ライフサイエンスコーパス: melting

1 effect that led to more cooperative membrane melting.

2 Mo2 B, alpha-MoB, beta-MoB, and MoB2 by arc-melting.

3 ethods; complexation, encapsulation, and hot melting.

4 line with improved shape preservation during melting.

5 tegration and dimensional reductions through melting.

6 amplification, primer annealing and product melting.

7 trongly at threat in case of rapid Greenland melting.

8 processed successfully using selective laser melting.

9 d by TFB2M binding and induction of promoter melting.

10 erconnections during baking, after margarine melting.

11 y a paucity of direct observations of mantle melting.

12 ty has been widely attributed to dehydration melting.

13 ient clamp closure as a prerequisite for DNA melting.

14 on a timescale coincident with the membrane melting.

15 ers all of the energy necessary for complete melting.

16 strongly associated MOF liquid, obtained by melting a zeolitic imidazolate framework.

17 As glacier melting accelerates under future climate warming, chemic

18 t is coupled to TFIIH's established promoter melting activity.

19 High-resolution melting analysis followed by Sanger sequencing was used

20 base pairing is further supported by thermal melting analysis of GNA-C and GNA-G containing duplexes

21 High-pressure melting anchors the phase diagram of a material, reveali

22 n microscopy (SEM) showed characteristics of melting and blistering of TD MPs and shredding and flaki

23 riations in the triacylglycerol contents and melting and crystallization thermograms evidenced the re

24 ons that impact primer annealing and product melting and eliminates the requirement for thermal calib

25 xperimental study of the atomic mechanism in melting and freezing processes remains a formidable chal

26 Simultaneously, the melting and freezing processes within the nanoparticles

27 During the melting and freezing, the formation of nucleation precur

28 concentration of boron were prepared by arc-melting and investigated for their mechanical properties

29 CO2 bearing silicate melting and its relevance in the upper mantle regime hav

30 e molybdenum (Mo) surface to measure surface melting and mass loss.

31 The pressure-temperature paths of both its melting and peritectic curves were measured, beginning a

32 By periodically melting and revitrifying the spherical spinning glass, w

33 FAM has 'post-recruitment' roles in promoter melting and RNA synthesis, which were revealed by studyi

34 Effective control of melting and solidification behaviours of materials is si

35 In this paper, nanoparticle-induced unusual melting and solidification behaviours of metals are repo

36 annot be additively manufactured because the melting and solidification dynamics during the printing

37 icles will not only have impacts on existing melting and solidification manufacturing processes, such

38 The discovery of the unusual melting and solidification of materials that contain nan

39 e heat-affected zone (HAZ) size during local melting and solidification of materials.

40 ash behaviour and develop a model to predict melting and sticking conditions for its global compositi

41 ge some physico-chemical properties, such as melting and sublimation temperatures, and solubility.

42 Thouless and he got motivated to investigate melting and suprafluidity in two dimensions.

43 s for local geoid changes resulting from ice melting and terrestrial freshwater storage and allows fo

44 eedbacks between the extent of exposed rock, melting and thinning of the ice sheet.

45 We argue that melting and vaporization on precursor bodies and possibl

46 he silicate Earth is consistent with partial melting and vaporization rather than with simple accreti

47 ion of MOFs has been demonstrated to undergo melting and vitrification upon cooling.

48 explained by TFAM playing a role in promoter melting and/or stabilization of the open complex on LSP.

49 omic-scale evidence for point defect induced melting, and a freezing mechanism mediated by crystalliz

50 ation steps of promoter binding, bending and melting, and abortive RNA synthesis.

51 es and processes such as ionic conductivity, melting, and crystallization.

52 chniques are used instead of selective laser melting, and will enable additive manufacturing of other

53 he meltwater outflows from beneath a rapidly melting Antarctic ice shelf to identify the mechanism re

54 The unusual extent and duration of the melting are linked to strong and sustained advection of

55 We conclude that changes in ocean-induced melting are the primary cause of retreat for glaciers in

56 lization process, with the beta-phase itself melting at 167-170 degrees C (DeltaHfus = 27 kJ.mol(-1))

57 hermal event associated to beta myo-inositol melting at 221.43 degrees C, suggesting that the solid-s

58 onding HAZ size is decreased by 67% in laser melting at a pulse energy of 0.18 mJ.

