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从中国东北三江平原地表温度的角度看稻田的变化及其对人类福祉的影响。

Change of Rice Paddy and Its Impact on Human Well-Being from the Perspective of Land Surface Temperature in the Northeastern Sanjiang Plain of China.

机构信息

School of Geography and Tourism, Qufu Normal University, Rizhao 276826, China.

Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

出版信息

Int J Environ Res Public Health. 2022 Aug 6;19(15):9690. doi: 10.3390/ijerph19159690.

Abstract

Large-scale and high-speed paddy land expansion has appeared in Northeast China since the 21st century, causing the change in land surface temperature. The lack of continuous investigation limits the exploration of discoveries in this region. To address this limitation, a collaborative approach that combined human-computer interaction technology, gravity center model and spatial analysis was established. It provided some new findings in spatiotemporal evolution, migration trajectory and surface cooling effect of the paddy field in Northeastern Sanjiang Plain, a center of paddy field planting in China. The results show that: (1) A sustained paddy expansion was monitored, with a total area ranging from 2564.58 km to 11430.94 km, along with a rate of growth of 345.72% from 2000 to 2020. Correspondingly, its reclamation rate changed to 47.53% from 10.66%, showing the improved planting level of the paddy field. (2) Gravity center of paddy field continued to be revealed northward with a 5-year interval from 2000 to 2020. Migration distance of the straight line reached 23.94 km, with the direction offset of 27.20° from east to north. (3) Throughout the growing season of crops, the land surface temperature of paddy field was 27.73°, 29.38°, 27.01°, 25.62° and 22.97° from May to October; and the cooling temperature effect of paddy field was investigated, with the reduced values of 0.61°, 0.79° and 1.10° in the low-, medium- and high-paddy field density regions from 2000 to 2020, respectively. Overall, these new findings in the cold temperate zone, high latitude region of the Northern Hemisphere, provided the reference for the investigation of paddy field monitoring and its environmental effects in China and other regions.

摘要

自 21 世纪以来,中国东北地区出现了大规模、高速的水田扩张,导致地表温度发生变化。由于缺乏连续的调查,限制了对该地区发现的探索。为了解决这个限制,采用了一种结合人机交互技术、重心模型和空间分析的协作方法,为中国三江平原水田种植中心的水田时空演变、迁移轨迹和表面冷却效应提供了一些新的发现。结果表明:(1)监测到持续的水田扩张,总面积从 2000 年的 2564.58 平方公里到 2020 年的 11430.94 平方公里,增长率为 345.72%。相应地,其开垦率从 10.66%变为 47.53%,表明水田种植水平有所提高。(2)2000 年至 2020 年,水田重心以 5 年为间隔持续向北移动。直线迁移距离达到 23.94 公里,从东到北的方向偏移为 27.20°。(3)在整个作物生长季节,水田的地表温度从 5 月到 10 月分别为 27.73°C、29.38°C、27.01°C、25.62°C 和 22.97°C;调查了水田的冷却温度效应,2000 年至 2020 年,低、中、高水田密度区的降温值分别为 0.61°C、0.79°C 和 1.10°C。总的来说,这些在北半球寒温带、高纬度地区的新发现为中国和其他地区的水田监测及其环境效应的调查提供了参考。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5f1/9368393/36fa23f3e58d/ijerph-19-09690-g001.jpg

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