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Preface: Enduring prosperity for Farmland?

机译:前言:耕地长盛不衰?

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Australian cropping farms have been increasing innproductivity by 3–4% per year for some decades. Theirnprofitability, however, has barely increased during that timenowing to steadily declining terms of trade (Knopke et al.n2000). Burgeoning problems of land degradation, especiallynsalinity, waterlogging, and soil acidity, threaten to restrictnfurther increases in productivity and thence endanger thenprosperity of these farms.nThe causes of these problems are in principle wellnunderstood. The replacement of perennial deep-rooted nativenvegetation by shallow-rooted annual crops has resulted innwetter subsoils with concomitantly larger deep drainage,nleading eventually to rising water tables, waterlogging, andnoften dryland salinity. The removal of nutrient cations,nwhether in harvested products or by leaching as nitrates, is anlarge contributor to falling soil pH in the topsoil and uppernsubsoil.nThe essential difference, hydrologically, between nativenperennial vegetation and winter-active annual crops is that thennatives use substantial amounts of water in the summer, therebyncapturing any water that has drained into the deep subsoilnbelow the effective rooting depth of annual crops. There is littlendifference during the winter growing season in water usenby annual and perennial vegetation. Thus, it has long been advocatednthat deep-rooted perennial pasture species be incorporatedninto cropping systems to tap the water in the deepnsubsoil and thereby help control drainage from croplands.nPhase farming is one such way of incorporatingnperennials into a cropping system. It involves the tacticalnrotation of herbaceous perennial pasture, suitable for grazingnor for hay, with a series of annual crops. The perennialnpasture dries the subsoil below the roots of annual crops,nthereby creating a buffer in which water and nutrients thatnleak below the crops can be held for a few seasons,nremaining largely accessible to the roots of the next phase ofndeep-rooted perennials.nA forum sponsored by the Grains Research andnDevelopment Corporation was held in April 1998 to explorenthe role of phase farming in controlling the deep drainagenthat leads to detrimental rising water tables. Contributions tonthis forum formed the basis of this Journal Issue, whosenterms of reference were extended to include strip farmingnwith the woody species, tagasaste.
机译:在过去的几十年中,澳大利亚的农庄每年一直在提高生产力,每年提高3-4%。然而,在此期间,他们的获利能力几乎没有增加,直到贸易条件稳定下降(Knopke等人,2000年)。土地退化的棘手问题,特别是盐度,涝渍和土壤酸度,有可能限制生产力的进一步提高,并因此危及这些农场的繁荣。多年生的根深蒂固的农作物取代了多年生的根深蒂固的植被,导致了土壤质量更好,随之而来的是深层排水,最终导致地下水位上升,水涝和旱地盐碱化。无论是在收获产品中还是通过作为硝酸盐的浸出去除营养阳离子,都是造成表层土壤和上层土壤中pH下降的重要原因。n从水文角度看,多年生植物和一年生冬季作物之间的本质区别是,移栖植物需要大量使用。夏季浇水,从而使流失到一年生作物有效生根深度以下的深层深层土壤的水无法适应。在冬季生长季节,一年生和多年生植被的用水几乎没有差异。因此,长期以来,人们一直主张将根深蒂固的多年生牧草种纳入耕作系统,以挖掘深层次土壤中的水,从而帮助控制农田的排水。n分阶段耕种是将多年生草种纳入耕作系统的一种方式。它涉及多年生草本植物的多年生草本植物的策略性旋转,适合放牧或干草。多年生牧草将一年生作物根部以下的地下土壤干燥,从而形成一个缓冲带,使渗入作物下的水分和养分可以保持几个季节,而下一季根深蒂固的多年生根部的根部仍难以获得。由谷物研究与开发公司赞助的项目于1998年4月举行,旨在探讨阶段性农业在控制深层排水中的作用,该深层排水会导致地下水位的上升。该论坛的贡献构成了本期杂志的基础,其职权范围已扩展至包括带木本植物的田间耕种。

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