59 and are thus a risk factor for further brain melting at birth.

60 he early stages of respective spring sea-ice melting at coastal sites in northeast Greenland and east

61 negative supercoiling that assists promoter melting at start sites.

62 The average rate of melting at the base of the large Filchner-Ronne Ice Shel

63 MCM to CMG might promote DNA untwisting and melting at the onset of replication.

64 s may generate energy that underlies initial melting at the origin.

65 after loading revealed that complete surface melting began at 1.0 MJ m(-2) (heat load parameter of 31

66 o not unfold as coaxial stacks, and thus its melting behavior cannot be accurately described by its c

67 Here, we examine the melting behavior in the MgO-FeO binary system at high pr

68 eathing mode frequency, revealing reversible melting bracketed to 105-151 degrees C and 87-117 degree

69 rates a barrier against strand unpeeling and melting-bubble formation.

70 uggested that TFB2M is required for promoter melting, but conclusive experimental proof for this effe

71 a water-rich fluid in the former and mantle melting by decompression in the latter.

72 hermal effusivity, it is possible that local melting can occur from deformation-induced heating.

73 The melting characteristics of surface free-fat analyzed by

74 redicting the impacts of Antarctic Ice Sheet melting concerns the vertical distribution of the export

75 f T(i) make it clear that the diamond is not melting, contradicting a recent suggestion.

76 vely after melting, thus offering a reliable melting criterion.

77 tes, shelf-life, physical properties such as melting, crystallization and blooming were analyzed.

78 Here we report a high-slope melting curve in molybdenum by synchrotron X-ray diffrac

79 s will intersect a deep depression along the melting curve of carbonated oceanic crust at depths of a

80 mallest amplicon, Vv3, produced a coincident melting curve shape in all sample types (leaf and wine)

81 heir hybrids through clearly-distinguishable melting curves.

82 for n >/= 8, and in the dialkyl series, the melting-decomposition temperature of the solid products

83 odel suggests melt production is highest and melting depths deepest early during continental breakup.

84 d for effective primer annealing and product melting during each cycle without interfering with the r

85 ure HIPing the fatigue life of electron beam melting (EBM) additively manufactured parts is currently

86 The Electron Beam Melting (EBM) process alleviates this to some extent as

87 ures for the insoluble complexes, whereas no melting endotherm was observed in the soluble complexes.

88 r storage, and visually broader peaks in the melting endotherms indicating a greater temperature was

89 only with very high melting transitions and melting enthalpies.

90 Melting point and melting enthalpy of CSO were -34 degrees C and 77.48J/g,

91 75%St+25%Su showed the smallest decrease of melting enthalpy with increasing temperature.

92 Our data indicate that abrupt ice melting events coincide with volcanogenic aerosol emissi

93 associated with winter storms and subsequent melting events, despite the degree of watershed developm

94 plexes form regular A-form helices and in UV-melting experiments the stability of the duplexes is onl

95 From measurements of the melting field [Formula: see text] of the vortex solid, w

96 With further climate-driven change and melting forecast for the twenty-first century, our findi

97 nts only associated with cocoa butter's high-melting fraction, with the oleic acid-based surfactants

98 es a novel means to achieving a PCM based on melting-free, low-entropy phase changes in contrast with

99 ly, these connections are formed without any melting/fusing of the beads, a key feature of this techn

100 Melting glaciers release previously ice-entrapped chemic

101 The acceleration of ice sheet melting has been observed over the last few decades.

102 interaction surface is important for origin melting, helicase assembly, and the recruitment of pol a

103 nnual glacial varve chronology recording the melting history of the Fennoscandian Ice Sheet at the en

104 As alternative, we propose high resolution melting (HRM) analysis as a simple tool to detect and id

105 High-resolution melting (HRM) analysis of DNA is a closed-tube single-nu

106 ated through comparison with high resolution melting (HRM) and showed high concordance with HRM (Pear

