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Related Concept Videos

Minerals01:26

Minerals

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Minerals are essential nutrients that the human body needs in small amounts to work properly. They play a vital role in many bodily functions, such as building strong bones and transmitting nerve impulses. Some minerals are needed for hormone production or to maintain a normal heartbeat. Major minerals include calcium, phosphorus, potassium, sulfur, sodium, chlorine, and magnesium, while trace minerals include iron, manganese, copper, iodine, zinc, cobalt, fluoride, and selenium.
 
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Solubility Equilibria: Overview01:09

Solubility Equilibria: Overview

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When a substance such as sodium chloride is added to water, it dissolves, forming an aqueous solution. The extent of dissolution is called solubility. The process of dissolution can exist in equilibrium, just like other chemical processes. Solubility equilibria are also called precipitation equilibria because the process of solubility can be reversible. The reverse of the solubility process is called precipitation.
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Essential Minerals for Bone Health01:31

Essential Minerals for Bone Health

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The minerals contained in all of the food we consume are essential for our organ systems. However, certain essential minerals, such as calcium, phosphorus, magnesium, manganese, and fluoride, largely affect bone health.
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Calcium is a critical component of bones, especially in the form of calcium phosphate and calcium carbonate. Since the body cannot make calcium, it must be obtained from the diet. However, calcium cannot be absorbed from the small intestine without...
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Electron Affinity03:07

Electron Affinity

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The electron affinity (EA) is the energy change for adding an electron to a gaseous atom to form an anion (negative ion).
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Halogens03:01

Halogens

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Group 17 elements, known as halogens, are nonmetals. At room temperature, fluorine and chlorine are gases, bromine is a liquid, and iodine a solid. Astatine is a highly unstable radioactive element, so currently, most of its properties are unknown due to its short half-life. Tennessine is a synthetic element also predicted to be in this group. 
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Electrophilic Aromatic Substitution: Fluorination and Iodination of Benzene01:13

Electrophilic Aromatic Substitution: Fluorination and Iodination of Benzene

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Bromination and chlorination of aromatic rings by electrophilic aromatic substitution reactions are easily achieved, but fluorination and iodination are difficult to achieve. Fluorine is so reactive that its reaction with benzene is difficult to control, resulting in poor yields of monofluoroaromatic products. To address this, Selectfluor reagent is used as a fluorine source in which a fluorine atom is bonded to a positively charged nitrogen.
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Updated: Dec 30, 2025

Micro-dissection of Enamel Organ from Mandibular Incisor of Rats Exposed to Environmental Toxicants
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Fluoride occurrence in the lower East African Rift System, Southern Malawi.

Marc J Addison1, Michael O Rivett1, Helen Robinson1

  • 1Department of Civil & Environmental Engineering, University of Strathclyde, Glasgow, Scotland, G1 1XJ.

The Science of the Total Environment
|January 17, 2020
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Summary

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Area of Science:

  • Geochemistry
  • Hydrogeology
  • Environmental Science

Background:

  • The East African Rift System (EARS) presents a significant groundwater fluoride risk, particularly in developing nations like Malawi.
  • Fluoride occurrence in Malawian groundwater remains poorly characterized, necessitating detailed investigation for effective risk management.

Purpose of the Study:

  • To document groundwater fluoride occurrence in Malawi.
  • To understand and manage fluoride risks in Malawian drinking water.
  • To inform policy revision and management strategies for fluoride in groundwater.

Main Methods:

  • Collation of historical fluoride data from literature and government archives.
  • Augmentation with new groundwater quality surveys in Southern Malawi (2016-2018).
  • Analysis of 1365 groundwater samples (borehole, spring, hot spring) for fluoride concentration, temperature, and hydrochemical parameters.

Main Results:

  • 83% of samples had fluoride below the WHO guideline of 1.5 mg/l.
  • 14% of samples showed fluoride concentrations between 1.5-6 mg/l.
  • 3% of samples exceeded the 6 mg/l guideline, with higher fluoride linked to increased groundwater temperature (>32°C) and proximity to geological faults.

Conclusions:

  • While fluoride occurrence in Malawi is lower than in other EARS regions, a significant portion of groundwater exceeds safe drinking water standards.
  • Geothermal influence and structural geology are key factors controlling high fluoride groundwater.
  • Recommendations include further documentation and enhanced management strategies for fluoride in Malawian drinking water, aligning with Sustainable Development Goal 6.