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. 2012 Jun 5;41(7):682–698. doi: 10.1007/s13280-012-0290-5

Table 1.

Changes in natural and human factors of the Yellow River over historical times

Period Major dynasties Socio-economic changes Middle river Lower river
Population density (persons per km2) Area south of the northern boundary of FGTZ (percentage) Grain yield (kg/ha) Sedimentation rate (mm/a) Number of avulsions Number of breaches Number of river management activities
21st–5th Century bc Xia, Shang, Western Zhou Agriculture, state <38 1–2 1 3
5th Century bc–70 ad Warring States, Qin, Western Han Plow, embankment, the Great wall, centralized imperial state, “farming and fight” military policy <26 38–88 Western Han: 1050 2–4 5 9 7
70 ad–1128 ad Eastern Han, Tang, Northern Song Northern Song: steep hillslop cultivation <36 60–97 Northern Song: 1400–1700 2–20 12 110 144
1128 ad–1855 ad Ming, Qing River control paradigm “restrict the current to attack the silt,” river management system 36–80 80–100 450–1000 20–30 40 419 1018
1855 ad–the present Qing, PRC Damming, industrialization, agricultural modernization 80–235 100 1000–3000 30–200 1 96 2120

Historical population densities in the middle river are estimated by dividing registered population sizes (Fig. 3c) by the middle basin areas south of the northern boundary of FGTZ in different periods (Fig. 5). Grain yields in the middle river are estimates on the basis of accounts in The Twenty-five Histories (Perkins and Wang 1969; Ning et al. 1999). The sedimentation rates of the lower river channel are after Xu (1998, 2003). The number of avulsions is the total number of historical records of natural and artificial avulsions; the number of breaches is the total number of historical records of natural and artificial breaches. The number of the river management activities is the sum of historical records of “construction” and “regulation”