107 f this work was the study of High Resolution Melting (HRM) application as a screening method for must

108 self-priming template using high-resolution melting (HRM) fluorescent dyes that intercalate into the

109 mini-barcodes combined with high resolution melting (HRM) for the authentication of gadoid species:

110 ed real-time PCR followed by high-resolution melting (HRM) to identify Plasmodium species, and we com

111 universal PCR amplification, High Resolution Melting (HRM), and machine learning within 20,000 picoli

112 Island Glacier (PIG) terminates in a rapidly melting ice shelf, and ocean circulation and temperature

113 sub-complex at upstream facilitates promoter melting in an ATP-independent manner, distinct from a DN

114 elated to laser ablation, fragmentation, and melting in liquids, this Article presents a timely and c

115 diness has advanced the time of onset of ice melting in mid-May through inhibiting sea-ice refreezing

116 ns control the promoter search and drive DNA melting in the absence of external energy sources.

117 0)Th and (226)Ra excesses, reflecting mantle melting in the presence of a water-rich fluid in the for

118 feedback process and accelerated the sea ice melting in the summer.

119 is interval caused enhanced pressure-release melting in the uppermost mantle, which may have induced

120 Differential thermal analysis of DNA melting in these assays allowed analytical discriminatio

121 the onset of fat phase transition (freezing/melting) in human abdominal adipose tissue.

122 We propose that DNA melting is an active process initiated in RPc and that t

123 tics of atomic clusters in the liquid phase, melting is instead barrier-less and limited by buoyancy-

124 erally present in all actinide metals before melting, is critically important for a proper interpreta

125 t alone or combined with high-melting or low-melting lecithins.

126 can melt into a metastable liquid below the melting line through a decompression process.

127 ve interactions between cholesterol and high-melting lipids.

128 crostructural variability in selective laser melting manufactured parts; thereby providing a means to

129 A melting mechanism is proposed for Ga, in which the atomi

130 The melting mechanisms have been addressed by several theore

131 graphy enabled us to observe both growth and melting morphologies of the 3D quasicrystal at temperatu

132 ncing, methylation-sensitive-high-resolution melting (MS-HRM) and methylation-specific-Taqman-based-d

133 antitatively reproduce the multistep thermal melting observed in experiments, thus validating our mod

134 n episode of extensive and prolonged surface melting observed in the Ross Sea sector of the WAIS in J

135 ehybridization, this optically triggered DNA melting occurs at a solution temperature that is 22 degr

136 se ice-shelf channels are loci where intense melting occurs to thin an ice shelf, these findings expo

137 We thus attribute it to partial melting of a locally thickened, denser- and hotter-than-

138 orogen were formed, at least in part, by the melting of a subducted carbonate-bearing slab, and that

139 tern United States is strongly influenced by melting of accumulated mountain snowpack.

140 endotherms: 1) starch gelatinization, and 2) melting of amylose-lipid complexes plus protein denatura

141 Accelerated warming and melting of Arctic sea-ice has been associated with signi

142 ocks (TTGs) that were formed through partial melting of hydrated low-magnesium basaltic rocks; notabl

143 265 K, so dramatic that it can be viewed as melting of hydrogen sublattice.

144 situ the sound wave velocity during partial melting of hydrous peridotite.

145 etween these two extremes, investigating the melting of ice in the entire mesoscopic regime.

146 The melting of lipid domains in 1,2-dimyristoyl-sn-glycero-3

147 ieved by optically sensing the annealing and melting of mirror-image l-DNA analogs of the reaction's

148 nking ( approximately 9 degrees ); and local melting of neighboring WC bps.

149 U lavas indicate derivation from the partial melting of peridotite, rather than from the pyroxenitic

150 analogy with the Lindemann criterion for the melting of solids, we demonstrate a common scaling of st

151 The instability and accelerated melting of the Antarctic Ice Sheet are among the foremos

152 mobility at constant density, suggestive of melting of the CDW correlations rather than excitation a

153 roduced by around 20 per cent to 30 per cent melting of the Coucal basalts along high geothermal grad

154 is no time-reversal symmetry upon growth and melting of the decagonal quasicrystal.

