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气态和沉积生物地球化学周期之间的差异

January 19, 2020Posted byDr.Samanthi

Thekey difference在气态和沉积生物地球化学周期之间main reservoir of the element. In gaseous biogeochemical cycles,the main reservoir of the element is the air or ocean.But, the main reservoir of the element is the Earth crust in sedimentary biogeochemical cycles.

Biogeochemical cycles are pathways by which substances mainly circulate through biotic (biosphere) and abiotic (lithosphere, atmosphere, and hydrosphere) parts of Earth. These cycles explain the movement of a particular element via living and nonliving matter in anecosystem。有几个自然循环,包括nitrogen cycle,carbon cycle, water cycle,phosphorus cycle, and sulfur cycle. These cycles are extremely important for the existence of life and transforming energy and mater into usable forms to support ecosystem functioning.

Each cycle shows a balance in cycling between different compartments. However, human activities have greatly affected these natural cycles, creating altered and accelerated cycles that can influence the climate and pose a threat to biodiversity, food security, human health, and water quality, etc. Generally, biogeochemical cycles can be categorized into two main types as gaseous and sedimentary.

内容

1.Overview and Key Difference
2.什么是气态生物地球化学周期
3.What are Sedimentary Biogeochemical Cycles
4.气态和沉积生物地球化学周期之间的相似性
5.Side by Side Comparison – Gaseous vs Sedimentary Biogeochemical Cycles in Tabular Form
6.概括

什么是气态生物地球化学周期?

Gaseous biogeochemical cycles circulate through the atmosphere and hydrosphere. Therefore, the main reservoirs of gaseous biogeochemical cycles are air and ocean. Nitrogen, oxygen, carbon, and water cycles are some of the gaseous biogeochemical cycles. Especially in the nitrogen cycle, the major reservoir is the atmosphere. In the atmosphere, more than 78% is occupied by nitrogen gas (N2)。此外,CO的主要水库2和o2is also the atmosphere.

Key Difference - Gaseous vs Sedimentary Biogeochemical Cycles

Figure 01: Gaseous Biogeochemical Cycle – Nitrogen Cycle

Atmospheric gases are absorbed by plants and aerobic organisms. Plants fix carbon dioxide and produce carbohydrates. We breathe air containing oxygen. In addition, gaseous cycles take place quickly than sedimentary cycles.

什么是沉积物地球化学周期?

Sedimentary biogeochemical cycles are the cycles in which the main reservoir is the soil and sedimentary rocks. Therefore, the elements of sedimentary biogeochemical cycles mainly circulate through the land to water to sediments. Basically, these cycles have a solution phase and rock phase.

气态和沉积生物地球化学周期之间的差异

Figure 02: Sedimentary Biogeochemical Cycle – Phosphorus Cycle

From the Earth’s crust, minerals are released by the weathering process. Then they become salts in water. These elements circulate through a series of organisms and finally come to the sea. Some salts deposit in rock while some salts settle in sediments. Most importantly, these elements do not move through the air. Iron, calcium, phosphorus, and other more earthbound elements are sedimentary biogeochemical cycles.

气态和沉积生物地球化学周期之间有什么相似之处?

  • Gaseous and sedimentary cycles are two main categories of biogeochemical cycles.
  • 他们描绘了元素通过地球不同隔室的运动。
  • They are natural cycles.
  • However, human activities accelerate and alter both types of cycles.

What is the Difference Between Gaseous and Sedimentary Biogeochemical Cycles?

气态循环是元素的主要储层是空气或水。同时,沉积周期是循环,其中该元素的主要储层是地壳。因此,这是气态和沉积生物地球化学周期之间的关键区别。例如,氮,氧气,碳和水周期是气态周期,而铁,钙,磷和其他更多地球元素循环是沉积周期。

Moreover, gaseous biogeochemical cycles are fast, while the sedimentary biogeochemical cycles are slow. Therefore, this is another difference between gaseous and sedimentary biogeochemical cycles.

以下信息图显示了有关气态和沉积生物地球化学周期之间差异的更多比较。

气态和沉积生物地球化学循环的差异以表格形式

总结——气体沉积生物地球化学Cy vscles

气态生物地球化学循环主要在大气中移动。因此,他们的主要水库是空气或海洋。相反,沉积物地球化学循环穿过土壤或地壳,因此其主要储层是岩石圈。因此,这是气态和沉积生物地球化学周期之间的关键区别。此外,气态循环发生得非常快,而沉积周期非常慢。例如,氮,氧气,碳和水周期是气态周期,而铁,钙,磷和其他更多地球元素循环是沉积周期。

Reference:

1.“Biogeochemical Cycle.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 16 June 2016,Available here。
2. Doršner, Kamala, et al. “3.2 Biogeochemical Cycles.” Environmental Biology,Available here。

Image Courtesy:

1. “Nitrogen Cycle” By Cicle_del_nitrogen_de.svg: *Cicle_del_nitrogen_ca.svg: Johann Dréo (User:Nojhan), traduction de Joanjoc d’après Image:Cycle azote fr.svg.derivative work: Burkhard (talk)Nitrogen_Cycle.jpg: Environmental Protection Agencyderivative work: Raeky (talk) – Cicle_del_nitrogen_de.svgNitrogen_Cycle.jpg(CC BY-SA 3.0)viaCommons Wikimedia
2. “Phosphorus cycle” By BonniemfIncorporates work by NASA Earth Science Enterprise – Reworked by Bonniemf from the public domain file File:Carbon cycle-cute diagram.svg(CC BY-SA 3.0)viaCommons Wikimedia

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Filed Under:Biology

About the Author:Dr.Samanthi

Samanthi Udayangani博士拥有B.Sc.植物科学学位,硕士在分子和应用微生物学和应用微生物学中的博士学位。她的研究兴趣包括生物肥料,植物 - 微生物相互作用,分子微生物学,土壤真菌和真菌生态学。

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