Isle of Man vs Kazakhstan: Cropland organic soils — Emissions
Isle of Man
0.0009 kt
in 2024
Kazakhstan
0.001 kt
in 2024
Isle of Man rank
98th
Kazakhstan rank
96th
Cropland organic soils — Emissions over time
- Isle of Man
- Kazakhstan
How they compare
Kazakhstan currently reports 0.001 kt against 0.0009 kt in Isle of Man, a difference of 0.0001 kt.
That makes Kazakhstan's figure about 1.1 times Isle of Man's.
Across all 33 years both countries report, Kazakhstan has been ahead every year.
Isle of Man ranks 98th and Kazakhstan ranks 96th of 221 countries.
Kazakhstan has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Isle of Man | Kazakhstan | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.0007 kt | 0.0017 kt | 0.001 kt | Kazakhstan |
| 2000s | 0.0007 kt | 0.0027 kt | 0.002 kt | Kazakhstan |
| 2010s | 0.0009 kt | 0.0025 kt | 0.0016 kt | Kazakhstan |
| 2020s | 0.0009 kt | 0.001 kt | 0.0001 kt | Kazakhstan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, Isle of Man or Kazakhstan?
- Kazakhstan, at 0.001 kt against 0.0009 kt in Isle of Man as of 2024.
- What is the difference in cropland organic soils — emissions between Isle of Man and Kazakhstan?
- 0.0001 kt, with Kazakhstan ahead.
- How many years of comparable data are there for Isle of Man and Kazakhstan?
- 33 years are reported by both, from 1992 to 2024.
- How do Isle of Man and Kazakhstan rank globally for cropland organic soils — emissions?
- Isle of Man ranks 98th and Kazakhstan ranks 96th 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.