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首页> 外文期刊>International Soil and Water Conservation Research >Advances in the prognosis of soil sodicity under dryland irrigated conditions
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Advances in the prognosis of soil sodicity under dryland irrigated conditions

机译:旱地灌溉条件下土壤钠盐预后的研究进展

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Salt-affected soils, both saline and sodic, may develop under both dryland and irrigated conditions,affecting the physical and chemical soil properties, with negative consequences in the environment, in cropproduction and in animal and human health. Among the development processes of salt-affected soils, theprocesses of sodification have generally received less attention and are less understood than thedevelopment of saline soils. Although in both, hydrological processes are involved in their development, inthe case of sodic soils we have to consider some additional chemical and physicochemical reactions,making more difficult their modeling and prediction. This is especially true where we have to consider theeffects of the groundwater level and composition. In this contribution there are presented three case studies:one related to the development of sodic soils in the lowlands of the Argentina Pampas, under dry-landconditions with sub-humid temperate climate and pastures for cattle production; the second deals with thedevelopment of sodic soils in the Colombia Cauca Valley, under irrigated conditions and tropical sub-humidclimate, in lands used for sugarcane cropping dedicated to sugar and ethanol production; and the last onerelated to the sodification of soils in the Western Plains of Venezuela, under irrigated conditions, sub-humidtropical climate and continuous cropping of rice under flooding. The development of sodicity in the surfacesoil is partially related to the composition and level of the ground-water, mainly affected in the Argentinacase by drainage conditions, in the case of Colombia to the inefficient irrigation and inadequate drainage,and in the case of Venezuela to the soil management and irrigation system. There is shown how the modelSALSODIMAR, developed by the author, based on the balance of water and soluble components of bothirrigation water and ground-water, under different water and land management conditions, may besuccessfully adapted for the diagnosis and prediction of the different processes and problems, and forselection of alternatives for their prevention and amelioration.
机译:受盐和盐分影响的土壤,无论是盐水还是苏打水,都可能在旱地和灌溉条件下生长,影响土壤的物理和化学性质,对环境,作物生产以及动物和人类健康产生负面影响。在盐渍土的发育过程中,与盐渍土的发展相比,酸化过程通常受到较少的关注和了解。尽管两者都参与了水文过程的发展,但在钠土的情况下,我们必须考虑一些其他的化学和物理化学反应,这使它们的建模和预测更加困难。当我们必须考虑地下水位和组成的影响时尤其如此。在这项贡献中,提出了三个案例研究:一个与阿根廷潘帕斯低地的苏打土壤发展有关,干旱条件下为半湿润的温带气候和牧场,用于生产牛;第二部分涉及在灌溉条件和热带亚湿润气候下,在哥伦比亚考卡山谷中的钠盐土壤的开发,这些土地用于种植甘蔗,专门用于生产糖和乙醇;最后一个与委内瑞拉西部平原的土壤增湿有关,包括灌溉条件,亚湿润气候和洪水下的水稻连作。地表土壤中碱度的发展部分与地下水的组成和水位有关,主要在阿根廷受到排水条件的影响,在哥伦比亚则是灌溉效率低下和排水不充分的情况,在委内瑞拉则是土壤管理和灌溉系统。展示了作者在不同水和土地管理条件下基于灌溉水和地下水的水和可溶性成分的平衡而开发的SALSODIMAR模型如何成功地适用于不同过程的诊断和预测,以及问题,并为预防和改善选择替代方案。

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