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  2. Ion channel - Wikipedia

    en.wikipedia.org/wiki/Ion_channel

    The archetypal channel pore is just one or two atoms wide at its narrowest point and is selective for specific species of ion, such as sodium or potassium. However, some channels may be permeable to the passage of more than one type of ion, typically sharing a common charge: positive or negative . Ions often move through the segments of the ...

  3. Voltage-gated ion channel - Wikipedia

    en.wikipedia.org/wiki/Voltage-gated_ion_channel

    Conformation of the four homologous domains showing the formation of a central pore. Voltage-gated ion channels are generally composed of several subunits arranged in such a way that there is a central pore through which ions can travel down their electrochemical gradients.

  4. Ferric - Wikipedia

    en.wikipedia.org/wiki/Ferric

    These same ligands can even dissolve iron(III) oxides and hydroxides. One of these ligands is EDTA, which is often used to dissolve iron deposits or added to fertilizers to make iron in the soil available (soluble) to plants. Citrate also solubilizes ferric ion at neutral pH, although its complexes are less stable than those of EDTA.

  5. Bioinorganic chemistry - Wikipedia

    en.wikipedia.org/wiki/Bioinorganic_chemistry

    Bioinorganic chemistry is a field that examines the role of metals in biology.Bioinorganic chemistry includes the study of both natural phenomena such as the behavior of metalloproteins as well as artificially introduced metals, including those that are non-essential, in medicine and toxicology.

  6. Ion-exchange membrane - Wikipedia

    en.wikipedia.org/wiki/Ion-exchange_membrane

    An ion-exchange membrane is generally made of organic or inorganic polymer with charged (ionic) side groups, such as ion-exchange resins. Anion-exchange membranes contain fixed cationic groups with predominantly mobile anions; because anions are the majority species, most of the conductivity is due to anion transport.

  7. Iron in biology - Wikipedia

    en.wikipedia.org/wiki/Iron_in_biology

    Iron can also be oxidized by marine microbes under conditions that are high in iron and low in oxygen. [53] Iron can enter marine systems through adjoining rivers and directly from the atmosphere. Once iron enters the ocean, it can be distributed throughout the water column through ocean mixing and through recycling on the cellular level. [54]