and mass balance.

61 ystems of Thwaites Glacier and their control on ice flow have not been characterized by geophysical a

62 We propose that sedimentary control on ice flow is a viable alternative to existing models o

63 magnitude larger, seasonal melt's influence on ice flow is likely confined to those regions dominate

64 diverse subglacial landscapes have an impact on ice flow, and present a challenge for modelling ice-s

65 ngle-chain antibody (Hu-P4G7) and incubating on ice for 15 min.

66 Thirty kidneys were stored on ice for 24 h before undergoing 4 h of HMP (n = 15) or

67 rs preconditioned with metformin were stored on ice for 4 hours and transplanted to confirm postopera

68 Procured kidneys were stored on ice for 44-48 h, then transplanted into ABO-compatibl

69 sence of Vi under ultraviolet (365 nm) light on ice for 60 min.

70 d storage techniques, pig livers were stored on ice for either 2 or 16 hr, after which phosphorus-31

71 p (gel), Na-Hep, Na-Hep (glass)], and placed on ice for transport to the lab for centrifugation.

72 y could partially compensate for the loss of on-ice foraging opportunities caused by climate change.

73 eir ability to nucleate ice and their impact on ice formation in clouds.

74 , no direct influence of the plasma channels on ice formation or precipitation processes could be det

75 mpact of twenty-first century climate change on ice-free areas under two Intergovernmental Panel on C

76 AGTATCTATGAG) and the 12-mer d(CTCATAATACTC) on ice gave a major product that could be reverted to th

77 of the aqueous solutions or vapor deposition on ice grains, exhibited unequivocal bathochromic shifts

78 Similar to their effects on ice growth, the AF(G)Ps can inhibit MDM crystal growt

79 Sputter yield of a 20 keV Ar(1800)(+) ion on ice has been determined as 1500 (+/-8%) water molecul

80 Data on ice hockey and martial arts were too sparse to allow

81 Blood samples were placed on ice immediately after collection and analyzed within

82 iles of the product HA were to chill samples on ice in the presence of both EDTA and UDP.

83 ts are indicative of active iodine recycling on ice in the upper troposphere (UT), support the upper

84 abile metabolite levels even in blood stored on ice is alarming and stresses the critical need to imm

85 The rate of AFP accumulation on ice is determined by an interplay between AFP diffusi

86 i membranes during a second-stage incubation on ice is fully sensitive to Tris extraction, indicating

87 ld be obtained if these lungs were preserved on ice is unknown and remains an area for future researc

88 dividual samples and show that keeping blood on ice markedly reduces changes to the transcriptome.

89 se clouds, resulting in a substantial impact on ice mass flux and evolution of cold cloud systems.

90 Left atrial thrombus identified on ICE may occur during LA catheter ablation procedures

91 However, the impact of hydrodynamic coupling on ice motion over decadal timescales remains poorly con

92 es, the net impact of hydro-dynamic coupling on ice motion remains poorly understood.

93 the solvation and ionization of HCl adsorbed on ice nanoparticles kept at progressively higher temper

94 Most research on ice nucleation (and crystallization in general) has f

95 This study focused on ice nucleation and propagation, related water shifts

96 may help to explain why experimental results on ice nucleation rates yield different results in diffe

97 s reactions with ozone and other trace gases on ice nucleation.

98 An association rate constant on ice of 1.9 x 10(2) M-1s-1 was obtained.

99 xture of methanol and chloroform, and stored on ice or on bench, at room temperature for different ti

100 le changes in the environment (e.g., walking on ice) or in ourselves (e.g., injury).

101 d impact of cirrus clouds on climate depends on ice particle number, size, morphology, and compositio

102 This suggests that modelling based on ice physics may be the best way of matching isotopic

103 The fourth reconstruction, which is based on ice physics, has a low enough Mississippi-routed melt

104 rature of -1.5 degrees C or directly chilled on ice prior to 144h of ice storage.

105 ight the unique properties of free-OH groups on ice, putatively linked to the high catalytic activiti

106 port the discovery of an ion-specific effect on ice recrystallization.

