3 research outputs found
In Situ Investigation on the Effect of Salinity and pH on the Asphaltene Desorption under Flowing Conditions
There
is a limited understanding of the microscale interactions
between fluid–oil–solid interfaces, which could be a
stumbling block to the development of relevant technologies and industries.
With this in mind, we applied an in situ method, quartz crystal microbalance
with dissipation (QCM-D), on the interactions among the fluid–oil–solid
phases and investigated the desorption process of the asphaltene model
molecule from silica surfaces during a flow of LSW at the conditions
of different ion types, salinities, or pH values. The salinity effect
plays a bigger role than that of the pH effect on the asphaltene desorption
and, furthermore, the divalent ions (such as SO42–, Mg2+, or Ca2+) show a stronger effect than
that of monovalent ions (such as Cl–, Na+, or K+). Our study provides a new strategy for the investigation
of the interactions between fluid–oil–solid interfaces
Ultrasensitive Fluorometric Angling Determination of <i>Staphylococcus aureus</i> in Vitro and Fluorescence Imaging in Vivo Using Carbon Dots with Full-Color Emission
Rapid, accurate,
and safe screening of foodborne pathogenic bacteria
is essential to effectively control and prevent outbreaks of foodborne
illness. Fluorescent sensors constructed from carbon dots (CDs) and
nanomaterial-based quenchers have provided an innovative method for
screening of pathogenic bacteria. Herein, an ultrasensitive magnetic
fluorescence aptasensor was designed for separation and detection
of Staphylococcus aureus (S. aureus). Multicolor fluorescent CDs with a long fluorescent lifetime (6.73
ns) and high fluorescence stability were synthesized using a facile
hydrothermal approach and modified cDNA as a highly sensitive fluorescent
probe. CD fluorescence was quenched by Fe3O4 + aptamer via fluorescence resonance energy transfer (FRET). Under
optimal conditions, the FRET-based aptasensor can detect S.
aureus accompanied by a wide linear range of 50–107 CFU·mL–1 and a detection limit of
8 CFU·mL–1. Compared with other standard methods,
this method was faster and more convenient, and the entire test was
finished within 30 min. The capability of the aptasensor was simultaneously
investigated on food samples. Additionally, the developed CDs exhibited
excellent biocompatibility and were thus applied as fluorescent probes
for bioimaging both in vitro and in vivo. This new platform provided
an excellent application of the CDs for detecting and bioimaging pathogenic
bacteria
Desorption Mechanism of Asphaltenes in the Presence of Electrolyte and the Extended Derjaguin–Landau–Verwey–Overbeek Theory
Desorption of asphaltenes from silica-coated
quartz crystals upon
exposure to a series of saline solutions was studied through the measurements
of quartz crystal microbalance with dissipation (QCM-D), atomic force
microscopy (AFM), and contact angle. Interestingly, it was found that
the mass loading and thickness of asphaltene film decreased during
the injection of sodium chloride solution at the concentrations ranging
from 1 to 10 mM, with the surface tending to be hydrophilic, whereas
the mass loading and film thickness increased gradually when the concentration
increased from 10 to 1000 mM, with the surface inclined to be hydrophobic.
It was also found that the electrostatic force had a great effect
on this process due to the interactions between the charged interfaces
of oil/water and water/solid. Besides, some additional interactions
may arise under small distance at the presence of the electrolyte
solution, and therefore, a direct force-measuring technique was introduced,
in which the functionalized AFM tips felt a solid surface to model
the interactions among three phases of oil, water, and solid. Based
on the computed results of disjoining pressure isotherms, the theory
of Derjaguin–Landau–Verwey–Overbeek (DLVO) was
extended, taking into account of the participation of hydration forces
which played an important role at short range. These structural forces
mostly originated from the overlap of the hydrated layers under a
variety of salinity concentrations, resulting in the balance of resultant
interactions
