China, mainland vs Sweden: Grassland organic soils — Area
China, mainland
59,424 ha
in 2024
Sweden
74,537 ha
in 2024
China, mainland rank
22nd
Sweden rank
21st
Grassland organic soils — Area over time
- China, mainland
- Sweden
How they compare
Sweden currently reports 74,537 ha against 59,424 ha in China, mainland, a difference of 15,113 ha.
That makes Sweden's figure about 1.3 times China, mainland's.
The two have swapped places 1 time across 35 shared years of data; in 1990 it was China, mainland ahead.
China, mainland ranks 22nd and Sweden ranks 21st of 221 countries.
Across the 4 decades both report, China, mainland averaged higher in 2 and Sweden in 2.
Head to head by decade
| Decade | China, mainland | Sweden | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 58,487 ha | 48,807 ha | 9,679 ha | China, mainland |
| 2000s | 58,619 ha | 51,722 ha | 6,897 ha | China, mainland |
| 2010s | 58,743 ha | 60,566 ha | 1,824 ha | Sweden |
| 2020s | 59,426 ha | 74,416 ha | 14,991 ha | Sweden |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland organic soils — area, China, mainland or Sweden?
- Sweden, at 74,537 ha against 59,424 ha in China, mainland as of 2024.
- What is the difference in grassland organic soils — area between China, mainland and Sweden?
- 15,113 ha, with Sweden ahead.
- How many years of comparable data are there for China, mainland and Sweden?
- 35 years are reported by both, from 1990 to 2024.
- How do China, mainland and Sweden rank globally for grassland organic soils — area?
- China, mainland ranks 22nd and Sweden ranks 21st of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Grassland 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.