โž ูƒุชุงุจ Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts โ  โค ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ

โž ูƒุชุงุจ Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts โ โค ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ


Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon between Earthโ€™s surface and its interior. However, there is still much to learn about the forms, transformations, and movements of carbon deep inside the Earth.
ุงู„ูƒุฑุจูˆู† ุงู„ู…ุญุงุตุฑ ููŠ ุงู„ู…ุงุณ ูˆุงู„ุตุฎูˆุฑ ุงู„ุญุงู…ู„ุฉ ู„ู„ูƒุฑุจูˆู†ุงุช ููŠ ู…ู†ุงุทู‚ ุงู„ุงู†ุฏุณุงุณ ู‡ูŠ ุฃู…ุซู„ุฉ ุนู„ู‰ ุงู„ุชุจุงุฏู„ ุงู„ู…ุณุชู…ุฑ ู„ู„ูƒุฑุจูˆู† ุงู„ูƒุจูŠุฑ ุจูŠู† ุณุทุญ ุงู„ุฃุฑุถ ูˆุฏุงุฎู„ู‡ุง. ูˆู…ุน ุฐู„ูƒ, ู„ุง ูŠุฒุงู„ ู‡ู†ุงูƒ ุงู„ูƒุซูŠุฑ ู„ู†ุชุนู„ู…ู‡ ุนู† ุฃุดูƒุงู„ ุงู„ุชุญูˆู„ุงุช ูˆุงู„ุญุฑูƒุงุช ุงู„ูƒุฑุจูˆู† ููŠ ุนู…ู‚ ุงู„ุฃุฑุถ.

Carbon in Earth's Interior presents recent research on the physical and chemical behavior of carbon-bearing materials and serves as a reference point for future carbon science research.
ูŠู‚ุฏู… ุงู„ูƒุฑุจูˆู† ููŠ ุจุงุทู† ุงู„ุฃุฑุถ ุฃุจุญุงุซุง ุญุฏูŠุซุฉ ุญูˆู„ ุงู„ุณู„ูˆูƒ ุงู„ููŠุฒูŠุงุฆูŠ ูˆุงู„ูƒูŠู…ูŠุงุฆูŠ ู„ู„ู…ูˆุงุฏ ุงู„ุญุงู…ู„ุฉ ู„ู„ูƒุฑุจูˆู† ูˆูŠุนู…ู„ ูƒู†ู‚ุทุฉ ู…ุฑุฌุนูŠุฉ ู„ุฃุจุญุงุซ ุนู„ูˆู… ุงู„ูƒุฑุจูˆู† ุงู„ู…ุณุชู‚ุจู„ูŠุฉ.

Data from mineral physics, petrology, geochemistry, geophysics, and geodynamics
Research on the deep carbon cycle and carbon in magmas or fluids
Dynamics, structure, stability, and reactivity of carbon-based natural materials
Properties of allied substances that carry carbon
Rates of chemical and physical transformations of carbonุจูŠุงู†ุงุช ู…ู† ููŠุฒูŠุงุก ุงู„ู…ุนุงุฏู† ุŒ ูˆุนู„ู… ุงู„ุจุชุฑูˆู„ ุŒ ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ุŒ ูˆุงู„ุฌูŠูˆููŠุฒูŠุงุก ุŒ ูˆุงู„ุฏูŠู†ุงู…ูŠูƒุง ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ
ุงู„ุจุญุซ ุนู† ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ุงู„ุนู…ูŠู‚ุฉ ูˆุงู„ูƒุฑุจูˆู† ููŠ ุงู„ุตู‡ุงุฑุฉ ุฃูˆ ุงู„ุณูˆุงุฆู„
ุฏูŠู†ุงู…ูŠุงุช ุงู„ู…ูˆุงุฏ ุงู„ุทุจูŠุนูŠุฉ ุงู„ู‚ุงุฆู…ุฉ ุนู„ู‰ ุงู„ูƒุฑุจูˆู† ูˆู‡ูŠูƒู„ู‡ุง ูˆุงุณุชู‚ุฑุงุฑู‡ุง ูˆุชูุงุนู„ู‡ุง
ุฎุตุงุฆุต ุงู„ู…ูˆุงุฏ ุงู„ู…ุชุญุงู„ูุฉ ุงู„ุชูŠ ุชุญู…ู„ ุงู„ูƒุฑุจูˆู†
ู…ุนุฏู„ุงุช ุงู„ุชุญูˆู„ุงุช ุงู„ูƒูŠู…ูŠุงุฆูŠุฉ ูˆุงู„ููŠุฒูŠุงุฆูŠุฉ ู„ู„ูƒุฑุจูˆู†

The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals.
ูŠุดุฌุน ุงู„ุงุชุญุงุฏ ุงู„ุฌูŠูˆููŠุฒูŠุงุฆูŠ ุงู„ุฃู…ุฑูŠูƒูŠ ุงู„ุงูƒุชุดุงู ููŠ ุนู„ูˆู… ุงู„ุฃุฑุถ ูˆุงู„ูุถุงุก ู„ุตุงู„ุญ ุงู„ุจุดุฑูŠุฉ. ุชู†ุดุฑ ู…ู†ุดูˆุฑุงุชู‡ุง ุงู„ู…ุนุฑูุฉ ุงู„ุนู„ู…ูŠุฉ ูˆุชูˆูุฑ ุงู„ู…ูˆุงุฑุฏ ู„ู„ุจุงุญุซูŠู† ูˆุงู„ุทู„ุงุจ ูˆุงู„ู…ู‡ู†ูŠูŠู†.

Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions
ูŠุณุชูƒุดู ุณู„ูˆูƒ ุงู„ูƒุฑุจูˆู† ููŠ ุงู„ู…ุนุงุฏู†, ูŠุฐูˆุจ, ูˆุงู„ุณูˆุงุฆู„ ููŠ ุธู„ ุงู„ุธุฑูˆู ุงู„ู‚ุงุณูŠุฉ

The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Carbon is the main component of biological compounds as well as a major component of many minerals such as limestone. Along with the nitrogen cycle and the water cycle
ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ู‡ูŠ ุงู„ุฏูˆุฑุฉ ุงู„ุจูŠูˆุฌูŠูˆูƒูŠู…ูŠุงุฆูŠุฉ ุงู„ุชูŠ ูŠุชู… ู…ู† ุฎู„ุงู„ู‡ุง ุชุจุงุฏู„ ุงู„ูƒุฑุจูˆู† ุจูŠู† ุงู„ุบู„ุงู ุงู„ุญูŠูˆูŠ ูˆุงู„ุบู„ุงู ุงู„ุฃุฑุถูŠ ูˆุงู„ุบู„ุงู ุงู„ู…ุงุฆูŠ ูˆุงู„ุบู„ุงู ุงู„ุฌูˆูŠ ู„ู„ุฃุฑุถ. ุงู„ูƒุฑุจูˆู† ู‡ูˆ ุงู„ู…ูƒูˆู† ุงู„ุฑุฆูŠุณูŠ ู„ู„ู…ุฑูƒุจุงุช ุงู„ุจูŠูˆู„ูˆุฌูŠุฉ ูˆูƒุฐู„ูƒ ู…ูƒูˆู† ุฑุฆูŠุณูŠ ู„ู„ุนุฏูŠุฏ ู…ู† ุงู„ู…ุนุงุฏู† ู…ุซู„ ุงู„ุญุฌุฑ ุงู„ุฌูŠุฑูŠ. ุฌู†ุจุง ุฅู„ู‰ ุฌู†ุจ ู…ุน ุฏูˆุฑุฉ ุงู„ู†ูŠุชุฑูˆุฌูŠู† ูˆุฏูˆุฑุฉ ุงู„ู…ูŠุงู‡
ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ - ูŠุนู…ู„ ูƒุฑูŠุฌ ุฅูŠ ู…ุงู†ูŠู†ุฌ ุฃุณุชุงุฐุงู‹ ู„ู„ุฌูŠูˆู„ูˆุฌูŠุง ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ููŠ ู‚ุณู… ุนู„ูˆู… ุงู„ุฃุฑุถ ูˆุงู„ูƒูˆุงูƒุจ ูˆุงู„ูุถุงุก ุจุฌุงู…ุนุฉ ูƒุงู„ูŠููˆุฑู†ูŠุง ุŒ ู„ูˆุณ ุฃู†ุฌู„ูˆุณ ุŒ ุญูŠุซ ุดุบู„ ู…ู†ุตุจ ุฑุฆูŠุณ ุงู„ู‚ุณู… ุจูŠู† ุนุงู…ูŠ 2009 ูˆ 2012. ุชุดู…ู„ ุงู‡ุชู…ุงู…ุงุช ู…ุงู†ูŠู†ุบ ุงู„ุจุญุซูŠุฉ ูƒูŠู…ูŠุงุก ุงู„ู…ูŠุงู‡ ูˆุงู„ุฏูŠู†ุงู…ูŠูƒุง ุงู„ุญุฑุงุฑูŠุฉ ูˆูƒูŠู…ูŠุงุก ุงู„ุบุงุฒ ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ูˆุนู„ู… ุงู„ุตุฎูˆุฑ ุงู„ู†ุงุฑูŠุฉ ูˆุนู„ู… ุงู„ุตุฎูˆุฑ ุงู„ู…ุชุญูˆู„ุฉ. โฐ ู„ู‡ ู…ุฌู…ูˆุนุฉ ู…ู† ุงู„ุฅู†ุฌุงุฒุงุช ูˆุงู„ู…ุคู„ูุงุช ุฃุจุฑุฒู‡ุง โž Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts โ โž Carbon in Earth's Interior: A Geologic Siโ€Oโ€C Pathway to Incorporate Carbon in Silicates โ โž Carbon in Earth's Interior: Hydrous Carbonatitic Liquids Drive CO2 Recycling From Subducted Marls and Limestones โ โž Carbon in Earth's Interior: Free Energies of Reaction for Aqueous Glycine Condensation Chemistry at Extreme Temperatures โ โž Carbon in Earth's Interior: Highโ€Pressure Naโ€Ca Carbonates in the Deep Carbon Cycle โ โž Carbon in Earth's Interior: Spin Transition of Iron in Deepโ€Mantle Ferromagnesite โ โž Carbon in Earth's Interior: Experimental Determination of Calcite Solubility in H2Oโ€KClโ€NaClโ€LiCl Solutions at 700ยฐC and 8 kbar โ โž Carbon in Earth's Interior: Phase Diagrams of Carbonate Materials at High Pressures, with Implications for Melting and Carbon Cycling in the Deep Earth โ โž Carbon in Earth's Interior: Diamondoids Under Pressure โ ุงู„ู†ุงุดุฑูŠู† : โž ูˆุงูŠู„ูŠ (ู†ุงุดุฑ) โ โฑ
ู…ู† ูƒุชุจ ุงู„ุชูƒู†ูˆู„ูˆุฌูŠุง ูˆุงู„ุนู„ู… - ู…ูƒุชุจุฉ ูƒุชุจ ุงู„ู‡ู†ุฏุณุฉ ูˆุงู„ุชูƒู†ูˆู„ูˆุฌูŠุง.


