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The impact of grazing intensity on soil characteristics of Stipa grandis and Stipa bungeana steppe in northern China (autonomous region of Ningxia)

机译:放牧强度对中国北方(宁夏自治区)大针茅和布氏针茅草原土壤特性的影响

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The effects of grazing intensity on selected soil characteristics in the feather-grass steppes of the autonomous region of Ningxia (northern China) were investigated by a comparison of non-grazed areas (grazing intensity 0), slightly grazed areas (grazing intensity 1), moderately grazed areas (II), intensively grazed areas (III) and over-grazed areas (IV). Even in areas used only minimally for grazing activities (1), a serious increase (doubling) in soil hardness was apparent in the upper soil layer. A continual decrease in organic matter in the surface soil can be correlated directly to soil compaction. The content of organic matter in soil of degree IV amounts to only a third of the organic matter found in non-grazed areas. This decrease can be attributed partly to the poor living conditions for soil organisms in compacted soils, but also to a significant reduction in litter. This is because intensive grazing causes reduced vegetation cover leading to litter being blown away by wind or washed away by heavy rainfall. Thus in level III hardly any plant litter remained to be incorporated into the soil as humus. Likewise root density also suffered its largest decrease in areas with a grazing intensity level III. With regard to the content of nitrogen and phosphorous (total and available) hardly any difference between soils of grazing intensity 0 and I was observed, whereas a noticeable decrease was apparent between levels I and II. Available Potassium was similar for all grazing levels. The pH-value of the soil solution is not significantly affected by grazing. We did not observe differences in the soils of the two main types of steppe vegetation (Stipa grandis and Stipa bungeana steppe) in response to grazing. Only the amount of litter in the S. grandis-steppe in non-grazed or slightly grazed areas is noticeably higher than in the S. bungeana steppe. (C) 2004 Elsevier SAS. All rights reserved.
机译:通过比较非放牧区(放牧强度为0),轻度放牧区(放牧强度为1),非放牧区(放牧强度为0)对放牧强度对宁夏(中国北部)羽毛草草原某些土壤特性的影响。中度放牧区(II),中度放牧区(III)和过度放牧区(IV)。即使在仅用于最小程度放牧活动的地区(1),在上层土壤中土壤硬度也明显增加(翻倍)。表层土壤中有机物的持续减少可以直接与土壤压实相关。 Ⅳ级土壤中有机物的含量仅为非格拉茨地区发现的有机物的三分之一。减少的部分原因可归因于压实土壤中土壤生物的恶劣生活条件,也可归因于凋落物的大量减少。这是因为密集的放牧会导致植被减少,导致垃圾被风吹走或被大雨冲走。因此,在第三级中,几乎没有任何植物凋落物以腐殖质的形式掺入土壤中。同样,在放牧强度等级为III的地区,根系密度也经历了最大的下降。关于氮和磷的含量(总和有效),在放牧强度0和I的土壤之间几乎未观察到任何差异,而在水平I和II之间则明显下降。所有放牧水平的有效钾含量都相似。放牧对土壤溶液的pH值影响不大。我们没有观察到两种主要类型的草原植被(Stipa grandis和Stipa bungeana草原)对放牧的土壤差异。在非放牧或轻度放牧的地区,只有S. grandis草原的凋落物数量明显高于S. bungeana草原。 (C)2004 Elsevier SAS。版权所有。

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