ライフサイエンスコーパス: melt

1 history between Al-Cu-Fe alloys and silicate melt.

2 e volume for atoms to rearrange, to form the melt.

3 own to reduce the albedo of snow and enhance melt.

4 enon of lipid crystal dewetting from its own melt.

5 ransition in this metallic alloy supercooled melt.

6 lvent and co-alloyed desired metals into the melt.

7 urrently be removed commercially once in the melt.

8 evidence of water-limited late-stage Martian melts.

9 a universal phenomenon of oxide glasses and melts.

10 meteorites suggests higher water content in melts.

11 ion and the preceding alpha6 helix partially melted.

12 on a timescale coincident with the membrane melting.

13 ers all of the energy necessary for complete melting.

14 effect that led to more cooperative membrane melting.

15 ethods; complexation, encapsulation, and hot melting.

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

17 erconnections during baking, after margarine melting.

18 ty has been widely attributed to dehydration melting.

19 ient clamp closure as a prerequisite for DNA melting.

20 How does a crystal melt?

21 A hot melt 3D inkjet printing method with the potential to man

22 Hence, it is likely that silicate melt above and below the mantle transition zone, and ato

23 the lower crust with new evidence for rapid melt accumulation in the upper crust before many volcani

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

25 ed in inflowing warm Atlantic Ocean water to melt all Arctic sea ice within a few years, a cold haloc

26 eater temperature was required to completely melt all of the fat.

27 culations show that the active metals in the molten alloys are atomically dispersed and negatively ch

28 Crystallization of microdroplets of molten alloys could, in principle, present a number of p

29 overturning circulation increases underwater melt along the calving face, triggering rapid margin ret

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

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

32 arine biosphere-climate link through sea ice melt and low altitude clouds that may have contributed t

33 Crustal pathways connecting deep sources of melt and the active volcanoes they supply are poorly und

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

35 Simultaneously, the melting and freezing processes within the nanoparticles

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

51 et as a possible hot zone, linking ascending melts and shallow reservoirs.

52 The most viscous volcanic melts and the largest explosive eruptions on our planet

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

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

55 te that CO2 component remains soluble in the melt at high pressures and the solution is nearly ideal.

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

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

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

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

60 e glasses as analogue materials for silicate melts at ultrahigh pressures.

61 into the skin, individual microneedle shafts melted away by interstitial fluid from the epidermis and

62 ions, with unconnected nanotubes selectively melted away.

63 Co-melts based on blends of two different glass-forming com

64 anifest as variations in the depths at which melt becomes interconnected and detectable, the CO2 flux

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

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

67 We show, using the "Rusty Rock" impact melt breccia, 66095, that volatile enrichment on the lun

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

69 ate change is expected to cause earlier snow melt but may not change the last frost-free day of the y

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

71 The segregation of dense core-forming melts by porous flow is a natural mechanism for core for

72 ailable silica/carbon (SiO2/C) precursors in molten calcium chloride.

73 Redox media of molten carbonate or molten metal facilitating the transp

74 e prepared from these materials using a bulk melt-casting procedure.

75 The melting characteristics of surface free-fat analyzed by

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

77 the environment and (Li2Fe)ChO (Ch = S, Se) melt congruently; the latter is advantageous for manufac

78 This hysteresis in melt connectivity allows percolative core formation in p

79 This suggests that the hysteresis in melt connectivity is a viable process for percolative co

80 n in the severe FDNPP accident: Melted fuel (molten core)-concrete interactions (MCCIs), incorporatin

81 Understanding the flow of multi-phase (melt, crystals and bubbles) magmas is of great importanc

82 , in particular where fluids are stable over melts.Current estimates of dissolved CO2 in subduction-z

83 ogenetic marker for HRM, we observed complex melt curve signatures as compared to 16S rDNA amplicons

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

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

86 rithm to identify bacterial species based on melt-curve profiles of the 16S rRNA gene in an automated

87 The resulting bacteria-specific melt curves are identified by Support Vector Machine lea

88 heir hybrids through clearly-distinguishable melting curves.

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

90 younger Proterozoic diamond suite formed by melt-dominated metasomatism related to the 1.1 Ga Umkond

91 infrared laser, the phase-change material is melted due to the photothermal effect of gold nanocages,

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

93 NLCs were prepared by a melt emulsification-ultra sonication technique.

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

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

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

97 75%St+25%Su showed the smallest decrease of melting enthalpy with increasing temperature.

