Items related to Earth's Deep Water Cycle: 168 (Geophysical Monograph...
Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 168.
The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0.025% of the planet's mass-far less water than thought to have been present during Earth's formation. If our planet is "missing" most of its original water, could it reside in the mantle? Can we detect it seismically?
Recognition of the capacity of some deep-mantle minerals to absorb water has propelled an interdisciplinary field of research addressing these two questions, and more. Earth's Deep Water Cycle advances the field with experimental, modeling, and seismic studies that focus on the physical characteristics of "hydrated" minerals, the potentially H2O-rich transition zone (410-660 km depth), and our detection abilities.
Integrated perspectives from four fields of research are featured:
- Mineral physics and geochemistry
- Seismology and electrical conductivity
- Properties of deep hydrous mantle
- Global models and consequences of a deep-Earth water cycle
From experimental synthesis and physical properties measurements to geophysical observations and geodynamic modeling, we are beginning to understand what parameters and data are needed to detect or refute the possibility of water in the deep Earth.
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Steven D. Jacobsen and Suzan van der Lee are the authors of Earth's Deep Water Cycle, published by Wiley.
Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 168
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- PublisherAmerican Geophysical Union
- Publication date2006
- ISBN 10 0875904335
- ISBN 13 9780875904337
- BindingHardcover
- Edition number1
- Number of pages313
- EditorJacobsen Steven D., Van Der Lee Suzan
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Book Description Hardcover. Condition: new. Hardcover. Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 168.The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0.025% of the planet's mass-far less water than thought to have been present during Earth's formation. If our planet is "missing" most of its original water, could it reside in the mantle? Can we detect it seismically? Recognition of the capacity of some deep-mantle minerals to absorb water has propelled an interdisciplinary field of research addressing these two questions, and more. Earth's Deep Water Cycle advances the field with experimental, modeling, and seismic studies that focus on the physical characteristics of "hydrated" minerals, the potentially H2O-rich transition zone (410-660 km depth), and our detection abilities. Integrated perspectives from four fields of research are featured: Mineral physics and geochemistrySeismology and electrical conductivityProperties of deep hydrous mantleGlobal models and consequences of a deep-Earth water cycle From experimental synthesis and physical properties measurements to geophysical observations and geodynamic modeling, we are beginning to understand what parameters and data are needed to detect or refute the possibility of water in the deep Earth. The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0. 025% of the planet's mass-far less water than thought to have been present during Earth's formation. Shipping may be from multiple locations in the US or from the UK, depending on stock availability. Seller Inventory # 9780875904337
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Book Description Hardcover. Condition: new. Hardcover. Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 168.The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0.025% of the planet's mass-far less water than thought to have been present during Earth's formation. If our planet is "missing" most of its original water, could it reside in the mantle? Can we detect it seismically? Recognition of the capacity of some deep-mantle minerals to absorb water has propelled an interdisciplinary field of research addressing these two questions, and more. Earth's Deep Water Cycle advances the field with experimental, modeling, and seismic studies that focus on the physical characteristics of "hydrated" minerals, the potentially H2O-rich transition zone (410-660 km depth), and our detection abilities. Integrated perspectives from four fields of research are featured: Mineral physics and geochemistrySeismology and electrical conductivityProperties of deep hydrous mantleGlobal models and consequences of a deep-Earth water cycle From experimental synthesis and physical properties measurements to geophysical observations and geodynamic modeling, we are beginning to understand what parameters and data are needed to detect or refute the possibility of water in the deep Earth. The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0. 025% of the planet's mass-far less water than thought to have been present during Earth's formation. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability. Seller Inventory # 9780875904337
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Book Description Hardcover. Condition: new. Hardcover. Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 168.The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0.025% of the planet's mass-far less water than thought to have been present during Earth's formation. If our planet is "missing" most of its original water, could it reside in the mantle? Can we detect it seismically? Recognition of the capacity of some deep-mantle minerals to absorb water has propelled an interdisciplinary field of research addressing these two questions, and more. Earth's Deep Water Cycle advances the field with experimental, modeling, and seismic studies that focus on the physical characteristics of "hydrated" minerals, the potentially H2O-rich transition zone (410-660 km depth), and our detection abilities. Integrated perspectives from four fields of research are featured: Mineral physics and geochemistrySeismology and electrical conductivityProperties of deep hydrous mantleGlobal models and consequences of a deep-Earth water cycle From experimental synthesis and physical properties measurements to geophysical observations and geodynamic modeling, we are beginning to understand what parameters and data are needed to detect or refute the possibility of water in the deep Earth. The distribution of H2O in the Earth is under debate. Although liquid water covers 70% of the surface, the oceans represent only about 0. 025% of the planet's mass-far less water than thought to have been present during Earth's formation. Shipping may be from our Sydney, NSW warehouse or from our UK or US warehouse, depending on stock availability. Seller Inventory # 9780875904337
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Book Description Condition: New. Editor(s): van der Lee, Suzan; Jacobsen, Steven D. Series: Geophysical Monograph Series. Num Pages: 314 pages. BIC Classification: RBKF. Category: (P) Professional & Vocational. Dimension: 229 x 152 x 21. Weight in Grams: 1179. . 2006. 1st Edition. Hardcover. . . . . Books ship from the US and Ireland. Seller Inventory # V9780875904337
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