印度印度河-恒河平原不同土壤阶磷组分的分布

Arbind Kumar Gupta
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摘要

研究了印度印度河-恒河平原不同土壤阶中磷组分的状态、分布及其与土壤特征的关系。2016年,土壤样品采集于3个深度(0-15、15-30和30-45 cm),覆盖完整溶土层、初始溶土层和溶土层。结果表明,随着土壤深度的增加,土壤pH值和粘粒含量呈增加趋势,而有机碳和EC含量呈下降趋势。在不同磷组分中,Ca-P占主导地位,分别占全磷含量的35%和20%,其次是Fe-P、RS-P和OC-P。在Alfisol, Fe-P占土壤全磷的21%,其次是Ca-P、RS-P和Al-P。Al-P、RS-P和Ca-P随土壤深度的增加而增加,而有机磷则随土壤深度的增加而减少。土壤pH与Ca-P呈显著正相关,与Al-P、Fe-P呈显著负相关。钙磷含量最高的是Entisols(35%)和ineptisols (20%), Fe-P含量最高的是Alfisols(21%)。在无机磷组分中,Ca-P是幼土和初生土中磷有效性的主要贡献者。磷在苜蓿醇中释放的主要组分是磷酸铁。总体上,随着土壤深度的增加,无机磷含量增加,有机速效磷含量减少。各P分数之间也存在关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution of phosphorus fractions in different soil orders of Indo-Gangetic plains of India
The status and distribution of phosphorus fractions in some soil orders and their relationship with soil characteristics under Indo-Gangetic plains of India was studied at Mohanpur, Nadia (W.B.). Soil samples were collected from three depths (0-15, 15-30 and 30-45 cm) covering Entisols, Inceptisols and Alfisols during 2016. Results revealed that soil pH and clay content increased whereas EC and organic carbon tended to decrease with increasing soil depth. Among different phosphorus fractions, Ca-P was dominant contributing 35% and 20% of total phosphorus content in Entisols and Inceptisols, respectively followed by Fe-P, RS-P and OC-P. In Alfisol, Fe-P fraction constituted 21% of the total soil P followed by Ca-P, RS-P and Al-P. The fractions Al-P, RS-P and Ca-P increased whereas organic P decreased with increasing soil depth. Soil pH was positively correlated with Ca-P and negative with Al-P, Fe-P of all the soil orders. Calcium-P was the highest in Entisols (35%) and Inceptisols (20%) while Fe-P (21%) in Alfisols. Among the inorganic P fractions, Ca-P was the dominant contributor to the availability of phosphorus in Entisols and Inceptisols. The dominant fraction for the release of P in Alfisols was iron phosphate. In general, inorganic P fractions increased while organic available P decreased with soil depth. Various P fractions also had relationships among themselves.
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