China, mainland vs Mongolia: Cropland organic soils — Emissions (N2O)
China, mainland
1.89 kt
in 2024
Mongolia
2.07 kt
in 2024
China, mainland rank
23rd
Mongolia rank
20th
Cropland organic soils — Emissions (N2O) over time
- China, mainland
- Mongolia
How they compare
Mongolia currently reports 2.07 kt against 1.89 kt in China, mainland, a difference of 0.18 kt.
That makes Mongolia's figure about 1.1 times China, mainland's.
Across all 35 years both countries report, Mongolia has been ahead every year.
China, mainland ranks 23rd and Mongolia ranks 20th of 221 countries.
Mongolia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | China, mainland | Mongolia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1.77 kt | 2.15 kt | 0.3785 kt | Mongolia |
| 2000s | 1.83 kt | 2.18 kt | 0.3448 kt | Mongolia |
| 2010s | 1.86 kt | 2.16 kt | 0.3041 kt | Mongolia |
| 2020s | 1.89 kt | 2.08 kt | 0.1917 kt | Mongolia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, China, mainland or Mongolia?
- Mongolia, at 2.07 kt against 1.89 kt in China, mainland as of 2024.
- What is the difference in cropland organic soils — emissions between China, mainland and Mongolia?
- 0.18 kt, with Mongolia ahead.
- How many years of comparable data are there for China, mainland and Mongolia?
- 35 years are reported by both, from 1990 to 2024.
- How do China, mainland and Mongolia rank globally for cropland organic soils — emissions?
- China, mainland ranks 23rd and Mongolia ranks 20th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Cropland organic soils — Emissions (N2O). Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
The FAOSTAT domain on Emissions from drained organic soils consists of nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from the mineralization and oxidation of organic matter in organic soils that are drained for agricultural activities.