155 The AP enables melting of the duplex to unmask the PQS, adopting a G-qu

156 Melting of the Greenland ice sheet (GrIS) and its periph

157 For example, increases in melting of the Greenland Ice Sheet and reductions in sea

158 fusion of H2O into the D2O ice, which favors melting of the interface, and the driving force for grow

159 Melting of the mantle during continental breakup leads t

160 onset and peak temperatures and enthalpy of melting of the polymorphic form V, at higher storage tem

161 o the West Antarctic continental shelf cause melting of the undersides of floating ice shelves.

162 , are carried out to monitor the microscopic melting of the water hexamer through the analysis of vib

163 therefore first require local dissociation (melting) of the duplex strands.

164 ity, including the temperature dependence of melting on salt concentration, the bias between open and

165 applicability, including where electron-beam melting or directed-energy-deposition techniques are use

166 Quillaja extract alone or combined with high-melting or low-melting lecithins.

167 A weakness with this approach arises when melting overhanging features, which have no prior melted

168 our understanding of the solidification and melting pathways of quasicrystals, we performed synchrot

169 genes to generate PCR products with specific melting peaks that differentiate pork, beef, horsemeat,

170 d during the early Holocene, associated with melting permafrost and retreating glaciers, while lowest

171 molecular dynamics simulations to study the melting phenomenon and the nature of the liquid obtained

172 olesterol and an exchangeable mimic of a low-melting phospholipid in liquid-disordered bilayers can b

173 e sterol and an exchangeable mimic of a high-melting phospholipid in liquid-ordered bilayers.

174 density of 100 A/cm(2), is above the boron melting point (2350 K).

175 ic spreading centers causes it to exceed the melting point (solidus), producing magmas that ascend to

176 ne or more of the powder reactants has a low melting point and low thermal effusivity, it is possible

177 Melting point and melting enthalpy of CSO were -34 degre

178 solid state which accounts for an increased melting point and stability.

179 The eutectic mixture has a well-defined melting point at 39 degrees C, and can be used as a bioc

180 Independently, the results show that the melting point for HfC0.98, (4232 +/- 84) K, is the highe

181 the particle was evident from the decreased melting point from 177+/-1 degrees C (native curcumin) t

182 native interfacial metal oxide layer of low melting point metal precursors (group III and IV) in liq

183 Circular dichroism measurements yielded a melting point of 62.8 degrees C, indicating unexceptiona

184 al which has a melting temperature above the melting point of boron.

185 h increasing initial fish oil concentration, melting point of the fish oil-loaded particles shifted t

186 olten salt state surfaces owing to the lower melting point of the used Na salts compared to the react

187 Van't Hoff equation), which was 98% and the melting point peak occurred at 171 degrees C.

188 upercooling, sustaining the liquid below the melting point such as supercooled water and silicon.

189 ntered at temperatures well below the silica melting point to form amorphous, solid, transparent glas

190 of 8.5 eV, a small formation energy, a high melting point, and desired mechanical properties.

191 )H and (13)C NMR spectroscopy, FTIR, EA, and melting point, and in the case of 1, 2, and 4-8, X-ray c

192 content, peroxide index, thermal properties, melting point, consistency, and solid fat content (SFC).

193 t maintains the sample temperature below its melting point, hyperpolarized (13)C-substrates can be ex

194 cation in fatty products for its appropriate melting point, SFC similar to that of soft table margari

195 ch show a high level of anisotropy up to the melting point, where the elastic and shear moduli vary b

196 the relationship between the spectra and the melting point, which can guide the selection of early dr

197 lid will always melt into a liquid above the melting point.

198 ing-point silicate glass cross-cutting lower melting-point Al-Cu-Fe alloys, as well as unambiguous ev

199 Binary mixtures of liquid metal (LM) or low-melting-point alloy (LMPA) in an elastomeric or fluidic

200 s were present on powder surface whereas low-melting-point fatty acids remained within powder particl

201 atty acid composition of P1 showed that high-melting-point fatty acids were present on powder surface

202 ructure-donating motif, while urea serves as melting-point reduction agent.

