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Table 1 Parameters used in this study

From: Subduction initiation from a stagnant lid and global overturn: new insights from numerical models with a free surface

  

Regional model

Global model

 
  

Non-dimensional

Dimensional

Non-dimensional

Dimensional

 

Parameter

Symbol

value

value

value

value

Units

Mantle depth

D

1

600

1

2890

km

Reference viscosity

η 0

1

6.92×1027

1

1023

Pa s

Surface Ra number

R a H,0

0.1

-

  

-

Internal Ra number

R a T,0

  

106

-

-

Frank-Kamenetskii parameter

θ

60

-

  

-

Stress exponent

n

1

-

  

-

Gravitational acceleration

g

-

9.81

-

9.81

ms −2

Thermal conductivity

k

-

3

-

3

Wm −1 K −1

Thermal diffusivity

κ

1

10−6

1

10−6

m 2 s −1

Thermal expansivity

α

-

3×10−5

-

3×10−5

K −1

Temperature gradient

Δ T

-

2500

-

2500

K

Reference density

ρ 0

-

3300

-

3300

kg m −3

Heat capacity

C p 0

-

1200

-

1200

Jkg −1 K −1

Internal heating rate

H

1

6.31×10−12

20

5.44×10−12

Wkg −1

Constant yield stress

σ y,const

variable b

variable b

variable b

variable b

MPa

Yield stress gradient

Δ σ y

variable b

variable b

variable b

variable b

-

Friction coefficient

μ

  

0.09 a

-

-

Cohesion

C

  

100

6.34×105

Pa

Activation energy

E act

  

11.55

240

kJmol −1

Activation volume

V act

  

4.0

8.8878×10−7

m 3mol

Upper viscosity cutoff

η max

102 η 0

6.92×1029

105 η 0

1028

Pa s

Lower viscosity cutoff

η min

10−8 η 0

6.92×1019

10−4 η 0

1019

Pa s

Sticky-air layer: c

 

Thickness

d st

0.05

30

0.05

145

km

Viscosity

η st

10−8 η 0

6.92×1019

10−2 η 0

1021

Pa s

C-condition d

C Stokes

1.5×10−7

-

0.175

-

-

  1. aIndicated is standard setup; parameter variation is mentioned separately
  2. bFor actual values, see Tables 2 and 3
  3. cIf applied
  4. dIndicates suitable free-surface approximation with sticky-air approach if C Stokes1 (Crameri et al. 2012a)