Fig. 1From: Changes in soil bacterial community structure in a short-term trial with different silicate rock powdersX-ray diffractometry depicting the mineralogy of the (A) soil (Gb: gibbsite; Gt: goethite; Kt: kaolinite; and Qz: quartz) and rocks (C) used in the experiments (Aeg: aegirine; Cpx: clinopyroxene; Eud: eudialite; Fsp: feldspar; Hem: hematite; Hul: heulandite; Mag: magnetite; Mca: mica; Ntr: natrolite; Nph: nepheline; Pl: plagioclase; Qz: quartz; and Sa: sanidine). B Textures of the soil and rock powders (VF: very fine, F: fine, M: medium, C: coarse, and VC: very coarse)Back to article page