6533b7ddfe1ef96bd127546e
RESEARCH PRODUCT
Temperature and pressure dependence of quercetin-3-O-palmitate interaction with a model phospholipid membrane: film balance and scanning probe microscopy study
Giovanni MarlettaFrancesco CastelliMaria Grazia SarpietroBruno PignataroLaura SardoneGiovanni Nicolosisubject
Membrane FluiditySurface PropertiesLipid BilayersAnalytical chemistryPhospholipidPalmitic AcidPhase separationPalmitic AcidsSurface pressureMole fractionMicroscopy Atomic ForcePhase TransitionBiomaterialsScanning probe microscopychemistry.chemical_compoundMembrane LipidsColloid and Surface ChemistryMonolayerLangmuir-Blodgett monolayersMolecular StructureTransition temperatureTemperatureQuercetin palmitateSurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsLangmuir–Blodgett monolayerMembranechemistryAluminum SilicatesQuercetinMicaStress MechanicalDimyristoylphosphatidylcholineAlgorithmsScanning force microscopydescription
The molecular interaction of quercetin-3-O-palmitate (QP) with dimyristoylphosphatidylcholine (DMPC) has been studied. Film balance measurements of the average molecular area vs QP molar fraction in DMPC/QP mixed monolayers showed that relevant positive deviations from ideality, i.e., a less dense monolayer packing, occurred for a temperature of 10 degrees C, below the critical melting transition temperature of DMPC monolayers T c m approximately equal 20 degrees C), while ideal behavior was observed at 37 degrees C, above this phase transition temperature. The positive deviation observed at low temperatures in the average molecular area increased with the surface pressure. Scanning probe microscopy measurements performed on mixed monolayers transferred on mica showed that the deviations from ideality were connected to the formation of nanometric-scale QP-rich domains. However, the formation of aggregates was observed only for relatively high-QP molar fractions X QPor = 0.25 at 10 degrees C, while it was not observed at 37 degrees C, i.e., when the ideal mixing was found at the air/water interface. The observed effects are explained in terms of a temperature- and surface pressure-dependent phase-separation process based on the predominance at low temperature and low molecular mobility of QP-QP and DMPC-DMPC aggregation forces, prompting the formation of QP-rich domains embedded in a DMPC-rich matrix. High temperature prompts the QP/DMPC ideal mixing.
| year | journal | country | edition | language |
|---|---|---|---|---|
| 2004-01-01 |