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浙西南典型森林土壤碳氮磷化学计量及土壤持水能力研究

Study on the Carbon, Nitrogen and Phosphorus Stoichiometry of Typical Forest Soils and Its Water-holding Capacity in Southwest of Zhejiang Province

  • 摘要: 研究土壤碳(C)、氮(N)、磷(P)的生态化学计量特征及土壤持水能力,可掌握不同森林土壤碳库、水库及养分库的差异,为森林营建和林分结构调整提供基础。本文以浙江省龙泉市龙渊森林公园石鼓山典型阔叶林、针阔混交林、针叶林为对象,在林分调查基础上,采样并分析了土壤C、N、P含量和土壤持水性能。结果表明,阔叶林和针阔混交林的径阶呈正偏态分布,针叶林则呈倒“J”形;阔叶林土壤C、N、P含量均显著高于针阔混交林和针叶林(P<0.05),林地土壤C/N、C/P、N/P在不同森林间的差异没有达到显著性水平(P>0.05);林地土壤容重、总孔隙度在不同森林间也没有显著性差异(P>0.05);阔叶林土壤田间持水量、毛管持水量、实际持水量和最大持水量分别为420.57、703.31、625.02、806.18 g·kg−1,均显著高于针阔混交林和针叶林(P<0.05);土壤C、N含量与容重间具有显著负相关(P<0.05),与土壤总孔隙度间具有显著正相关(P<0.05),与田间持水量、毛管持水量、实际持水量、最大持水量之间的正相关性达极显著水平(P<0.01);土壤P含量与毛管持水量、实际持水量的正相关性达显著水平(P<0.05)。综上,高C、N含量的森林土壤也具有良好的持水能力,今后在森林营建和林分改造过程中可适当增加阔叶树的比例。

     

    Abstract: The eco-chemical characteristics research of forest soil carbon (C), nitrogen (N), and phosphorus (P) and the soil water-holding capacity exploration are helpful for mastering the differences in soil carbon, water and nutrient reservoirs of different forests, providing a foundation for forest construction and stand structure adjustment. In this study, with the typical broad-leaved forest, coniferous and broad-leaved mixed forest and coniferous forest in Shigu Mountain, Longyuan Forest Park, Longquan City, Zhejiang Province as the research objects, the samples are collected, the soil C, N, P content and soil water-holding performance are analyzed on the basis of investigation of forest stands. It is found that the diameter distribution of broad-leaved forest and coniferous broad-leaved mixed forest was positively skewed, while that of the coniferous forest was in an inverted “J” shape. The soil C, N, P content of the broad-leaved forest were significantly higher than those of the remaining (P<0.05). The differences in soil C/N, C/P, and N/P ratios among different forests weren’t significant (P>0.05), there were no significant differences in soil bulk density and total porosity of different forests (P>0.05). The field water-holding capacity, capillg capacity, actual water-holding capacity, and maximum water-holding capacity of the broad-leaved were 420.57, 03.31, 625.02, and 806.18 g kg-1, respectively, all of which significantly higher than those of the others (P<0.05). There was a significant negative correlation between the soil C, N content and the bulk density (P<0.05), a significant positive correlation between the soil C, N content and the total porosity (P<0.05), and an extremely significant positive correlation among the soil C, N content, water-holding capacity, capillary water-holding capacity, actual water-holding capacity, and maximum water-holding (P<0.01). The significant positive correlation between soil P content and capillary water-holding capacity and actual water-holding capacity existed (P<0.05). In conclusion, forest soil with high C and N content still has excellent water-holding capacity, the proportion of broad-leaved tree can be appropriately increased in forest construction and stand reconstruction in the future.

     

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