ne element is the backbone of all forms of life weโ€™ve ever discovered on Earth: carbon. Number six on the periodic table is, to the best of our knowledge, impossible to live without. In this episode of Reactions, discover what makes carbon so exceptional, its nearly infinite capabilities

ู†ุจุฐุฉ ุนู† ุงู„ูƒุชุงุจ:
Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts

2020ู… - 1445ู‡ู€

Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon between Earthโ€™s surface and its interior. However, there is still much to learn about the forms, transformations, and movements of carbon deep inside the Earth.
ุงู„ูƒุฑุจูˆู† ุงู„ู…ุญุงุตุฑ ููŠ ุงู„ู…ุงุณ ูˆุงู„ุตุฎูˆุฑ ุงู„ุญุงู…ู„ุฉ ู„ู„ูƒุฑุจูˆู†ุงุช ููŠ ู…ู†ุงุทู‚ ุงู„ุงู†ุฏุณุงุณ ู‡ูŠ ุฃู…ุซู„ุฉ ุนู„ู‰ ุงู„ุชุจุงุฏู„ ุงู„ู…ุณุชู…ุฑ ู„ู„ูƒุฑุจูˆู† ุงู„ูƒุจูŠุฑ ุจูŠู† ุณุทุญ ุงู„ุฃุฑุถ ูˆุฏุงุฎู„ู‡ุง. ูˆู…ุน ุฐู„ูƒ, ู„ุง ูŠุฒุงู„ ู‡ู†ุงูƒ ุงู„ูƒุซูŠุฑ ู„ู†ุชุนู„ู…ู‡ ุนู† ุฃุดูƒุงู„ ุงู„ุชุญูˆู„ุงุช ูˆุงู„ุญุฑูƒุงุช ุงู„ูƒุฑุจูˆู† ููŠ ุนู…ู‚ ุงู„ุฃุฑุถ.

Carbon in Earth's Interior presents recent research on the physical and chemical behavior of carbon-bearing materials and serves as a reference point for future carbon science research.
ูŠู‚ุฏู… ุงู„ูƒุฑุจูˆู† ููŠ ุจุงุทู† ุงู„ุฃุฑุถ ุฃุจุญุงุซุง ุญุฏูŠุซุฉ ุญูˆู„ ุงู„ุณู„ูˆูƒ ุงู„ููŠุฒูŠุงุฆูŠ ูˆุงู„ูƒูŠู…ูŠุงุฆูŠ ู„ู„ู…ูˆุงุฏ ุงู„ุญุงู…ู„ุฉ ู„ู„ูƒุฑุจูˆู† ูˆูŠุนู…ู„ ูƒู†ู‚ุทุฉ ู…ุฑุฌุนูŠุฉ ู„ุฃุจุญุงุซ ุนู„ูˆู… ุงู„ูƒุฑุจูˆู† ุงู„ู…ุณุชู‚ุจู„ูŠุฉ.

Data from mineral physics, petrology, geochemistry, geophysics, and geodynamics
Research on the deep carbon cycle and carbon in magmas or fluids
Dynamics, structure, stability, and reactivity of carbon-based natural materials
Properties of allied substances that carry carbon
Rates of chemical and physical transformations of carbonุจูŠุงู†ุงุช ู…ู† ููŠุฒูŠุงุก ุงู„ู…ุนุงุฏู† ุŒ ูˆุนู„ู… ุงู„ุจุชุฑูˆู„ ุŒ ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ุŒ ูˆุงู„ุฌูŠูˆููŠุฒูŠุงุก ุŒ ูˆุงู„ุฏูŠู†ุงู…ูŠูƒุง ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ
ุงู„ุจุญุซ ุนู† ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ุงู„ุนู…ูŠู‚ุฉ ูˆุงู„ูƒุฑุจูˆู† ููŠ ุงู„ุตู‡ุงุฑุฉ ุฃูˆ ุงู„ุณูˆุงุฆู„
ุฏูŠู†ุงู…ูŠุงุช ุงู„ู…ูˆุงุฏ ุงู„ุทุจูŠุนูŠุฉ ุงู„ู‚ุงุฆู…ุฉ ุนู„ู‰ ุงู„ูƒุฑุจูˆู† ูˆู‡ูŠูƒู„ู‡ุง ูˆุงุณุชู‚ุฑุงุฑู‡ุง ูˆุชูุงุนู„ู‡ุง
ุฎุตุงุฆุต ุงู„ู…ูˆุงุฏ ุงู„ู…ุชุญุงู„ูุฉ ุงู„ุชูŠ ุชุญู…ู„ ุงู„ูƒุฑุจูˆู†
ู…ุนุฏู„ุงุช ุงู„ุชุญูˆู„ุงุช ุงู„ูƒูŠู…ูŠุงุฆูŠุฉ ูˆุงู„ููŠุฒูŠุงุฆูŠุฉ ู„ู„ูƒุฑุจูˆู†

