Nanjing University, Nanjing, China.
Ambio. 2012 Nov;41(7):682-98. doi: 10.1007/s13280-012-0290-5. Epub 2012 Jun 5.
We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops, critical thresholds of natural processes, and abrupt transitions caused by socio-economic factors. Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embarkment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river.
我们通过调查历史文献和流域环境变化的定量时间序列数据,分析了黄河下游 4000 年的洪水历史和中游地区的农业发展历史。洪水动态的特点是正反馈循环、自然过程的临界阈值以及社会经济因素引起的突然转变。技术和组织创新是洪水历史的主要驱动因素。公元前 4 世纪铁犁的普及和黄河下游的淤高启动了决堤的正反馈循环。反馈循环的强度因粗泥沙产沙区的耕种、陡坡耕种以及新的河流管理范式而增强,最终在 17 世纪将洪水频率推向了顶峰。河流动力学与中国社会的共同演化引人注目,特别是中游地区的农业和土壤侵蚀以及下游地区的中央权威和河流管理。