ライフサイエンスコーパス: sublimation

1 Si(001) near dislocations during growth and sublimation.

2 emely ice-rich glacier-like viscous flow and sublimation.

3 e Zn liquid droplets, surface oxidation, and sublimation.

4 ble for chromatographic isolation and vacuum sublimation.

5 d by varying the temperature and duration of sublimation.

6 ys after TAE was described as hepatic tissue sublimation.

7 terface has a profound effect on the rate of sublimation.

8 transport (VPT) technique based on molecule sublimation.

9 at can preserve a porous structure after ice sublimation.

10 3, beta-H2CO3 was regarded to decompose upon sublimation.

11 1,5-diaminonaphthalene matrix deposition by sublimation.

12 pids from tissue section after deposition by sublimation.

13 and can be co-purified by crystallization or sublimation.

14 he surface through 'impact gardening' and/or sublimation.

15 it increases to the value of bulk Ca heat of sublimation (178 kJ/mol) at approximately 1.2 ML, attrib

16 r ice on the surface of some asteroids, with sublimation a potential reason for the dust activity obs

17 different atmospheric models that low-level sublimation accounts for a 17% reduction of total snowfa

18 agment and to the total mass lost from water sublimation after 21 July 2000 (about 3 x 10(8) kilogram

19 Combustion calorimetry and heats of sublimation also were measured for benzil and 3,5-di-ter

20 ber of metabolites detected when compared to sublimation and airbrush.

21 is controlled by feedbacks between volatile sublimation and condensation, changing insolation condit

22 This possibility of sublimation and recondensation cycles of beta-H2CO3 adds

23 f the 67P nucleus, finding changes driven by sublimation and recondensation of water ice.

24 unique to quasi-2-dimensional (2D) graphene sublimation and reconstructions.

25 sing the usual postcoating approach, such as sublimation and spraying, in terms of the sharpness of s

26 ng the realization of the new engine to both sublimation and the instantaneous vapourization of liqui

27 veal changes in the relative contribution of sublimation and volcanic sources to the atmosphere.

28 (prepared beforehand by a protocol utilizing sublimation) and were washed with ammonium formate solut

29 bda-DNA and recovered on a coldfinger of the sublimation apparatus after heating to 450 degrees C.

30 , >99% of the graphene edges observed during sublimation are BLEs rather than monolayer edges (MLEs),

31 observations also provide strong support for sublimation as the driver of activity in 288P and show t

32 y of fullerene nanostructures, such as their sublimation at high temperature is also very important f

33 the crystal, 5Me-HQE.HCl, was lost HCl upon sublimation but did not tautomerize.

34 sealed glass tube, so that a small amount of sublimation can be utilized to create films.

35 We find that CO2 sublimation can mobilise grains to form (i) pits and (ii

36 aggregates is different - graphitic with the sublimation carbon source and amorphous with the atomic

37 ne layers grown on hBN and sapphire with the sublimation carbon source and the atomic carbon source a

38 erved in the MBE growth of graphene with the sublimation carbon source.

39 In this confinement controlled sublimation (CCS) process, very high-quality graphene is

40 As a result of sublimation, condensation and restructuring, initially e

41 licated spatial distributions resulting from sublimation, condensation, and glacial flow acting over

42 g a kinetic model of disk chemistry, and the sublimation/condensation temperatures of primitive molec

43 lectively prepared by careful control of the sublimation conditions, with the alpha-phase crystallizi

44 The ability to apply DPH via sublimation coupled with its low volatility allows us to

45 ed for imaging mass spectrometry (IMS) after sublimation, DAN has demonstrated to be of high efficien

46 Sublimation describes a change of physical state from so

47 ent from that of H2O, which implies that H2O sublimation did not control the CS2 or dust production d

48 on, pits expand slowly in diameter, owing to sublimation-driven retreat of the walls.

49 The values also correlate with their bulk sublimation energies, which suggests that covalent metal

50 ion is 730-780 kJ/mol, much higher than Ca's sublimation energy (178 kJ/mol).

51 th the sum of magnitudes of the metal's bulk sublimation energy plus the heat of formation of the bul

52 ks, and pitting, the latter likely caused by sublimation erosion and/or collapse.

53 Hepatic tissue sublimation following TAE has so far not been reported i

54 the first documented case of hepatic tissue sublimation following TAE.

55 standard molar enthalpies of vaporization or sublimation (for 4-fluorobenzonitrile), at T = 298.15 K,

56 bove the solid at room temperature, enabling sublimation (freeze drying) under ambient conditions.

57 We therefore propose that sublimation from millimetre-sized icy grains ejected fro

58 The maps sample the evolution of sublimation from the north polar cap, revealing that the

59 The graphene sublimation fronts consisted of mostly {1100} zigzag edg

60 Sublimation has been shown to be a rapid and effective t

61 Matrix sublimation has demonstrated to be a powerful approach f

62 Tissue sublimation has hardly been reported in medical literatu

63 Here we present a sublimation heat engine, which can convert temperature d

64 Heat transport and ice sublimation in comets are interrelated processes reflect

65 ecules inside interstellar ices before their sublimation in star-forming regions such as SgrB2(N).

66 amily of fragments, resulting in accelerated sublimation in the Sun's intense radiation field.

67 mide A/II frequencies seen immediately after sublimation indicated an increased extent of hydrogen bo

68 We propose that the dark surface layer is a sublimation lag deposit that may be rich in impact-deriv

69 reat and growth of ground ice as a result of sublimation loss and recharge reveal forty major ice age

70 dging of droplets cooled via evaporation and sublimation (low environmental pressure) or convection (

71 Airbrush, automatic sprayer, and sublimation matrix application methods were optimized in

72 Sublimation matrix deposition yielded high spatial resol

73 ace pressure or via creation of overhangs by sublimation, may be a major mass loss process.

