黄土高原农业耕作历史与水土流失的关系
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国家自然科学基金资助项目


Relationship between the history and present condition of agricult; ire cultivation and loss of soil and water an the Loess Plateau
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    摘要:

    本文首次从黄土高原主要耕种土壤、林地土壤的入渗和抗冲等物理特性出发,对黄土高原森林草原与农业耕作的历史变迁和近30年来毁林毁草耕作与水土流失的关系作了综合研究。给果认为,长期农业开荒耕作造成犁底层的形成,是黄土高原水土流失加剧的主要原因;在黄土高原加速恢复植被,则是实现“全部降水就地入渗拦蓄”,根治黄河后患唯一有效的治本途径。

    Abstract:

    The relationship between changes of history and the present condition of forest and grasslands and the loss of soil and water on the Loess Plateau is comprehensively studied first in the paper, based on physical properties (e.g.soil infiltration and anti-scouringbility) in the cultivated and forest soils, The study results show that the plough sole resulted from agriculturally protracted cultivation is the main cause of increasing loss of soil and water on the Loess Plateau.Speeding up the renew of vegetation in the region is the only effective approach of all precipitation inFiltrating on the spot and brings the Huanghe River under the permanent control.

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李勇,田积莹,朱显谟.黄土高原农业耕作历史与水土流失的关系[J].水土保持通报,1989,(2):22-26

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  • 在线发布日期: 2014-12-01
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