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Evaluation of the effect of groundwater condition on water and salinity stresses at crop field in Isahaya Central Polder, Japan

机译:日本Isahaya Central Bolder在田间田间水土条件对水土条件影响的评价

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More than 70% of Japanese lands are classified as mountainous or hill slope land. Particularly the Nagasaki prefecture located in the south-west of Japan is well-known for its fields with steep slopes. A project to reclaim the Isahaya Bay in Nagasaki prefecture and develop prime and large-scale agricultural lands has been conducted. Cultivation in the newly reclaimed land known as Isahaya Central polder started in 2008. As the crop fields in Isahaya Central polder are flat and large-scale, agricultural productivity and farming efficiency is relatively high. However serious concerns exist on future cultivation in Isahaya Central polder because plans are made to open the gates of the reclamation dike because of seaweed crop failure. Although the present soil conditions in the root zone have been improved and agricultural productivity has been increased, the crop stress due to salinity is concerned after opening gates because of groundwater salinization. The aim of this study is to evaluate of the effect of the groundwater salinization on crop fields. A simulation model describing the soil water and solute transports was introduced. Model accuracy was verified by field observation conducted in Isahaya Central polder. The stresses due to wetness, drought and salinity were evaluated under the scenarios of groundwater salinization and drought year. Simulated result indicated that groundwater salinization produced the salinity stress and the effect was marked on the deep-rooted crops. The groundwater salinization in the drought year had significant impact on not only deep-rooted crops but also shallow-rooted crops.
机译:超过70%的日本土地被归类为山区或山坡山坡土地。特别是位于日本西南部的长崎县以其陡峭的斜坡而闻名。已经进行了一个项目,在长崎县举办Isahaya湾,并进行了发展素线和大规模农业土地。被称为Isahaya Central Bolder的新开垦土地的培养于2008年。随着Isahaya中央圩区的作物领域是平坦的,农业生产力和农业效率相对较高。然而,由于海藻作物失败,在未来的Isahaya Central Bolder中未来修炼存在严重担忧。虽然根部区域的土壤条件已经提高,但农业生产力增加,由于地下水盐渍化打开门后由于盐度引起的作物应力。本研究的目的是评估地下水盐渍化对田间的影响。引入了描述土壤水和溶质转运的仿真模型。通过在Isahaya Central Bolder中进行的现场观察验证了模型精度。根据地下水盐渍化和干旱年度的情况评估了由于湿度,干旱和盐度引起的应力。模拟结果表明,地下水盐渍化产生了盐度应力,并且效果标记在根深蒂固的作物上。干旱年份的地下水盐渍化对不仅对根深蒂固的作物而且浅根作物产生重大影响。

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