青海高山草甸土的形成及其肥力评价
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FORMATION AND FERTILITY OF THE ALPINE MEADOW SOIL IN QINGHAI PROVINCE
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    摘要:

    青海为全国五大牧区之一.高山草甸土是其重要的草场土壤,分布十分广泛.高山草甸土的形成、性状和变化,直接影响草场生产力的高低和植被演替,并间接影响畜牧业生产的发展.现将初步调查研究的结果,总结汇报如后.

    Abstract:

    Alpine meadow soil is widely spread in tha South Qinghai Plateau and partly distributed in Haibei,Hainan and Huangnan regions on the Qinghai-Tibet Plateau.Alpine meadow soil,being the principal soil of the range is situated in the regions of 4,000-4,700 metres above sea level on the South Qinghai Plateau,and 3,300-4,000 metres in other regions respectively.It develops under the conditions of cold semihumid mountainous climate with mean annual air temperature of 0-5.7℃ and precipitation of 270-550 mm.Its predominant vegetative cover is Kobresia pygmaea.Such distribution may be considered as a result of the influence by the combined actions of horizontal and vertical zonality.

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左克成,乐炎舟.青海高山草甸土的形成及其肥力评价[J].土壤学报,1980,17(4):308-318. Zuo Ke-cheng, Le Yan-zhou. FORMATION AND FERTILITY OF THE ALPINE MEADOW SOIL IN QINGHAI PROVINCE[J]. Acta Pedologica Sinica,1980,17(4):308-318.

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  • 在线发布日期: 2013-02-25
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