Research Article

Soil Water Characteristics of Gleysols in the Bamenda (Cameroon) Wetlands and Implications for Agricultural Management Strategies

Table 4

Summary statistics of the soil moisture characteristics in the Bamenda wetlands (n = 20).

ParametersHWWPFCAWRAWCRAWCWUWWHCDGWAC
(%)(%)(%)(%)(mm/m)(mm/m)(%)(%)(mm/m)(dm/m)(%)(%)

Minimum7.2022.1448.1611.13215.83289.2129.040.11431.662.650.726.49
Maximum23.0258.8675.3445.80423.61567.6457.0027.59847.224 .4413.5231.86
Mean13.7244.8067.0022.20339.854554048.098.48679.703.837.4624.76
SD4.8711.167.0910.1662.8784.246.658.25125.730.454.086.89
CV36.0025.0011.0046.0018.0018.0014.0097.0018.0012.0055.0028.00
Skew0.59−0.66−1.151.27−0.48−0.48−1.211.33−0.48−1.06−0.14−1.19
Kurtosis−0.53−0.451.100.63−0.70−0.702.160.47−0.700.81−1.400.97
K-S stat0.130.130.160.200.130.130.120.250.130.220.130.20

HW: hygroscopic water; WP: permanent wilting point; FC: field capacity; AWR: available water reserve; AWC: available water content; RAW: readily available water; CW: capillary water; UW: unavailable water; WHC: water-holding capacity; D: weighting depth; AC: air content; GW: gravity water; CV: coefficient of variation; SD: standard deviation; K-S stat: Kolmogorov–Smirnov statistics.