The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals.
ูŠุดุฌุน ุงู„ุงุชุญุงุฏ ุงู„ุฌูŠูˆููŠุฒูŠุงุฆูŠ ุงู„ุฃู…ุฑูŠูƒูŠ ุงู„ุงูƒุชุดุงู ููŠ ุนู„ูˆู… ุงู„ุฃุฑุถ ูˆุงู„ูุถุงุก ู„ุตุงู„ุญ ุงู„ุจุดุฑูŠุฉ. ุชู†ุดุฑ ู…ู†ุดูˆุฑุงุชู‡ุง ุงู„ู…ุนุฑูุฉ ุงู„ุนู„ู…ูŠุฉ ูˆุชูˆูุฑ ุงู„ู…ูˆุงุฑุฏ ู„ู„ุจุงุญุซูŠู† ูˆุงู„ุทู„ุงุจ ูˆุงู„ู…ู‡ู†ูŠูŠู†.

Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions
ูŠุณุชูƒุดู ุณู„ูˆูƒ ุงู„ูƒุฑุจูˆู† ููŠ ุงู„ู…ุนุงุฏู†, ูŠุฐูˆุจ, ูˆุงู„ุณูˆุงุฆู„ ููŠ ุธู„ ุงู„ุธุฑูˆู ุงู„ู‚ุงุณูŠุฉ

The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Carbon is the main component of biological compounds as well as a major component of many minerals such as limestone. Along with the nitrogen cycle and the water cycle
ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ู‡ูŠ ุงู„ุฏูˆุฑุฉ ุงู„ุจูŠูˆุฌูŠูˆูƒูŠู…ูŠุงุฆูŠุฉ ุงู„ุชูŠ ูŠุชู… ู…ู† ุฎู„ุงู„ู‡ุง ุชุจุงุฏู„ ุงู„ูƒุฑุจูˆู† ุจูŠู† ุงู„ุบู„ุงู ุงู„ุญูŠูˆูŠ ูˆุงู„ุบู„ุงู ุงู„ุฃุฑุถูŠ ูˆุงู„ุบู„ุงู ุงู„ู…ุงุฆูŠ ูˆุงู„ุบู„ุงู ุงู„ุฌูˆูŠ ู„ู„ุฃุฑุถ. ุงู„ูƒุฑุจูˆู† ู‡ูˆ ุงู„ู…ูƒูˆู† ุงู„ุฑุฆูŠุณูŠ ู„ู„ู…ุฑูƒุจุงุช ุงู„ุจูŠูˆู„ูˆุฌูŠุฉ ูˆูƒุฐู„ูƒ ู…ูƒูˆู† ุฑุฆูŠุณูŠ ู„ู„ุนุฏูŠุฏ ู…ู† ุงู„ู…ุนุงุฏู† ู…ุซู„ ุงู„ุญุฌุฑ ุงู„ุฌูŠุฑูŠ. ุฌู†ุจุง ุฅู„ู‰ ุฌู†ุจ ู…ุน ุฏูˆุฑุฉ ุงู„ู†ูŠุชุฑูˆุฌูŠู† ูˆุฏูˆุฑุฉ ุงู„ู…ูŠุงู‡ .
ุงู„ู…ุฒูŠุฏ..

ุชุนู„ูŠู‚ุงุช ุงู„ู‚ุฑู‘ุงุก:

ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ุงู„ุฃุญูŠุงุก

ุฃู‡ู…ูŠุฉ ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู†

ุฏุฑุงุณุฉ ุฌูŠูˆููŠุฒูŠุงุฆูŠุฉ ูˆุงูŠู„ูŠ

ุฃุบูˆ ูƒุชุงุจ ุณู„ุณู„ุฉ ุงู„ุชุบูŠุฑ ุงู„ุจูŠุฆูŠ ูˆุงู„ู…ุญุงูุธุงุช ุงู„ู†ุงุฑูŠุฉ ุงู„ูƒุจูŠุฑุฉ

