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Related Concept Videos

Diversity of Protists III01:27

Diversity of Protists III

Rhizaria are a diverse group of unicellular protists characterized by their threadlike cytoplasmic extensions known as pseudopodia. These structures aid in both locomotion and feeding, giving Rhizaria an amoeboid appearance. Their amoeboid morphology once led to taxonomic confusion, but molecular phylogenetics has clarified their evolutionary placement and emphasized their shared use of pseudopodia despite divergent lineages.This clade comprises diverse lineages such as Chlorarachniophyta,...
Ion-Exchange Chromatography01:09

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Ion-exchange chromatography, or IEC, is a technique for separating ions based on their affinity for the stationary phase. The stationary phase is a cross-linked polymer resin with covalently attached ionic functional groups. The functional groups can be either positively charged (cation exchangers) or negatively charged (anion exchangers). A cation exchanger consists of a polymeric anion and active cations, while an anion exchanger is a polymeric cation with active anions. The choice of...
Formation of Complex Ions03:45

Formation of Complex Ions

A type of Lewis acid-base chemistry involves the formation of a complex ion (or a coordination complex) comprising a central atom, typically a transition metal cation, surrounded by ions or molecules called ligands. These ligands can be neutral molecules like H2O or NH3, or ions such as CN− or OH−. Often, the ligands act as Lewis bases, donating a pair of electrons to the central atom. These types of Lewis acid-base reactions are examples of a broad subdiscipline called coordination...
Redox Titration: Iodimetry and Iodometry01:23

Redox Titration: Iodimetry and Iodometry

Iodometry and iodimetry are analytical methods used to determine the concentration of oxidizing or reducing agents using iodine. In iodometric titrations, the oxidizing analyte solution is usually acidified and treated with an excess of iodide ions, which generates an equivalent amount of iodine in equilibrium with triiodide. The released iodine is subsequently titrated directly against a standardized reducing agent. As the dilute iodine color becomes pale yellow, a few drops of freshly...
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Precipitation of Ions

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Ion Exchange01:17

Ion Exchange

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Related Experiment Video

Updated: Jun 28, 2026

Photochemical Oxidative Growth of Iridium Oxide Nanoparticles on CdSe@CdS Nanorods
05:41

Photochemical Oxidative Growth of Iridium Oxide Nanoparticles on CdSe@CdS Nanorods

Published on: February 11, 2016

Iridium in sea-water.

J Fresco1, H V Weiss, R B Phillips

  • 1Department of Chemistry, McGill University, Montreal, Quebec, Canada.

Talanta
|August 1, 1985
PubMed
Summary
This summary is machine-generated.

Seawater contains extremely low iridium concentrations, measured at 1.02 x 10^-14 g/g. This finding suggests seawater is not the source of high iridium levels found in Cretaceous-Tertiary boundary sediments.

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Published on: April 21, 2022

Area of Science:

  • Geochemistry
  • Marine Chemistry
  • Nuclear Chemistry

Background:

  • Iridium anomalies in Cretaceous-Tertiary boundary sediments suggest extraterrestrial impact events.
  • Understanding iridium's oceanic concentration is crucial for distinguishing between impact and terrestrial sources.

Purpose of the Study:

  • To accurately measure the concentration of iridium in seawater.
  • To evaluate the role of seawater as a potential source for sedimentary iridium anomalies.

Main Methods:

  • Iridium isolation from seawater using magnesium reduction.
  • Neutron bombardment for activation analysis.
  • Radiochemical purification and high-resolution gamma-ray spectroscopy for detection.

Main Results:

  • Measured Pacific coastal seawater iridium concentration at 1.02 +/- 0.26 x 10^-14 g/g.
  • Demonstrated extremely low levels of dissolved iridium in marine environments.

Conclusions:

  • Seawater is an improbable source for the anomalously high iridium concentrations observed in Cretaceous-Tertiary boundary sediments.
  • The study supports extraterrestrial origins for the iridium spike at the Cretaceous-Tertiary boundary.