ライフサイエンスコーパス: freezing point

1 onse when the temperature approaches the RSG freezing point.

2 n aqueous solution at temperatures above the freezing point.

3 ase sharply on cooling below the equilibrium freezing point.

4 astically enhanced on supercooling below the freezing point.

5 ynamics for the hard-sphere fluid around its freezing point.

6 mportant contributor to depressing the serum freezing point.

7 ng to ice crystals, effectively lowering the freezing point.

8 growth at temperatures below the colligative freezing point.

9 ed ice crystal and consequently lowering the freezing point.

10 5 and 100 and temperatures (T) between their freezing point and 298.15 K (25 degrees C).

11 duce a difference between the nonequilibrium freezing point and the melting point, termed thermal hys

12 teins (AFPs) bind ice nuclei and depress the freezing point by a noncolligative absorption-inhibition

13 ve an especially high ability to depress the freezing point by far exceeding the abilities of other A

14 They are frequently used to lower the freezing point by preventing the growth of larger ice cr

15 and inhibited microbial growth at soil water freezing points compared to warmer temperatures.

16 In this study we report and examine how the freezing point depression also impacts the lipid phase t

17 quilibrium by a mechanism similar to that of freezing point depression by antifreeze proteins.

18 e osmolality of plasma was measured by using freezing point depression by microosmometer and osmolari

19 Serum osmolality was measured by using freezing point depression in a cross-sectional study.

20 (+)-selective electrodes and osmolality with freezing point depression yielded values consistent with

21 ing for the effect of 50-200 p.p.m. H(2)O on freezing point depression, the onset of silicate melting

22 ia XAS, (1)H NMR, ESI-MS, conductometry, and freezing-point depression experiments.

23 We measured the freezing-point depression of glycine-water up to 30% sup

24 negative feedback between ice growth and the freezing-point depression of the brine.

25 ssment was performed by measuring Posm using freezing-point depression osmometry.

26 ne osmolality was determined with the use of freezing-point depression osmometry.

27 meric in benzene solution as determined from freezing point determinations.

28 By taking advantage of the vastly different freezing points for aqueous solutions and immiscible oil

29 Four mutants are characterized by freezing point hysteresis (activity), circular dichroism

30 e that may help sequester water or lower the freezing point in the vicinity of the cell.

31 in the character of the fluctuations as the freezing point is traversed is beyond the scope of this

32 inding supports the view that, far below the freezing point, liquid water inside ice and permafrost i

33 c mechanism resembling the depression of the freezing point of a solvent due to the presence of a sol

34 specific proteins that are able to lower the freezing point of aqueous solutions relative to the melt

35 ly 245 K critical point is >/=10 K below the freezing point of interbilayer water, and we were unable

36 with mean global temperatures well below the freezing point of pure water.

37 latively homogeneous and within error of the freezing point of seawater at the ocean's surface.

38 antifreeze proteins (AFPs), which lower the freezing point of solutions noncolligatively and inhibit

39 reviously noted substantial reduction in the freezing point of the solvent phase.

40 he critical temperature is located above the freezing point of the system.

41 thetics are known to cause depression of the freezing point of transitions in biomembranes.

42 Antifreeze proteins lower the noncolligative freezing point of water (in the presence of ice) below t

43 chemical evolution in the range between the freezing point of water and the limit of stability of li

44 cta warmed the surface, keeping it above the freezing point of water for periods ranging from decades

45 tion has been known since the mid-1970s, the freezing point of water has prevented detailed and struc

46 ration occurs at temperatures well below the freezing point of water or pressures above 5 kbar, respe

47 ble to warm Hesperian Mars anywhere near the freezing point of water, and other gases are required to

48 atalysis of chemical reactions even near the freezing point of water, remains a fundamental puzzle in

49 eme, whereas at temperatures approaching the freezing point of water, the equilibrium shifts in the d

50 is of proteins at temperatures far below the freezing point of water, thus opening a window to the co

51 when temperature variations occur around the freezing point of water.

52 cold denaturation, T(c), is often below the freezing point of water.

53 d possibly more than 145 degrees C below the freezing point of water.

54 s (TH), a difference between the melting and freezing points of a solution that is indicative of the

55 cay of the correlation function at the known freezing points of monodisperse and moderately polydispe

56 displayed a sharp increase in the ket as the freezing points of the solvents methylene chloride and a

57 formamide, formamide, and methanol for their freezing point suppression capabilities, effects on pept

58 on into (from) the bulk water phase near the freezing point, Tf.

59 y rapidly cooling the ink solution below its freezing point using solid carbon dioxide (CO2) in an is

60 respectively, whereas the depression of the freezing point was observed for the 1.15 nm nanotube bet

61 ure is reduced as temperature approaches the freezing point, with potential consequences for global o