水稻土的排水及其意义
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DRAINAGE OF PADDY SOILS AND ITS SIGNIFICANCE
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    摘要:

    我国种植水稻的历史十分悠久,种植面积亦甚广.水稻土遍及全国,南起热带的海南岛,北至寒温带的黑龙江,东自台湾省,西到新疆、西藏自治区,总面积约三亿九千万亩.据1980年的统计[3],1979年水稻种植面积占全国粮食播种总面积的28.4%.

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    In China the paddy yield per unit area varies from 4-5 times between the lowest and the highest.In order to low-yield paddy soils,protinote their fertility and increase the rice yield,it is primarily necessary to work out a proper drainage project in paddy Field.end to lower,the ground water table so as to fundamentally improve the aeration condition in the root-layer of paddy soil.The higher rnntrnt of organic matter in paddy soil is related to the poor water regiame,hawing nothing to do avith the fertility level.The effect of soil organic matter on the iinprovetrient of physical properties of paddy soil is conditional.For the clayey soils of,low-yield and those located in lowland,only by ameliorating their poor water regime can the organic matter be brought into full play.For the well-drained paddy soils,the effect of organic matter on physical properties of the soil is remarkable.

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程云生.水稻土的排水及其意义[J].土壤学报,1983,20(3):214-224. Cheng Yunsheng. DRAINAGE OF PADDY SOILS AND ITS SIGNIFICANCE[J]. Acta Pedologica Sinica,1983,20(3):214-224.

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  • 在线发布日期: 2013-02-25
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