ライフサイエンスコーパス: melt

1 um who perceives the right side of faces as 'melted'.

2 density liquid transition in the supercooled melt.

3 lusion until the final quench of the tektite melt.

4 ng and extensive vesiculation in the tektite melt.

5 for simulating entangled linear polyethylene melts.

6 rostructures in other high temperature alloy melts.

7 es on the right side of faces as if they had melted.

8 f the transcription bubble to drive promoter melting.

9 e temperature variations affecting degree of melting.

10 h H(2)O is assumed to be incompatible during melting.

11 phere decreased EAIS susceptibility to ocean melting.

12 r phonons are a lot less sensitive to stripe melting.

13 owing warm water layer and the rate of basal melting.

14 portance of heat-capacity changes during DNA melting.

15 examples of glasses that exhibit first-order melting.

16 Increased surface melting(17) could trigger hydrofracturing if it leads to

17 fic presenting a single dissociation peak (T(melting) = 88.7 degrees C).

18 In addition, we find that submarine iceberg melting accounts for over 95% of heat used for ice melt

19 are indicative that changes in snow and ice melt across glacial environments will influence the abun

20 Molten alkali metal borates embody a new class of high-t

21 t correlating inversely with their degree of melting, although H(2)O is assumed to be incompatible du

22 ral decomposition, nanoparticle lubrication, melting among others) that are typically thermal in orig

23 lvenes showed the expected reversible heated melt and cooling recrystallization in only a few example

24 lly available deltamethrin crystals, form I, melt and crystallize upon cooling into a polymorph, form

25 pends on lithospheric processes that control melt and volatile transport(1,3,7).

26 Sorbic acid melted and decomposed under dynamic heating.

27 l cycling commonly employed for nucleic acid melting and annealing, this is achieved by raising and l

28 s to a post-shock decompression that induced melting and extensive vesiculation in the tektite melt.

29 he Antarctic Ice Sheet by increasing surface melting and facilitating 'hydrofracturing'(1-7), where m

30 enhanced by lower degrees of sub-arc mantle melting and higher extents of intracrustal differentiati

31 ects the volatile partitioning during mantle melting and subsequent volatile speciation near the surf

32 yroxene was not exhausted at high degrees of melting and was retained in the residuum.

33 Uncharged bottlebrush polymer melts and highly charged polyelectrolytes in solution ex

34 As the cryosphere melts and thaws, alpine lakes and streams will experienc

35 elt), Antarctic ice shelves (increased ocean melting), and Greenland and Antarctic outlet glaciers (d

36 microstructures exist in Al-12.2at.%Si alloy melt, and the large Si-rich microstructures disrupt into

37 infectious keratitis, 3 (2.48%) for corneal melting, and 1 (0.83%) for corneal perforation.

38 is sensitive to phase transitions, including melting, and allows gathering insights on compositional

39 ss from coastal Greenland (increased surface melt), Antarctic ice shelves (increased ocean melting),

40 -rich microstructures in Al-12.2at.%Si alloy melt are probably aggregates comprising multiple small S

41 single-crystalline fusion zone after e-beam melting are unacceptable (e.g., prone to cracking), or,

42 e domains, which contribute little to mantle melting, are under-represented in compilations of mantle

43 ating interstrand base stacking, rather than melting as generally thought.

44 engineering-lightweight Al-12.2at.%Si alloy melt at 1100 degrees C, via melt-spinning (MS) of Al(1-x

45 i-rich microstructure in Al-12.2at.%Si alloy melt at 1100 degrees C.

46 does not dry out under arid conditions, not melt at 50 degrees C, and not change significantly under

47 o changes in the chemical composition of the melt at the crystal-melt interface with the growth of th

48 he meteoritic record that document incipient melting at the onset of planetary differentiation.

49 Adcumulus growth of plagioclase from such melts at the chamber floor results in the formation of m

50 ponse to pressure reduction, these ascending melts become first superheated and then saturated in pla

51 functional theory, that similar evidence for melting behavior in zeolitic imidazolate frameworks (ZIF

52 Here, we report the freezing and melting behavior of water (D(2)O) nanoconfined in archit

53 We reproduce both the re-entrant melting behaviour and the polymorphism of the solid phas

54 s may indicate increasing degrees of partial melting beneath D.