carbon in earth's interior agu monograph

percentage of carbon in earth's crust

carbon cycle

carbon cycle biology

importance of carbon cycle

geophysical monograph wiley

agu book series environmental change and large igneous provinces the

Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon between Earth’s surface and its interior. However, there is still much to learn about the forms, transformations, and movements of carbon deep inside the Earth.
ุงู„ูƒุฑุจูˆู† ุงู„ู…ุญุงุตุฑ ููŠ ุงู„ู…ุงุณ ูˆุงู„ุตุฎูˆุฑ ุงู„ุญุงู…ู„ุฉ ู„ู„ูƒุฑุจูˆู†ุงุช ููŠ ู…ู†ุงุทู‚ ุงู„ุงู†ุฏุณุงุณ ู‡ูŠ ุฃู…ุซู„ุฉ ุนู„ู‰ ุงู„ุชุจุงุฏู„ ุงู„ู…ุณุชู…ุฑ ู„ู„ูƒุฑุจูˆู† ุงู„ูƒุจูŠุฑ ุจูŠู† ุณุทุญ ุงู„ุฃุฑุถ ูˆุฏุงุฎู„ู‡ุง. ูˆู…ุน ุฐู„ูƒ, ู„ุง ูŠุฒุงู„ ู‡ู†ุงูƒ ุงู„ูƒุซูŠุฑ ู„ู†ุชุนู„ู…ู‡ ุนู† ุฃุดูƒุงู„ ุงู„ุชุญูˆู„ุงุช ูˆุงู„ุญุฑูƒุงุช ุงู„ูƒุฑุจูˆู† ููŠ ุนู…ู‚ ุงู„ุฃุฑุถ.

Carbon in Earth's Interior presents recent research on the physical and chemical behavior of carbon-bearing materials and serves as a reference point for future carbon science research.
ูŠู‚ุฏู… ุงู„ูƒุฑุจูˆู† ููŠ ุจุงุทู† ุงู„ุฃุฑุถ ุฃุจุญุงุซุง ุญุฏูŠุซุฉ ุญูˆู„ ุงู„ุณู„ูˆูƒ ุงู„ููŠุฒูŠุงุฆูŠ ูˆุงู„ูƒูŠู…ูŠุงุฆูŠ ู„ู„ู…ูˆุงุฏ ุงู„ุญุงู…ู„ุฉ ู„ู„ูƒุฑุจูˆู† ูˆูŠุนู…ู„ ูƒู†ู‚ุทุฉ ู…ุฑุฌุนูŠุฉ ู„ุฃุจุญุงุซ ุนู„ูˆู… ุงู„ูƒุฑุจูˆู† ุงู„ู…ุณุชู‚ุจู„ูŠุฉ.

Data from mineral physics, petrology, geochemistry, geophysics, and geodynamics
Research on the deep carbon cycle and carbon in magmas or fluids
Dynamics, structure, stability, and reactivity of carbon-based natural materials
Properties of allied substances that carry carbon
Rates of chemical and physical transformations of carbonุจูŠุงู†ุงุช ู…ู† ููŠุฒูŠุงุก ุงู„ู…ุนุงุฏู† ุŒ ูˆุนู„ู… ุงู„ุจุชุฑูˆู„ ุŒ ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ุŒ ูˆุงู„ุฌูŠูˆููŠุฒูŠุงุก ุŒ ูˆุงู„ุฏูŠู†ุงู…ูŠูƒุง ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ
ุงู„ุจุญุซ ุนู† ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ุงู„ุนู…ูŠู‚ุฉ ูˆุงู„ูƒุฑุจูˆู† ููŠ ุงู„ุตู‡ุงุฑุฉ ุฃูˆ ุงู„ุณูˆุงุฆู„
ุฏูŠู†ุงู…ูŠุงุช ุงู„ู…ูˆุงุฏ ุงู„ุทุจูŠุนูŠุฉ ุงู„ู‚ุงุฆู…ุฉ ุนู„ู‰ ุงู„ูƒุฑุจูˆู† ูˆู‡ูŠูƒู„ู‡ุง ูˆุงุณุชู‚ุฑุงุฑู‡ุง ูˆุชูุงุนู„ู‡ุง
ุฎุตุงุฆุต ุงู„ู…ูˆุงุฏ ุงู„ู…ุชุญุงู„ูุฉ ุงู„ุชูŠ ุชุญู…ู„ ุงู„ูƒุฑุจูˆู†
ู…ุนุฏู„ุงุช ุงู„ุชุญูˆู„ุงุช ุงู„ูƒูŠู…ูŠุงุฆูŠุฉ ูˆุงู„ููŠุฒูŠุงุฆูŠุฉ ู„ู„ูƒุฑุจูˆู†

The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals.
ูŠุดุฌุน ุงู„ุงุชุญุงุฏ ุงู„ุฌูŠูˆููŠุฒูŠุงุฆูŠ ุงู„ุฃู…ุฑูŠูƒูŠ ุงู„ุงูƒุชุดุงู ููŠ ุนู„ูˆู… ุงู„ุฃุฑุถ ูˆุงู„ูุถุงุก ู„ุตุงู„ุญ ุงู„ุจุดุฑูŠุฉ. ุชู†ุดุฑ ู…ู†ุดูˆุฑุงุชู‡ุง ุงู„ู…ุนุฑูุฉ ุงู„ุนู„ู…ูŠุฉ ูˆุชูˆูุฑ ุงู„ู…ูˆุงุฑุฏ ู„ู„ุจุงุญุซูŠู† ูˆุงู„ุทู„ุงุจ ูˆุงู„ู…ู‡ู†ูŠูŠู†.

Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions
ูŠุณุชูƒุดู ุณู„ูˆูƒ ุงู„ูƒุฑุจูˆู† ููŠ ุงู„ู…ุนุงุฏู†, ูŠุฐูˆุจ, ูˆุงู„ุณูˆุงุฆู„ ููŠ ุธู„ ุงู„ุธุฑูˆู ุงู„ู‚ุงุณูŠุฉ

The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Carbon is the main component of biological compounds as well as a major component of many minerals such as limestone. Along with the nitrogen cycle and the water cycle
ุฏูˆุฑุฉ ุงู„ูƒุฑุจูˆู† ู‡ูŠ ุงู„ุฏูˆุฑุฉ ุงู„ุจูŠูˆุฌูŠูˆูƒูŠู…ูŠุงุฆูŠุฉ ุงู„ุชูŠ ูŠุชู… ู…ู† ุฎู„ุงู„ู‡ุง ุชุจุงุฏู„ ุงู„ูƒุฑุจูˆู† ุจูŠู† ุงู„ุบู„ุงู ุงู„ุญูŠูˆูŠ ูˆุงู„ุบู„ุงู ุงู„ุฃุฑุถูŠ ูˆุงู„ุบู„ุงู ุงู„ู…ุงุฆูŠ ูˆุงู„ุบู„ุงู ุงู„ุฌูˆูŠ ู„ู„ุฃุฑุถ. ุงู„ูƒุฑุจูˆู† ู‡ูˆ ุงู„ู…ูƒูˆู† ุงู„ุฑุฆูŠุณูŠ ู„ู„ู…ุฑูƒุจุงุช ุงู„ุจูŠูˆู„ูˆุฌูŠุฉ ูˆูƒุฐู„ูƒ ู…ูƒูˆู† ุฑุฆูŠุณูŠ ู„ู„ุนุฏูŠุฏ ู…ู† ุงู„ู…ุนุงุฏู† ู…ุซู„ ุงู„ุญุฌุฑ ุงู„ุฌูŠุฑูŠ. ุฌู†ุจุง ุฅู„ู‰ ุฌู†ุจ ู…ุน ุฏูˆุฑุฉ ุงู„ู†ูŠุชุฑูˆุฌูŠู† ูˆุฏูˆุฑุฉ ุงู„ู…ูŠุงู‡



ุณู†ุฉ ุงู„ู†ุดุฑ : 2020ู… / 1441ู‡ู€ .
ุญุฌู… ุงู„ูƒุชุงุจ ุนู†ุฏ ุงู„ุชุญู…ูŠู„ : 0.6 ู…ูŠุฌุงุจุงูŠุช .
ู†ูˆุน ุงู„ูƒุชุงุจ : pdf.
ุนุฏุงุฏ ุงู„ู‚ุฑุงุกุฉ: ุนุฏุฏ ู‚ุฑุงุกุฉ Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts

ุงุฐุง ุงุนุฌุจูƒ ุงู„ูƒุชุงุจ ูุถู„ุงู‹ ุงุถุบุท ุนู„ู‰ ุฃุนุฌุจู†ูŠ
ูˆ ูŠู…ูƒู†ูƒ ุชุญู…ูŠู„ู‡ ู…ู† ู‡ู†ุง:

ุชุญู…ูŠู„ Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts
ุดูƒุฑู‹ุง ู„ู…ุณุงู‡ู…ุชูƒู…

ุดูƒุฑุงู‹ ู„ู…ุณุงู‡ู…ุชูƒู… ู…ุนู†ุง ููŠ ุงู„ุฅุฑุชู‚ุงุก ุจู…ุณุชูˆู‰ ุงู„ู…ูƒุชุจุฉ ุŒ ูŠู…ูƒู†ูƒู… ุงุงู„ุชุจู„ูŠุบ ุนู† ุงุฎุทุงุก ุงูˆ ุณูˆุก ุงุฎุชูŠุงุฑ ู„ู„ูƒุชุจ ูˆุชุตู†ูŠูู‡ุง ูˆู…ุญุชูˆุงู‡ุง ุŒ ุฃูˆ ูƒุชุงุจ ูŠูู…ู†ุน ู†ุดุฑู‡ ุŒ ุงูˆ ู…ุญู…ูŠ ุจุญู‚ูˆู‚ ุทุจุน ูˆู†ุดุฑ ุŒ ูุถู„ุงู‹ ู‚ู… ุจุงู„ุชุจู„ูŠุบ ุนู† ุงู„ูƒุชุงุจ ุงู„ู…ูุฎุงู„ู:

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ุงู„ู…ุคู„ู:
ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ - Craig E. Manning

