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1 n aqueous solution at temperatures above the freezing point.
2 ase sharply on cooling below the equilibrium freezing point.
3 astically enhanced on supercooling below the freezing point.
4 ynamics for the hard-sphere fluid around its freezing point.
5 mportant contributor to depressing the serum freezing point.
6 ng to ice crystals, effectively lowering the freezing point.
7 growth at temperatures below the colligative freezing point.
8 ed ice crystal and consequently lowering the freezing point.
9 ling the liquid from room temperature to the freezing point.
10 atures substantially higher than the in situ freezing point.
11  lies in how ion-water interplay affects its freezing point.
12 ensitive to humidity and can't operate under freezing point.
13 s on a substrate that is subcooled below the freezing point.
14 le viscosity and ionic conductivity, and low freezing point.
15 onse when the temperature approaches the RSG freezing point.
16 le properties, such as reduced viscosity and freezing points.
17 .320%), salt content (0.66 +/- 0.1673%), and freezing point (- 0.5814 +/- 0.1827 degrees C) were also
18  for cumulative degree days (higher than the freezing point [0 degrees C or 32 degrees F]) for T(max)
19 e-off to air temperatures varying around the freezing point, a condition which occurs more frequently
20                          Waters cooled below freezing point adjacent to Cape Darnley, Antarctica gene
21 5 and 100 and temperatures (T) between their freezing point and 298.15 K (25 degrees C).
22 n inhibit ice crystal growth by lowering the freezing point and preventing ice crystallization withou
23 ion by decreasing the bulk temperature below freezing point and separating pure ice crystals from con
24 duce a difference between the nonequilibrium freezing point and the melting point, termed thermal hys
25  A higher tetrahedral entropy leads to lower freezing point, and the freezing temperature is directly
26 on of metastable polymorphs, a depression of freezing points, and the formation of crystals with pref
27 teins (AFPs) bind ice nuclei and depress the freezing point by a noncolligative absorption-inhibition
28 ve an especially high ability to depress the freezing point by far exceeding the abilities of other A
29        They are frequently used to lower the freezing point by preventing the growth of larger ice cr
30 and inhibited microbial growth at soil water freezing points compared to warmer temperatures.
31 , pivotal to all theoretical descriptions of freezing point depression activity, but also reveal that
32  lost and adsorption becomes reversible when freezing point depression activity, but not ice recrysta
33  In this study we report and examine how the freezing point depression also impacts the lipid phase t
34 s hydrogenivorans, to induce non-equilibrium freezing point depression and thermal hysteresis in orde
35 quilibrium by a mechanism similar to that of freezing point depression by antifreeze proteins.
36 e osmolality of plasma was measured by using freezing point depression by microosmometer and osmolari
37       Serum osmolality was measured by using freezing point depression in a cross-sectional study.
38 hereas protein-treated soil showed a maximum freezing point depression of - 8.54 degrees C and therma
39 (+)-selective electrodes and osmolality with freezing point depression yielded values consistent with
40 ing for the effect of 50-200 p.p.m. H(2)O on freezing point depression, the onset of silicate melting
41 ia XAS, (1)H NMR, ESI-MS, conductometry, and freezing-point depression experiments.
42                              We measured the freezing-point depression of glycine-water up to 30% sup
43 negative feedback between ice growth and the freezing-point depression of the brine.
44 ne osmolality was determined with the use of freezing-point depression osmometry.
45 ssment was performed by measuring Posm using freezing-point depression osmometry.
46 ing the abrupt soil-freezing stress near the freezing-point depressions, elevating alkB1 gene-harbori
47 meric in benzene solution as determined from freezing point determinations.
48  By taking advantage of the vastly different freezing points for aqueous solutions and immiscible oil
49            Four mutants are characterized by freezing point hysteresis (activity), circular dichroism
50 e that may help sequester water or lower the freezing point in the vicinity of the cell.
51 d-liquid phase transition in water below the freezing point, in the so-called supercooled regime, has
52  in the character of the fluctuations as the freezing point is traversed is beyond the scope of this
53 inding supports the view that, far below the freezing point, liquid water inside ice and permafrost i
54                 The controlled soil showed a freezing point of - 4.59 degrees C and thermal hysteresi
55 c mechanism resembling the depression of the freezing point of a solvent due to the presence of a sol
56 ion of 30% (w/w) Pluronic F127 depressed the freezing point of an electrolyte comprising 50 mM ubiqui
57 ever, the poor stability and the unfavorable freezing point of aqueous electrolytes hinder their actu
58 specific proteins that are able to lower the freezing point of aqueous solutions relative to the melt
59 ly 245 K critical point is >/=10 K below the freezing point of interbilayer water, and we were unable
60 with mean global temperatures well below the freezing point of pure water.
61 latively homogeneous and within error of the freezing point of seawater at the ocean's surface.
62  antifreeze proteins (AFPs), which lower the freezing point of solutions noncolligatively and inhibit
63 ng with cryoprotective agents to depress the freezing point of the liver tissue.
64 reviously noted substantial reduction in the freezing point of the solvent phase.
65 he critical temperature is located above the freezing point of the system.
66 thetics are known to cause depression of the freezing point of transitions in biomembranes.
67 Antifreeze proteins lower the noncolligative freezing point of water (in the presence of ice) below t
68  chemical evolution in the range between the freezing point of water and the limit of stability of li
69 cta warmed the surface, keeping it above the freezing point of water for periods ranging from decades
70 tion has been known since the mid-1970s, the freezing point of water has prevented detailed and struc
71 t temperatures above the pressure-controlled freezing point of water ice on exo-Earths.
72 vity, with demonstrated T(c) approaching the freezing point of water in binary hydrides at megabar pr
73 ration occurs at temperatures well below the freezing point of water or pressures above 5 kbar, respe
74  upper surface due to the suppression of the freezing point of water with pressure, as might be induc
75 ble to warm Hesperian Mars anywhere near the freezing point of water, and other gases are required to
76 tions and have melting point higher than the freezing point of water, referred herein as phase-switch
77 atalysis of chemical reactions even near the freezing point of water, remains a fundamental puzzle in
78 eme, whereas at temperatures approaching the freezing point of water, the equilibrium shifts in the d
79 is of proteins at temperatures far below the freezing point of water, thus opening a window to the co
80 when temperature variations occur around the freezing point of water.
81  cold denaturation, T(c), is often below the freezing point of water.
82 d possibly more than 145 degrees C below the freezing point of water.
83 es where it occurs at temperatures above the freezing point of water.
84 s (TH), a difference between the melting and freezing points of a solution that is indicative of the
85 cay of the correlation function at the known freezing points of monodisperse and moderately polydispe
86 displayed a sharp increase in the ket as the freezing points of the solvents methylene chloride and a
87 formamide, formamide, and methanol for their freezing point suppression capabilities, effects on pept
88 inement leads to the decrease in the melting/freezing point temperature, density, and surface tension
89 on into (from) the bulk water phase near the freezing point, Tf.
90 erties such as reduced viscosity and a lower freezing point to acetyl-TAG, providing advantages for u
91 ce of perchlorate salts that depress water's freezing point to ~-60 degrees C, our approach provides
92 y rapidly cooling the ink solution below its freezing point using solid carbon dioxide (CO2) in an is
93  respectively, whereas the depression of the freezing point was observed for the 1.15 nm nanotube bet
94 , viscosity, heating value, flash point, and freezing point were found to meet the standards of SAF.
95 s the H-bond network, thereby depressing the freezing point while maintaining high ionic conductivity
96 ure is reduced as temperature approaches the freezing point, with potential consequences for global o