55 nate) (PBS) and poly(lactic acid) (PLA) were melt-blended and formed into a film by hot press forming

56 As the very vibrations invoked in ZIF melting but heretofore unobserved for carboxylate MOFs,

57 ospholipids occupy an ordered array that has melted by 40 degrees C.

58 this paper, the AISI4140 steel samples were melted by laser with different parameters.

59 Once the phase change polymer is temporarily melted by transient laser heating, the orientation of th

60 of a lattice (similarly one can create local melting by creating divacancies).

61 rget site DNA base unstacking, flipping, and melting by RAG1 methionine 848 explain how this residue

62 We examine the melt capture performance at industrially relevant concen

63 NS synthesis splits CO(2) by electrolysis in molten carbonate and has a carbon negative footprint.

64 iency of the 4-electron CO(2) reduction in a molten carbonate electrolyte.

65 lly obtained drinking water by using fire to melt cave ice, and sheds light on one of many human-envi

66 d more gas than the shallower impact-induced melt chamber brines.

67 ere primarily sourced from an impact-induced melt chamber, with some contribution from a deeper, pre-

68 ng activity date is largely dictated by snow melt characteristics and that changing snow melt conditi

69 between the mixture components) and the same melting characteristics as the ice cream samples made wi

70 esent the same spectroscopic signatures upon melting, common to those observed for other pure late 3d

71 emonstrate the suitability of XAS to extract melt compositional information in situ, such as the evol

72 melt characteristics and that changing snow melt conditions may result in earlier spring activity.

73 occur under high-power, low-scan speed laser melting conditions.

74 Snow melt end date, melt rate, and melt consistency explained 45% of the variation in sprin

75 ice motion in response to increased surface melt, consistent with previous research.

76 t (and so relatively low viscosity) silicate melt cooled to form glass.

77 Here we find that submarine iceberg melting cools and freshens the fjord by up to ~5 degrees

78 The presented melting criterion seems to be general for late 3d metals

79 lipid (glycerol monostearate) influences the melting, crystallisation and enthalpy of NLCs and their

80 l stages of lunar magma ocean (LMO) or later melt crystallization.

81 iction and design of probes and primers, but melt curve analyses are low-throughput and produce inacc

82 ile keeping it cool enough to stay below the melt curve.

83 ltiplexing, referred to as amplification and melting curve analysis (AMCA), which leverages the kinet

84 plexity of the assay and enabling the use of melting curve analysis for validation.

85 Using gel electrophoresis and DNA melting curve analysis, we showed that LiCl-isopropanol

86 3 +/- 0.13%, an increase of 10.0% over using melting curve analysis.

87 Here, we investigated the melting curve and the eutectic composition of four geoph

88 In olive samples, the derived melting curve was specific presenting a single dissociat

89 hogens having the most similar sequences and melt curves are still reliably identifiable in the prese

90 s task and are in some cases able to resolve melt curves with single-nucleotide resolution.

91 lting experiments; however, acquiring enough melt data to derive accurate NN parameters with modified

92 mising agreement with available experimental melt data.

93 Surprisingly, MELT dephosphorylation can occur normally under these co

94 multiplexing using a digital high-resolution melt (dHRM) after the digital PCR (dPCR).

95 Digital High-Resolution Melt (dHRM) is an emerging technology with potential to

96 g Miscanthus in an energy application is the melting during the combustion due to its high alkali sil

97 to crack-free 3D printing via electron beam melting (EBM) with preheat as well as selective laser me

98 NLCs were produced by melt-emulsification using ultra-homogenisation followed

99 Snow melt end date, melt rate, and melt consistency explained

100 tain monotonous activity while the volume of melt entering the crust is high, raising the possibility

101 the importance of diffusion coefficients and melting enthalpies in controlling the growth rates, and

102 reflected by a higher thermal stability and melting enthalpy changes of the starches.

103 hysical studies involving circular dichroism melting experiments, microscale thermophoresis measureme

104 ameters are derived from a series of optical melting experiments; however, acquiring enough melt data

105 systems contain extreme heterogeneity, with melts extending to rhyolitic compositions.