ูƒุชุจ ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ ูŠุนู…ู„ ูƒุฑูŠุฌ ุฅูŠ ู…ุงู†ูŠู†ุฌ ุฃุณุชุงุฐุงู‹ ู„ู„ุฌูŠูˆู„ูˆุฌูŠุง ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ููŠ ู‚ุณู… ุนู„ูˆู… ุงู„ุฃุฑุถ ูˆุงู„ูƒูˆุงูƒุจ ูˆุงู„ูุถุงุก ุจุฌุงู…ุนุฉ ูƒุงู„ูŠููˆุฑู†ูŠุง ุŒ ู„ูˆุณ ุฃู†ุฌู„ูˆุณ ุŒ ุญูŠุซ ุดุบู„ ู…ู†ุตุจ ุฑุฆูŠุณ ุงู„ู‚ุณู… ุจูŠู† ุนุงู…ูŠ 2009 ูˆ 2012. ุชุดู…ู„ ุงู‡ุชู…ุงู…ุงุช ู…ุงู†ูŠู†ุบ ุงู„ุจุญุซูŠุฉ ูƒูŠู…ูŠุงุก ุงู„ู…ูŠุงู‡ ูˆุงู„ุฏูŠู†ุงู…ูŠูƒุง ุงู„ุญุฑุงุฑูŠุฉ ูˆูƒูŠู…ูŠุงุก ุงู„ุบุงุฒ ูˆุงู„ูƒูŠู…ูŠุงุก ุงู„ุฌูŠูˆู„ูˆุฌูŠุฉ ูˆุนู„ู… ุงู„ุตุฎูˆุฑ ุงู„ู†ุงุฑูŠุฉ ูˆุนู„ู… ุงู„ุตุฎูˆุฑ ุงู„ู…ุชุญูˆู„ุฉ.โฐ ู„ู‡ ู…ุฌู…ูˆุนุฉ ู…ู† ุงู„ุฅู†ุฌุงุฒุงุช ูˆุงู„ู…ุคู„ูุงุช ุฃุจุฑุฒู‡ุง โž Carbon in Earth's Interior: Carbon Speciation and Solubility in Silicate Melts โ โž Carbon in Earth's Interior: A Geologic Siโ€Oโ€C Pathway to Incorporate Carbon in Silicates โ โž Carbon in Earth's Interior: Hydrous Carbonatitic Liquids Drive CO2 Recycling From Subducted Marls and Limestones โ โž Carbon in Earth's Interior: Free Energies of Reaction for Aqueous Glycine Condensation Chemistry at Extreme Temperatures โ โž Carbon in Earth's Interior: Highโ€Pressure Naโ€Ca Carbonates in the Deep Carbon Cycle โ โž Carbon in Earth's Interior: Spin Transition of Iron in Deepโ€Mantle Ferromagnesite โ โž Carbon in Earth's Interior: Experimental Determination of Calcite Solubility in H2Oโ€KClโ€NaClโ€LiCl Solutions at 700ยฐC and 8 kbar โ โž Carbon in Earth's Interior: Phase Diagrams of Carbonate Materials at High Pressures, with Implications for Melting and Carbon Cycling in the Deep Earth โ โž Carbon in Earth's Interior: Diamondoids Under Pressure โ ุงู„ู†ุงุดุฑูŠู† : โž ูˆุงูŠู„ูŠ (ู†ุงุดุฑ) โ โฑ. ุงู„ู…ุฒูŠุฏ..