203 We show higher melting-point silicate glass cross-cutting lower melting

204 ow temperature of 650 degrees C by using low-melting-point ternary molten salts CaCl2 -MgCl2 -NaCl, w

205 ransition metal borides and carbides possess melting points above 3000 degrees C, are ablation resist

206 highly inviscid liquids characterized by low melting points and high solubility of rare earth element

207 fluidic device were investigated between the melting points of D2O ice (3.8 degrees C) and H2O ice (0

208 The secondary structures and melting points of the chimeric DNA fragment and its comp

209 eaction at a temperature much lower than the melting points of the composite materials, followed by a

210 adients, and the Gibbs-Thomson effect on the melting points of the convex and concave features.

211 reening single substitutions against thermal melting points to both produce minimally mutated stable

212 somers indicated that they possess different melting points, NMR spectra, crystal structures, and sta

213 ven-numbered n-alkanes near their respective melting points.

214 Here we demonstrate that a melting probe embedded with a single locked thymidine mo

215 , no effort has been made to design a simple melting probe that can reliably distinguish all four SNP

216 While recently developed melting probes have demonstrated significantly improved

217 The melting procedure necessary to transform the frozen soli

218 ezing in the winter and accelerating the pre-melting process in the spring, and in turn triggered the

219 Here we examine the melting processes that occurred during accretion on Eart

220 omer is rate-limiting for both annealing and melting processes.

221 Melting profiles from each species, as well as from seve

222 ture of phase Iota breaks up at the onset of melting, providing sufficient free volume for atoms to r

223 ease in surface albedo and eventually higher melting rates.

224 The development of microstructure during melting, reactive wetting and solidification of solder p

225 Reconciling geophysical observations of the melting regime beneath the East Pacific Rise with our ex

226 o freshwater discharge coming from Greenland melting reveals a significant decrease of the West Afric

227 r, outcomes remain poor secondary to corneal melting, scarring, and perforation.

228 CP8.5) baseline experiment a Greenland flash melting scenario corresponding to an additional sea leve

229 ogenic precursors released by open water and melting sea ice regions.

230 er and ample water supply during summer from melting snow and ice as well as thawing permafrost, cont

231 partitioning of BTs to the liquid phase of a melting snowpack leads to early peaks in summation opera

232 con, cutlets, blade loin, uncooked ham) or a melting step (salami sausage and liver paste).

233 Optical melting studies were performed with RNA duplexes contain

234 3-perovskite), with current estimates of the melting T at the base of the mantle ranging from 4800 K

235 We predict the correct low-pressure melting T, and at high-pressure we show that the melting

236 erent temperatures using the selective laser melting technique.

237 e at pH 8 but a ca. 50 degrees C drop in the melting temperature (Tm ) was observed at pH 2.5: DeltaD

238 Leishmania spp., followed by analysis of the melting temperature (Tm) of the amplicons on qPCR platfo

239 a significant negative shift in NBD1 thermal melting temperature (Tm), pointing to direct VX-809 inte

240 ng a ssNMR-observed reduction in the lipids' melting temperature (Tm).

241 ode made from a refractory metal which has a melting temperature above the melting point of boron.

242 e, double-nested PCR approach allowed robust melting temperature analysis with enhanced limits of det

243 me PCR assays followed by electrophoresis or melting temperature analysis, respectively.

244 previous experiments showed nearly constant melting temperature as a function of pressure, in large

245 -carbon increases the peptide's triple helix melting temperature by 8.6 degrees C.

246 the temperature of maximum stability and the melting temperature decreased on encapsulation.

247 ing T, and at high-pressure we show that the melting temperature is only 5000 K at 120 GPa, a value l

248 (Ni, Pt, Pd), when dissolved in inactive low-melting temperature metals (In, Ga, Sn, Pb), produce sta

249 Phonon density of states, entropy and melting temperature of aluminum were calculated using th

250 milar to each other and should not reach the melting temperature of any of the matched hybrids.

