土壤磷形态变化特征对毛乌素沙区湿地退化的响应

Response of Soil Phosphorus Form Changes to Wetland Degradation in the Mu Us Sandy land

  • 摘要:
    目的 研究毛乌素沙区磷素含量分布特征,以明确湿地退化对土壤磷形态变化特征的影响。
    方法 以毛乌素沙地秃尾河流域的两个湿地的未退化(UD)、轻度退化(LD)、中度退化(MD)、重度退化(SD)四个区域为研究对象,采用改进后的Hedley磷素分级方法,测定并比较不同退化程度下0-20cm土层土壤磷形态含量差异,阐明影响干旱区退化湿地0 ~ 20 cm土层土壤磷形态的环境因素。
    结果 毛乌素沙地退化湿地0 ~ 20 cm土层土壤磷水平较低,其中无机磷占51.35% ~ 79.57%,且随着退化程度的加剧,无机磷占比有提高趋势。随着退化程度的加剧,各种磷形态含量均呈下降趋势,H2O-P和NaHCO3-P含量均处于较低水平,仅为1.71 ~ 8.19 mg kg−1,且随退化加剧呈下降趋势;土壤无机磷组分中HCl-Pi和土壤有机磷组分中Residual-P所占的比例最高(> 50%),随着退化程度的加剧含量变化最为明显。土壤有机质、全氮与各形态磷均有较高的相关性,尤其是对H2O-P、NaHCO3-Pi、NaOH-Pi的影响最为显著,相关性系数可达0.90以上。
    结论 土壤各形态磷含量均随湿地退化加剧而呈现出不同程度的降低,其中土壤有机磷含量的下降幅度最为明显。研究结果可为未来毛乌素干旱区湿地土壤养分保持及沙地恢复管理提供科学依据。

     

    Abstract:
    Objective The aims were to understand the distribution characteristics of phosphorus (P) content in the Mu Us Sandy Land, and to clarify the influence of wetland degradation on the morphological characteristics of soil P.
    Method four regions of un-degraded (UD), mildly degraded (LD), moderately degraded (MD), and severely degraded (SD) of two wetlands in the Tuwei River Basin of Mu Us Sandy Land were studied. The Hedley P grading method was used to measure and compare the differences in soil P form contents under different degrees of degradation, and to elucidate the environmental factors affecting soil P forms in degraded wetlands in arid areas.
    Result ① The overall soil P level in the degraded wetland of Mu Us Sandy Land was low, with inorganic P accounting for 51.35% - 79.57%, and the proportion of inorganic P showed an increasing trend with the intensification of degradation. ② As the degree of degradation intensifies, the overall content of various P forms showed a downward trend, while the contents of H2O-P and NaHCO3-P were at a relatively low level, only 1.71 - 8.19 mg kg−1, and showed a downward trend as degradation intensifies. The proportion of HCl-Pi in soil inorganic P components and Residual-P in soil organic P components was the highest (> 50%), and the contents changed most significantly with the intensification of degradation. ③ Soil organic matter and total nitrogen had a high correlation with various forms of P, especially with H2O-P, NaHCO3-Pi, and NaOH-Pi, with a correlation coefficient of over 0.90.
    Conclusion All P forms in the soil show varying degrees of decrease with the intensification of wetland degradation, with the most significant decrease in soil organic P. The research results are expected to provide scientific basis for the maintenance of wetland soil nutrients and the restoration management of sandy land in the Mu Us Sandy land in the future.

     

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