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青藏高原高寒沙地沙丘中间锦鸡儿人工林建立后土壤养分的空间异质性

Spatial Heterogeneity of Soil Nutrients after the Establishment of Caragana intermedia Plantation on Sand Dunes in Alpine Sandy Land of the Tibet Plateau.

作者信息

Li Qingxue, Jia Zhiqing, Zhu Yajuan, Wang Yongsheng, Li Hong, Yang Defu, Zhao Xuebin

机构信息

Institute of Desertification Studies, Chinese Academy of Forestry, Beijing, 100091, China.

Research Institute of Forestry, Chinese Academy of Forestry, Beijing 100091, China.

出版信息

PLoS One. 2015 May 6;10(5):e0124456. doi: 10.1371/journal.pone.0124456. eCollection 2015.

Abstract

The Gonghe Basin region of the Tibet Plateau is severely affected by desertification. Compared with other desertified land, the main features of this region is windy, cold and short growing season, resulting in relatively difficult for vegetation restoration. In this harsh environment, identification the spatial distribution of soil nutrients and analysis its impact factors after vegetation establishment will be helpful for understanding the ecological relationship between soil and environment. Therefore, in this study, the 12-year-old C. intermedia plantation on sand dunes was selected as the experimental site. Soil samples were collected under and between shrubs on the windward slopes, dune tops and leeward slopes with different soil depth. Then analyzed soil organic matter (SOM), total nitrogen (TN), total phosphorus (TP), total potassium (TK), available nitrogen (AN), available phosphorus (AP) and available potassium (AK). The results showed that the spatial heterogeneity of soil nutrients was existed in C. intermedia plantation on sand dunes. (1) Depth was the most important impact factor, soil nutrients were decreased with greater soil depth. One of the possible reasons is that windblown fine materials and litters were accumulated on surface soil, when they were decomposed, more nutrients were aggregated on surface soil. (2) Topography also affected the distribution of soil nutrients, more soil nutrients distributed on windward slopes. The herbaceous coverage were higher and C. intermedia ground diameter were larger on windward slopes, both of them probably related to the high soil nutrients level for windward slopes. (3) Soil "fertile islands" were formed, and the "fertile islands" were more marked on lower soil nutrients level topography positions, while it decreased towards higher soil nutrients level topography positions. The enrichment ratio (E) for TN and AN were higher than other nutrients, most likely because C. intermedia is a leguminous shrub.

摘要

青藏高原共和盆地地区受荒漠化影响严重。与其他荒漠化土地相比,该地区的主要特点是多风、寒冷且生长季节短,导致植被恢复相对困难。在这种恶劣环境下,识别植被建立后土壤养分的空间分布并分析其影响因素,将有助于理解土壤与环境之间的生态关系。因此,在本研究中,选择沙丘上12年生的中间锦鸡儿人工林作为试验地。在迎风坡、沙丘顶部和背风坡不同土壤深度的灌木下及灌木之间采集土壤样本。然后分析土壤有机质(SOM)、全氮(TN)、全磷(TP)、全钾(TK)、有效氮(AN)、有效磷(AP)和有效钾(AK)。结果表明,沙丘中间锦鸡儿人工林中土壤养分存在空间异质性。(1)深度是最重要的影响因素,土壤养分随土壤深度增加而降低。一个可能的原因是风吹来的细颗粒物质和凋落物积累在表层土壤上,当它们分解时,更多的养分聚集在表层土壤上。(2)地形也影响土壤养分分布,更多的土壤养分分布在迎风坡。迎风坡的草本覆盖度较高,中间锦鸡儿地径较大,这两者可能都与迎风坡较高的土壤养分水平有关。(3)形成了土壤“肥沃岛”,在土壤养分水平较低的地形位置“肥沃岛”更为明显,而在土壤养分水平较高的地形位置则降低。TN和AN的富集率(E)高于其他养分,最有可能是因为中间锦鸡儿是一种豆科灌木。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8763/4422674/cc15a4be0f8b/pone.0124456.g001.jpg

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