Autopore 4 9510
The AutoPore IV 9510 is a mercury-intrusion porosimeter designed to measure pore size distribution and pore volume in solid materials. It can analyze pore sizes ranging from 0.003 to 360 micrometers. The instrument uses a controlled high-pressure mercury intrusion method to determine the porous structure of a sample.
Lab products found in correlation
24 protocols using autopore 4 9510
Comprehensive Characterization of HNXP Paper
Membrane Characterization by Porosimetry
Characterization of CS-P24/HA Scaffold
Characterization of Dried and Heat-Treated Gel Morphology
and microstructure
of the fractured surfaces of the dried gels and heat-treated gels
were characterized by a scanning electron microscope (SEM, SU-70,
Hitachi, Ltd., Japan). The macropore size distribution over the diameter
from 20 nm to 100 mm of the dried gels and heat-treated gel monoliths
were evaluated by mercury intrusion porosimetry (Belsorp mini II,
Bel Japan Inc., Toyonaka, Japan, and AutoPore IV 9510, Micromeritics
Instrument Corp.). The crystal structure of the samples after heat-treatment
was confirmed by powder X-ray diffraction (XRD: Empyrean 200895, PAN
analytical B.V., Holland). The porosity (%) of each sample was calculated
as [(1 – ρb)/ρs] –
100, (ρb and ρs are the bulk and
skeletal densities, respectively). Carrier concentrations of C12A7:e– were characterized by Hall measurement (HL5500, Nanometrics).
Comprehensive Characterization of Porous Materials
were characterized by X-ray
diffraction (3kw-D/MAX2500V, Rigaku) using a Cu Kα radiation
(λ = 1.5406 Å), where the data were collected at a scanning
rate of 4°/min, and X-ray fluorescence spectroscopy (XRF-1800,
Shimadzu). TG-DSC measurements were performed using a NETZSCH thermal
analyzer, where the samples were heated at 5 °C/min in air. X-ray
photoelectron spectroscopy (XPS) measurements were performed using
a Thermo ESCALAB 250XI equipped with a monochromatic Al Kα X-ray
source. The microstructure and surface morphology were examined by
scanning electron microscopy (using an FEI JFM-7500F scanning electron
microscope) and an optical profiler (Contour GT-K, Bruker). The surface
area and mesopore analyses were performed using a nitrogen gas sorption
porosity analyzer (Autosorb-IQ2, Quantachrome). The porosity and macropore
size distribution were obtained by mercury intrusion porosimetry (MIP,
AutoPore Iv 9510, Micromeritics). The CA and SA were measured with
water droplets at room temperature using a JCY-2 instrument (Fangrui,
China). The three-point flexural strengths of the sintered samples
were measured with a strength testing machine at a loading rate of
2 N/s (Instron-5566, 10 kN).
Comprehensive Coal Characterization Protocol
standards (ASTM: 2007), the proximate analysis of coal was carried
out using a 5E-MAG6600 automatic industrial analyzer. Based on the
international standards (ISO 7404-5: 1984), vitrinite reflectance
(Ro) was measured using (Zeiss, Germany)
a microscope photometer. The maximum paleo temperature (Tpeak, the coal/intrusion contact temperature) can be calculated
by the following formula established by Barker and Pawlewicz:51
Referring to Taylor
and Glick,52 the maceral composition of
the coals can be obtained through incident light microscopy and oil
immersion. The porosity of the coal was measured by the mercury injection
method of Auto Pore IV 9510 (Micromeritics, USA). During the methane
adsorption experiment, 50 g crushed coal with a particle size of 0.2–0.25
mm were set at 30 °C, and the adsorption equilibrium gas pressure
reached 6 MPa. The determination of gas content adopts the direct
method and follows the Chinese national standard (State Administration
of Coal Mine Safety of China: 2008). The gas desorption experiment
of coal samples with different moisture contents was carried out for
120 min. The gas desorption amount of coal samples with various moisture
contents at different times can be obtained by the drainage method.
Pore Size Analysis of Fiber Samples
Mercury Porosimetry of Drug Tablet Porosity
In the case of leached tablets, the porosity results have been normalized by subtracting the initial mercury intrusion, in order to perform a clearer comparison of the structure of the pore network inside these systems.
Comprehensive Material Characterization
Quantifying Shale Porosity and Pore-Throat Size
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