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泉州湾3种典型红树林群落土壤养分及生态化学计量特征

Soil nutrients and ecological stoichiometric characteristics of three typical mangrove communities in Quanzhou Bay

  • 摘要: 为了揭示泉州湾河口湿地红树林群落土壤养分及生态化学计量特征差异,以泉州湾河口湿地内桐花树(Aegiceras corniculatum)群落、秋茄(Kandelia obovata)群落和秋茄+桐花树混交群落3种典型的红树林群落为研究对象,测定0~20 cm深度土壤的主要养分指标、碳储量及化学计量比,采用单因素方差分析检验土壤各养分指标、碳储量及化学计量特征在不同红树林恢复类型下的差异,再采用内梅罗指数法对各群落类型土壤肥力进行综合评价。研究结果表明,3种同龄的典型红树林群落中,秋茄+桐花树混交群落土壤养分含量显著高于桐花树群落和秋茄群落(p<0.05),其中桐花树群落的土壤养分含量略高于秋茄群落;对于土壤碳储量,其在桐花树群落与秋茄群落之间均无显著差异,而在桐花树群落、秋茄群落与秋茄+桐花树混交群落之间均有显著差异,混交群落的土壤碳储量显著大于桐花树群落、秋茄群落(p<0.05);3种典型红树林土壤碳磷比和氮磷比均存在显著差异(p<0.05),其中碳磷比在14.58~34.18之间,氮磷比在1.51~2.65之间,2个指标由高到低均依次为秋茄+桐花树混交群落、桐花树群落、秋茄群落;土壤指标全氮的肥力系数在3个群落间的差异较明显(混交群落最大为2.94,秋茄群落最小为1.93,桐花树群落居中为2.44),其他土壤指标(有机质、全磷、全钾、速效磷和有效钾)的肥力系数在3个群落间的差异不明显。在泉州湾河口湿地,3种典型红树林在土壤养分、土壤生态化学计量特征和土壤碳储量上的差异反映了混交模式的优越性,秋茄+桐花树混交群落通过调控元素平衡,实现了碳汇功能与养分积累的协同提升,相较于桐花树纯林和秋茄纯林的红树林恢复模式,该地区湿地可优先考虑秋茄+桐花树混交的红树林恢复模式。

     

    Abstract: To reveal the differences in soil nutrients and ecological stoichiometric characteristics among three mangrove communities in the Quanzhou Bay estuary wetland, the Aegiceras corniculatum community, Kandelia obovata community, and K. obovata + A. corniculatum mixed community were selected as research subjects. The main soil nutrient indices, carbon storage, and stoichiometric ratios at 0-20 cm depth were measured. One-way ANOVA was used to examine the differences in soil nutrient indices, carbon storage, and stoichiometric characteristics under different mangrove restoration types, and the Nemerow index method was employed to comprehensively evaluate soil fertility for each community type. The results showed that, among the three typical mangroves of same age, the soil nutrient content of the K. obovata + A. corniculatum mixed community was significantly higher than that of the A. corniculatum community and the K. obovata community (p<0.05), while the soil nutrient content of the A. corniculatum community was slightly higher than that of the K. obovata community. For soil carbon storage, there was no significant difference between the A. corniculatum community and the K. obovata community, but significant differences were found among the A. corniculatum community, K. obovata community, and K. obovata + A. corniculatum mixed community, and the soil carbon storage of the mixed forest was significantly greater than that of both the A. corniculatum and K. obovata communities. The C:P and N:P ratios of the three typical mangrove soils showed significant differences (p<0.05), with C:P ratios ranging from 14.58 to 34.18 and N:P ratios ranging from 1.51 to 2.65; both indices ranked from high to low as follows: K. obovata + A. corniculatum mixed community, A. corniculatum community, and K. obovata community. The fertility coefficient of total nitrogen differed markedly among the three communities (the mixed community was the highest at 2.94, the K. obovata community was the lowest at 1.93, and the A. corniculatum community was in the middle at 2.44), whereas the fertility coefficients of other soil indices (organic matter, total phosphorus, total potassium, available phosphorus, and available potassium) showed no significant differences among the three communities. In the Quanzhou Bay estuary wetland, the differences in soil nutrients, ecological stoichiometric characteristics, and soil carbon storage among the three typical mangroves reflected the superiority of the mixed community model. The K. obovata + A. corniculatum mixed community achieved synergistic enhancement of carbon sink function and nutrient accumulation through regulating elemental balance. Compared with the pure forest restoration models of A. corniculatum and K. obovata, the K. obovata + A. corniculatum mixed mangrove restoration model can be prioritized for wetland restoration in this region.

     

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