摘要
秦至南北朝时期,成都城址位于岷江水系二级阶地上。成都秦城由大、少二城东、西并列组成“龟城”形态的主因是缺乏修造土壤和郫江洪水。秦城及内部建筑方位顺应地形,考虑排水和防洪因素,呈北偏东30度偏转。结合考古、文献资料可以大致复原成都秦城城门、墙垣、中壁的位置。成都秦城西垣距郫江尚有距离,南垣距郫江较近,史载其有十八门、周长十二里应属无误。
The site of Chengdu during the Qin to the Northern and Southern dynasties was located on the second terrace of the Min River(岷江)system.The scarcity of construction soil and the floods of the Pi River(郫江)were the main reasons for the formation of the‘Tortoise City’layout of Chengdu's Qin city,which consisted of two cities,the larger and the smaller,arranged side by side to the east and west.The orientation of the Qin city and its internal structures followed the natural terrain,with a deliberate inclination of about 30 degrees northeast to facilitate drainage and flood control.By combining archaeological and documentary evidence,the approximate positions of the gates,walls,and central partitions of Chengdu's Qin city can be reconstructed.The western wall of Chengdu's Qin city was a considerable distance from the Pi River,while the southern wall was closer.The historical records mentioning 18 gates and a circumference of twelve li are considered accurate.
作者
伍磊
Wu Lei(College of Literature and Journalism,Chengdu University,Chengdu 610106,China)
出处
《历史地理研究》
CSSCI
2024年第4期89-101,150,共14页
The Chinese Historical Geography
基金
2024年度四川省哲学社会科学基金青年项目“唐五代宋时期成都城市治理研究”(SCJJ24ND194)。
关键词
成都
秦城
城市形态
Chengdu
Qin City
urban morphology
