[1]尹玲玲 黄 强.也论浦阳江下游的河道变迁[J].中国农史,2017,36(05):107-118.
　YIN Ling-ling HUANG Qiang.Research on the River Trail Transformation in the Downstream of Puyang[J].SAMSON,2017,36(05):107-118.
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也论浦阳江下游的河道变迁()
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《中国农史》[ISSN:1000-4459/CN:32-1061/S]

卷:
36
期数:
2017年05期
页码:
107-118
栏目:
出版日期:
2017-10-28

文章信息/Info

Title:
Research on the River Trail Transformation in the Downstream of Puyang
作者:
尹玲玲 黄 强
（上海师范大学 人文与传播学院，上海 200234）
Author(s):
YIN Ling-ling HUANG Qiang
（College of Humanities and Communications, Shanghai Normal University,Shanghai 200234）
关键词:
浦阳江;  萧绍平原;  河道变迁;  水利体系
Keywords:
Puyang;  Xiaoshao plains; river trail transformation; water systems
分类号:
S-09；K207
文献标志码:
A
摘要:
浦阳江下游的河道变迁事关整个浙东地区的河湖水利体系变迁，研究意义十分重大。关于浦阳江下游河道历史时期的流向，历来有多种不同观点，陈桥驿教授在二十世纪八十年代推翻明代以来的说法，近年来朱海滨教授通过对史料的再考证，指出陈教授对宋、明地方史料判读的失误，否定了其关于浦阳江下游河道变迁的观点。朱教授关于渔浦、临浦等地名的考辨十分有益于对问题的认识，但浦阳江下游河道明中期之前一直东流的观点可能仍需讨论。本文认为浦阳江下游在唐代之前西出渔浦，散漫北流，唐后期至南宋时东西分流，南宋至明时主流东入三江口，明后期主道复归西流。浦阳江下游河道的流向既受制于萧绍地区东西地形地势的对比，也与钱塘江出海口门的南北摆动密切相关。从东西地形地势特点的对比而言，浦阳江西出由西北向汇聚钱塘江，比之迂回曲折而东注入海，比降更大，流速更快，流路则更短。浦阳江这一顺直的西北向流路，则取决于其地质背景上的地层断裂线。
Abstract:
The river trail transformation in the downstream of Puyang is of great importance to the whole of the water system in Zhedong area, the academic value is extremely significant. Over the years, there have been several opinions on the flow direction of the river in downstream Puyang, Professor Cheng managed to overturn the idea formed since Ming Dynasty during the 1980s, the evidence that Professor Zhu found in historical articles in recent years pointed out the errors of Professor Cheng in his understanding of the localized historical articles during the Song and Ming Dynasty, in turn denying his opinions on the transformation of downstream Puyang. The research that Professor Zhu made on the names of Yupu and Linpu can be very beneficial to the understanding of the problem, but the idea of downstream Puyang flowing toward the east before Mid-Ming Dynasty might still require discussion. This paper believes that downstream Puyang exits Yupu from the west before Tang Dynasty, and spreading out North-ward, later separating in both east and west during the late Tang Dynasty until south Song Dynasty, after that mainly flowing east into Sanjiangko from South Song Dynasty to Ming Dynasty, and in the late-Ming the main course returns to the west. The flow direction of downstream Puyang is both limited by the difference in the landscape of eastern and westernXiaoshao, and closely related to the back and forth movement of the exit to the sea of Qiantang River in southern and northern directions. Comparing the specialty of eastern and western terrains, Puyang exits through the west and flows toward Qiantang River from north-west, and as it makes its way easy into the sea, the more descent it completes, and in turn causing increased flow speed, then making the distance of flow even shorter. As for the straight north-west direction of Puyang, it depends on the fault line in its geological background.

相似文献/References:

[1]耿 金.明中后期浙东河谷平原的湖田水患与水利维持——以诸暨为中心[J].中国农史,2016,35(02):96.
　GENG Jin.The Lake Fields Floods and Water Conservancy Maintenance in the River Valley Plain of the Eastern Zhejiang Province in Late Ming Dynasty——An Analysis of the Zhuji County[J].SAMSON,2016,35(05):96.

备注/Memo

备注/Memo:
[收稿日期] 2017-04-12?
[基金项目] 国家哲学社会科学基金重大项目“中国历史上的滨海地域研究”的子课题“明清时期滨海地域的环境、生计、贸易与社会——以浙江滨海地域为中心”?
[作者简介] 尹玲玲（1973- ），女，上海师范大学人文与传播学院教授，研究方向为历史地理、区域环境史与社会史；黄 强（1987- ），男，上海师范大学2012届历史地理学硕士。
更新日期/Last Update: 1900-01-01