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• 研究报告 • 上一篇    下一篇

贵州普定喀斯特关键带土壤磷分布特征及其控制因素

张倩1,2,韩贵琳1*,柳满1,阳昆桦1,刘强3   

  1. (1中国地质大学(北京), 北京 100083; 2中国科学院地理科学与资源研究所, 北京 100101;3山东世纪阳光纸业集团有限公司, 山东潍坊 262400)
  • 出版日期:2019-02-10 发布日期:2019-02-10

Spatial distribution of soil phosphorus and controlling factors from Puding karst critical zone, Guizhou Province, Southwest China.

ZHANG Qian1,2, HAN Gui-lin1*, LIU Man1, YANG Kun-hua1, LIU Qiang3   

  1. (1China University of Geosciences (Beijing), Beijing 100083, China; 2 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 3Shandong Century Sunshine Paper Group Co., Ltd, Weifang 262400, Shandong, China).
     
  • Online:2019-02-10 Published:2019-02-10

摘要: 以贵州普定喀斯特关键带为研究对象,于2016年6月采集了5种土地利用类型的土壤剖面,包括农田、灌丛、次生林、草坡和弃耕地,分析了土壤剖面总磷、有效磷的分布特征,并讨论了有机碳、总氮、pH值和团聚体组成等理化性质对总磷和有效磷含量的影响。结果表明:土壤总磷和有效磷含量均随深度增加呈现降低趋势,在剖面0~30 cm处剧烈降低,30 cm以下减少趋势减缓。相对于其他类型的土地利用方式,耕地表层土壤总磷和有效磷含量有明显的差异,可能受人为干扰活动的影响。除次生林外,其他4种土地利用类型的土壤有效磷含量均处于较低水平。土壤总磷和有效磷含量与总氮、有机碳含量呈正相关,农田土壤相关性最好。土壤磷素主要受土壤有机质含量控制,可以通过增施有机肥,增加土壤有机质含量,改善土壤供磷状况,提高农作物对磷素的吸收。土壤团聚体粒径以大团聚体占优势,土壤总磷和有效磷含量与大团聚体组分呈正相关。土壤大团聚粒径组分的增加促进了磷素的积累。

关键词: 养分循环, 数据管理, 概念模型

Abstract: Soil samples of five land-use types, including cropland, shrubbery, secondary forest, grassland, and abandoned cropland, were collected in Puding County in June 2016, which is a typical karst critical zone in Southwest China. Spatial distribution of total phosphorus (TP) and available phosphorus (Olsen-P) in soils were investigated. We further analyzed the controlling factors of spatial variation of soil P, including pH, soil organic carbon (SOC), total nitrogen (TN), and aggregate composition. The results showed the contents of TP and Olsen-P decreased with increasing of soil depth, and the variations were more obvious in the upper 30 cm than those in the lower 30 cm. The TP and Olsen-P contents were different under cropland from other land use types due to the impacts of human activity. The Olsen-P contents were very low except for the secondary forest soils. The positive correlations were observed between the contents of TP, Olsen-P, SOC and TN, with the best correlation coefficients being found in the cropland. The SOC contents were the most important factor affecting TP and Olsen-P contents. The high contents of organic matters facilitated the absorption of P in crops. The proportion of macro-aggregates was dominant in the most soils, which were positively correlated with TP and Olsen-P contents, indicating that the increases of the proportion of macro-aggregates promoted soil P accumulation.

Key words: Nutrients cycling, Data management, Conceptual model