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  • Title: [Effects of broadleaved tree plantation on soil phosphorus fractions and availability in diffe-rent soil layers in a logged Cunninghamia lanceolata woodland].
    Author: Wang T, Wan XH, Wang L, Zou BZ, Wang SR, Huang ZQ.
    Journal: Ying Yong Sheng Tai Xue Bao; 2020 Apr; 31(4):1088-1096. PubMed ID: 32530182.
    Abstract:
    Phosphorus (P) limitation is one of the major issues for the management of subtropical plantations. Understanding the effects of tree species transition from conifer to broadleaved trees on soil P fraction and availability in different soil layers are of great significance for the sustainable development of subtropical forests. We compared changes in soil chemical properties, P fraction and availability across 0-100 cm soil profile between Mytilaria laosensis and Cunninghamia lanceolata plantations, which were initially reforested from C. lanceolata plantation in the spring of 1993. The results showed that soil organic P content in both plantations decreased significantly with soil depth. Compared with C. lanceolata, the M. laosensis plantation significantly increased soil available P content by 35.7% and 86.2% in the 0-10 and 10-20 cm, respectively. The contents of soil labile P and moderately labile P decreased significantly with soil depth in both plantations. The contents of labile P and moderately labile P were significantly higher in the surface soil (0-20 cm), while the non-labile P in the 80-100 cm was increased by 13.6%, and the free iron content in the 20-80 cm significantly decreased. Results of redundancy analysis showed that dissolved organic carbon and free iron were the most important factors influencing P fraction in those plantations. Tree species transition from C. lanceolata to M. laosensis could change the pattern of soil P fraction in soil profile, and greatly enhance soil P availability. 磷限制是亚热带人工林经营面临的主要问题之一,研究阔叶树代替针叶树造林对不同土壤层次磷组分和有效性的影响对维持亚热带地区森林生态系统的可持续发展具有重要意义。以1993 年春天在二代杉木林采伐迹地上同时营造的阔叶树米老排人工林和针叶树杉木人工林为对象,研究0～100 cm不同土层土壤理化性质、磷组分及其有效性的变化。结果表明: 两种林分下土壤有机磷含量均随土层加深而显著下降;与杉木林相比,米老排林0～10 和10～20 cm土层有效磷含量显著增加,分别增加35.7%和86.2%,易分解态磷和中等易分解态磷均随土层加深而显著降低,表层(0～20 cm)土壤易分解态磷和中等易分解态磷含量显著增加,80～100 cm土层难分解态磷含量显著降低,下降13.6%,20～80 cm土层游离态铁含量显著降低。冗余分析表明,可溶性有机碳和游离态铁是土壤磷组分变化的关键影响因子。在杉木采伐迹地上营造阔叶树改变了磷在土壤剖面上的分布格局,有利于提高磷的有效性。.
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