announcements - department of earth and space sciencesejohnson/ess103a/1_3_heat_gotherms.pdf ·...
TRANSCRIPT
![Page 1: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/1.jpg)
Announcements
Field trip 1 conflicts: April 22-23 vs. April 29-30
Reading: p. 46-47(Lab: Chapter 2 and 3; optical mineralogy book)
Homework 1 should be ready soon
![Page 2: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/2.jpg)
Today’s topics:
• Pressure as a function of depth in the Earth
• Geothermal gradients
• Mechanisms for generating melt in tectonic settings
![Page 3: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/3.jpg)
Hydrostatic and lithostatic pressure
Always lithostatic?
![Page 4: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/4.jpg)
The Pressure Gradient
• P increases = ρgh• Nearly linear through
mantle~ 30 MPa/km≈ 1 GPa at base of ave crust
• Core: ρ incr. more rapidly since alloy more dense
Figure 1-8. Pressure variation with depth. From Dziewonski and Anderson (1981). Phys. Earth Planet. Int., 25, 297-356. © Elsevier Science.
![Page 5: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/5.jpg)
Converting pressure and depth units
• 1 GPa = 10 kbar = 1000 MPa
• 1 GPa/35 km • About 3 kbar/km
• Example of how we will use these conversions:
bar
![Page 6: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/6.jpg)
Measuring the temperature as a function of depth
• What do you expect the temperature profile of Earth (geothermal gradient) to look like?
• How could we make measurements of temperature as a function of depth?
LJ
![Page 7: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/7.jpg)
The geothermal gradient• ~25°C / km near
surface• Oceanic geotherm
“cooler” than continental geotherm
• ~0.3°C / km mantle below 200-250 km
• Why is geothermal gradient so much steeper in crust?
From Winter, Intro to Igneous and Metamorphic Petrology
![Page 8: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/8.jpg)
Heat Sources in the Earth
• 1. Heat from the early accretion and differentiation of the Earth
– still slowly reaching surface• 2. Heat released by the radioactive
breakdown of unstable nuclides238U 206Pb235U 207Pb232Th 208Pb
40K 40Ar
0.2 cal/g/yr for 40K
![Page 9: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/9.jpg)
Radiogenic isotopes: important production of heat in the crust
U, Th, K
• How do these elements partition between minerals (olivine, pyroxene) and melt?
K heat generation ~100x greater in crust than in mantle
![Page 10: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/10.jpg)
Mechanisms for transfer of heat
1. Conduction: transfer of kinetic (vibrational) energy
2. Convection: movement of material3. Advection: passive transfer of heat
with rocks that are already in motion4. Radiation: transfer energy with light-
need to be translucent or transparent!
Which apply to the Earth?
![Page 11: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/11.jpg)
The Geothermal
Gradient
Pattern of global heat flux variations compiled from observations at over 20,000 sites and modeled on a spherical harmonic expansion to degree 12. From Pollack, Hurter and Johnson. (1993) Rev. Geophys. 31, 267-280.
Cross-section of the mantle based on a seismic tomography model. Arrows represent plate motions and large-scale mantle flow and subduction zones represented by dipping line segments. EPR =- East pacific Rise, MAR = Mid-Atlantic Ridge, CBR = Carlsberg Ridge. Plates: EA = Eurasian, IN = Indian, PA = Pacific, NA = North American, SA = South American, AF = African, CO = Cocos. From Li and Romanowicz (1996). J. Geophys. Research, 101, 22,245-72.
![Page 12: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/12.jpg)
Convection in action
• Water on stove Tectonic plates on mantle
Red is rising, hot materialBlue is falling, cold material
![Page 13: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/13.jpg)
More Specific Convection Diagram
![Page 14: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/14.jpg)
Mechanisms for transfer of heat
1. Conduction: transfer of kinetic (vibrational) energy
2. Convection: movement of material3. Advection: passive transfer of heat
with rocks that are already in motion4. Radiation: transfer energy with light-
need to be translucent or transparent!
![Page 15: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/15.jpg)
Melting in the Earth
What are mechanisms for melt generation?
Cross-section of the mantle based on a seismic tomography model. Arrows represent plate motions and large-scale mantle flow and subduction zones represented by dipping line segments. EPR =- East pacific Rise, MAR = Mid-Atlantic Ridge, CBR = Carlsberg Ridge. Plates: EA = Eurasian, IN = Indian, PA = Pacific, NA = North American, SA = South American, AF = African, CO = Cocos. From Li and Romanowicz (1996). J. Geophys. Research, 101, 22,245-72.
![Page 16: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/16.jpg)
Ways to instigate melting (phase change)
1. Heat something up (melt butter on stove)
2. Add something to lower the melting temperature (add salt to ice)
3. Decompress (shaving cream, liquid nitrogen)
Match these processes to where they occur in the Earth
![Page 17: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/17.jpg)
Plate Tectonic - Igneous Genesis
1. Mid-ocean Ridges2. Intracontinental Rifts3. Island Arcs4. Active Continental
Margins
5. Back-arc Basins6. Ocean Island Basalts7. Miscellaneous Intra-
Continental Activity
kimberlites, carbonatites, anorthosites...
![Page 18: Announcements - Department of Earth and Space Sciencesejohnson/ess103a/1_3_Heat_gotherms.pdf · Melting in the Earth What are mechanisms for melt generation? Cross-section of the](https://reader034.vdocuments.us/reader034/viewer/2022050314/5f764f56ce69ce728a78ed66/html5/thumbnails/18.jpg)
Summary of important points
• Pressure gradient and conversion between pressure and depth
• Thermal gradient and heat sources in Earth
• Generation of melts in tectonic settings