中国农业科学 ›› 2020, Vol. 53 ›› Issue (12): 2435-2449.doi: 10.3864/j.issn.0578-1752.2020.12.011

• 土壤肥料·节水灌溉·农业生态环境 • 上一篇    下一篇

中国北方新增耕地的时空变化及驱动因素分区

王鸣雷1,2,史文娇1,2()   

  1. 1 中国科学院地理科学与资源研究所陆地表层格局与模拟院重点实验室,北京 100101;
    2 中国科学院大学资源与环境学院,北京 100049
  • 收稿日期:2019-08-26 出版日期:2020-06-16 发布日期:2020-06-25
  • 通讯作者: 史文娇
  • 作者简介:王鸣雷,E-mail:wangml.18s@igsnrr.ac.cn。
  • 基金资助:
    中国科学院战略性先导科技专项(XDA23100202);国家自然科学基金(41771111);中国科学院地理科学与资源研究所优秀青年人才基金(2016RC201);中国科学院青年创新促进会(会员号:2018071)

Spatial-Temporal Changes of Newly Cultivated Land in Northern China and Its Zoning Based on Driving Factors

WANG MingLei1,2,SHI WenJiao1,2()   

  1. 1 Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101;
    2 College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049
  • Received:2019-08-26 Online:2020-06-16 Published:2020-06-25
  • Contact: WenJiao SHI

摘要:

【目的】新增耕地的时空变化格局受气候变化和人类活动的双重影响,明确新增耕地时空格局变化及其驱动因素,为保障耕地资源和农业可持续发展提供指导。【方法】基于1980s—1990s、1990s—2000s、2000s—2010s 3个时段中国北方的新增耕地数据,利用重心转移模型和区域统计等方法,探讨中国北方新增耕地的重心变化以及时空格局变化;基于气候数据计算3个时段≥10 ℃积温(AAT10)以及标准化降水蒸散指数(SPEI),分析气候因素对耕地开垦的驱动作用;基于1980s以来的社会经济统计数据,结合空间叠加模型、区域统计模型等分析人为因素对耕地开垦的促进作用;综合气候和人为因素,结合地理分区的方法对中国北方的新增耕地进行分区。【结果】1980s以来,中国北方新增耕地重心呈现由东北向西北转移的态势;大多数耕地开垦地区的气候有暖干化趋势,2000年以来具有暖湿趋势的耕地开垦区比例逐渐增加;农业为主人口的增加、农业技术进步以及国家政策的影响为东北、新疆等地耕地资源扩张提供了必要的基础;新疆、黑龙江、吉林等地丰富的耕地后备资源以及平坦的地势条件为耕地开垦提供了可能;基于对气候和人为驱动因素分析,将中国北方分为7个分区,即东北北部气候驱动林草-耕地转换区、东北气候+人为驱动林草-耕地转换区、东北中部气候+人为驱动水旱转换区、北方气候+人为驱动林草-耕地转换区、黄土高原人为驱动生态恢复区、西北人为驱动荒地-耕地转换区以及新疆人为驱动绿洲农业开垦区。【结论】1980s以来,中国北方新增耕地时空格局表现出明显的差异性;暖干气候并未成为耕地开垦的限制因素,而较为湿润的气候在一定程度上促进了耕地的开垦;农业人口的增加、农业技术的进步以及国家政策的影响,对耕地开垦起到重要作用。

关键词: 中国北方, 新增耕地, 土地利用变化, 气候变化, 驱动因素

Abstract:

【Objective】 The spatial and temporal change pattern of newly cultivated land is affected by both climate change and human activities. It is important to clarify the spatial and temporal change pattern of newly cultivated land and its driving factors to ensure the sustainable development of cultivated land resources and agriculture. 【Method】 Based on the data of newly cultivated land in north China of 1980s-1990s, 1990s-2000s and 2000s-2010s, the spatial-temporal changes of newly cultivated land in north China were analyzed by using gravity model and regional statistics; Based on the climate data of the three times, we calculated the active accumulated temperature (≥10℃, AAT10) and the standardized precipitation evapotranspiration index (SPEI), and analyzed the driving effect of climatic factors on cultivated land reclamation; Based on the socio-economic statistics since the 1980s, the paper analyzed the promotion of human factors on cultivated land reclamation by combining spatial superposition model and regional statistical model; Based on the combination of climatic and human factors and the method of geographical subdivision, the new cultivated land in north China was subdivided. 【Result】 The center of gravity of new cultivated land in northern China has shifted from northeast to northwest; the most cultivated land reclamation existed in warm and dry climate, but the proportion of cultivated land reclamation occurring in warm and humid climate conditions was gradually increasing; the increase of agricultural population, the advancement of agricultural technology and the influence of national policies provided necessary foundation for the expansion of cultivated land resources in Northeast China and Xinjiang. Abundant cultivated land reserve resources and flat terrain conditions in the Xinjiang, Heilongjiang, Jilin and other regions provided a possibility for land reclamation; based on the climate and human activities factors, the northern China was divided into seven regions, which included the zone of grass to cropland due to climate in Northeast, the zone of forest and grass to cropland due to climate and human activities in north region of Northeast of China, the zone of paddy field to dry land due to climate and human activities in middle region of Northeast, the zone of forest and grass to cropland due to climate and human activities in the North, the zone of ecological restoration dues to human activities in the loess plateau, the zone of unused land to cropland due to human activities in the northwest region, and zone of the oasis agriculture due to human activities in Xinjiang. 【Conclusion】 Since the 1980s, the spatial and temporal patterns of the new cultivated land in northern China showed obvious differences. The warm and dry climate did not become the limiting factor of cultivated land reclamation, but the wetter climate promoted the cultivated land reclamation to some extent. The increase of agricultural population, the progress of agriculture and the influence of national policies played an important role in cultivated land reclamation.

Key words: Northern China, new cultivated land, land use change, climate change, driving factor