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Subsidence of rice paddy and upland crop fields in Shinotsu Peatland, Hokkaido, Japan

机译:稻田稻田和高地庄稼领域的沉降在Shinotsu Peatland,北海道,日本

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Agricultural land use on peatlands inevitably causes ongoing land surface subsidence resulting in a reduction of productivity. In addition, oxidation of the peat substrate associated with subsidence is responsible for greenhouse gas emission with the ensuing consequence for global climatic stability. A concept of "paludi-culture", the utilisation of wet or rewetted peatlands for agriculture, has been proposed in European countries to avoid further subsidence and greenhouse gas emission. However, few studies have documented a long-term record of subsidence through agriculture in wet peatlands such as paddy fields for rice cultivation. In this study, we measured the subsidence rates of peatland in rice paddy use and compared them to the rates in peatland with upland crop cultivation. The average subsidence between 2006 and 2016 for the paddy plots was 3.6 ± 1.9 cm (± SE) and significantly less than that of 25.6 ± 1.7 cm for the upland plots, and the subsidence reduced linearly as the period of paddy use increased. These results suggest that paddy use of peatlands can effectively reduce subsidence. Our results will encourage the use of peatlands with a wet environment as one of the valid options for future peatland management in terms of mitigation of land subsidence and peat loss.
机译:泥炭地的农业用地使用不可避免地导致持续的陆地表面沉降导致生产力降低。此外,与沉降相关的泥炭基材的氧化是对全球气候稳定性的随后导致温室气体排放。在欧洲国家提出了欧洲国家的“Paludi文化”,利用湿润或湿润的泥炭块的概念,以避免进一步的沉降和温室气体排放。然而,很少有研究已经记录过湿法泥炭地区的农业长期记录,例如水稻种植稻田。在这项研究中,我们测量了泥炭地在水稻稻田使用中的沉降率,并将其与高地农作物栽培的泥炭地汇率进行了比较。对于麦地板的2006和2016之间的平均沉降为3.6±1.9厘米(±SE),对于高于地图,显着小于25.6±1.7厘米,随着稻田的时期增加,沉降率为线性降低。这些结果表明,泥浆使用泥炭地可以有效地减少沉降。我们的结果将鼓励使用湿地使用污染物环境作为未来泥炭地管理的有效选项之一,以减轻土地沉降和泥炭损失。

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