251 PPO, isotactic PPO is semicrystalline with a melting temperature of approximately 67 degrees C.

252 temperatures between 0.5 and 0.64 times the melting temperature of the matrix (1,356 kelvin) under a

253 Upon heated over the melting temperature of the polymer, the pores of the nan

254 iscriminatory power comes from the decreased melting temperature of the tL.C mismatched hybrid as com

255 e, cooperative unfolding transition having a melting temperature of Tm = 71 +/- 2 degrees C, in agree

256 A decrease in melting temperature resulted from the interesterificatio

257 ntrinsic lack of strength, ductility and low melting temperature severely restricts practical applica

258 s, allowing genotype discrimination based on melting temperature values.

259 o undergo an exceptionally steep increase in melting temperature when compressed.

260 ed of ternary mixtures of a lipid with a low melting temperature, a lipid with a high melting tempera

261 though different solvents modify the protein melting temperature, a unique dynamical regime is attain

262 low melting temperature, a lipid with a high melting temperature, and cholesterol.

263 s transition temperature Tg, and the crystal melting temperature, TL.

264 d abnormal electrophoretic migration and low melting temperature.

265 ture that is 22 degrees C lower than the DNA melting temperature.

266 ntiate the four SNP alleles by four distinct melting temperatures (termed the "4Tm probe").

267 The melting temperatures and latent heat of CPCMs are in the

268 decreasing differences between the polyester melting temperatures and the experimental temperatures,

269 However, transition melting temperatures derived from the differential scann

270 Acetylation decreased onset and peak melting temperatures for the insoluble complexes, wherea

271 First, melting temperatures of all mismatched hybrids should be

272 orithms were developed to accurately predict melting temperatures of nanoparticles of various composi

273 currently considerable uncertainty over the melting temperatures of the high-pressure mantle mineral

274 that of the t.C mismatched hybrid, while the melting temperatures of the tL-A, tL.G and tL.T hybrids

275 erall structure but displayed differences in melting temperatures possibly arising from C-terminal co

276 oil-loaded particles shifted to lower onset melting temperatures, and major polymorphic form transfo

277 ng of the energy landscape at the respective melting temperatures.

278 is a dynamically robust feature of Antarctic melting that should be incorporated into climate-scale m

279 ticles atop of each other whilst selectively melting the corresponding part cross-section into each l

280 fied in mid-ocean-ridge basalts that form by melting the upper mantle (about 8Ra; ref.

281 to 130 gigapascals, appear exclusively after melting, thus offering a reliable melting criterion.

282 did not affect the final temperatures of fat melting (Tmelting) or xanthine oxidase denaturation (Tde

283 he chimera, the Tsr HAMP undergoes a thermal melting transition at a temperature much lower than that

284 ure predict that relatively few mRNAs show a melting transition between 30 and 42 degrees C, consiste

285 also allows accurate differentiation between melting transitions and generic heating effects observed

286 ed a stereocomplex phase only with very high melting transitions and melting enthalpies.

287 Although experimental melting transitions are conceived as a loss of well-defi

288 sm (CD) spectroscopy in detecting the domain melting transitions of Ca(2+)-free (apo) CaM (reduction

289 easing ice mass and increasing decompression melting under the WAIS, increasing volcanism.

290 e crystals of these oftentimes incongruently melting, unstable or metastable materials.

291 long overnight hybridization time, lack of a melting verification of proper hybrid, and complicated s

292 nt in Earth's mantle affects the dynamics of melting, volcanic eruption style and the evolution of Ea

293 oter but alone was insufficient for promoter melting, which only occurred when TFB2M joined the compl

294 tions yields spatiotemporal order and active melting with no equilibrium counterparts.

295 ting sufficiently high temperatures to reach melting with relatively weak shocks.

296 tion upon treatment could limit both crystal melting (with a residual crystalline content up to 38% i

297 e that experienced shock metamorphism, local melting (with conditions exceeding 5 GPa and 1,200 degre

298 gle inductive coil is placed on the top of a melting wood alloy to examine the changes of its inducta

299 The limited size of this ideal melting zone explains the low number of LIVS typically o

300 ightning discharge channel there is an ideal melting zone that represents roughly 10% or less of the