Search results for "PRECURSOR"
showing 10 items of 490 documents
3,4,5-Trimethoxy-4'-methylbiphenyl
2013
In the title compound, C16H18O3, the dihedral angle between the benzene rings is 33.4 (2)°. In the crystal, molecules are packed in a zigzag arrangement along the b-axis and are interconnected via weak C—H⋯O hydrogen bonds, and C—H⋯π interactions involving the methoxy groups and the benzene rings of neighbouring molecules.
3,5-Dimethoxy-4'-methylbiphenyl
2013
The title compound, C15H16O2, crystallizes with three independent molecules in the asymmetric unit. The intramolecular torsion angle between the aromatic rings of each molecule are −36.4 (3), 41.3 (3) and −37.8 (3)°. In the crystal, the complicated packing of the molecules forms wave-like layers along the b and c axes. The molecules are connected via extensive methoxy–phenyl C—H…π interactions. A weak C—H…O hydrogen-bonding network also exists between methoxy O atoms and aromatic or methoxy H atoms.
3,4-Dimethoxy-4'-methylbiphenyl
2013
In the title compound, C15H16O2, the dihedral angle between the planes of the aromatic rings is 30.5 (2). In the crystal, molecules are linked via C—HO hydrogen bonds and C— H interactions, forming a two-dimensional network lying parallel to (100). peerReviewed
Methyl 3',5'-dimethoxybiphenyl-4-carboxylate
2013
In the title compound, C16H16O4, the dihedral angle between the benzene rings is 28.9 (2)°. In the crystal, molecules are packed in layers parallel to the b axis in which they are connected via weak intermolecular C-H...O contacts. Face-to-face π-π interactions also exist between the benzene rings of adjacent molecules, with centroid-centroid and plane-to-plane shift distances of 3.8597 (14) and 1.843 (2) Å, respectively.
Methyl 3',4',5'-trimethoxybiphenyl-4-carboxylate
2013
In the title compound, C17H18O5, the dihedral angle between the benzene rings is 31.23 (16)°. In the crystal, the molecules are packed in an antiparallel fashion in layers along the a axis. In each layer, very weak C-H...O hydrogen bonds occur between the methoxy and methyl ester groups. Weak C-H...[pi] interactions between the 4'- and 5'-methoxy groups and neighbouring benzene rings [methoxy-C-ring centroid distances = 4.075 and 3.486 Å, respectively] connect the layers.
Torque teno virus como marcador subrogado de inmunocompetencia en el trasplante
2019
El torque teno virus (TTV), es un virus de pequeño tamaño de ADN de cadena sencilla, desnudo y capsulado perteneciente a la familia Anelloviridae con una prevalencia aproximada del 95% independiente del sexo y del estado socioeconómico y cuya carga plasmática está relacionada con la funcionalidad del sistema inmune y por tanto puede ser útil para evaluar el riesgo de eventos adversos relacionados con la inmunosupresión. El efecto del acondicionamiento sobre la ADNemia de TTV en pacientes sometidos a trasplante alogénico de precursores hematopoyéticos (alo-TPH) ocasiona un descenso de las cargas del virus que se ve acompañado por un descenso paralelo del recuento absoluto de linfocitos. Tras…
Parámetros biológicos predictivos de la infección activa precoz por Citomegalovirus en el trasplante alogénico de precursores hematopoyéticos
2021
El trasplante alogénico de células precursoras hematopoyéticas es la única solución curativa para un variado número de neoplasias hematológicas de alto riego. Por esta razón, la infección sistémica causada por CMV ocasiona frecuente morbilidad y mortalidad en el paciente receptor de este tipo de trasplantes. En la actualidad se emplean dos estrategias terapéuticas. Sin embargo, ninguna está exenta de riesgos y ambas son mejorables. Disponer de marcadores biológicos que permitan estratificar a los pacientes de acuerdo al riesgo de desarrollo de infección sistémica haría posible una profilaxis dirigida, lo que resultaría en una menor toxicidad para el paciente y en menor incidencia de complic…
A CO2-gas precursor to the March 2015 Villarrica volcano eruption
2017
We present here the first volcanic gas compositional time-series taken prior to a paroxysmal eruption of Villarrica volcano (Chile). Our gas plume observations were obtained using a fully autonomous Multi-component Gas Analyser System (Multi-GAS) in the 3 month-long phase of escalating volcanic activity that culminated into the 3 March 2015 paroxysm, the largest since 1985. Our results demonstrate a temporal evolution of volcanic plume composition, from low CO$_2$/SO$_2$ ratios (0.65-2.7) during November 2014-January 2015 to CO$_2$/SO$_2$ ratios up to ≈ 9 then after. The H$_2$O/CO$_2$ ratio simultaneously declined to <38 in the same temporal interval. We use results of volatile saturatio…