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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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Updated: Jul 19, 2026

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

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Patrones de abundancia de elementos del grupo del platino en diferentes entornos del manto.

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
Resumen

Los patrones de elementos del grupo del platino (PGE) en los xenolitos del manto revelan distintas historias del manto superior. Los xenolitos de la línea de Camerún sugieren un manto homogéneo, mientras que los xenolitos de Tanzania indican un origen de una zona de suprasubducción rica en fluidos.

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Área de la Ciencia:

  • La geoquímica es la geoquímica.
  • Petrología Petrología.
  • Estudios sobre el xenolito del manto.

Sus antecedentes:

  • Los xenolitos derivados del manto proporcionan información crucial sobre la composición y evolución del manto superior de la Tierra.
  • Los elementos del grupo del platino (PGEs) son trazadores sensibles de los procesos del manto, incluida la extracción del fundido y la alteración del fluido.

Objetivo del estudio:

  • Para comparar los patrones de abundancia del elemento del grupo del platino (PGE) en los xenolitos del manto de la Línea de Camerún y el norte de Tanzania.
  • Para aclarar las distintas historias de evolución del manto de estas dos regiones basadas en su sistemática PGE.

Principales métodos:

  • Análisis de las concentraciones de elementos del grupo del platino (EGP) en los xenolitos del manto (lerzolitas y peridotitas).
  • Comparación de los patrones de PGE observados con los reservorios conocidos del manto y los entornos geológicos (por ejemplo, ofiolitos, zonas de suprasubducción).

Principales resultados:

  • Las herzolitas de la línea de Camerún exhiben patrones uniformes de PGE con proporciones condríticas, indicativas de un manto superior homogéneo.
  • Las peridotitas de Tanzania muestran patrones de PGE similares a las rocas ultramaficas de los ofiolitos, lo que sugiere una evolución diferente del manto.
  • Las diferencias observadas se atribuyen a un desarrollo litosférico contrastante: suprasubducción rica en fluidos para Tanzania y extracción de fundición a partir de peridotitas anidras para Camerún Line.

Conclusiones:

  • El manto superior debajo de la Línea de Camerún se interpreta como homogéneo y en gran parte anhidro.
  • La litosfera en el norte de Tanzania probablemente se formó en un ambiente de zona de suprasubducción rica en fluidos.
  • Los patrones de abundancia de PGE en los xenolitos del manto sirven como poderosos indicadores de diversos procesos del manto y entornos tectónicos.