Chi Guangyu, Zeng Fanpeng, Wang Yang, Chen Xin
Key Laboratory of Pollution Ecology and Environment Engineering, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang, China.
College of Life Science, Nanchang Normal University, Nanchang, China.
Front Plant Sci. 2022 Oct 7;13:1010458. doi: 10.3389/fpls.2022.1010458. eCollection 2022.
The dynamics of phosphorus (P) in litter-soil systems during litter decomposition across a plantation chronosequence remain to be underinvestigated, especially in terms of the nutrient cycle in plantations. In this study, the P dynamics in a litter-soil system of larch () plantations at three stand ages (10, 25, and 50 years old) were examined through a 4-year decomposition experiment (experiment 1) and a 360-day indoor incubation experiment (experiment 2). The aim of experiment 1 and experiment 2 is to determine the P dynamics in litter and soil, respectively. The results in experiment 1 suggested that litter mass retained 34.1%-42.5% of the initial mass after a 4-year decomposition period, and the turnover time (t) of the decomposition was 11.3, 13.9, and 11.8 years for 10-, 25- and 50-year-old stand larch plantations, respectively. Litter exhibited a net P decrease during the first 180 days, followed by a phase of a net P increase. The lowest P accumulation rate was found in the 25-year-old stand during the P immobilization stage. This immobilization phase was followed by a slow litter P decrease. Highly correlated relations were found between the litter decomposition rate and the initial litter N concentration and C/N, whereas the P accumulation rate was noticeably correlated with the initial litter P and C/P. The results in experiment 2 showed that litter addition promoted the accumulation of the highly labile P (resin P, NaHCO-P, and NaHCO-P), as well as moderately labile P (NaOH-P) in the soil. The findings obtained suggest that soil microbial biomass P and acid phosphatase activity were the primary factors driving the activation of soil P during litter decomposition. These findings would be beneficial to the systematic understanding of the nutrient cycle in plant-soil systems and litter management during the development of larch plantations.
在人工林时间序列上,凋落物分解过程中凋落物 - 土壤系统中磷(P)的动态变化仍有待深入研究,尤其是在人工林养分循环方面。在本研究中,通过为期4年的分解实验(实验1)和为期360天的室内培养实验(实验2),研究了三个林龄(10年、25年和50年)的落叶松人工林凋落物 - 土壤系统中的磷动态。实验1和实验2的目的分别是确定凋落物和土壤中的磷动态。实验1的结果表明,经过4年的分解期后,凋落物质量保留了初始质量的34.1% - 42.5%,10年、25年和50年林龄的落叶松人工林分解的周转时间(t)分别为11.3年、13.9年和11.8年。凋落在最初180天内表现出净磷减少,随后是净磷增加阶段。在25年林龄的林分中,磷固定阶段的磷积累速率最低。这个固定阶段之后是凋落物磷的缓慢减少。凋落物分解速率与初始凋落物氮浓度和C/N之间存在高度相关关系,而磷积累速率与初始凋落物磷和C/P显著相关。实验2的结果表明,添加凋落物促进了土壤中高活性磷(树脂磷、NaHCO - P和NaHCO - P)以及中度活性磷(NaOH - P)的积累。研究结果表明,土壤微生物生物量磷和酸性磷酸酶活性是凋落物分解过程中驱动土壤磷活化的主要因素。这些发现将有助于系统理解落叶松人工林发育过程中植物 - 土壤系统的养分循环和凋落物管理。