ライフサイエンスコーパス: thawing

1 xtural changes that occur after freezing and thawing.

2 atocyte proliferative capacity in vivo after thawing.

3 of the conventional problems of freezing and thawing.

4 ic matter in the soil increased 10-fold upon thawing.

5 naturation or aggregation due to freezing or thawing.

6 psulation of ATP or other reagents by freeze-thawing.

7 ocess of virion purification or freezing and thawing.

8 ges in potency occurring during freezing and thawing.

9 frost soils are now within ~0.5 degrees C of thawing.

10 pore scale dynamics related to freezing and thawing.

11 s are mostly affected by seasonal permafrost thawing.

12 ial membranes were disrupted by freezing and thawing.

13 expansion and the resulting PLC occur during thawing.

14 cted to 42 h of freezing followed by 24 h of thawing.

15 eratures, whereas no UE were recorded during thawing.

16 ting the deleterious effects of freezing and thawing.

17 ates >98% reduction in activity after freeze-thawing.

18 is expected to increase with warming-induced thawing.

19 this is detrimental to metabolic function on thawing.

20 not EPCs retained functional activity after thawing.

21 milar C-H insertion product is obtained upon thawing a frozen CH(2)Cl(2) solution of the nitride comp

22 and necrotic death were both observed after thawing and after 24 hours of culture.

23 n environmental conditions upon freezing and thawing and demonstrates the enormous complexity of free

24 The entire process is rapid since thawing and filtering take place simultaneously, and if

25 a tracheid will embolize due to freezing and thawing and found that it decreased from 35 microm at a

26 sured and the actual practices at receiving, thawing and frying during French fries preparation were

27 robial mats throughout that are viable after thawing and has a history that extends to at least 2,800

28 aintain membrane fluidity after freezing and thawing and improves freeze-thaw (FT) survival.

29 , glycine addition during both vitrification/thawing and maturation further enhanced the oocyte quali

30 investigates the effects of repeated freeze-thawing and oxidation on the anti-HIV activity of rSLPI.

31 Freeze-thawing and pasteurization increased the milk lipolysis

32 different storage (room temperature, frozen, thawing and refreezing) and buffer conditions on glucosi

33 After freezing-thawing and sonication, the resultant larger liposomes a

34 0 years, and are available for 14 days after thawing and washing.

35 during and after CPA loading, freezing, and thawing, and during CPA unloading.

36 -season ice permeability and/or complete ice thawing at the bottom of ponds permit alpha-HCH rich sea

37 l integrity throughout the process of freeze-thawing (at -25 degrees C).

38 also becoming more commonplace as methods of thawing become more sophisticated.

39 ived marrow cells that had been primed after thawing but before transplantation had similar recovery

40 rger than 10 kDa which survives freezing and thawing, but is inactivated by boiling.

41 However, repeated freeze-thawing caused a more than 10% monomer loss.

42 concentrations, and strand length as well as thawing conditions.

43 lated and cryopreserved and, upon subsequent thawing, continue to self renew.

44 frozen stocks suggests that freezing and/or thawing contributes to heterogeneity in the outgrowth po

45 ere exposed to different numbers of freezing/thawing cycles and separated into three batches, namely

46 reshness according to the number of freezing/thawing cycles they exposed.

47 ty of stresses, including heat, freezing and thawing, dehydration, hyperosmotic shock, and oxidant in

48 After thawing, dissection was performed with blunt dissectors.

49 Permafrost in the Arctic is thawing, exposing large carbon and nitrogen stocks for d

50 g dimethyl sulfoxide and were assessed after thawing for morphology, proliferative capacity, gene exp

51 In boreal lowlands, thawing forested permafrost peat plateaus ('forest') lea

52 From first thawing frozen ampules of D17 cells, investigators can e

53 ere cryopreserved and cultured ex vivo after thawing in a single laboratory to assay invasion of targ

54 traditional low pH pulse produced by freeze-thawing in mixed sodium phosphate buffer induces the oli

55 Repeated freezing and thawing increased the reduction of all tested microbial

56 gment or delayed resection after a 15-minute thawing interval.

57 release from Arctic soils due to permafrost thawing is known to be substantial, but growing evidence

58 inducing factor(s), which can survive freeze-thawing, is heat labile and also can be inhibited by sup

59 ears) of methane emitted from hotspots along thawing lake margins indicates that this positive feedba

60 es, while storage that involves freezing and thawing leads to irreversible changes due to phase chang

61 er hydrological connectivity from permafrost thawing may potentially increase transport of MeHg from

62 Additionally, global warming has led to the thawing of ancient permafrost soils, particularly in Arc

63 Freeze-thawing of both bevacizumab and placebo samples led to >

64 The evaluation of freshness and freeze-thawing of fish fillets was carried out by assessment of

65 permeability of mitochondria by quick freeze-thawing of fresh homogenates just before assay did not i

66 Thermokarst is the process whereby the thawing of ice-rich permafrost ground causes land subsid

67 probably, it is related to the freezing and thawing of internal fluctuations of the protein, known a

68 Freezing-thawing of PBPC had no effect on porcine CFUs but reduce

69 Both heavy precipitation events and thawing of permafrost are increasing the net transfer of

70 It is thought that the thawing of permafrost can lead to a loss of soil carbon

71 of pathogenic DNA viruses, suggests that the thawing of permafrost either from global warming or indu

72 l waters through increases in precipitation, thawing of permafrost, and changes in vegetation.