106 ntains a long-lived component that formed by melt extraction from a domain with chondritic (143)Nd/(1

107 tle source that is geochemically depleted by melt extraction rather than primitive.

108 here geochemical depletion refers to ancient melt extraction) common to most oceanic island basalts,

109 The iDES were manufactured using a hot melt extrusion process with accurate irinotecan drug loa

110 ellose processing include spray draying, hot-melt extrusion, 3D printing, and electrospinning.

111 cal technologies including spray drying, hot-melt extrusion, 3D printing, nanoprecipitation and elect

112 g above the melting region, where water-rich melt flows faster than residual peridotites through duni

113 s intergranular corrosion of Ni-Cr alloys in molten fluoride salt at 650 degrees C.

114 cic activity given a decrease in the crustal melt flux.

115 Laser surface melting followed by rapid solidification is an effective

116 s has been attributed to condensed vapor and melt from an extraterrestrial impactor or to volcanism.

117 Al(1-x)Si(x) (x = 0.03,0.07,0.122,0.2) alloy melts from different initial melt temperatures, 800 degr

118 cles, nucleated homogeneously in the tektite melt, froth vesicles nucleated heterogeneously on relict

119 vent resulted in deposition of spheroids and melt glass, followed by deposition of diamectite and car

120 emin disassociation from partially unfolded, molten globular species during early disassembly and lat

121 tes the formation of a compact and transient molten globule intermediate state.

122 The dynamics of the acid unfolded and molten globule state are similar in the framework of the

123 nfolded and presence of alpha-helices in the molten globule state lead to internal friction to a simi

124 myoglobin, for the unfolded and even for the molten globule states, models from polymer science are e

125 s fully synthesized, without collapsing into molten globule-like states or forming stable intermediat

126 However, the use of molten gold is not favoured by industry, owing to its hi

127 Alternately, melted grains of quartz, chromferide, and magnetite in A

128 highly incompatible component, suggests post-melting H(2)O enrichment.

129 ative reactions and amplicon high-resolution melt (HRM) analysis to distinguish true positives from f

130 Two methods - high-resolution melting (HRM) and rhAmp(R) SNP genotyping - were develop

131 to the local coordination environment during melting impact the entropy and enthalpy of metal-organic

132 g accounts for over 95% of heat used for ice melt in Sermilik Fjord.

133 s Ice Shelf Program hot water drill borehole melted in the central region of the shelf in December 20

134 an ocean model to simulate submarine iceberg melting in Sermilik Fjord, east Greenland.

135 This transition from carbonate slab melting in the transition zone to slab dehydration in th

136 amic models to characterise the diversity of melts in magmatic systems beneath monotonous shield volc

137 , as well as for constraining entrainment of melts in the mantle and in the present-day core-mantle b

138 n trace element and isotopic fingerprints of melt inclusions.

139 In the partially melted initiation complex (PmIC), transcription factor M

140 ng substitution and elimination reactions in molten inorganic salts.

141 copy measurements of dynamics at the crystal-melt interface during the radiation induced formation of

142 mical composition of the melt at the crystal-melt interface with the growth of the Se nano-crystallit

143 stic of the parent crystals transformed upon melting into a single tetrahedral site with a broad dist

144 processes from icy cometary bodies to fully melted iron meteorites with isotopic affinities to carbo

145 of microstructures in high temperature alloy melts is important for manufacturing of metallic compone

146 -7 years, based on the extent of heating and melting its host rocks.

147 tood solid polymorphism(1,3-5), an anomalous melting line(6) and the possible transition to a superco

148 no first-order transition observed above the melting line.

149 In a pure molten lithium carbonate electrolyte, thicker walled CNT

150 that the addition of calcium carbonate to a molten lithium carbonate supports the electrosynthesis o

151 r(1.4) Ta(0.6) O(12) solid-electrolyte-based molten lithium-molybdenum-iron(II) chloride battery (den

152 atinum, nickel, and cobalt suggest mixing of melted local sediment with small quantities of meteoriti

153 Solid-electrolyte-based molten-metal batteries have attracted considerable atten

154 s that deposited high-temperature meltglass, melted microspherules, and/or platinum at other YDB site

155 ents requiring keratoplasty owing to corneal melting might benefit from the strengthening effect of p

156 ritical CO(2) (sc-CO(2)) physical foaming of melt mixed systems was conducted.