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

99 and giant magneto-impedance (GMI) in Co-rich melt-extracted microwires is key to optimizing their mag

100 Direct visualization at 1873 K of 0% to 8% molten FeAl droplets suspended in a SiO2 enriched oxide

101 s mantle heterogeneity or change in depth of melt formation within the martian mantle due to crustal

102 rated melt network remains connected down to melt fractions of only 1 to 2%.

103 uring meltdown in the severe FDNPP accident: Melted fuel (molten core)-concrete interactions (MCCIs),

104 must balance slow (plate tectonic) rates of melt generation and segregation in the lower crust with

105 Melting glaciers release previously ice-entrapped chemic

106 f the folding transitions from native (N) to molten globule (MG) to kinetic intermediates (U) pathway

107 guiding a large structural transition from a molten globule apo-state to a compact holoconformation.

108 that the almost fully folded protein retains molten globule characteristics with severe NMR line broa

109 onsistent with an experimental report of the molten globule state of ApoE4, simulations identify mult

110 ures up to 200MPa resulted in a structurally molten globule-like state where PepX maintained its seco

111 0, generating a conformationally fluctuating molten globule-like state.

112 Thus, it has some features of a molten globule.

113 adopted by these intermediates, also called molten globules (MG), to understand protein folding.

114 e lifetime in nanoprecipitates of CsPbBr3 in melt-grown CsBr host crystals and CsPbBr3 evaporated fil

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

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

117 t study the development of a high resolution melt (HRM) screening method for the identification of ei

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

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

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

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

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

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

124 The evolution of melt/ice interfaces thereafter is monitored by Mie scatt

125 tate, spatial distribution, and longevity of melt in the crust.

126 water content of this gravitationally stable melt in the LVL corresponds to a total water content in

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

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

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

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

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

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

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

134 using in situ measurements of quartz-hosted melt inclusions, the authors demonstrate that preserved

135 The molten ink undergoes directional solidification upon pri

136 ed by recent studies indicating that surface-melted inorganic NPs are in a 'glassy' state that is an

137 c materials) form stable colloids in various molten inorganic salts.

138 hould exhibit a dynamics similar to 'surface-melted' inorganic nanoparticles (NPs).

139 mal heating, a crystalline solid will always melt into a liquid above the melting point.

140 gh-pressure crystalline phase of bismuth can melt into a metastable liquid below the melting line thr

141 is whether a crystalline solid may directly melt into a sustainable metastable liquid.

142 We also demonstrate that MELT is a robust platform for MEI discovery and analysis

143 Evidence for the percolation of metallic melt is provided by X-ray microtomography of primitive a

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

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

146 he assembly approach a maximally-disordered, melt-like state which may be called the liquid state of

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

148 ponent of field along the magnetic easy-axis melts long-range order, revealing a bistable, strongly c

149 s semimetallic at the conditions of the deep molten mantle of early Earth and super-Earths, raising t

150 ng overhanging features, which have no prior melted material directly beneath them.

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

152 The melting mechanisms have been addressed by several theore

153 Redox media of molten carbonate or molten metal facilitating the transportation of ions off

154 Accelerated aging experiments on co-melt mixtures ranging from 0% to 100% of each component

155 clustering and percolation radically affect melt mobility, central to understanding industrial and g

156 te forcing scenarios using temperature-index melt modelling.

157 e-mantle equilibration in a largely to fully molten Moon.

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

159 Mps1 kinase phosphorylates KNL1 on conserved MELT motifs to generate a binding site for the Bub3-Bub1

160 etries reveal that a texturally equilibrated melt network remains connected down to melt fractions of

161 The melt network therefore remained close to textural equili

162 lution based on CHARMM36 force field and pre-melted Ni NPs (Voter-Chen Embedded Atom Method potential

163 ggers strongly localized heating adequate to melt non-covalently attached double-stranded oligonucleo

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

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

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

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

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

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

170 265 K, so dramatic that it can be viewed as melting of hydrogen sublattice.

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

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

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

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

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

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

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

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

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

180 composed of inorganic particles in inorganic melts offer opportunities for introducing colloidal tech

181 ng the intensity of the electron beam not to melt or deform the quartz nanotip without a metal coatin

182 GS data and simulations, we demonstrate that MELT outperforms existing MEI discovery tools in terms o

183 ric/oceanic warming and increases in glacial melt over the past half century.