107 ealed in 10 min, whereas 60% of cells placed on ice remained propidium-permeable even in 30 min.

108 ant to understanding heterogeneous catalysis on ice, remains an experimental challenge.

109 ieval, through warm ischemia, transportation on ice, right through to cold preservation and reperfusi

110 We collected a multiyear data set on ice scouring frequency from Antarctica by using uniqu

111 Here we combine glaciological evidence on ice sheet elevation from the TALDICE ice core with of

112 streams exerted progressively less influence on ice sheet mass balance during the retreat of the Laur

113 identify mineral dust as a secondary control on ice sheet melting.

114 methane sequestration and subsequent release on ice sheet retreat that led to the formation of a suit

115 th the Antarctic Ice Sheet but their control on ice-sheet dynamics and their ability to harbour life

116 -water environments and CO2-climate feedback on ice-sheet growth.

117 e caused glacial cycles through their impact on ice-sheet mass balance.

118 ospheric warming may have the largest impact on ice-sheet mass balance.

119 stimates of global mean sea-level rise based on ice-sheet reconstructions and previously limited earl

120 at magmatic flux acts as a negative feedback on ice-sheet size.

121 ulations cluster mainly on coasts and rarely on ice sheets.

122 full impact of recent calving-front changes on ice-shelf buttressing has not been understood.

123 ing glaciers contrast with steady velocities on ice-shelf-terminating glaciers and slow speeds on lan

124 However, surface rivers forming on ice shelves could potentially export stored meltwater

125 ce Sheet that incorporate meltwater's impact on ice shelves, but ignore the movement of water across

126 unding lines and ~60% (>80% by area) develop on ice shelves, including some potentially vulnerable to

127 nds, or directly, mostly through its effects on ice shelves.

128 ioligand in binding assays with intact cells on ice, similar to that for the wild-type receptor.

129 expected if subglacial erosion rate depends on ice sliding velocity.

130 ion rate, with most of this growth occurring on Ice Stream C.

131 Tidally induced motion on ice streams has previously been thought to be limited

132 Remarkably, ice diatoms can glide on ice substrates, a capability absent in temperate diat

133 e the molecular origin of icephobicity based on ice-surface interactions and characterize the correla

134 In fact, the transformation of HCl adsorbed on ice surfaces from a predominantly molecular form to i

135 cess also occurs in small water clusters and on ice surfaces, and recent attention has focused on the

136 yme levels was more dramatic in blood stored on ice than on bench, at room temperature.

137 We find that as diverse AFPs accumulate on ice, their concentration in the aqueous solution does

138 l melting, our simulations put a lower limit on ice thickness at the locations and times of impact.

139 estimation of dCHO concentrations from data on ice thickness, salinity, and vertical position in cor

140 nd the band areas showed a linear dependence on ice thickness.

141 proximately 5.1 m, respectively, which based on ice thicknesses at the summit drill sites in 2000 rep

142 polyether chain length has a profound effect on ICE, tissue iron decorporation, and ligand physiochem

143 ion for 30 s, followed by cooling the sample on ice to room temperature (~40 s) and then intermittent

144 ardiac surgery and stored in saline solution on ice until transplantation.

145 h (reference protocol), and holding samples on ice versus room temperature during a 3 h delay to pro

146 effects of immediately placing blood samples on ice versus room temperature for 1 h (reference protoc

147 ice temperature provide crucial constraints on ice viscosity and the thermodynamic processes occurri

148 the present, implying that tropical controls on ice volumes were asynchronous with those in the North

149 rt-term storage of freshly collected samples on ice was effective without interfering with the chemis

150 ane at 37 degreesC, followed by AP-1 binding on ice, we find that the high-affinity nucleating sites

151 Thrombi on ICE were mobile, averaged 18 +/- 5.9 mm long by 4.4 +

152 helix (minihelix(Phe)) when annealed rapidly on ice, while the same molecule formed a duplex structur

153 s of age were preserved in Optisol, received on ice within 24 to 36 hours of death, and immediately f