也論浦陽江下游的河道變遷
發(fā)布時間：2018-11-13 19:32
【摘要】：浦陽江下游的河道變遷事關(guān)整個浙東地區(qū)的河湖水利體系變遷,研究意義十分重大。關(guān)于浦陽江下游河道歷史時期的流向,歷來有多種不同觀點(diǎn),陳橋驛教授在二十世紀(jì)八十年代推翻明代以來的說法,近年來朱海濱教授通過對史料的再考證,指出陳教授對宋、明地方史料判讀的失誤,否定了其關(guān)于浦陽江下游河道變遷的觀點(diǎn)。朱教授關(guān)于漁浦、臨浦等地名的考辨十分有益于對問題的認(rèn)識,但浦陽江下游河道明中期之前一直東流的觀點(diǎn)可能仍需討論。本文認(rèn)為浦陽江下游在唐代之前西出漁浦,散漫北流,唐后期至南宋時東西分流,南宋至明時主流東入三江口,明后期主道復(fù)歸西流。浦陽江下游河道的流向既受制于蕭紹地區(qū)東西地形地勢的對比,也與錢塘江出海口門的南北擺動密切相關(guān)。從東西地形地勢特點(diǎn)的對比而言,浦陽江西出由西北向匯聚錢塘江,比之迂回曲折而東注入海,比降更大,流速更快,流路則更短。浦陽江這一順直的西北向流路,則取決于其地質(zhì)背景上的地層斷裂線。
[Abstract]:The river channel changes in the lower reaches of Puyang River are of great significance to the changes of river and lake water conservancy systems in the whole eastern Zhejiang. There have always been many different views on the flow of the lower reaches of the Puyang River during the historical period. Professor Chen Qiaoyi overthrew the view of the Ming Dynasty in the 1980s. In recent years, Professor Zhu Haibin has pointed out that Professor Chen's comments on the Song Dynasty are based on a re-examination of historical data. The mistakes in the interpretation of the local historical materials in Ming Dynasty negated his view on the river channel changes in the lower reaches of the Puyang River. Professor Zhu's research on the names of Yupu and Linpu is very helpful to the understanding of the problem, but the point of view that the river in the lower reaches of Puyang River has been flowing eastward until the middle of tomorrow may still need to be discussed. This paper holds that the lower reaches of the Puyang River leave Yupu in the west before the Tang Dynasty, diffuse the north current, split east and west from the late Tang Dynasty to the Southern Song Dynasty, the mainstream flows east into the Sanjiangkou from the Southern Song to the Ming Dynasty, and the main road returns to the west in the latter part of the Ming Dynasty. The flow direction of the lower reaches of the Puyang River is not only restricted by the comparison of the topography between east and west in Xiaoshao area, but also closely related to the north-south swing of the entrance gate of Qiantang River. Compared with the east and west topographic features, the west of Puyang River converges from northwest to Qiantang River, which flows more slowly and eastward into the sea, with faster velocity and shorter flow path. The northwestern flow of Puyang River depends on the stratigraphic fault line in its geological setting.
【作者單位】： 上海師范大學(xué)人文與傳播學(xué)院;
【基金】：國家哲學(xué)社會科學(xué)基金重大項(xiàng)目“中國歷史上的濱海地域研究”的子課題“明清時期濱海地域的環(huán)境、生計、貿(mào)易與社會——以浙江濱海地域?yàn)橹行摹?
【分類號】：K928.6
本文編號：2330220
[Abstract]:The river channel changes in the lower reaches of Puyang River are of great significance to the changes of river and lake water conservancy systems in the whole eastern Zhejiang. There have always been many different views on the flow of the lower reaches of the Puyang River during the historical period. Professor Chen Qiaoyi overthrew the view of the Ming Dynasty in the 1980s. In recent years, Professor Zhu Haibin has pointed out that Professor Chen's comments on the Song Dynasty are based on a re-examination of historical data. The mistakes in the interpretation of the local historical materials in Ming Dynasty negated his view on the river channel changes in the lower reaches of the Puyang River. Professor Zhu's research on the names of Yupu and Linpu is very helpful to the understanding of the problem, but the point of view that the river in the lower reaches of Puyang River has been flowing eastward until the middle of tomorrow may still need to be discussed. This paper holds that the lower reaches of the Puyang River leave Yupu in the west before the Tang Dynasty, diffuse the north current, split east and west from the late Tang Dynasty to the Southern Song Dynasty, the mainstream flows east into the Sanjiangkou from the Southern Song to the Ming Dynasty, and the main road returns to the west in the latter part of the Ming Dynasty. The flow direction of the lower reaches of the Puyang River is not only restricted by the comparison of the topography between east and west in Xiaoshao area, but also closely related to the north-south swing of the entrance gate of Qiantang River. Compared with the east and west topographic features, the west of Puyang River converges from northwest to Qiantang River, which flows more slowly and eastward into the sea, with faster velocity and shorter flow path. The northwestern flow of Puyang River depends on the stratigraphic fault line in its geological setting.
【作者單位】： 上海師范大學(xué)人文與傳播學(xué)院;
【基金】：國家哲學(xué)社會科學(xué)基金重大項(xiàng)目“中國歷史上的濱海地域研究”的子課題“明清時期濱海地域的環(huán)境、生計、貿(mào)易與社會——以浙江濱海地域?yàn)橹行摹?
【分類號】：K928.6
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