157 sponsiveness is determined by the number of 'MELT' motifs in the kinetochore protein Spc105/KNL1 and

158 dapt a Methylation-sensitive High-Resolution Melting (MS-HRM) approach from dried blood spot (DBS) sa

159 metal oxides and graphite is deoxidised in a melt of CaCl(2) at a temperature of only 1173 K.

160 ularly in association with the formation and melt of sea ice, with distinct microalgal communities th

161 suggests a possible route to creating local melting of a lattice (similarly one can create local mel

162 ple preparation has a profound effect on the melting of a pure substance, and this could be criticall

163 are consistent with very-low-degree partial melting of a Vigarano-type carbonaceous chondrite (CV) f

164 gia Rift is caused by syn-rift decompression melting of a warm, enriched mantle.

165 The melting of any pure crystalline material at constant pre

166 The melting of cave ice under current climate conditions is

167 in the lake is very low and is sourced from melting of glacial ice and direct release of occluded CO

168 e noritic diogenite was derived from partial melting of pre-existing rocks and had crystallized in th

169 These factors drive the melting of promoter DNA, but how they support RNA primin

170 Melting of the bent crystal starts at the kink and often

171 (MIS) 101 (~2.55 Ma) also signal substantial melting of the EAIS, and peak sea levels during MIS G7 (

172 Enhanced basal melting of the ice shelves is thought to be the ultimate

173 ions results from their crystallization from melts of carbonate-rich subducted oceanic crust.

174 ht inhibit degrading processes in idiopathic melting or in ocular inflammatory diseases of the sclera

175 No episodes of corneal melts or ulcers occurred.

176 e in summer) in the 1990s to nearly complete melt-out in summer (<5% coverage) in the 2010s.

177 n proposed to serve as the "inert" anode for molten oxide electrolysis (MOE).

178 citric acid had two polymorphs identified by melting peaks at 129.97 degrees C and 145.04 degrees C a

179 ase this ecosystem respiration dominate snow melt period causing larger greenhouse gas losses during

180 The snow melt period coincides with rising ecosystem respiration

181 The first order chain-melting phase transition of lipid membranes is observed

182 he BUB complex, which can otherwise maintain MELT phosphorylation in an autocatalytic manner.

183 late like scales consisting of layers of low melting point alloy (LMPA) phase change materials fully

184 the degree to which particle size lowers the melting point and is found to vary between 300 and 1800

185 nce as well as physical properties including melting point and physical state at room temperature.

186 ical additives are characterized to identify melting point depressants capable of rapidly denaturing

187 Melting point depression increases with decreasing parti

188 This work reviews existing data on the melting point depression to constrain a simple parameter

189 ing is postulated as the root cause of their melting point depressions and physicochemical properties

190 The ice melting point in larvae was -32.5 degrees C as determine

191 ould be critically important where the exact melting point is used as a means for polymorph identific

192 MPA and one with two enclosures of different melting point LMPAs.

193 in a small yet significant decrease in their melting point of about 0.3-0.4 K.

194 solvents need to be mixed with suitable low melting point supporting electrolytes (e.g., ionic liqui

195 Additionally, the melting point transitions and the resulting heat of fusi

196 own illustration is the zigzag plot of their melting point versus chain length.

197 approach for chemical depth profiling of low-melting point, high surface roughness SnAg solder bump f

198 f the associated phase change in addition to melting-point depression in deformed or damaged crystals

199 chloroplast phospholipid, contains >40% high-melting-point molecular species (HMP-PG; molecules that

200 characterized by significant depressions in melting points compared to those of the neat constituent

201 the trend in deracemization correlates with melting points.

