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林业科学 ›› 2022, Vol. 58 ›› Issue (5): 10-17.doi: 10.11707/j.1001-7488.20220502

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杉木人工林土壤磷素形态及含量的林龄变化

陈嘉琪,赵光宇,李仰龙,董玉红,厚凌宇,焦如珍*   

  1. 中国林业科学研究院林业研究所 林木遗传育种国家重点实验室 国家林业和草原局林木培育重点实验室 北京 100091
  • 收稿日期:2021-01-10 出版日期:2022-05-25 发布日期:2022-08-19
  • 通讯作者: 焦如珍
  • 基金资助:
    国家重点研发计划项目"杉木速生材高效培育技术研究"(2016YFD0600302);中央级公益性科研院所基本科研业务费专项资金项目"森林土壤功能微生物种质资源筛选及研究"(CAFYBB2018SY001)

Age Changes of Soil Phosphorus Form and Content in Chinese Fir Plantations

Jiaqi Chen,Guangyu Zhao,Yanglong Li,Yuhong Dong,Lingyu Hou,Ruzhen Jiao*   

  1. Research Institute of Forestry, CAF State Key Laboratory of Tree Genetics and Breeding Key Laboratory of Tree Breeding and Cultivation of National Forestry and Grassland Administration Beijing 100091
  • Received:2021-01-10 Online:2022-05-25 Published:2022-08-19
  • Contact: Ruzhen Jiao

摘要:

目的: 研究不同林龄杉木人工林土壤磷素形态及其含量变化特征, 分析各磷素形态的相关性, 以期为提高杉木人工林土壤磷素的有效性、促进杉木人工林的可持续发展提供依据。方法: 在江西分宜县山下林场选择7个林龄(3、6、12、18、25、32和49年生)的杉木人工林, 采用钼锑钪比色法测定土壤全磷和有效磷含量, 采用分级法测定土壤铝结合态磷(Al-P)、高铁结合态磷(Fe-P)、闭蓄态磷(O-P)和钙结合态磷(Ca-P)含量, 分析各磷素形态间的相关性, 揭示不同林龄土壤磷素动态变化。结果: 不同林龄杉木人工林土壤无机磷含量占全磷含量的55.37%~74.22%, 而无机磷组分含量表现为O-P>Fe-P>Ca-P>Al-P; 土壤全磷、有效磷、Al-P、O-P含量随林龄的增加呈先减后增的趋势, 在12年生或18年生时最小, Fe-P含量逐渐升高但差异不显著, Ca-P含量呈先增加后减小的趋势; 不同林龄土壤无机磷含量动态变化表明, 中林龄(11~20年)时期杉木处在快速生长阶段, 大量吸收土壤养分; 而从18年生到49年生, Ca-P含量显著下降, 表明近成熟林(21~25年生)开始, 杉木对Ca-P吸收速率增大; 相关性分析表明土壤有效磷含量与Al-P含量、Fe-P含量和O-P含量正相关(P>0.05), O-P含量与Al-P含量和Fe-P含量正相关(P>0.05)。结论: 不同林龄杉木人工林土壤中不同形态磷素含量的变化呈现一定的规律性, 且无机磷为全磷的主要组成部分, 相关性分析表明不同磷素形态间存在相互作用。

关键词: 杉木人工林, 林龄, 土壤全磷, 有效磷, 无机磷

Abstract:

Objective: This study was designed to characterize the variation in soil phosphorus forms and their contents in differently aged Chinese fir plantations, and analyze the correlations among various phosphorus forms, in order to provide a basis for improving the availability of soil phosphorus in Chinese fir plantations and promoting the sustainable development of Chinese fir plantations. Method: Seven Chinese fir plantations at different ages (3, 6, 12, 18, 25, 32 and 49 years) were selected from the Shanxia Forest Farm in Fenyi County, Jiangxi Province, China. Total soil phosphorus and available phosphorus were detected by molybdenum antimony scandium colorimetric method. The contents of soil aluminum-bound P (Al-P), high-iron-bound P (Fe-P), occluded P (O-P) and calcium-bound P (Ca-P) were detected by a grading method, and the correlations among various phosphorus forms were analyzed, to reveal the dynamic changes of soil phosphorus at different forest ages. Result: The soil inorganic phosphorus contents of differently aged Chinese fir plantations accounted for 55.37%~74.22% of the total phosphorus content, and the amount of inorganic phosphorus fractions was in an order: O-P> Fe-P> Ca-P> Al-P; The content of total phosphorus, available phosphorus, Al-P and O-P in soil showed a trend of first decreasing followed by increasing with age, and the minimum appeared at 12-year-old or 18-year-old, the Fe-P content displayed a gradual increased but not significantly, the Ca-P content displayed an increase first followed by a decrease. The dynamic changes of soil inorganic phosphorus with forest age indicate that the Chinese fir plantation is in the rapid growth stage during the middle forest age and absorbs a large amount of soil nutrients, prompting the activation of O-P and the release of Al-P and Fe-P under the action of root exudates, but due to the different rates of release and absorption, the content of different phosphorus forms varies. From 18-year-old to 49-year-old, the Ca-P content decreased significantly, indicating that starting from the near-mature forest, the Chinese fir plantations increased the Ca-P absorption rate and slowed down the absorption rate of other phosphorus forms, resulting in an increase of the content. The correlation analysis of various phosphorus proved that soil available phosphorus was positively correlated with Al-P, Fe-P, and O-P content (P>0.05), and O-P was positively correlated with Al-P and Fe-P content (P>0.05). Conclusion: The changes of content of different phosphorus forms in the soils of Chinese fir plantations at different ages show certain patterns. The inorganic phosphorus is the main component of the total phosphorus. And correlation analysis shows that different phosphorus forms can be transformed into each other.

Key words: Chinese fir plantation, age of forest, total soil phosphorus, available phosphorus, inorganic phosphorus

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