Table 2 Fluid properties and non-dimensional parameters

From: Iron diapirs entrain silicates to the core and initiate thermochemical plumes

 

Symbol

Units

Laboratory

Earth

Fluid 1 (S1)

  Viscosity

μ 1

Pa s

0.004–115

10−3–102(14)

  Density

ρ 1

kg/m3

970–1385

2750–4000(66)

  Surface tension

γ

mN/m

65

350(53)

  Layer height

h 1

m

0.025–0.045

105–106

Fluid 2 (S2)

  Viscosity

μ 2

Pa s

103–104

1018–1021

  Density

ρ 2

kg/m3

1417–1520

3300–5500

  Layer height

h 2

m

0.24–0.26

3×106

Metal (M)

  Viscosity

μ m

Pa s

10−3

10−3

  Density

ρ m

kg/m3

5910

7000

  Surface tension

γ

mN/m

707(64)

1720(51, 52)

  Layer height

h m

m

10−3–10−2

102–105

Dimensionless parameters

  Reynolds # (droplets in S1)

Re S1

10−2–102

10−1–107(a)

  Reynolds # (diapir in S2)

Re S2

10−7–10−6

10−23–10−18(b)

  Reynolds # (S1plume in S2)

Re thch

10−11–10−8

10−21–10−19(c)

 Bond #

B diapir

8–50

1014–1015

 

B droplet

10−3–10−1

10−2–100

 Buoyancy ratio

ρm/ρ2

3.8–4.2

1.3–2.1

 

ρ2/ρ1

1.1–1.6

1.4–2.3

 Buoyancy diff

ρmρ2

kg/m3

4390–4493

1500–3700

 

ρ2ρ1

kg/m3

150–550

1500–3100

  1. Note: The range is given for the total difference, e.g. buoyancy ρmρ2 (text written as (ρm−2))
  2. aRe determined using Stokes settling velocity and rdroplet = 10−4–10−3 m
  3. bRe determined using Eq. (3) and rdiapir = 105 m
  4. cRe determined using Stokes velocity and rthch = 104–105 m