73 Thawing of PF-C must also have brought about an enhanced

74 These changes, along with thawing of previously frozen organic material, can alter

75 applications from food science to the freeze-thawing of proteins it is important to understand the of

76 death) was produced in vivo by the freezing-thawing of rat thymus and in cell culture of Jurkat cell

77 Moreover, repeated freezing-and-thawing of the dry vaccine powder did not cause aggregat

78 Slower freezing and thawing of the mixture led to the production of more and

79 on with warmer active layer temperatures and thawing of the near surface permafrost.

80 need to confirm that the cryopreserving and thawing of the reconstituted solution did not compromise

81 nnot be associated exclusively with enhanced thawing of the rock glacier in recent years.

82 ybridization was facilitated by freezing and thawing of the solutions, and the denaturation of these

83 significant loss of titer after freezing and thawing of the stock virus.

84 The effect of freeze-thawing on cytosolic lactate dehydrogenase and lysosomal

85 effects of time, temperature, freezing, and thawing on the cerebrospinal fluid viral load by using t

86 ong-term freezing, and repeated freezing and thawing, on indigenous coliforms, fecal streptococci, an

87 han 10 kDa that is sensitive to freezing and thawing or boiling.

88 In human platelet lysates prepared by freeze-thawing or by the addition of nonionic detergent, the Vn

89 cine supplementation in either vitrification/thawing or maturation medium significantly improved the

90 Freeze-thawing or other mishandling can further increase levels

91 cations in the food industry such as baking, thawing or pasteurisation.

92 Levels were unaffected by freezing/thawing or prolonged storage and did not display any con

93 ed by sample dilution, repeated freezing and thawing, or extended benchtop or frozen storage.

94 n Mire (68.35 degrees N, 19.05 degrees E), a thawing peat plateau in northern Sweden.

95 The effect on RNA quality of freeze-thawing peripheral blood cells and storage in preserving

96 We find that thawing permafrost along lake margins accounts for most

97 The bog (thawing permafrost and low radiative forcing signature)

98 ited understanding of the decomposability of thawing permafrost and relevant mechanistic controls ove

99 na Flats in central Alaska for centuries, as thawing permafrost collapses forests that transition to

100 making it difficult to predict how inputs of thawing permafrost DOM may alter its photodegradation.

101 Thawing permafrost due to Arctic warming will continue t

102 roduction and release of methane (CH4 ) from thawing permafrost has the potential to be a strong sour

103 spheric CH4 and terrigenous biomarkers, that thawing permafrost in high northern latitudes could have

104 Release of greenhouse gases from thawing permafrost is potentially the largest terrestria

105 Thawing permafrost opens pathways for this CH4 to migrat

106 Thawing permafrost promotes microbial degradation of cry

107 Carbon release from thawing permafrost soils could significantly exacerbate

108 ical for carbon budgets in the Arctic, where thawing permafrost soils increase opportunities for DOC

109 Carbon in thawing permafrost soils may have global impacts on clim

110 Thawing permafrost soils will change the chemical compos

111 Increasing river discharge and thawing permafrost suggest that the impacts of continent

112 ial organic matter, by nutrient release from thawing permafrost that stimulated lake productivity and

113 In thawing permafrost, Candidatus 'M. stordalenmirensis' ap

114 summer from melting snow and ice as well as thawing permafrost, contrasting earlier notions of limit

115 d to detect the onset of carbon release from thawing permafrost.

116 soils are promising for Arctic wetlands and thawing permafrost.

117 of rapid cycling of methane and nitrogen in thawing permafrost.

118 t microbial activity in intact, let alone in thawing, permafrost.

119 Lung inflammation is associated with the thawing phase of cryoablation and may be related to solu

120 t the start of frying, product/oil ratio and thawing practice.

121 tion with the N-terminal domain via a freeze-thawing procedure.

122 ethyl sulfoxide for several weeks can, after thawing, reform characteristic polarized monolayers in 3

123 oth related to minimum temperature and, upon thawing, related to vapor pressure deficit and soil temp

124 eveloped MSC that retain >95% viability upon thawing, remain responsive to inflammatory signals, and

125 ation is investigated by repeatedly freezing/thawing short strands followed by matrix-assisted laser

126 changing nitrogen (N) availability in these thawing soil profiles.

127 N as the soil-stream flowpath deepens due to thawing soils.

128 eragrams (1 Tg = 10(6) tons) of methane from thawing subsea permafrost on shallow continental shelves

129 ol size together with significant permafrost thawing suggests a risk of carbon emissions and positive

130 peripheral blood cells at -180 degrees C and thawing them thereafter, RNA integrity is maintained.

131 eeper permafrost layers promoting permafrost thawing, thereby enhancing groundwater discharge.

132 phtheria toxin were produced by freezing and thawing under a variety conditions, including in various

133 red for channel freezing (valve closure) and thawing (valve opening) were measured.

134 e production of DT oligomers by freezing and thawing was expanded to include a salt-mediated pathway.

135 itionally, we demonstrate that freezing then thawing water trapped in the multilayer graphene oxide m

136 he effect on the metabolic profile of freeze-thawing were examined.

137 ting the effect of temperature, freezing and thawing, where the exclusion of salt and AuNPs by the gr

138 Freeze-thawing, which involves a mild denaturing step, may prod

139 CD34(+)CD38(-) cells isolated by FACS after thawing yielded >250-fold ex vivo expansion of HPC.