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Related Concept Videos

The Nitrogen Cycle01:49

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Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
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Geographic Information Systems (GIS) rely on two core types of data: spatial data and attribute data.Spatial DataSpatial data defines the physical location of features within a coordinate system, typically expressed in terms of latitude and longitude. It provides precise positioning for elements like roads, rivers, or buildings.Attribute DataAttribute data complements spatial data by adding descriptive information about these features. For example, a road's spatial data includes its start and...
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Inorganic Nitrogen Assimilation01:22

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Nitrogen is an essential element in biological systems, forming a crucial component of proteins, nucleic acids, and other cellular constituents. Many bacteria and archaea acquire nitrogen in the form of nitrate (NO₃⁻) or ammonia (NH₃), which are then assimilated into biomolecules through specific enzymatic pathways.Assimilatory Nitrate ReductionWhen nitrate enters the cell, it undergoes a two-step reduction process known as assimilatory nitrate reduction. Initially, the enzyme...
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Overview of Nitrogen Metabolism01:20

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Nitrogen is a very important element for life because it is a major constituent of proteins and nucleic acids. It is a macronutrient, and in nature, it is recycled from organic compounds and stored in the form of  ammonia, ammonium ions, nitrate, nitrite, or  nitrogen gas by many metabolic processes. Many of these metabolic processes are carried out only by prokaryotes.
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Related Experiment Video

Updated: Jul 18, 2025

Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers
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Data-driven modeling on the global annual soil nitrous oxide emissions: Spatial pattern and attributes.

Jiaqiang Liao1, Yuanyuan Huang2, Zhaolei Li3

  • 1Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China.

The Science of the Total Environment
|August 25, 2023
PubMed
Summary
This summary is machine-generated.

This study maps global soil nitrous oxide (N2O) emissions using field data, revealing lower rates than previous models. Soil nitrogen availability, not climate, is the key driver of N2O emissions.

Keywords:
CroplandData-driven modelForestGrasslandSoil nitrous oxideSpatial pattern

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Area of Science:

  • Environmental Science
  • Soil Science
  • Atmospheric Chemistry

Background:

  • Previous global terrestrial soil nitrous oxide (N2O) emission estimates were divergent and poorly matched observed data.
  • Accurate N2O emission mapping is crucial for understanding its role in climate change and developing mitigation strategies.

Purpose of the Study:

  • To generate a data-driven global map of terrestrial soil N2O emissions using extensive field observations.
  • To identify key environmental variables influencing global N2O emission variations.
  • To compare data-driven estimates with previous model-based assessments.

Main Methods:

  • Utilized a dataset of 5549 global field observations of soil N2O emissions.
  • Employed the random forest approach to create spatially explicit maps of annual soil N2O emission rates.
  • Quantified the predictive importance of various factors including soil nitrogen substrates (nitrate, ammonium, fertilizer) and climatic variables (temperature, precipitation).

Main Results:

  • The global mean soil N2O emission rate was estimated at 0.059 ± 0.006 g N m⁻² year⁻¹, lower than previous model ensemble estimates.
  • Soil N2O emissions were found to be higher in the Northern Hemisphere compared to the Southern Hemisphere.
  • Cropland soils exhibited higher average annual N2O emission rates (0.094 ± 0.009 g N m⁻² year⁻¹) than forest (0.039 ± 0.004 g N m⁻² year⁻¹) and grassland (0.045 ± 0.007 g N m⁻² year⁻¹).
  • Soil nitrogen substrates (nitrate, ammonium, fertilizer) were more influential in predicting N2O emissions than mean annual temperature and precipitation.

Conclusions:

  • Data-driven models based on extensive field observations provide more reliable estimates of global soil N2O emissions.
  • Previous process-based models may overestimate N2O emissions due to limited validation data and simplified assumptions.
  • Global field observations are essential for constraining and improving process-based models for accurate N2O emission predictions.