Biogeochemical cycles

From WikiMD.org
Jump to navigation Jump to search

Biogeochemical cycles

Biogeochemical cycles (pronunciation: bio-geo-chemical cycles, from the Greek words bios meaning life, ge meaning earth, and chemical referring to the study of matter and its interactions) are natural processes that allow the transfer and circulation of matter in different forms among the biosphere, atmosphere, lithosphere, and hydrosphere.

Definition

Biogeochemical cycles are the pathways by which elements like carbon, nitrogen, oxygen, and others flow between living organisms (biota) and the physical environment (geosphere and atmosphere). These cycles are crucial for life on Earth as they regulate the availability of these essential elements.

Types of Biogeochemical Cycles

There are several types of biogeochemical cycles, including:

Each of these cycles represents the processes by which these elements are converted into usable forms, used by organisms, and then returned to the environment.

Importance of Biogeochemical Cycles

Biogeochemical cycles are essential for life on Earth. They ensure the continuous availability of essential elements to living organisms. They also help in maintaining the balance of these elements in the environment, preventing their depletion or over-accumulation, which could be harmful to life.

Human Impact on Biogeochemical Cycles

Human activities, such as industrialization, deforestation, and pollution, have significantly altered biogeochemical cycles. This alteration can lead to environmental problems like climate change, ozone depletion, and biodiversity loss.

See Also

External links

Esculaap.svg

This WikiMD article is a stub. You can help make it a full article.


Languages: - East Asian 中文, 日本, 한국어, South Asian हिन्दी, Urdu, বাংলা, తెలుగు, தமிழ், ಕನ್ನಡ,
Southeast Asian Indonesian, Vietnamese, Thai, မြန်မာဘာသာ, European español, Deutsch, français, русский, português do Brasil, Italian, polski