穆晓慧, 李世清, 党蕊娟. 黄土高原石灰性土壤不同形态磷组分分布特征[J]. 中国生态农业学报(中英文), 2008, 16(6): 1341-1347. DOI: 10.3724/SP.J.1011.2008.01341
引用本文: 穆晓慧, 李世清, 党蕊娟. 黄土高原石灰性土壤不同形态磷组分分布特征[J]. 中国生态农业学报(中英文), 2008, 16(6): 1341-1347. DOI: 10.3724/SP.J.1011.2008.01341
MU Xiao-Hui, LI Shi-Qing, DANG Rui-Juan. Distribution of phosphorus fractionations in calcareous soils of the Loess Plateau[J]. Chinese Journal of Eco-Agriculture, 2008, 16(6): 1341-1347. DOI: 10.3724/SP.J.1011.2008.01341
Citation: MU Xiao-Hui, LI Shi-Qing, DANG Rui-Juan. Distribution of phosphorus fractionations in calcareous soils of the Loess Plateau[J]. Chinese Journal of Eco-Agriculture, 2008, 16(6): 1341-1347. DOI: 10.3724/SP.J.1011.2008.01341

黄土高原石灰性土壤不同形态磷组分分布特征

Distribution of phosphorus fractionations in calcareous soils of the Loess Plateau

  • 摘要: 以黄土高原自北向南采集的12个0~20 cm耕层土壤为供试土样,采用Tiessen和Moir修正的Hedley土壤有机无机磷分级方法研究了黄土高原石灰性土壤中不同形态磷组分的分布特征。结果表明:供试土壤各形态P总体分布特征为:HCl-P>Residual-P>NaHCO3-Po>NaHCO3-Pi>NaOH-Po>NaOH-Pi>H2O-P,以HCl-P和Residual-P为主,分别占土壤全磷的54.00%~88.96%和0~39.11%。黄土高原土壤磷含量总体分布表现为南高北低。在各土壤类型间,NaOH-Po、Residual-P和全磷平均含量表现为干润砂质新成土<黄土正常新成土<简育干润均腐土<土垫旱耕人为土,自北向南依次增加;H2O-P和HCl-P表现为简育干润均腐土<黄土正常新成土<干润砂质新成土<土垫旱耕人为土,自北向南先降后升,且上升幅度较大。黄土高原土壤全氮与全磷及各形态磷含量相关性均达显著水平,其中与NaOH-Pi、NaOH-Po、HCl-P及全磷含量达到极显著水平。C/N、pH及砂粒与全磷及各形态磷含量呈负相关关系,其中pH与NaHCO3-Po呈显著负相关,与H2O-P、NaHCO3-Pi、NaOH-Pi及HCl-P呈极显著负相关;砂粒与NaHCO3-Pi、Residual-P及全磷呈显著负相关。除NaHCO3-Po、NaOH-Po及Residual-P,CaCO3与其他各形态磷含量具有一定程度负相关。除NaOH-Pi和NaOH-Po外黏粒与其他各形态磷及全磷也具有一定程度负相关。土壤各形态磷组分和有效磷的多元回归分析发现,各形态磷中对有效磷贡献最大的是H2O-P,其次为NaOH-Pi和NaHCO3-Po;土壤各形态磷组分和有效磷逐步回归分析结果,进一步说明H2O-P的有效性最高。

     

    Abstract: Twelve soil samples from 0~20 cm soil layer were collected from north to south in the Loess Plateau calcareous soil and analyzed for fractionation of organic and inorganic soil phosphorus by Hedley method, amended by Tiessen and Moir. The results show that contents of different P fractionations in soil are in the following order: HCl-P > Residual-P > NaHCO3-Po > NaHCO3-Pi > NaOH-Po > NaOH-Pi > H2O-P. The content of HCl-P and Residual-P are higher and respectively account for 54.00%~88.96% and 0~39.11% of soil total P. The overall distribution of soil P on the Loess Plateau increases from north to south. In all soil types, the average content of NaOH-Po, residual-P and total P is in the following order: Ust Sandic Entisols < Los Orthic Entisols < Hap Ustic Isohumisols < Eum Orthic Anthrosols; generally increasing from north to south. The average content of H2O-P and HCl-P is in the following order: Hap Ustic Isohumisols < Los Orthic Entisols < Ust Sandic Entisols < Eum Orthic Anthrosols; which initially decreases from north to south and then successively inversely increases. Significant correlations exist between soil total N and P as well as different forms of P; and also highly significant correlations between soil total N and NaOH-Pi, NaOH-Po, HCl-P and total P. C/N ratio, pH and sand content have negative correlations with total P, and different forms of P; pH and NaHCO3-Po is in significant negative correlation. pH and H2O-P, NaHCO3-Pi, NaOH-Pi and HCl-P are in extremely significant negatire correlation. Sand content and NaHCO3-Pi, Residual-P and total P are significantly negatively correlated. Calcium carbonate is negatively correlated with other forms of P except NaHCO3-Po, NaOH-Po, Residual-P. Clay content and other forms of P, including total P have a certain degree of negative correlation, except for NaOH-Pi and NaOH-Po. Multiple regression analysis on different forms of P and available P indicates that H2O-P is the largest contributor of available P among different forms of P, followed by NaOH-Pi and NaHCO3-Po. Stepwise regression analysis on the different forms of P and available P further shows that H2O-P has the highest bioavailability.

     

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