Table 1 Basic statistics for soil properties at a depth of 0–20 cm in the study region.

From: Spatial variability of saturated hydraulic conductivity and its links with other soil properties at the regional scale

Properties

N

Mean

Minimum

Maximum

SD

CV(%)

Skewness

Kurtosis

K

216

2.597

0.010

11.54

2.009

77.3

1.951

4.826

sand

691

74.0

45.0

95.0

9.3

12.6

0.094

– 0.130

silt

691

24.5

4.0

54.0

9.2

37.5

– 0.074

– 0.142

clay

691

1.52

0.0

6.0

0.905

59.4

1.537

4.183

pHH2O

691

5.27

4.04

7.2

0.728

13.8

0.680

– 0.158

OC

691

0.862

0.002

3.8

0.427

49.5

0.904

3.684

CEC

691

9.675

3.050

21.2

3.109

32.1

0.654

0.956

WCgrav

228

0.067

0.009

0.287

0.045

67.4

1.626

3.586

WCTDR

228

0.071

0.001

0.232

0.038

53.7

1.330

2.218

BD

228

1.413

0.998

1.681

0.125

8.9

– 0.540

0.030

FI

228

0.425

0.308

0.525

0.038

8.9

0.000

– 0.030

Transformed data with a square root (sqr) and natural logarithm (ln)

sqr(K)

216

1.507

0.100

3.400

0.573

38.0

0.640

1.080

sqr(clay)

691

1.166

0.000

2.450

0.403

34.6

– 0.610

2.570

ln(pHH2O)

691

1.653

1.400

1.980

0.134

8.1

0.410

– 0.510

sqr(OC)

691

0.895

0.040

1.940

0.248

27.7

– 0.520

1.490

sqr(CEC)

691

3.070

1.750

4.600

0.499

16.3

0.100

0.300

ln(WCgrav)

228

– 2.914

– 4.710

– 1.250

0.667

22.9

– 0.200

– 0.250

sqr(WCTDR)

228

0.258

0.032

0.482

0.068

26.5

0.450

0.680

  1. N—number of samples, SD—standard deviation, CV—coefficient of variation, K—saturated hydraulic conductivity (m day−1), sand—(2–0.05 mm), silt—(0.05–0.002 mm), clay < 0.002 mm, pHH2O—acidity (−), OC—organic carbon (%), CEC—cation exchange capacity (cmol kg−1), WCgrav—gravimetric water content (m3 m−3), WCTDR—water content in time-domain reflectometry (m3 m−3), BD—bulk density (Mg m−3), FI—porosity (m3 m−3).