Belarus vs Indonesia: Drained organic soils — Emissions (N2O)
Belarus
29.79 kt
in 2024
Indonesia
38.14 kt
in 2024
Belarus rank
4th
Indonesia rank
2nd
Drained organic soils — Emissions (N2O) over time
- Belarus
- Indonesia
How they compare
Indonesia currently reports 38.14 kt against 29.79 kt in Belarus, a difference of 8.35 kt.
That makes Indonesia's figure about 1.3 times Belarus's.
The two have swapped places 1 time across 33 shared years of data; in 1992 it was Belarus ahead.
Belarus ranks 4th and Indonesia ranks 2nd of 221 countries.
Across the 4 decades both report, Belarus averaged higher in 1 and Indonesia in 3.
Head to head by decade
| Decade | Belarus | Indonesia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 30.24 kt | 30.02 kt | 0.2264 kt | Belarus |
| 2000s | 30.57 kt | 32.13 kt | 1.56 kt | Indonesia |
| 2010s | 30.17 kt | 36.65 kt | 6.48 kt | Indonesia |
| 2020s | 29.79 kt | 38.14 kt | 8.35 kt | Indonesia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — emissions, Belarus or Indonesia?
- Indonesia, at 38.14 kt against 29.79 kt in Belarus as of 2024.
- What is the difference in drained organic soils — emissions between Belarus and Indonesia?
- 8.35 kt, with Indonesia ahead.
- How many years of comparable data are there for Belarus and Indonesia?
- 33 years are reported by both, from 1992 to 2024.
- How do Belarus and Indonesia rank globally for drained organic soils — emissions?
- Belarus ranks 4th and Indonesia ranks 2nd of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Drained 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.