74 Torques exerted by sublimation measurably influence the spin rates of activ

75 CO2 ice sublimation mechanisms have been proposed for a host of

76 ized automatic sprayer method and humidified sublimation method resulted in double the number of meta

77 tion methods, specifically aerosol spray and sublimation methods.

78 ce (that is, total precipitation minus total sublimation minus runoff) and a dynamic term.

79 We reproduced the "coastline" sublimation morphologies by kinetic Monte Carlo (kMC) si

80 models of one site show that millimeters of sublimation occurred during this fading period, indicati

81 In contrast, sublimation of 1 on cleaved succinic acid (SA) substrate

82 onization (MALDI) imaging mass spectrometry, sublimation of 2,5-dihydroxybenzoic acid as the MALDI ma

83 This was achieved by sublimation of a low ionization energy matrix compound,

84 he porphyrin sample onto the Si substrate or sublimation of a neat sample onto the Si substrate.

85 The sublimation of adenine, cytosine, guanine, and thymine f

86 th heliocentric distance was consistent with sublimation of an icy body near its subsolar point.

87 water ice, but close to what is expected for sublimation of carbon dioxide ice.

88 We report sublimation of crystalline GeTe nanowires at elevated te

89 Sublimation of DAN represents an interesting approach to

90 h incident luminosity, which arises from the sublimation of dust; by the gravitational potential of t

91 The partial sublimation of enantioenriched amino acids was performed

92 f the asteroids called main-belt comets, the sublimation of excavated volatiles causes transient come

93 An optional etching step, involving vacuum sublimation of ice, may be carried out after fracturing.

94 ave been observed; they come mostly from the sublimation of ices at the surface or in the subsurface

95 ation process not found on Earth: springtime sublimation of Mars' CO(2) seasonal polar caps.

96 ved water vapour is probably produced by the sublimation of migrating icy bodies, and provides a pote

97 Additional pulse irradiations cause sublimation of only the separated silicon element and su

98 pentacene during the high-temperature vacuum sublimation of pentacene (P) in the presence of trace am

99 The data demonstrate that sublimation of serine under relatively mild conditions y

100 this dry air leads to significant low-level sublimation of snowfall.

101 We induced sublimation of suspended few-layer graphene by in situ J

102 of the capping layer, but that x-rays cause sublimation of the CBST film, which is prevented by the

103 Purification of 1a and 1b is achieved by sublimation of the excess Hhpp and subsequent recrystall

104 ze their liquid content while preventing any sublimation of the latter, the samples were kept frozen

105 age was required for the analysis to prevent sublimation of the molecules into the vacuum chamber.

106 ature with the aim to determine the rules of sublimation of these compounds.

107 n, providing a sustained heat source for the sublimation of up to ~300 kilograms of water ice during

108 If the plume is generated by the sublimation of water ice and if the sublimation source i

109 elion 2011, suspected to be sustained by the sublimation of water ice and supported by rapid rotation

110 agnitude larger than can be explained by the sublimation of water ice, but close to what is expected

111 oor of crater Occator that exhibits probable sublimation of water ice, producing haze clouds inside t

112 ase (WO3)3 and (MoO3)3 clusters generated by sublimation of WO3 and MoO3 powders.

113 he heat eventually reaches Ca's bulk heat of sublimation on all PMMA surfaces, where pure, bulk-like

114 aper, we disclose the detailed phenomenon of sublimation on the atomic scale.

115 water evaporation could be due to comet-like sublimation or to cryo-volcanism, in which volcanoes eru

116 duced emission (AIE) active, and through the sublimation process displays self-assembling crystalline

117 During in situ observation of the sublimation process of the nanowires, the evolution and

118 matographic analysis confirmed that L-serine sublimation produced DL-alanine, glycine, and ethanolami

119 in ultrahigh vacuum is poor due to the high sublimation rates at relatively low temperatures.

120 ally high daytime temperatures and water ice sublimation rates for a given albedo.

121 results showed that the detection of unequal sublimation rates within a freeze-dryer shelf was possib

122 However, to date, the sublimation, self-assembly and atomistic insights of exp

123 d by the sublimation of water ice and if the sublimation source is visible to CIRS, then sublimation

124 oss of volatiles through some combination of sublimation, space weathering, outgassing, or pyroclasti

125 developed a clean, low-pressure evaporation/sublimation system to remove water from samples and coup

126 A sublimation technique was developed to isolate purines a

127 for beta-H2CO3, whereas they are not at the sublimation temperature of 210 K for alpha-H2CO3.

128 two monomers are entropically favored at the sublimation temperature of 250 K for beta-H2CO3, whereas

129 sublimation source is visible to CIRS, then sublimation temperatures of at least 180 kelvin are requ

130 ico-chemical properties, such as melting and sublimation temperatures, and solubility.

131 ples were placed in a humidity chamber after sublimation, there was enhanced detection of higher mass

132 al extent, showing a magic number octamer on sublimation; this octamer can be ionized and characteriz

133 results demonstrate the feasibility of using sublimation to isolate purines and pyrimidines from nati

134 Porous single crystals are doped by vapor sublimation to produce diamondoid arrangements of guests

135 We find that sublimation torques have caused the nucleus to spin up i

136 the driver of activity in 288P and show that sublimation torques may play an important part in binary

137 meates the thin comet atmosphere formed from sublimation, until the size and plasma pressure of the i

138 When sublimation was completed in the cake region illuminated

139 An unexpected period of sublimation was observed during northern hemisphere autu

140 ferent sample preparation methods, including sublimation with two common organic matrixes for matrix-