首页|鄱阳湖消落区湿地土壤磷形态分布特征及其影响因素

鄱阳湖消落区湿地土壤磷形态分布特征及其影响因素

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消落区是水陆生态系统中物质、能量输移和转化的活跃地带.本文在鄱阳湖典型消落区湿地选择不同景观带(泥滩带、苔草带和南荻带),评价消落区不同景观带土壤磷形态与土壤理化性质的关系.结果表明,不同湿地土壤中各磷形态含量整体表现为C.HCl-Pi>NaOH-Pi>NaOH-Po>D.HCl-Pi>NaHCO3-Pi>NaHCO3-Po>C.HCl-Po>Residual-P>H2O-Pi.消落区泥滩带中有机磷形态显著低于植被带,而无机磷形态则相反,这可能与植被生长对无机磷(Pi)的吸收,以及凋落物输入导致有机磷(Po)的积累有关.除C.HCl-Pi外,消落区南荻带和苔草带土壤磷形态并未表现出显著的差异.RDA结果表明,植被带土壤磷形态主要受土壤pH影响,其中全氮、有机质和pH与NaHCO3-Po和NaOH-Po呈负相关关系;而泥滩带则主要受土壤全氮水平的影响,其中全氮、有机质与NaHCO3-Pi和D.HCl-Pi呈正相关关系.相关分析表明Fe、Mn金属元素含量与NaOH-Pi呈显著正相关.消落区湿地土壤磷形态含量变化是景观差异、金属元素含量和土壤理化性质共同作用的结果.此外,相较于泥滩带,植被带提高了湿地土壤中等活性磷的含量,降低了稳定性磷含量,这表明湿地植被的存在促进了湿地土壤磷的循环.研究结果有助于明晰干湿交替控制下淡水湿地土壤磷转化过程,为淡水湿地保护和水环境治理提供依据.
Distribution characteristics and driving factors of phosphorus in the water-level-fluctuating wetland soil of the Poyang Lake
The water-level-fluctuating area is an active area of material and energy transport and transformation between aquatic and terrestrial ecosystems.In this paper,different landscape belts(mudflat belt,Carex cinerascens belt and Triarrhena lutarioriparia belt)were selected in the wetland of the Poyang Lake to evaluate the relationship between soil phosphorus forms and soil physicochemical properties.The results showed that the content of phosphorus forms in different wetland soils was followed as C.HCl-Pi>NaOH-Pi>NaOH-Po>D.HCl-Pi>NaHCO3-Pi>NaHCO3-Po>C.HCl-Po>Residual-P>H2O-Pi.The content of organic phosphorus(Po)was significantly lower in the mudflat belt than it was in the vegetation belt,while inorganic phosphorus(Pi)showed the opposite result,which possibly drived the uptake of inorganic phosphorus by vegetation growth and the accumulation of organic phosphorus due to the input of litter.Except C.HCl-Pi,there was no significant difference in content of soil phosphorus forms between the Carex cinerascens and Triarrhena lutarioriparia belt.The results of RDA showed that content of soil phosphorus forms was mainly affected by soil pH;total nitrogen,organic matter and pH showed the significant negative correlation with NaHCO3-Po and NaOH-Po.Soil phosphorus forms in the mudflat belt was mainly affected by the soil total nitrogen level,and the total nitrogen and organic matter positively correlated with NaHCO3-Pi and D.HCl-Pi.The correlation analysis indicated that the content of Fe and Mn positively correlated with NaOH-Pi content.The variation of phosphorus forms in wetland soil was regulated by landscape difference,metal content and soil physicochemical properties.In addition,compared with mudflat belt,vegetation belt increased the level of medium active phosphorus in wetland soil and decreased the stable phosphorus level,indicating that vegetation promoted the circulation of phosphorus in wetland soil.The results are helpful to clarify the soil phosphorus conversion process in freshwater wetland under the alternation of wetting and drying,and provide the scientific basis for freshwater wetland protection and water environment management.

the Poyang Lakewater-level-fluctuating areaphosphorus formsdistributiondriving factor

陈红梅、张华、曾欢、程莉瑶、熊佳欣

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江西师范大学地理与环境学院,南昌 330022

江西师范大学鄱阳湖湿地与流域研究教育部重点实验室,南昌 330022

鄱阳湖 消落区 磷形态 分布 驱动因子

2025

环境科学学报
中国科学院生态环境研究中心

环境科学学报

北大核心
影响因子:1.645
ISSN:0253-2468
年,卷(期):2025.45(1)