ูƒุชุจ ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ
ุงู„ู†ุงุดุฑ:
ูˆุงูŠู„ูŠ (ู†ุงุดุฑ)
ูƒุชุจ ูˆุงูŠู„ูŠ (ู†ุงุดุฑ) โฐ ู†ุงุดุฑูŠู† ู„ู…ุฌู…ูˆุนุฉ ู…ู† ุงู„ู…ุคู„ูุงุช ุฃุจุฑุฒู‡ุง โž Taguchi's Quality Engineering Handbook: Case 5 Application of Dynamic Optimization in Ultra Trace Analysis โ โž Food and Package Engineering: Front Matter โ โž Social Engineering: The Science of Human Hacking โ โž Chemical Micro Process Engineering, Fundamentals, Modelling and Reactions: Gas/Liquid Reactions: Sections 5.4โ€“5.7 โ โž The Web Application Hacker's Handbook 2nd Edition โ โž Chemical Micro Process Engineering, Fundamentals, Modelling and Reactions: Gas/Liquid Reactions: Sections 5.1โ€“5.3 โ โž Multiโ€Dimensional Imaging: Passive Polarimetric Imaging โ โž Taguchi's Quality Engineering Handbook: Chapter 44 Role of Taguchi Methods in Design for Six Sigma โ โž Chemical Micro Process Engineering, Fundamentals, Modelling and Reactions: Liquidโ€ and Liquid/Liquidโ€Phase Reactions: Sections 4.12โ€“4.14 โ โž Building Electroโ€Optical Systems: Exotic Optical Components โ ูˆู…ู† ุฃุจุฑุฒ ุงู„ู…ุคู„ููŠู† : โž ุฌูŠู†ุดูŠ ุชุงุบูˆุดูŠ โ โž ุบุงูุฑูŠู„ ุณุงู„ููŠู†ุฏูŠ โ โž Prof. Dr. Volker Hessel โ โž ูƒุฑูŠุณุชูˆู ู‡ู€. ู„ูˆุฎ โ โž Harold R. Booher โ โž Jeanโ€Louis Briaud โ โž ูƒุฑูŠุบ ุฅูŠ ู…ุงู†ูŠู†ุบ โ โž Kailash C. Kapur โ โž ูƒู„ูŠุฉ ุงู„ู‡ู†ุฏุณุฉ ุงู„ูƒู‡ุฑุจุงุฆูŠุฉ ูˆุงู„ุงู„ูƒุชุฑูˆู†ูŠุฉ ููŠ ุฌุงู…ุนุฉุญู„ุจ โ โž Derek K. Hutchins DIET โ โž Juan Martinezโ€Vega โ โž ุดูˆ ูƒูŠูˆ ู„ูŠูˆ โ โž Madhusanka Liyanage โ โž Konstantinos Samdanis โ โž ู…ุงูƒูŠ ูƒุงูŠ ุญุจูŠุจ โ โž ุฃูˆู„ูŠูุฑ ู‡ูŠูƒู…ุงู† โ โž ูƒูŠู…ุจุฑู„ูŠ ุณ ูŠูˆู†ุบ โ โž Gordana Vunjakโ€Novakovic โ โž Peter Williams โ โž ุฌูŠู…ุณ ู„ุงุฑู…ูŠู†ูŠ โ โž ุจู‡ุฑุงู… ุฌุงููŠุฏ โ โž ูˆูŠู„ูŠุงู… ุจุงู†ูŠูƒ โ โž Joerg Lahann โ โž Luis Puigjaner โ โž Ferran Martรญn โ โž ุฅุณ ุขูŠ ุฑูŠุชุดุงุฑุฏุฒ โ โž ุณูƒูˆุช ุขูŠ ู…ูˆุฑูŠุณ โ โž ุงู„ุฃุณุชุงุฐ ุฌูŠู‡ ุฅูŠู‡ ุจุฑุงู†ุฏุงูˆ ูุงุฑูŠุง โ โž ู…ุงุฑุฌุฑูŠุช ู‡ุงู†ุจูˆูƒูŠู† โ โž ุฃู†ุทูˆู†ูŠูˆุณ ูƒ. ุงู„ูƒุณู†ุฏุฑูŠุฏูŠุณ โ โž Robert C. Brown โ โž ุฌูˆู† ุจูŠู„ูŠู†ุฌุณู„ูŠ โ โž ุฃู†ุฏุฑูŠุงุณ ุณู…ุจุฑ โ โž Klausโ€Viktor Peinemann โ โž ุฏูŠููŠุฏ ุจ. ู„ูˆุฑุงู†ุณ โ โž Natalia V. Plechkova โ โž ุฌูˆุฑุฌ ุจูŠู„ุฒ โ โž ุฑุงููŠ ุจูŠุฑู„ุง โ โž ููŠู„ูŠุจ ุณูŠ ุฌูŠ ู‡ูˆุจุฒ โ โž ุฏุงู†ูŠุงู„ ู…ูŠู†ูˆู„ูŠ โ โž Daniel A. Vallero โ โž ูƒุฑูŠุณุชูˆูุฑ ุฌุงูŠ ู‡ุงุฏู†ุงุฌูŠ โ โž ู…ุงุฑูƒูˆุณ ุจูŠู†ุชูˆุŒ ุฏุงููŠุฏ ุณุชุงุชุงุฑุฏ โ โž ูƒูˆุฑูŠ ุฃู„ุซูˆู โ โž ุจู‡ุฒุงุฏ ุฑุถูˆูŠ โ โž Jean-Louis Vanham โ โž ุฌุงู†ูŠุช ูุงู„ุงุฏูŠ โ โž ุงู„ูƒุณู†ุฏุฑ ุจุงุชุดูŠู โ โž ู…ุงุณูŠุฌ ูƒุฑุงู†ุฒ โ โž ุฑูŠุชุดุงุฑุฏ ุจู„ูˆู…ุŒ ูƒุฑูŠุณุชูŠู† ุจุฑูŠุฒู†ุงู† โ โž ุจูŠุชุฑ ูˆูŠููŠุฑูƒุง โ โž ุฑูŠุชุดุงุฑุฏ ุจู„ูˆู… โ โž Madhvanand N. Kashid โ โž ู…ุงุชูŠูˆ ู‡ูŠูƒูŠ โ โž ุฌูˆู† ู‡ุงุฑูˆุจ โ โž ูƒูŠุซ ู…ูŠุฑููŠุŒ ุดูŠุฑูŠ ูƒุงุจุฑุงู„ โ โž ูˆูŠู„ ุฃู„ุณูˆุจ โ โž ุฑุงู†ุฏุงู„ ูƒ.ู…ุงูŠูƒู„ โ โž ู„ูŠุฒุง ุจูˆูƒูŠ โ โž ู„ูŠู†ุฏุง ุฅู ุฌูˆู†ุณูˆู† โ โž ุฌุงูƒูˆุจ ู†ูŠู„ุณู† โ โž ุฏูŠููŠุฏ ุณูŠู„ โ โž ุฏุงู†ุง ุชุดูŠุณู†ูŠู„ โ โž ุฌูŠุฑูŠู…ูŠ ุจู„ูˆู… โ โž ุจูŠูƒูŠ ุณุชูŠูˆุงุฑุช โ โž ู…ูŠูƒูŠ ู…ุงูƒู…ุงู†ูˆุณ โ โž ุจูŠุฑูŠ ุดูŠุงูˆ โ โฑ.ุงู„ู…ุฒูŠุฏ.. ูƒุชุจ ูˆุงูŠู„ูŠ (ู†ุงุดุฑ)