鄱阳湖枯水季湿地土壤碳氮磷生态化学计量特征及其影响因素
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邓通(2000—),男,硕士研究生,主要从事自然地理学研究。E-mail:deng1001001@163.com

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X171.1;S152.3

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江西省自然科学基金面上项目(20212BAB203002);国家自然科学基金项目(41561105);东华理工大学博士科研启动基金项目(DHBK201909838);江西省自然资源厅科技创新项目(ZRKJ20242616)


Ecological Stoichiometric Characteristics of Soil Carbon, Nitrogen and Phosphorus in Poyang Lake Wetland during Dry Season and Their Influencing Factors
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    摘要:

    [目的] 探讨湿地土壤营养元素生态化学计量特征及其影响机制有助于深入了解土壤养分循环过程及其内部驱动机制。[方法] 以江西鄱阳湖国家级自然保护区内蚌湖(半控湖)和泗洲头(开放水域)湿地为研究对象,基于相关性分析和结构方程模型(structural equation model,SEM)研究2017—2019年表层土壤在不同水位高程梯度下碳、氮、磷生态化学计量特征及其关键影响因子。[结果] 蚌湖湿地土壤有机碳(SOC)、全氮(TN)和全磷(TP)质量分数平均值(9.33、1.18、0.43 g/kg)显著高于泗洲头湿地SOC、TN和TP质量分数平均值(2.65、0.31、0.19 g/kg)(p<0.05),在相同水位高程梯度下均未随着年份变化而显著变化(p>0.05)。蚌湖湿地土壤C∶N平均值(9.24)显著低于泗洲头湿地(10.19),但C∶P、N∶P平均值(53.18、6.23)显著高于泗洲头湿地(40.90、4.05)(p<0.05)。蚌湖和泗洲头湿地土壤C∶N未受到水位高程梯度的显著影响(p>0.05),C∶P和N∶P随着水位高程梯度的增加呈递增到递减的变化趋势,且相同水位高程下蚌湖C∶P随年份的变化发生显著变化(p<0.05)。蚌湖和泗洲头C∶P和N∶P均与地上生物量(AGB)、电导率(EC)呈显著正相关,与pH呈显著负相关(p<0.05)。湿地土壤碱解氮(AN)、氨态氮(NH4+-N)和AGB对蚌湖和泗洲头湿地土壤生态化学计量值产生直接影响,同时蚌湖土壤生态化学计量值还受土壤体积质量(BD)和pH的直接影响,泗洲头土壤生态化学计量值还受土壤水分体积分数(SWC)和EC的直接影响。蚌湖土壤中AGB为C∶N的关键影响因子,AN为C∶P和N∶P的关键影响因子;泗洲头土壤中NH4+-N是C∶N的主控因子,同时AGB也是泗洲头湿地C∶P和N∶P的关键影响因子。[结论] 鄱阳湖湿地植被生物量和土壤氮素对土壤碳氮磷生态化学计量特征具有重要影响,具有半控湖特征的蚌湖湿地土壤碳氮磷生态化学计量值主要受AGB和AN的影响,而开放水域泗洲头主要受NH4+-N和AGB的影响,未来可考虑通过湿地植被恢复与重建技术模式促进鄱阳湖湿地生态恢复与保护。

    Abstract:

    [Objective] Investigating the ecological stoichiometry of soil nutrients and the driving mechanisms in wetlands can provide key insights into soil nutrient cycling processes and the internal driving factors. [Methods] This study focused on the wetlands of Banghu(semi-controlled lake)and Sizhoutou(open-water area)in the National Nature Reserve of Jiangxi Poyang Lake. Based on correlation analysis and structural equation modeling(SEM), the ecological stoichiometric characteristics of surface soil carbon(C),nitrogen(N),and phosphorus(P)and their key influencing factors under different elevation gradients from 2017 to 2019 were analyzed. [Results] The mean concentrations of soil organic carbon(SOC),total nitrogen(TN),and total phosphorus(TP)in the Banghu wetland(9.33,1.18 and 0.43 g/kg,respectively)were significantly higher than those in the Sizhoutou wetland(2.65,0.31 and 0.19 g/kg,respectively)(p<0.05). At the same elevation gradient,SOC,TN,and TP concentrations in both wetlands did not vary significantly over the years(p>0.05). Although the mean soil C∶N ratio in the Banghu wetland(9.24)was significantly lower than that in the Sizhoutou wetland(10.19),the mean C∶P and N∶P ratios in the Banghu wetland(53.18 and 6.23,respectively)were significantly higher than those in the Sizhoutou wetland(40.90 and 4.05,respectively)(p<0.05). Elevation gradient had no significant effect on the C∶N ratio in either wetland(p>0.05). However,C∶P and N∶P ratios exhibited an increasing – decreasing trend along the elevation gradient. At the same elevation,C∶P in the Banghu wetland showed a significant interannual variation(p<0.05),while there was no significant change observed in the Sizhoutou wetland(p> 0.05). Both wetlands exhibited significant positive correlations of C∶P and N∶P ratios with the aboveground biomass(AGB)and electrical conductivity(EC),and significant negative correlations with pH(p<0.05). Soil alkaline nitrogen (AN), ammonium-nitrogen (NH4+-N), and AGB had direct effects on soil ecological stoichiometry of both wetlands. In addition,the ecological stoichiometric characteristics in the Banghu wetland were directly influenced by soil bulk density(BD)and pH,while those in the Sizhoutou wetland were influenced by soil volumetric water content(SWC)and EC. In the Banghu wetland,AGB was the key factor influencing C∶N,while AN was the primary determinant of C∶P and N∶P. In the Sizhoutou wetland,NH4+-N was the main controlling factor for C∶N,and AGB was the critical factor affecting C∶P and N∶P. [Conclusion] Vegetation biomass and soil nitrogen play crucial roles in the ecological stoichiometric characteristics of soil carbon,nitrogen, and phosphorus in the Poyang Lake wetlands. The soil stoichiometric values in the semi-controlled Banghu wetland are primarily driven by AGB and AN,whereas those in the open-water Sizhoutou wetland are mainly influenced by NH4+-N and AGB. Therefore,technical model of vegetation restoration and reconstruction in wetlands could be considered to promote ecological restoration and protection of Poyang Lake wetland in the future.

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邓通, 钱海燕, 周杨明, 谢冬明.鄱阳湖枯水季湿地土壤碳氮磷生态化学计量特征及其影响因素[J].水土保持学报,2025,39(2):279~288

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  • 收稿日期:2024-10-28
  • 最后修改日期:2024-12-09
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  • 在线发布日期: 2025-05-07
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