Japanese Journal of Southeast Asian Studies
Online ISSN : 2424-1377
Print ISSN : 0563-8682
ISSN-L : 0563-8682
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Hydrography of Rice Land in the Vietnamese Part of the Mekong Delta
Yoshihiro Kaida
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1974 Volume 12 Issue 2 Pages 143-156

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Abstract
 Vietnamese part of the Mekong delta is a wet terrain, being signified by the plentiful monsoonal rainfall with even distribution over the rainy months, and by low lying topography. The delta is, however, subdivided into two parts with respect to the hydrographic conditions, in which the alternation of dry and wet cycles are more pronounced in one region, and less significant in the other. These two classes are solely determined by physiography of the area. Trans-Bassac Plate, Flood Plain and Coastal Flat comprise the former region, and Modern Delta, Broad Depression and Lagoonal Swale belong to the latter category.
 A perfect adaptation of the rice growing methods to the given hydrographic conditions is the character that defines the rice culture of the delta. Rice growing does not rely on [table] the river water, if not at all, but it depends more on rainfall and its localized run-off which is controlled by micro-relief. At the present stage, abundant flow of rivers, creeks and canals which are often perennial being induced by the significant tidal fluctuation of water level in the sea and in the major rivers, are not playing the major role in supplying sufficient water for rice plants at their critical periods, although they are readily usable. However, the river water will have to be tapped to meet the requirement of water for TN rice which is rapidly extending its acreage as the early rainy season's crop as well as the dry season's crop. The possible types of water control and utilization are illustrated in Table 1,in view of giving the favorable conditions to the extended TN rice cultivation in the delta. The characteristics of the present hydrography in the delta are also summarized in the same Table in corresponding to the physiography and the possible types of water control.
 The most parts of the modification of the hydrographic conditions in the area can be achieved by the efforts of individual farmers and of communal level. The government will be required to participate in building major water works that are a prerequisite of those efforts made by communal human powers.
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© 1974 Center for Southeast Asian Studies, Kyoto University
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