202 ed into a poly(anhydride-ester) backbone via melt-polymerization, with the active antimetabolite GMT,

203 We derived criteria to stabilize the melt pool dynamics and minimize defects.

204 challenge is to control complex laser-powder-melt pool interdependency (dependent upon each other) dy

205 instability generates acoustic waves in the melt pool that provide additional yet vital driving forc

206 anching frequently happening on the sides of melt pools enables crystals to follow drastic changes in

207 changes in thermal gradient across adjacent melt pools, resulting in substantial broadening of grain

208 olumnar grains confined to the centreline of melt pools, side-branching frequently happening on the s

209 s less-differentiated stereotypes, as in the melting pot metaphor.

210 The post-electron-beam-melting, pre-solutionizing recovery via sub-solvus annea

211 spheric mantle (SCLM), whereas after 107 Ma, melt predominantly derived from an asthenospheric source

212 contribution from the removed SCLM, despite melts predominantly deriving from the asthenosphere.

213 porative losses experienced during the laser melting process resulted in clad layers with lower chrom

214 riginal toughness upon repeated fracture and melt processing.

215 4-11 can be considered the long-sought first melt produced during partial differentiation of a carbon

216 in temperatures higher than the acid without melting, producing the respective carbonates and oxides

217 cooling and a ~15% reduction in mean surface melt production relative to 2003-2012.

218 ime amplification data and the thermodynamic melting profile using an affordable intercalating dye (E

219 trade based on their unique high-resolution melting profiles from COI, cytochrome b, and 16S ribosom

220 RCP) scenarios and Antarctic Ice Sheet (AIS) melt propagate into uncertainties in projected mean sea-

221 d with organic molecules by immersion in hot melts, providing single crystals suitable for X-ray diff

222 ubject of interest as a distinct category of melt quenched glass, and have potential applications in

223 The chiral MHP can thus be melt-quenched into a stable glassy state, otherwise inhi

224 The structure of melt-quenched zeolitic imidazole framework (ZIF) glasses

225 zation and ultrasonic treatment narrowed the melting range.

226 been found to be a better indicator of basal melt rate variability than the heat transported onto the

227 Snow melt end date, melt rate, and melt consistency explained 45% of the var

228 far exceeds that required to match observed melt rates(2,7,8), suggesting that other critical contro

229 for simulating ocean heat fluxes and induced melt rates.

230 ically have cold ice cavities with low basal melt rates.

231 ed by hydrous flux melting which changed the melting reactions such that clinopyroxene was not exhaus

232 nt diffusion of hydrogen occurring above the melting region, where water-rich melt flows faster than

233 Submarine iceberg melting releases large volumes of freshwater within Gree

234 lase only but where and how to produce these melts remains a contentious issue.

235 t in this regard is the dephosphorylation of MELT repeats on KNL1, which removes SAC proteins from th

236 the restriction-induced double-stranded DNA melting resets the systems.

237 Much of the melting, resolidification, and subsequent cooling take p

238 udies have demonstrated that ice shelf basal melting, resulting from the inflow of warm water onto th

239 suggests that olivines were deformed within melt-rich mush piles accumulating within the summit rese

240 review summarizes recent achievements in the molten salt electrochemistry of silicon, highlighting su

241 safety, which is different from traditional molten-salt Li metal batteries using a pristine metallic

242 Here, we report molten-salt syntheses of NiO particles exposing a variet

243 alic anorthosites appear to require parental melts saturated in plagioclase only but where and how to

244 understanding how current and future glacial melt seasons may influence downstream environments.

245 mal stability assay to examine proteome-wide melting shifts after treatment with DMSO, 1 or 20 uM sta

246 core in the early Earth was surrounded by a molten silicate layer, a basal magma ocean that may have

247 n contrast, if these reflections were frozen melt sills, they would imply the presence of thick young

248 xplained either by the presence of partially molten sills or frozen gabbroic sills.

249 EBM) with preheat as well as selective laser melting (SLM) with limited preheat.

250 her retention of the long-chain compounds in melting snow and ice.

251 12.2at.%Si alloy melt at 1100 degrees C, via melt-spinning (MS) of Al(1-x)Si(x) (x = 0.03,0.07,0.122,

252 etry to form Frank-Kasper phases in the neat-melt state undergo an interconversion from body-centered

253 s C to maintain the metallic electrodes in a molten state.

