Table 1.
θt (m3·m−3) | ψmz (MPa) |
---|---|
0.40 | −0.08 ay |
0.35 | −0.03 a |
0.30 | −0.04 a |
0.25 | −0.23 ab |
0.20 | −0.26 ab |
0.15 | −0.56 bc |
0.10 | −0.51 b |
0.05 | −0.89 c |
Linear | NSx |
Quadratic | * |
Cubic | **** |
ψm was calculated from measurements of a handheld soil moisture sensor (Hydro Sense; Campbell Scientific) using a substrate-specific water retention curve estimated using the van Genuchten equation (van Genuchten, 1980), of which the residual water content is 0, the saturated water content is 0.74 m3·m−3, the inverse of the air entry suction is 771.43 MPa−1, and the dimensionless pore-size distribution is 1.33.
Means with same lowercase letters are not significantly different among treatments by Tukey–Kramer method with a significance level specified at 0.05.
NS, *, **** Nonsignificant, significant at p ≤ 0.05 or 0.0001, respectively.