- 【Updated on May 12, 2025】 Integration of CiNii Dissertations and CiNii Books into CiNii Research
- Trial version of CiNii Research Automatic Translation feature is available on CiNii Labs
- Suspension and deletion of data provided by Nikkei BP
- Regarding the recording of “Research Data” and “Evidence Data”
Greenhouse gases from early flooded organic paddy field
-
- YOSHIDA Kouhei
- Graduate school of Dairy Science, Rakuno Gakuen University
-
- SHIMIZU Hikari
- Graduate school of Dairy Science, Rakuno Gakuen University
-
- IZUMI Kaho
- College of Agriculture, Food and Environment Sciences, Rakuno Gakuen University
-
- SAWAMOTO Takuji
- Graduate school of Dairy Science, Rakuno Gakuen University College of Agriculture, Food and Environment Sciences, Rakuno Gakuen University
-
- YOSHIDA Osamu
- Graduate school of Dairy Science, Rakuno Gakuen University College of Agriculture, Food and Environment Sciences, Rakuno Gakuen University
Bibliographic Information
- Other Title
-
- 早期湛水水田における温室効果気体の動態
- ソウキ タンスイ スイデン ニ オケル オンシツ コウカ キタイ ノ ドウタイ
Search this article
Description
Methane (CH4) and nitrous oxide (N2O) are greenhouse gases; further, paddy fields are one of the anthropogenic sources of CH4. In particular, “Fuyumizu-tambo,” an early flooded organic paddy field, is known to be the primary source of CH4. Thus, we observed CH4 and N2O emissions using the chamber method in the “Fuyumizu-tambo” customary paddy fields from 2013 to 2014 at Bibai City, Hokkaido, Japan. Thus, a relation could be observed between the soil’s degree of dryness during mid-summer drainage, which is a CH4 release-inhibiting period; furthermore, CH4 was observed to be slightly released until the soil became completely dry. Because of the water retentivity of the “torotoro layer,” a type of soil containing abundant organic matter content owing to the stirring action of worm fish, drying is difficult, which results in the formation of an oxidation-reduction border domain. Therefore, the release of CH4 is easy owing to the “torotoro layer.” In addition, although the abundant nitrogen content of the “torotoro layer” inhibited CH4 emission, N2O emission is not correlated to the total nitrogen (TN) concentration of the “torotoro layer,” and hence, nitrogen content directly does not cause N2O production. Therefore, controlling the water retentivity and TN concentration of the “torotoro layer” could suppress CH4 and N2O emissions from the paddy fields.
Journal
-
- Wetland research
-
Wetland research 10 (0), 67-78, 2020
Japan Wetland Society
- Tweet
Details 詳細情報について
-
- CRID
- 1390285300181861760
-
- NII Article ID
- 130007886577
- 120007193525
-
- NII Book ID
- AA12606426
-
- ISSN
- 24341762
- 21854238
-
- HANDLE
- 10659/00007015
-
- NDL BIB ID
- 030539776
-
- Text Lang
- ja
-
- Article Type
- journal article
-
- Data Source
-
- JaLC
- IRDB
- NDL Search
- CiNii Articles
-
- Abstract License Flag
- Disallowed