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Merge pull request #812 from danieldouglas92/add_water_content_cookbook
Create a Cookbook of a Hydrated Slab
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cookbooks/2d_cartesian_hydrated_slab/2d_cartesian_hydrated_slab.grid
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# Grid File for creating vtk files to view in Paraview or Visit | ||
grid_type = cartesian | ||
dim = 2 | ||
compositions = 1 | ||
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# domain of the grid (x and y are the surface, z is vertical with 0 at the bottom) | ||
x_min = 0e3 | ||
x_max = 3000e3 | ||
z_min = 0e3 | ||
z_max = 1600e3 | ||
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# grid properties | ||
n_cell_x = 1500 | ||
n_cell_z = 800 |
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cookbooks/2d_cartesian_hydrated_slab/2d_cartesian_hydrated_slab.wb
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{ | ||
"version":"1.1", | ||
"coordinate system":{"model":"cartesian"}, | ||
"cross section":[[0,0],[8000e3,0]], | ||
"surface temperature":273, | ||
"thermal expansion coefficient":3.1e-5, "specific heat":1000, "thermal diffusivity":1.0e-6, | ||
"features": | ||
[ | ||
{"model":"mantle layer", "name":"Mantle", "max depth":1600e3, | ||
"coordinates":[[0,-100e3],[0,100e3],[3000e3,100e3],[3000e3,-100e3]]}, | ||
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{"model":"oceanic plate", "name":"Overriding Plate", | ||
"min depth":0, "max depth":200e3, | ||
"coordinates":[[0,-100e3],[0,100e3],[2000e3,100e3],[2000e3,-100e3]], | ||
"temperature models":[ {"model":"plate model", | ||
"min depth":-10e3, "max depth":300e3, | ||
"top temperature":273, "bottom temperature":-1, | ||
"spreading velocity":0.05, | ||
"ridge coordinates": [[[-1000e3,-100e3],[-1000e3,100e3]]]}] | ||
}, | ||
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{"model":"oceanic plate", "name":"Subducting Plate", | ||
"min depth":0, "max depth":300e3, | ||
"coordinates" :[[2000e3,100e3],[2000e3,-100e3],[3000e3,-100e3],[3000e3,100e3]], | ||
"temperature models":[{"model":"plate model", | ||
"min depth":0, "max depth":300e3, | ||
"top temperature":273, "bottom temperature":-1, | ||
"spreading velocity":0.1, | ||
"ridge coordinates": [[[8000e3,-100e3],[8000e3,100e3]]]}], | ||
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"composition models": [ | ||
{"model":"tian water content", "compositions":[0], "min depth": 0, "max depth": 3e3, "lithology":"sediment", "initial water content":3, "cutoff pressure":1}, | ||
{"model":"tian water content", "compositions":[0], "min depth": 3e3, "max depth": 7e3, "lithology":"MORB", "initial water content":1, "cutoff pressure":16}, | ||
{"model":"tian water content", "compositions":[0], "min depth": 7e3, "max depth": 11e3, "lithology":"gabbro", "initial water content":0.5, "cutoff pressure":26}, | ||
{"model":"tian water content", "compositions":[0], "min depth": 11e3, "max depth": 20e3, "lithology":"peridotite", "initial water content":2, "cutoff pressure":10}] | ||
}, | ||
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{"model":"subducting plate", "name":"Slab", | ||
"coordinates":[[2000e3,-100e3],[2000e3,100e3]], | ||
"dip point":[0,0],"max depth":10000e3, | ||
"segments":[{"length":250e3,"thickness":[300e3],"top truncation":[-50e3],"angle":[0,60]}, | ||
{"length":300e3, "thickness":[300e3],"top truncation":[-50e3], "angle":[60,80]}, | ||
{"length":500e3, "thickness":[300e3],"top truncation":[-50e3], "angle":[80,60]}, | ||
{"length":300e3, "thickness":[300e3],"top truncation":[-50e3], "angle":[60,40]}, | ||
{"length":300e3, "thickness":[300e3],"top truncation":[-50e3], "angle":[40,20]}], | ||
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"composition models":[ | ||
{"model":"tian water content", "compositions":[0], "density":3300, "min distance slab top":0, "max distance slab top":3e3, "lithology":"sediment", "initial water content":3, "cutoff pressure":1}, | ||
{"model":"tian water content", "compositions":[0], "density":3300, "min distance slab top":3e3, "max distance slab top":7e3, "lithology":"MORB", "initial water content":1, "cutoff pressure":16}, | ||
{"model":"tian water content", "compositions":[0], "density":3300, "min distance slab top":7e3, "max distance slab top":11e3, "lithology":"gabbro", "initial water content":0.5, "cutoff pressure":26}, | ||
{"model":"tian water content", "compositions":[0], "density":3300, "min distance slab top":11e3, "max distance slab top":20e3, "lithology":"peridotite", "initial water content":2, "cutoff pressure":10}], | ||
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"temperature models":[{"model":"mass conserving", | ||
"reference model name": "plate model", | ||
"density":3300, | ||
"adiabatic heating":true, | ||
"spreading velocity":0.1, | ||
"subducting velocity":0.1, | ||
"ridge coordinates":[[[8000e3,-100e3],[8000e3,100e3]]], | ||
"coupling depth":80e3, | ||
"forearc cooling factor":1.0, | ||
"taper distance":100e3, | ||
"min distance slab top":-200e3, "max distance slab top":300e3}] | ||
} | ||
] | ||
} |
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(part:user_manual:chap:cookbooks:sec:2d_cartesian_hydrated_slab)= | ||
2D Hydrated Subducting Plate | ||
====================== | ||
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A simple setup of a subducting plate in a Cartesian box which contains hydrated lithologies. There are four lithologies, a 3 km | ||
thick sediment layer, a 4 km thick mid-ocean ridge basalt (MORB) layer, a 4 thick gabbro layer, and a 9 km thick peridotite layer. The lithologies are specified to have an upper bound on the amount of bound water that they can hold of 3 wt%, 1 wt%, 0.5 wt%, and 2 wt% for sediment, MORB, gabbro, and peridotite, respectively. | ||
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The relevant part of the World Builder file for prescribing the water content within the unsubducted oceanic plate looks like this: | ||
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:::{literalinclude} ../2d_cartesian_hydrated_slab.wb | ||
:language: json | ||
:lineno-start: 22 | ||
:lines: 22-36 | ||
::: | ||
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while the relevant part of the World Builder file for prescribing the water content within the subducting oceanic plate looks like this: | ||
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:::{literalinclude} ../2d_cartesian_hydrated_slab.wb | ||
:language: json | ||
:lineno-start: 38 | ||
:lines: 38-65 | ||
::: | ||
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And the bound water content within the subducting plate looks like this: | ||
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:::{figure} bound-water_isotherms.png | ||
:name: slab_bound_water | ||
:alt: 3D Cartesian Rift cookbook temperature contour. | ||
:align: center | ||
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The background is coloured by the bound wt% water, and isotherms are overlain on top at from 273 K to 1373 K at intervals of 100 K. | ||
::: |
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