Research Article

Soil Physical Characteristics and Saturated Hydraulic Conductivity in the Landform of Barito Delta, Kalimantan, Indonesia

Figure 8

Soil profile for cross-section GH and IJ in Barito Delta. The location of cross-section GH and IJ can be checked in Figure 1. It is constructed based on the result of interpolation of soil fraction applying Bayesian statistics. Horizontal axis is land surface, while soil depth is vertical axis. Horizontal and vertical scales are different for layout configuration only.