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Results showed that iron coated crushed brick possess more micro pores and a higher surface area owing to its clay nature.
Compared to parent zeolite, there were decrease of relative crystallinity, some blockage effects of micro pores and less strong acid sites after Ni loading.
For over-maturation and organic-rich shale, a high TOC content and a high silica content are beneficial for micro pores and fractures to be preserved.
Micro pores and fractures exist in internal minerals, such as calcite, quartz, and pyrite, as well as in their intervals with fracture surfaces, which reduce the capacity of fractures to resist tension and shear.
On the contrary, micro pores and transition pores are mainly with open pores in shale.
There are a lot of semi closed pores in micro pores and transition pores in coal, but in shale micro pores and transition pores are mainly with open pores.
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However it caused a reduction in the size of micro-pores and surface roughness of M.A.O.
The KOH activated material had significant micro-pores, and demonstrated electrokinetics of an ideal electric double layer.
Kinetic sorption/desorption of U VI) is characterized by mass transfer between stagnant micro-pores and mobile flow zones.
Further, Field Emission Scanning Electron Microscopy (FE-SEM) and Transmission Electron Microscopy (TEM) analysis reveal the existence of interconnected micro-pores and voids.
In the present study, bioactive coatings enriched with micro-pores and Ca-P-Sr elements were formed on pore walls of porous titanium by micro-arc oxidation (MAO).
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