“…The porous material L23 is KSK-G silica gel with the SiO 2 skeleton material, the surface of which was chemically modified with alkylsilanes, to produce hydrophobic properties to the pore surface [25]. Using the methods of low-temperature nitrogen adsorption [26], helium pycnometry [26], and liquid porometry [17], the following characteristics of porous media were determined and within the limits of the error coincide with the results obtained in [27]: specific pore volume (V por ) (0.56 ± 0.02) cm 3 /g, skeleton density (ρ pm ) (1.7798 ± 0.0016) g/cm 3 , specific surface area (S por ) (212 ± 7) m 2 /g (multipoint BET), specific volume of the porous medium (V pm = 1/ρ pm + V por ) ∼ 1.22 cm 3 /g, granule size (L) ∼ 10 µm, average pore size (< R >) (5.0 ± 0.2) nm, porosity (ϕ) ∼ 0.52 and characteristic of the pore size distribution function (δR/ < R >) ∼ 0.1. In addition, the compressibility of an unfilled porous medium (χ pm ) ∼ 0.41 • 10 −2 MPa −1 , the pressure value of the beginning of filling of pores under the conditions of a slow (quasistatic) pressure change (P c0 ) (15 ± 1) MPa, independent of the velocity of the rod according to [17].…”