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Biogeochemical cycles and the effects of human activities upon them Essay Example

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Biogeochemical cycles include the fluxes of compound components among various earth parts from components that are living to those not living. These are referred to as cycles and since matter is continuously preserved and that components move to and from significant pools using an assortment of two-way fluxes, albeit a few components are put away in areas or in structures that are respectfully available to living things (Bethke, 2007). The activities that are done on the Earth components have a significant effect on the Biogeochemical, for instance, there is an increase in the measure of nitrogen absorption in the biosphere for a long period (Schlesinger, 2005)

Human activities have mobilized carbon, nitrogen, and phosphorus from the Earth and air into nature by more than 36 contrasted with geographical sources over the period of times. Fossil fuel burning, concrete and cement creation, and the extraction and generation of manure to bolster horticulture are significant reasons for the increase (Hedges, 1992). CO2 is the most plentiful and is associated with greenhouse, the heat-trapping has currently increased because of human exercises, thus causing worldwide environmental change. Europe, the sulfur emanations, have declined in the course of recent decades, particularly since the mid-1990s, on account of endeavors to lessen air contamination (Crutzen, 1990). Changes in biogeochemical cycles of carbon, nitrogen, phosphorus, and different components and the coupling of those cycles have an impact on the climate (Berner, 1989).

Considering the whole climatic CO2 budget, contrasted with the sources, more CO2 is radiated than can be taken up. Other components and compounds influence directly or indirectly the carbon cycle e.g. nitrogen directly affects carbon uptake while nitrogen indirectly reduces the soil methane sink. The net impact of Earth’s energy parity changes in a key biogeochemical cycle (carbon, nitrogen, sulfur, and phosphorus) relies on procedures that specifically influence how the planet absorption or reflection of daylight thus influence on greenhouse effect (Ciais, 2014)

Every single living thing has a carbon composition on their system Carbon is likewise a part of the sea, air, and even shakes. Since the Earth moving carbon does not stay still. Plants in presence of sunlight they consume carbon dioxide they are able to produce food and also oxygen for sustenance and growth of other living things to use. In case fossil are burnt the greater part of the carbon rapidly enters the air as carbon dioxide. Carbon dioxide traps heat in the environment and there is higher presence of carbon dioxide gas in the climate than which has increased over past years. Some of human activities that affect carbon cycle are

Fossil Fuels burning

• Burning the coal release carbon into the atmosphere at a faster rate. Normal gas, oil and coal are fossil are have fossil energy and that when they are burnt to produce power, for transportation, in the houses and in modern buildings. The essential primary activities affect and transmit carbon dioxide thus affecting the carbon cycle. These include other activities such as petroleum refining, mining and the chemical production.

Sequestration of Carbon

Plants expel carbon dioxide from the air and store it, the procedure is called carbon sequestration. Human activities such as agricultural influence the amount of carbon dioxide available in the environment and put away by the plants. These sinks of carbon dioxide influence the carbon cycle by diminishing the measure of carbon dioxide presence in the air.


• Deforestation clearing of trees from forests or other natural inhabitants and not planting new trees to replace then. This has resulted to an increase in carbon dioxide levels in the atmosphere reason being that trees do not absorb the carbon dioxide in the atmosphere to make their food through a process called photosynthesis. This process affect the carbon cycle is, agriculture is the major cause of deforestation as human beings clear the forest on a large-scale basis to increase the area that is available to cultivate and keep animals.

The U.S. was the world’s biggest cause of human-created CO2 outflows from 1950 until 2007 when it was surpassed by China. U.S. emanations represent around 85% of North American discharges of CO2 and 18% of worldwide emissions. The Ecosystems shows potential «sinks» for CO2, which are spots where carbon can for a period. There have been an extensive and moderately reliable expansion in forest carbon stocks in the course of the most recent two decades, because of recuperation from past deforestation (Wolfe, 1992)

In conclusion the activities of human being have an effect on the atmosphere, they are responsible for increasing in CO2 in the environment and level of nitrogen in the biosphere. The change in climate has an impact on the change in the quality of water, biodiversity vulnerability, and food security.


Bethke, C. M. (2007). Geochemical and biogeochemical reaction modeling. Cambridge University Press.

Schlesinger, W. H. (2005). Biogeochemistry (Vol. 8). Gulf Professional Publishing.

Hedges, J. I. (1992). Global biogeochemical cycles: progress and problems. Marine chemistry, 39(1), 67-93.

Crutzen, P. J., & Andreae, M. O. (1990). Biomass burning in the tropics: impact on atmospheric chemistry and biogeochemical cycles. Science, 250(4988), 1669-1678.

Berner, R. A. (1989). Biogeochemical cycles of carbon and sulfur and their effect on atmospheric oxygen over Phanerozoic time. Global and Planetary Change, 1(1), 97-122.

Wolfe, G. V. (1992). Global biogeochemical cycles. R. J. Charlson, & G. H. Orians (Eds.). San Diego: Academic Press.

Ciais, P., Sabine, C., Bala, G., Bopp, L., Brovkin, V., Canadell, J., … & Jones, C. (2014). Carbon and other biogeochemical cycles. In Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (pp. 465-570). Cambridge University Press.