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相关概念视频

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.
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...
The Soil Ecosystem02:23

The Soil Ecosystem

Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
Microbes and the Carbon Cycle01:24

Microbes and the Carbon Cycle

The carbon cycle is a fundamental Earth process involving the transfer of carbon among the biosphere, lithosphere, atmosphere, and hydrosphere. It plays a critical role in regulating the planet’s climate and supporting life by cycling carbon through various chemical forms and reservoirs. Carbon primarily circulates as carbon dioxide (CO₂), representing its oxidized form, while reduced forms such as methane (CH₄) and organic compounds also play essential roles.Microbial activity is central to...
Soil Microbial Ecology01:29

Soil Microbial Ecology

Soil microbial ecology is defined by highly diverse, spatially structured communities that drive nutrient cycling, organic matter turnover, and overall ecosystem stability. Although a gram of soil can contain thousands of bacterial and archaeal taxa, the ecological processes they mediate are even more crucial for sustaining terrestrial life.Microhabitats and NichesSoil is a heterogeneous mixture of minerals, organic matter, water, and air. Microbes inhabit distinct microhabitats formed by...
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...

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相关实验视频

Updated: Jul 8, 2026

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

Published on: June 4, 2021

土壤作为大气中一氧化碳的沉降池.

    Science (New York, N.Y.)
    |June 19, 1981
    PubMed
    概括

    土壤微生物有效地消耗一氧化碳 (CO),这是遵循迈凯利斯-门运动的过程. 这种自然土壤吸收大气中的二氧化碳是相当大的,几乎与化石燃料的排放相当.

    科学领域:

    • 环境科学 环境科学
    • 土壤科学 土壤科学
    • 大气化学 大气化学

    背景情况:

    • 一氧化碳 (CO) 是一个重要的大气污染物.
    • 土壤微生物群落在大气气体循环中发挥作用.
    • 了解CO土壤氧化对于大气中的CO预算至关重要.

    研究的目的:

    • 量化不同土壤类型的一氧化碳氧化率.
    • 为了研究二氧化碳度与土壤氧化率之间的关系.
    • 为了估计全球土壤对大气一氧化碳的吸收.

    主要方法:

    • 收集了20个土壤样本以确定氧化率.
    • 在温度范围 (0-30°C) 中测量CO氧化率.
    • 应用迈凯利斯-门动力学来分析二氧化碳氧化数据.

    主要成果:

    • 土壤CO氧化率随着气相CO度的增加而增加.
    • 在测试的土壤和温度中,氧化率遵循迈凯利斯-门动力学.
    • 计算出全球土壤吸收率为4.1 x 10^14 g CO/年.

    结论:

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    相关实验视频

    Last Updated: Jul 8, 2026

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
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    Published on: June 4, 2021

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    09:19

    Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools

    Published on: December 16, 2022

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    07:22

    Design and Construction of an Experimental Setup to Enhance Mineral Weathering through the Activity of Soil Organisms

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    • 土壤是大气中一氧化碳的重要沉积点.
    • 全球土壤二氧化碳吸收量相当于每年化石燃料二氧化碳排放量.
    • 这凸显了土壤生态系统在调节大气中二氧化碳水平方面的重要性.