Fire-induced geochemical changes in soil: Implication for the element cycling

Ajmal Roshan1, Ashis Biswas1

  • 1Environmental Geochemistry Laboratory, Department of Earth and Environmental Sciences, Indian Institute of Science Education and Research (IISER) Bhopal, Bhopal Bypass Road, Bhauri, Bhopal 462066, MP, India.

Related Concept Videos

The Sulfur Cycle01:22

The Sulfur Cycle

Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
45.7K
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
39.2K
What are Biogeochemical Cycles?00:54

What are Biogeochemical Cycles?

The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
33.8K
Influences on Weathering01:26

Influences on Weathering

Influences On WeatheringWeathering is the natural process that breaks down rocks into smaller pieces. Both mechanical and chemical weathering shape Earth’s surface, but the rate and type of weathering depend on several important factors. One major influence is climate. In warm, wet climates, chemical weathering happens faster because moisture and heat speed up chemical reactions. In cold climates, mechanical weathering, like ice wedging, is more common. The type of rock also affects...
Chemical Weathering01:23

Chemical Weathering

Chemical WeatheringChemical weathering is the process of breaking down rocks through chemical changes. Unlike mechanical weathering, which breaks rocks physically, chemical weathering changes the minerals inside rocks. This happens when water, oxygen, carbon dioxide, or acids react with the rock’s surface. One example is when rainwater mixes with carbon dioxide in the air to form a weak acid that slowly dissolves limestone, creating caves or sinkholes. Rusting is another example, where oxygen...
Chemical Changes01:20

Chemical Changes

Chemical ChangeA chemical change occurs when a substance transforms into a new substance with different properties. Examples include rusting iron, burning wood, and baking a cake. These changes are usually irreversible, meaning the original substance cannot quickly recover. Chemical changes are crucial for advancements in areas such as medicine, environmental science, and materials manufacturing.Science and Engineering Practices (SEP): Analyzing and Interpreting DataScientists investigate...
3