首页|钦州湾不同林龄无瓣海桑人工林表层沉积物生态化学计量特征

钦州湾不同林龄无瓣海桑人工林表层沉积物生态化学计量特征

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[目的]生态化学计量学是探索耦合元素平衡和循环的有效工具,研究无瓣海桑人工林表层沉积物关键元素含量及其生态化学计量特征,为外来植物科学管控提供理论依据。[方法]以钦州湾滨海湿地 3 块不同林龄(10、15和20 a)的无瓣海桑人工林为研究对象,每个林分设置3块20 m×20 m的样地,每块样地内采用蛇形布点法采集0~20 cm表层沉积物样品,测定样品的有机碳(TOC)、全氮(TN)、全磷(TP)、有效磷(AP)、全硫(TS)、有效硫(AS)、全钾(TK)、有效钾(AK)等含量,研究表层沉积物C、N、P等元素生态化学计量特征及其影响因素。[结果]1)无瓣海桑林龄对沉积物TOC、TN、TP、TS、AS等理化性质及C/N、C/P、C/S、C/K、N/S、P/S、P/K、S/K等生态化学计量具有显著影响;2)研究区沉积物C/N均值(20。41)略高于中国湿地土壤C/N均值(18。22),C/P均值(64。91)、N/P均值(3。19)远低于中国湿地土壤C/P均值(245。22)、N/P均值(13。6),C∶N∶P均值为 20。3,处于中国湿地土壤中C∶N∶P变化范围 7。08~41。44 之间;3)相关性分析与冗余分析结果表明,TOC、TN和TP是影响沉积物生态化学计量变化的关键因子。[结论]研究区沉积物具有富C、P而少N的特点,沉积物P素矿化能力较强,无瓣海桑生长需P量大、受N限制。在无瓣海桑人工林管理过程中,建议科学调控沉积物TOC含量、降低入海口N素和P素输入来减缓无瓣海桑的扩散速度,以降低其生态风险。
Ecological stoichiometry characteristics in surface sediments of Sonneratia apetala plantation of different ages in Qinzhou bay
[Objective]Ecological stoichiometry is an efficient tool to explore the balance and cycling of coupled elements,this study aims to provide a theoretical basis for the scientific management of alien plants by investigating the contents of key elements and their ecological stoichiometric characteristics in the surface sediments of Sonneratia apetala plantations of different ages.[Method]The study focused on three artificially established S.apetala forests of different ages(10,15,and 20 years)in the Qinzhou bay coastal wetland.Three plots of 20 m×20 m were set up in each forest age group.Surface sediment samples were collected within each plot using a zigzag pattern to a depth of 0-20 cm.Samples were analyzed to determine the contents of total organic carbon(TOC),total nitrogen(TN),total phosphorus(TP),available phosphorus(AP),total sulfur(TS),available sulfur(AS),total potassium(TK),available potassium(AK)and so on.The ecological stoichiometric characteristics of C,N,P and other elements in surface sediments and their influencing factors were studied.[Result]1)The age of S.apetala forests had a significant influence on the physicochemical properties that included TOC,TN,TP,TS and AS,as well as the ecological stoichiometry that contained C/N,C/P,C/S,C/K,N/S,P/S,P/K,and S/K in sediments;2)The average C/N values of sediments in the study area(20.41)were slightly higher than those of Chinese wetland soils(18.22).Conversely,the mean C/P values(64.91)and N/P values(3.19)were much lower than those of Chinese wetland soils(245.22 and 13.6,respectively).The average C∶N∶P ratio of 20.3 fell within the range of 7.08 to 41.44 that was observed in Chinese wetland soils.(3)Correlation analysis and redundancy analysis revealed that TOC,TN,and TP were the key factors influencing the variation in ecological stoichiometry of surface sediments.[Conclusion]The sediments in the study area were characterized by rich C and P but less N,with a higher mineralization capacity of sedimentary phosphorus.The growth of S.apetala requires a large amount of phosphorus while being limited by nitrogen.During the management process of S.apetala plantations,the diffusion rate of S.apetala can be slowed down by scientifically regulating the sediment organic carbon content and reducing the influx of nitrogen and phosphorus into the estuary,thus reducing ecological risks.

Sonneratia apetalastand agesurface sedimentsecological stoichiometryplantation management

甘国娟、陈永意、田红灯、李嘉佳、刘秀、覃杰

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南宁师范大学 环境与生命科学学院,广西 南宁 530001

广西壮族自治区林业科学研究院,广西 南宁 530002

广西优良用材林资源培育重点实验室,广西 南宁 530002

无瓣海桑 林龄 表层沉积物 生态化学计量 人工林管理

广西科技界智库重点课题中央财政林业科技推广示范项目广西林业科技推广示范项目广西壮族自治区级大学生创新创业训练计划项目

桂科协[2023]K-113[2022]TG18号gl2019kt16S202310603161

2024

中南林业科技大学学报
中南林业科技大学

中南林业科技大学学报

CSTPCD北大核心
影响因子:1.442
ISSN:1673-923X
年,卷(期):2024.44(6)