Rediscovering the Yellow River and the Yangtze River: the Circulation of Discourses on the North–South Dichotomy between Late Qing China and Meiji Japan

2019 ◽  
Vol 16 (1) ◽  
pp. 33-51
Author(s):  
Fei Chen

AbstractMany novels, poems, and academic works produced in the last decades of Qing China were characterized by a structure of North–South dichotomy. While existing studies have investigated the root of this narrative structure in Chinese traditions, this article tries to uncover Japan's lesser-known role in the revitalization of traditional discourses. It first discusses how Japanese intellectuals, such as Shiga Shigetaka and Naitō Konan, reconfigured Chinese discourses on the North–South dichotomy as theories to assert Japan's superiority over China. It goes on to examine how Liang Qichao appropriated Japanese theories to mobilize southern Chinese to participate in state politics. It then explores how Chinese revolutionary students in Japan exploited Japanese intellectuals’ and Liang's discourses to promote a cross-provincial consciousness by representing China as a river-based region writ large. Lastly, it reveals how the restructured discourses on the North–South dichotomy were manipulated by revolutionaries after they flowed back to China.

2014 ◽  
Vol 577 ◽  
pp. 1185-1188 ◽  
Author(s):  
Jun Chen

The study area was located in central coast of Jiangsu Province, China. The coast between Wanggang estuary and Chuandonggang estuary belonged to a typical accumulation muddy coast. When the Yellow River flowed into the Yellow Sea using the Huai River course, the coast deposited rapidly and the coastline advanced to the sea about 60 km. The deposition source stopped after the Yellow River returned to the north and flowed into the Bohai Sea. The entral coast of Jiangsu still maintained a high deposition rate in the supratidal zone because of the erosion supply of the abandoned Yellow River delta. But the subtidal zone was in the erosion state. The coast entered into the adjustment period in the 21st century and showed the equilibrium of the erosion and deposition. In recent years, the supratidal area decreased because of the reclaimation. The living space of the salt marshes was limited. The reclamation potentiality will be limited too in the future.


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