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

185 from degassing processes rather than mineral-melt partitioning.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

208 While Antarctic surface melt ponds are relatively well documented on some ice sh

209 ce onto and across ice shelves, feeding vast melt ponds up to 80 kilometres long.

210 lly significant phenomena in LPBF, including melt pool dynamics, powder ejection, rapid solidificatio

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

212 While recently developed melting probes have demonstrated significantly improved

213 The melting procedure necessary to transform the frozen soli

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

215 higher than 10(5) , a record performance for melt-processed organic field-effect transistors.

216 Seasonal sea-ice melt processes may alter the exchange rates of selected

217 Melt-processing of complementary semiconducting polymer

218 plate motion exposes high- and low-pressure melt products as geographically distinct volcanoes, expl

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

220 ining oceanic biological production, and the melt rate of ice shelves.

221 as of ice shelves vulnerable to collapse, as melt rates increase this century.

222 ease in surface albedo and eventually higher melting rates.

223 dary pyroxenite, which is formed as eclogite melt reacts with peridotite, dominates the low-pressure

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

225 with peridotite, dominates the low-pressure melt region beneath Loa-track volcanism, yielding the sy

226 ment at the WAIS ice divide, downwind of the melt region, provided detailed insight into the physical

227 e patients who developed progressive corneal melt required therapeutic penetrating keratoplasty.

228 hat might affect the growth and stability of melt-rich layers, focusing particularly on conditions th

229 from the snowpack through the entire spring melt runoff period for two years.

230 The non-molten salt ion exchange method used to prepare Li2Mg2P3

231 This reaction may proceed on molten salt state surfaces owing to the lower melting po

232 t lower temperatures can be applied to other molten salt systems and is also promising for waste glas

233 of high-quality Si films from a CaCl2 -based molten salt.

234 degrees C by using low-melting-point ternary molten salts CaCl2 -MgCl2 -NaCl, which still retains hig

235 bundant and inexpensive Si source soluble in molten salts, at a low temperature of 650 degrees C by u

236 on mobilities as high as those in liquids or molten salts, have been employed as solid-state electrol

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

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

239 During warmer melt seasons, these drainage networks adapt to changing

240 al rates of MeHg production in snowpacks and melted snow using mercury stable isotope tracer experime

241 snow deposition, surface snow, streams from melted snow, coastal seawater, and plankton samples were

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

243 sily with thermoplastics as the extruded hot melt solidifies rapidly during the printing process.

244 al separation between high- and low-pressure melt source regions; second, the recent azimuthal change

245 Here we measure the viscosity of a series of melts spanning the compositional range of the Yellowston

246 to a Dy-free Nd30.0Fe61.8Co5.8Ga0.6Al0.1B0.9 melt spun powder (MQU-F, neo Magnequench).

247 [2+2] addition have focused on solid-state, molten-state, or host-guest systems under ultraviolet-li

248 by current viscosity models and result from melt structure reorganization, as confirmed by Raman spe

249 This correlation between melt structure, viscosity and eruptive behaviour holds d

250 Optical melting studies were performed with RNA duplexes contain

251 alloys, and Al2O3 enrichment in the silicate melt surrounding the alloys.

252 erent temperatures using the selective laser melting technique.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

267 d abnormal electrophoretic migration and low melting temperature.

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

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

270 However, transition melting temperatures derived from the differential scann

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

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

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

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

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

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

277 dius at which temperatures are sufficient to melt the ash, regardless of peak current.

278 osed to temperatures sufficient to partially melt the constituent stonework, leading to the preservat

279 tes that POLRMT needs both TFB2M and TFAM to melt the promoter.

280 complexes lack the mechanism to efficiently melt the promoter.

281 lid (ice) floats on its liquid; pressure can melt the solid rather than freezing the liquid; heating

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

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

284 After snow melt, the cities return to being strongly controlled by

285 In addition to using MELT to discover MEIs in modern humans as part of the 10

286 athways connect subduction-induced ascending melts to shallow magma reservoirs.

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

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

289 in 4-ethylpyridine, tri-n-butylphosphine, or molten tri-n-octylphosphine oxide solution results in na

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

291 ids always become softer when vitrifying the melts under higher cooling rates.

292 nd find that in a narrow compositional zone, melt viscosity increases by up to two orders of magnitud

293 Here we report how major changes in melt viscosity, together with glass Raman and Nuclear Ma

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

295 with air temperatures warming prior to snow melt, which preceded forest canopy closure.

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

297 punctate epitheliopathy to bilateral corneal melt with subsequent perforation.

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