Brunei Darussalam vs Peru: Grassland organic soils — Emissions (N2O)
Brunei Darussalam
0.002 kt
in 2024
Peru
0.0021 kt
in 2024
Brunei Darussalam rank
84th
Peru rank
83rd
Grassland organic soils — Emissions (N2O) over time
- Brunei Darussalam
- Peru
How they compare
Peru currently reports 0.0021 kt against 0.002 kt in Brunei Darussalam, a difference of 0.0001 kt.
The two have swapped places 1 time across 35 shared years of data; in 1990 it was Brunei Darussalam ahead.
Brunei Darussalam ranks 84th and Peru ranks 83rd of 221 countries.
Across the 4 decades both report, Brunei Darussalam averaged higher in 2 and Peru in 2.
Head to head by decade
| Decade | Brunei Darussalam | Peru | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.0022 kt | 0.0009 kt | 0.0013 kt | Brunei Darussalam |
| 2000s | 0.0021 kt | 0.0018 kt | 0.0003 kt | Brunei Darussalam |
| 2010s | 0.0019 kt | 0.0021 kt | 0.0002 kt | Peru |
| 2020s | 0.002 kt | 0.0021 kt | 0.0001 kt | Peru |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland organic soils — emissions, Brunei Darussalam or Peru?
- Peru, at 0.0021 kt against 0.002 kt in Brunei Darussalam as of 2024.
- What is the difference in grassland organic soils — emissions between Brunei Darussalam and Peru?
- 0.0001 kt, with Peru ahead.
- How many years of comparable data are there for Brunei Darussalam and Peru?
- 35 years are reported by both, from 1990 to 2024.
- How do Brunei Darussalam and Peru rank globally for grassland organic soils — emissions?
- Brunei Darussalam ranks 84th and Peru ranks 83rd of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Grassland 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.