254 menable because the promoter recognition and melting steps are much less complicated than in eukaryot

255 structural changes occurring in the silicate melts studied up to pressures and temperatures exceeding

256 Applying the diode laser, molten substrate material is incorporated into the glass

257 re we present the observation of a partially melted superconductivity in which pairing fluctuations c

258 l Si-rich microstructures with increasing of melt temperature from 800 to 1100 degrees C.

259 t an unusual confluence of exceptionally low melting temperature (175 degrees C) and inhibited crysta

260 ght about a significant increase in apparent melting temperature (DeltaT(m) >= +3 degrees C).

261 me digital LAMP (dLAMP) with high-resolution melting temperature (HRM) analysis and use this single-m

262 is results in a tunable wavelength-dependent melting temperature (T(m) ) window (4.5-15 degrees C) an

263 ting in an 490 bp amplicon with a consistent melting temperature (T(m) = 87.8 degrees C).

264 Cl) crystals, a well-studied sample with low melting temperature and quantum super-shells of clusters

265 Changes in melting temperature and transitional pH depended on both

266 rolactone), affording independent control of melting temperature and Young's modulus by concurrently

267 experiments in which pressurized ice at its melting temperature is slid over a water-saturated till

268 We find that crowders can increase the melting temperature of both an 8-mer DNA duplex and a ha

269 the more stable, while being lower than the melting temperature of the original orange, or final yel

270 rmal stability (up to 29 degrees C increased melting temperature) when compared to that of the linear

271 ed significant changes on beta-lactoglobulin melting temperature, unfolded conformation and subsequen

272 We attribute a major role to post-melting temperature-dependent diffusion of hydrogen occu

273 r, as indicated by a 9 degrees C increase in melting temperature.

274 .122,0.2) alloy melts from different initial melt temperatures, 800 degrees C and 1100 degrees C, und

275 thalate (PET) which has glass transition and melting temperatures of 76 and 250 degrees C, respective

276 Tropomyosins displayed different melting temperatures, which did not correlate with amino

277 states of yeast mtRNAP that explain promoter melting, template alignment, DNA scrunching, abortive sy

278 clad thickness of 65.8 um was achieved after melting ten 50 um thick powder layers.

279 jecta material sustained a greater degree of melting than that likely derived from reactor Unit 3.

280 ggests a previously unobserved transient DNA melting that may occur during double-stranded DNA survei

281 How much melting the ocean causes depends on the temperature of t

282 ted in a solid matrix are released only upon melting the PCM to trigger a solid-to-liquid phase trans

283 If partially molten, the shallower sill would define the base of a th

284 ography (EUV) for the chip production, where molten tin is used to generate the EUV radiation.

285 at relies on a controlled failure mechanism (melting) to protect a circuit from overcurrent.

286 networks can undergo tunable, high-enthalpy melting transitions over a wide temperature range.

287 s are inconsistent with fractional anhydrous melting typically associated with a mid-ocean ridge sett

288 and the softening temperature preceding the melting was also lower on the convex (outer) side of the

289 c outlet glaciers (dynamic response to ocean melting) was partially compensated by mass gains over ic

290 led surface; in inkjet printing, where often molten wax is used; in additive manufacturing or metal-p

291 e samples are best explained by hydrous flux melting which changed the melting reactions such that cl

292 om these ice shelves is through ocean-driven melting which is controlled by largely unobserved oceani

293 are products of the chamber replenishment by melts whose saturation in plagioclase as a single liquid

294 iding conduits, and mixing of impact-induced melt with deeper endogenic brines, could also allow ocea

295 idified water- and salt-rich mud-like impact melts with scattered endogenic pits, troughs, and bright

296 cocoa butter nucleation and growth from the melt, with PGPR showing the smallest enhancement.

297 tion between dimensionless micro-hardness of molten zone (H*) and dimensionless laser energy density(

298 sionless, a monitoring system of hardness of molten zone was established; by testing under different

299 ns for both emission spectra and hardness of molten zone were researched in this work.

300 a method to monitor the properties of laser molten zone, in this paper, the AISI4140 steel samples w