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The Periodic Table03:25

The Periodic Table

As early chemists discovered more elements, they realized that various elements could be grouped by their similar chemical behaviors. One such grouping includes lithium (Li), sodium (Na), and potassium (K). All of these elements are shiny, conduct heat and electricity well, and have similar chemical properties. A second grouping includes calcium (Ca), strontium (Sr), and barium (Ba), which also are shiny, good conductors of heat and electricity, and have chemical properties in common. However,...
Periodic Classification of the Elements04:00

Periodic Classification of the Elements

The periodic table arranges atoms based on increasing atomic number so that elements with the same chemical properties recur periodically. When their electron configurations are added to the table, a periodic recurrence of similar electron configurations in the outer shells of these elements is observed. Because they are in the outer shells of an atom, valence electrons play the most important role in chemical reactions. The outer electrons have the highest energy of the electrons in an atom...
Metallic Solids02:37

Metallic Solids

Metallic solids such as crystals of copper, aluminum, and iron are formed by metal atoms. The structure of metallic crystals is often described as a uniform distribution of atomic nuclei within a “sea” of delocalized electrons. The atoms within such a metallic solid are held together by a unique force known as metallic bonding that gives rise to many useful and varied bulk properties.
All metallic solids exhibit high thermal and electrical conductivity, metallic luster, and malleability. Many...
Properties of Transition Metals02:58

Properties of Transition Metals

Transition metals are defined as those elements that have partially filled d orbitals. As shown in Figure 1, the d-block elements in groups 3–12 are transition elements. The f-block elements, also called inner transition metals (the lanthanides and actinides), also meet this criterion because the d orbital is partially occupied before the f orbitals.
The Periodic Table and Organismal Elements01:27

The Periodic Table and Organismal Elements

Elements are the smallest units of matter that cannot be broken down further by chemical processes. There are 118 known elements, but not all of these are naturally occurring, and only a few of them are essential for life. Living matter is composed primarily of carbon, nitrogen, hydrogen, and oxygen, with smaller amounts of other elements like calcium, phosphorus, potassium, and sulfur. Other elements are also necessary for life but only in trace amounts.
Periodic Table Provides Information...
Microbes and Other Elemental Cycles01:24

Microbes and Other Elemental Cycles

Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...

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関連する実験動画

Updated: Jul 19, 2026

Clean Sampling and Analysis of River and Estuarine Waters for Trace Metal Studies
10:44

Clean Sampling and Analysis of River and Estuarine Waters for Trace Metal Studies

Published on: July 1, 2016

異なるマントルの環境におけるプラチナ群の元素の豊富さのパターン

Rehkamper1, Halliday, Barfod

  • 1M. Rehkamper, A. N. Halliday, D. Barfod, Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063, USA. J. G. Fitton and J. B. Dawson, Department of Geology and Geophysics, University of Edinburgh, Edinburgh EH9 3JW, UK.

Science (New York, N.Y.)
|December 5, 1997
PubMed
まとめ

マントル・キセノリトのプラチナ群元素 (PGE) のパターンは,マントルの上部マントルの異なる歴史を明らかにする. カメルーンラインのゼノライトは,均質なマントルを示唆し,タンザニアのゼノライトは,流体豊富な,スーパーサブダクションゾーンの起源を示しています.

さらに関連する動画

Bulk and Thin Film Synthesis of Compositionally Variant Entropy-stabilized Oxides
09:41

Bulk and Thin Film Synthesis of Compositionally Variant Entropy-stabilized Oxides

Published on: May 29, 2018

Resource Recycling of Red Soil to Synthesize Fe2O3/FAU-type Zeolite Composite Material for Heavy Metal Removal
05:52

Resource Recycling of Red Soil to Synthesize Fe2O3/FAU-type Zeolite Composite Material for Heavy Metal Removal

Published on: June 2, 2022

関連する実験動画

Last Updated: Jul 19, 2026

Clean Sampling and Analysis of River and Estuarine Waters for Trace Metal Studies
10:44

Clean Sampling and Analysis of River and Estuarine Waters for Trace Metal Studies

Published on: July 1, 2016

Bulk and Thin Film Synthesis of Compositionally Variant Entropy-stabilized Oxides
09:41

Bulk and Thin Film Synthesis of Compositionally Variant Entropy-stabilized Oxides

Published on: May 29, 2018

Resource Recycling of Red Soil to Synthesize Fe2O3/FAU-type Zeolite Composite Material for Heavy Metal Removal
05:52

Resource Recycling of Red Soil to Synthesize Fe2O3/FAU-type Zeolite Composite Material for Heavy Metal Removal

Published on: June 2, 2022

科学分野:

  • 地質化学 地質化学
  • ペトロロジー・ペトロロジーとは
  • マントル・キセノリト研究 マントル・キセノリト研究

背景:

  • マントルから派生したクセノライトは,地球の上層マントルの組成と進化に関する重要な洞察を提供します.
  • プラチナ群元素 (PGEs) は,溶融抽出と流体変異を含むマントルのプロセスの敏感なトレーサーです.

研究 の 目的:

  • カメルーンラインとタンザニア北部のマントル・キセノリトにおけるプラチナ系元素 (PGE) の豊富度パターンを比較する.
  • この2つの領域の異なるマントルの進化史を,それらの PGE 体系論に基づいて解明する.

主な方法:

  • マントルのキセノリート (レルゾライトとペリドライト) のプラチナ群元素 (PGE) 濃度の分析.
  • 観測されたPGEパターンを,既知のマントルの貯水池と地質学的な環境 (例えば,オフィオライト,スーパーサブダクションゾーン) と比較する.

主要な成果:

  • カメルーンラインのヘルゾライトは,均一なPGEパターンとコンドリート比率を示し,均質な上層マントルの兆候を示しています.
  • タンザニアのペリドータイトは,オフィオライトからの超マフィック岩に似たPGEパターンを示し,異なるマントルの進化を示唆しています.
  • 観測された差異は,対照的な石層の発達に起因する:タンザニアの場合は液体豊富な超流出,カメルーンラインの場合は無水質のペリドータイトから溶融の抽出.

結論:

  • カメルーン線の下の上層マントルは,均質で,主に無水質であると解釈されています.
  • タンザニア北部の石層は,おそらく,液体豊富な超吸収ゾーン環境で形成された.
  • マントルのキセノリトにおけるPGEの豊富性のパターンは,マントルの多様なプロセスと構造的設定の強力な指標として機能します.