Belize vs Serbia and Montenegro: Drained organic soils — Emissions
Belize
0.034 kt
in 2024
Serbia and Montenegro
0.0263 kt
in 2005
Belize rank
81st
Serbia and Montenegro rank
82nd
Drained organic soils — Emissions over time
- Belize
- Serbia and Montenegro
How they compare
Belize currently reports 0.034 kt against 0.0263 kt in Serbia and Montenegro, a difference of 0.0077 kt.
That makes Belize's figure about 1.3 times Serbia and Montenegro's.
The two have swapped places 1 time across 14 shared years of data; in 1992 it was Belize ahead.
Belize ranks 81st and Serbia and Montenegro ranks 82nd of 221 countries.
Across the 2 decades both report, Belize averaged higher in 1 and Serbia and Montenegro in 1.
Head to head by decade
| Decade | Belize | Serbia and Montenegro | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.0275 kt | 0.0237 kt | 0.0038 kt | Belize |
| 2000s | 0.0257 kt | 0.0263 kt | 0.0006 kt | Serbia and Montenegro |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — emissions, Belize or Serbia and Montenegro?
- Belize, at 0.034 kt against 0.0263 kt in Serbia and Montenegro as of 2024.
- What is the difference in drained organic soils — emissions between Belize and Serbia and Montenegro?
- 0.0077 kt, with Belize ahead.
- How many years of comparable data are there for Belize and Serbia and Montenegro?
- 14 years are reported by both, from 1992 to 2005.
- How do Belize and Serbia and Montenegro rank globally for drained organic soils — emissions?
- Belize ranks 81st and Serbia and Montenegro ranks 82nd 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.