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Types of Collisions - II01:19

Types of Collisions - II

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When two or more objects collide with each other, they can stick together to form one single composite object (after collision). The total mass of the object after the collision is the sum of the masses of the original objects, and it moves with a velocity dictated by the conservation of momentum. Although the system's total momentum remains constant, the kinetic energy decreases, and thus such a collision is an inelastic collision. Most of the collisions between objects in daily life are...
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The Soil Ecosystem02:23

The Soil Ecosystem

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Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
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The Carbon Cycle01:14

The Carbon Cycle

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Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
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The Sulfur Cycle01:22

The Sulfur Cycle

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Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
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The Phosphorus Cycle01:21

The Phosphorus Cycle

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Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
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What are Biogeochemical Cycles?00:54

What are Biogeochemical Cycles?

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The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
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地球 の 構成 は 衝突 侵食 に よっ て 変化 し まし た

Paul Frossard1,2, Claudine Israel1, Audrey Bouvier3,4

  • 1Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans, F-63000 Clermont-Ferrand, France.

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|September 29, 2022
PubMed
まとめ

サマリウム-146 (Sm) ネオジミウム-142 (Nd) システムは,初期の惑星進化を明らかにしています. 核合成の異常を修正すると,地球が

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Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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科学分野:

  • 地化学
  • 宇宙化学
  • 惑星科学

背景:

  • サマリウム-146 (Sm) ネオジミウム-142 (Nd) 崩壊系は,マントルの初期の地殻の進化を追跡するために重要である.
  • 観測された142Nd/144Ndの過剰は,核合成異常から生じ,分化史の解釈を複雑にする可能性がある.

研究 の 目的:

  • 核合成によるコンドライトの成分を定量化する.
  • これらの異常を修正することで 初期の地球の分化の歴史を再評価する.

主な方法:

  • 原始的なコンドライトの段階的な溶解により,同位体成分を分析する.
  • 同位体データの核合成異常を修正する.

主要な成果:

  • コンドライトの構成に対する核合成の量化.
  • 異常修正後の地球における142Ndの過剰と微分化プラネティシマルの解明.
  • 原始的な地殻の衝突による侵食がこれらの組成を説明することを示した.

結論:

  • 惑星の増殖過程における衝突侵食は早期の分化に大きく影響した.
  • このプロセスは,ウラン,トリウム,カリウムなどの熱を生成する元素を含む,相容れない元素の実質的な損失をもたらしました.