diff --git a/docs/4_Static-Maps_soil-hydraulic-properties/index.md b/docs/4_Static-Maps_soil-hydraulic-properties/index.md
index cac0fdd1..c1b34cd9 100644
--- a/docs/4_Static-Maps_soil-hydraulic-properties/index.md
+++ b/docs/4_Static-Maps_soil-hydraulic-properties/index.md
@@ -49,13 +49,13 @@ The table below shows the PTFs developed in [Toth et al. (2015)](https://onlinel
| Parameter | Pedotransfer function* | Condition |
| :---| :--- | :--- |
-|Theta saturated |$Thetas = (0.83080 - 0.28217 \cdot D + 0.0002728 \cdot C + 0.000187 \cdot S)$ |$Thetas <1$ (hurdle) |
+|Theta saturated |$Thetas = (0.83080 - 0.28217 \cdot BD + 0.0002728 \cdot C + 0.000187 \cdot S)$ |$Thetas <1$ (hurdle) |
|Theta residual |$Sand = 100 -S-C$
$Thetar=0.179$ if Sand<2.0
$Thetar=0.041$ if Sand≥2.0 |Thetar < Thetas (hurdle) |
|Lambda |$log10(λ) =$
$ 0.22236 - 0.30189 \cdot BD - 0.05558 \cdot T - 0.005306 \cdot C - 0.003084 \cdot S - 0.01072 \cdot OC$ |lambda≤0.42 (recommended)|
-|Genu Alpha | $log10(Alpha) =$
$ -0.43348 - 0.41729 \cdot D - 0.04762 \cdot OC + 0.21810 \cdot T - 0.01581 \cdot C - 0.01207 \cdot S$ |alpha≤0.055(recommended)|
+|Genu Alpha | $log10(Alpha) =$
$ -0.43348 - 0.41729 \cdot BD - 0.04762 \cdot OC + 0.21810 \cdot T - 0.01581 \cdot C - 0.01207 \cdot S$ |alpha≤0.055(recommended)|
|K saturated** | $log10(KSat) =$
$ 0.40220 + 0.26122 \cdot pH + 0.44565 \cdot T - 0.02329 \cdot C - 0.01265 \cdot S - 0.01038 \cdot CEC $| Ksat>0 (hurdle) |
-*where D is bulk density, C - % of clay, S - % of silt, OC - organic content, CEC - cation exchange capacity, pH - soil pH, and T is the topsoil and subsoil distinction. FAO_2008 (link) defines topsoil as 0-30 cm layer and subsoil as 30-100 cm layer. When soil depth is within the definition of topsoil then T = 1, otherwise T = 0.
+*where BD is bulk density, C - % of clay, S - % of silt, OC - organic content, CEC - cation exchange capacity, pH - soil pH, and T is the topsoil and subsoil distinction. FAO_2008 (link) defines topsoil as 0-30 cm layer and subsoil as 30-100 cm layer. When soil depth is within the definition of topsoil then T = 1, otherwise T = 0.
**K saturated results for Toth equation are in cm/day, the LISFLOOD model requires mm/day.