“…Soil is a loose, porous, dielectric material composed of water, air, and soil particles (Schaap, et al, 1997). The compactness and moisture content are important soil parameters that affect the plant growth, water movement, seedling emergence, and root penetration (Cui et al, 2015;Goutal et al, 2013;Ogée and Brunet, 2002). In early days, soil compactness was measured primarily by destructive sampling (Ronai and Shmulevich, 1995); later, instruments based on pressure-based soil cone-index measurement ( ASABE Standards, 2009;Erbach et al, 1991;Pillinger et al, 2018;Perumpral, 1987), microwave reflection measurement (Luo and Perumpral, 1995;Zoughi et al,1994), and volume and porosity measurement were used (Ronai and Shmulevich, 1995).…”