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Table 3 Regression analysis of COD and NH3-N pollutants

From: Characterizing and explaining spatio-temporal variation of water quality in a highly disturbed river by multi-statistical techniques

Station

COD

NH3-N

Const

β T

β Q

F sig

R 2 adj

VIF

Cl

Const

β T

β Q

F sig

R 2 adj

VIF

Cl

Baidukou

1.5627

− 0.0020

− 0.0017

0.01

0.28

1.01

4.89

1.0625

− 0.0104

− 0.0078

0.01

0.40

1.01

4.89

Zhifang

1.2708

− 0.0014

0.0015

0.01

0.17

1.08

4.09

0.2282

− 0.0067

−0.0125

0.01

0.15

1.08

4.09

Chengwan

1.2321

−0.0032

–

0.60

0.04

1.12

4.33

0.1321

− 0.0391

0.001

0.01

0.38

1.12

4.87

Lifen

1.3748

–

− 0.0012

0.02

0.01

1.00

2.94

–

–

–

–

–

–

–

Zhidian

1.3933

−0.0030

− 0.0004

0.01

0.17

1.24

4.85

0.603

− 0.0190

− 0.0005

0.01

0.50

1.24

4.85

  1. Estimated coefficients (Const: constant intercept, \(\beta_{T}\): water temperature, \(\beta_{Q}\): water discharge) in bolditalic or italic mean 0.05 or 0.10 significant level of t test). \(F_{sig}\) and \(R_{adj}^{2}\) are the significant level of F test and determination coefficient for the estimated model. VIF and Cl are variance inflation factor and maximum condition index