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生态学杂志 ›› 2025, Vol. 44 ›› Issue (7): 2277-2284.doi: 10.13292/j.1000-4890.202507.032

• 研究报告 • 上一篇    下一篇

乌兰布和沙漠不同生境土壤养分分布

牧仁,李新乐,徐光甫,韩进夫,崔健,俞潇,郭俊廷,辛智鸣*   

  1. (中国林业科学研究院沙漠林业实验中心/内蒙古磴口荒漠生态系统定位观测研究站, 内蒙古巴彦淖尔 015200)
  • 出版日期:2025-07-10 发布日期:2025-07-11

Soil nutrient distributions in different habitats of the Ulanbuh Desert.

MU Ren, LI Xinle, XU Guangfu, HAN Jinfu, CUI Jian, YU Xiao, GUO Junting, XIN Zhiming*   

  1. (Experimental Center of Desert Forestry, Chinese Academy of Forestry/Inner Mongolia Dengkou Desert Ecosystem  Observation Research Station, Bayannaoer 015200, Inner Mongolia, China).

  • Online:2025-07-10 Published:2025-07-11

摘要: 研究乌兰布和沙漠不同生境类型土壤养分分布状况,为揭示荒漠地区不同生境类型土壤养分限制性提供科学依据。将乌兰布和沙漠划分为半流动沙丘、固定/半固定沙地、戈壁、盐碱地和草地5种生境类型,进行土壤理化性质测定及化学计量比分析。结果表明:(1)乌兰布和沙漠土壤速效氮和全钾较为稳定(CV=8.17%和CV=9.44%),生境类型是影响土壤有机质、速效氮、速效钾等含量的主要因素,而土壤全氮、全磷、速效磷等含量则受土壤母质的影响。(2)草地0~10 cm土层速效氮较10~20 cm增加132.90%(P<0.05),速效磷较20~40 cm增加96.43%(P<0.05),速效钾较40~60 cm增加52.11%(P<0.05),草地表层土壤养分富集现象明显。(3)主成分分析表明,土壤有机质在不同生境类型土壤化学计量贡献率均为最大。同时,土壤有机质与全氮、全磷、速效磷等呈显著或极显著正相关关系(P<0.05和P<0.01)。因此,土壤有机质可以作为评价乌兰布和沙漠不同生境土壤养分限制性的指标。本研究结果对明晰乌兰布和沙漠不同生境土壤理化性质及化学计量比差异与调控因素具有重要意义,可为荒漠生态系统的保护和恢复提供科学依据。


关键词: 生态化学计量, 生境, 沙漠, 主成分分析

Abstract: Clarifying the distribution of soil nutrients in different habitat types in the Ulanbuh Desert can provide scientific basis for revealing nutrient limitation patterns. The habitats in the Ulanbuh Desert were classified into five types: semi-mobile sand dune, fixed/semi-fixed sand land, Gobi, saline alkali land, and grassland. Soil physical and chemical properties of those five habitat types were measured and stoichiometric ratios were calculated. Results showed that: (1) In the Ulanbuh Desert, soil available nitrogen and total potassium exhibited high stability, with coefficients of variation (CV) being 8.17% and 9.44%, respectively. Habitat type was the principal factor influencing the levels of soil organic matter, available nitrogen, and available potassium. The levels of soil total nitrogen, total phosphorus, and available phosphorus were influenced by the parent material. (2) Soil available nitrogen in the 0-10 cm layer of grassland was 132.90% higher (P<0.05) than the 10-20 cm layer, the available phosphorus was 96.43% higher (P<0.05) compared to 20-40 cm, and the available potassium was 52.11% higher (P<0.05) compared to 40-60 cm, highlighting a pronounced phenomenon of nutrient enrichment in the surface layer. (3) Principal component analysis indicated that soil organic matter contributed the most to soil stoichiometry across different habitat types. Moreover, there were significant positive correlations (P<0.05 or P<0.01) between soil organic matter and total nitrogen, total phosphorus, and available phosphorus. Therefore, soil organic matter can be used as an indicator to evaluate soil nutrient limitations of different habitats in the Ulanbuh Desert. Our results are of great significance for clarifying the differences in soil physical and chemical properties, stoichiometric ratios, and regulatory factors in different habitats of the Ulanbuh Desert, providing scientific basis for the protection and restoration of desert ecosystems.


Key words: ecological stoichiometry, habitat, desert, principal component analysis