Skip to main content
. 2018 May 17;9:647. doi: 10.3389/fpls.2018.00647

Figure 1.

Figure 1

Effect of pH and content of organic matter on the availability of Si(OH)4 in soil (A,D), concentration of Si (as SiO2) in plant dry weight (B,E), and its accumulation in the tomato plant (C,F) under two conditions of average soil temperature: 15°C (A–C) and 25 ° C (D–F). Data obtained from the proposed dynamic model considering as inputs of the growth model: PAR = 400 μmol m−2 s−1 (12 h per day); CO2 = 400 ppm; and Temperature: 30°C. As soil conditions were considered: a soil profile of 30 cm, soil humidity of 25% (w/w), and availability of Si as Si(OH)4 in irrigation water of 5 mg L−1.