scholarly journals Liquid segregation parameters from amphibolite dehydration melting experiments

1995 ◽  
Vol 100 (B8) ◽  
pp. 15611-15621 ◽  
Author(s):  
Michael B. Wolf ◽  
Peter J. Wyllie
Keyword(s):  
Dehydration Melting ◽  
Liquid Segregation ◽  
Melting Experiments

Effects of pressure and H2O content on the compositions of primary crustal melts

1996 ◽  
Vol 87 (1-2) ◽  
pp. 11-21 ◽  
Author(s):  
Alberto E. Patiño Douce
Keyword(s):  
High Pressure ◽  
Wide Spectrum ◽  
Low Pressure ◽  
Source Material ◽  
Stability Field ◽  
Dehydration Melting ◽  
Isothermal Conditions ◽  
The Stability ◽  
Melting Experiments

ABSTRACT:Melting experiments with and without added H2O on a model metagreywacke and a natural metapelite demonstrate how pressure and H2O content control the compositions of melts and residual assemblages. Several effects are observed under isothermal conditions. Firstly, the stability field of biotite shrinks with decreasing pressure and with increasing H2O content, whereas that of plagioclase shrinks with increasing pressure and H2O content. Secondly, the ferromagnesian content of melts at the source (i.e. coexisting with their residual assemblages) decreases with decreasing H2O activity. Thirdly, with increasing pressure the Ca/Mg and Ca/Fe ratios of melts decrease relative to those of coexisting garnet. As a consequence, a wide spectrum of melts and crystalline residues can be generated from the same source material. For example, H2O-starved dehydration melting of metagreywacke at low pressure (≤10 kbar) generates K-rich (granitic) melts that coexist with pyroxene- and plagioclase-rich residues, whereas melting of the same material at high pressure (≍15 kbar) and with minor H2O infiltration can generate leucocratic Na-rich and Ca-poor (trondhjemitic) melts that coexist with biotite- and garnet-rich residues. An increased H2O content stabilises orthopyroxene at the expense of garnet + biotite + plagioclase, causing melts to shift towards granodioritic or perhaps tonalitic compositions.

scholarly journals Locking up the AS1411 Aptamer with a Flanking Duplex: Towards an Improved Nucleolin-Targeting

2021 ◽  
Vol 14 (2) ◽  
pp. 121
Author(s):  
André Miranda ◽  
Tiago Santos ◽  
Eric Largy ◽  
Carla Cruz
Keyword(s):  
Loop Structure ◽  
Binding Properties ◽  
Stem Loop ◽  
Affinity Ligand ◽  
Stem Loop Structure ◽  
Topology Maintenance ◽  
G Quadruplex ◽  
Dimeric Form ◽  
Biophysical Techniques ◽  
Melting Experiments

We have designed AS1411-N6, a derivative of the nucleolin (NCL)-binding aptamer AS1411, by adding six nucleotides to the 5′-end that are complementary to nucleotides at the 3′-end forcing it into a stem-loop structure. We evaluated by several biophysical techniques if AS1411-N6 can adopt one or more conformations, one of which allows NCL binding. We found a decrease of polymorphism of G-quadruplex (G4)-forming sequences comparing to AS1411 and the G4 formation in presence of K+ promotes the duplex folding. We also studied the binding properties of ligands TMPyP4, PhenDC3, PDS, 360A, and BRACO-19 in terms of stability, binding, topology maintenance of AS1411-N6, and NCL recognition. The melting experiments revealed promising stabilizer effects of PhenDC3, 360A, and TMPyP4, and the affinity calculations showed that 360A is the most prominent affinity ligand for AS1411-N6 and AS1411. The affinity determined between AS1411-N6 and NCL denoting a strong interaction and complex formation was assessed by PAGE in which the electrophoretic profile of AS1411-N6 showed bands of the dimeric form in the presence of the ligands and NCL.

Correlation of Melting Results for Both Pure Substances and Impure Substances

1986 ◽  
Vol 108 (3) ◽  
pp. 649-653 ◽  
Author(s):  
E. M. Sparrow ◽  
G. A. Gurtcheff ◽  
T. A. Myrum
Keyword(s):  
Solid Phase ◽  
Equilibrium Phase ◽  
Equilibrium Phase Diagram ◽  
Vertical Tube ◽  
Step Change ◽  
Pure Substance ◽  
Characteristic Temperatures ◽  
Pure Substances ◽  
T Values ◽  
Melting Experiments

Melting experiments were performed encompassing both pure and impure substances. The pure substances included n-octadecane paraffin and n-eicosane paraffin, while the impure substances were mixtures synthesized from the pure paraffins. The experiments were carried out in a closed vertical tube whose wall was subjected to a step-change increase in temperature to initiate the melting. For each impure substance, supplementary measurements were made of two characteristic temperatures: the temperature T** at which melting of the solid phase first begins and the lowest temperature T* at which the melting can go to completion. For a pure substance, T** = T*. The time-dependent melting results for all the investigated substances, both pure and impure, were well correlated as a function of FoSte**(Gr**)1/8 alone, where the ** signifies the presence of T** in the temperature difference which appears in Ste and Gr. This correlation enables melting rates for impure substances to be determined from melting rates for pure substances. The T** values needed for the implementation of the correlation can be obtained from simple experiments, obviating the need for the complete equilibrium phase diagram.

Dehydration melting at the top of the lower mantle

Science ◽  
2014 ◽  
Vol 344 (6189) ◽  
pp. 1265-1268 ◽  
Author(s):  
B. Schmandt ◽  
S. D. Jacobsen ◽  
T. W. Becker ◽  
Z. Liu ◽  
K. G. Dueker
Keyword(s):  
Lower Mantle ◽  
Dehydration Melting

XPS study of iodine released in core melting experiments

1985 ◽  
Vol 7 (1) ◽  
pp. 22-28 ◽  
Author(s):  
H. Moers ◽  
J. G. Dillard ◽  
H. Klewe-Nebenius ◽  
G. Kirch ◽  
G. Pfennig ◽  
...  
Keyword(s):  
Xps Study ◽  
Melting Experiments
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