Belarus vs Indonesia: Drained organic soils — Area
Belarus
1.50 million ha
in 2024
Indonesia
4.93 million ha
in 2024
Belarus rank
4th
Indonesia rank
2nd
Drained organic soils — Area over time
- Belarus
- Indonesia
How they compare
Indonesia currently reports 4.93 million ha against 1.50 million ha in Belarus, a difference of 3.43 million ha.
That makes Indonesia's figure about 3.3 times Belarus's.
Across all 33 years both countries report, Indonesia has been ahead every year.
Belarus ranks 4th and Indonesia ranks 2nd of 221 countries.
Indonesia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Belarus | Indonesia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1.52 million ha | 3.88 million ha | 2.36 million ha | Indonesia |
| 2000s | 1.54 million ha | 4.15 million ha | 2.61 million ha | Indonesia |
| 2010s | 1.52 million ha | 4.73 million ha | 3.22 million ha | Indonesia |
| 2020s | 1.50 million ha | 4.93 million ha | 3.43 million ha | Indonesia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — area, Belarus or Indonesia?
- Indonesia, at 4.93 million ha against 1.50 million ha in Belarus as of 2024.
- What is the difference in drained organic soils — area between Belarus and Indonesia?
- 3.43 million ha, 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 — area?
- 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 — Area. 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.