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草业学报 ›› 2015, Vol. 24 ›› Issue (8): 218-224.DOI: 10.11686/cyxb2014388

• 论文 • 上一篇    下一篇

连续6年施磷肥对土壤磷素积累、形态转化及有效性的影响

李新乐1, 2, 侯向阳1*, *, 穆怀彬1, 李西良1, 郭丰辉1   

  1. 1.中国农业科学院草原研究所,内蒙古 呼和浩特 010010;
    2.中国林业科学研究院沙漠林业实验中心, 内蒙古 磴口 015200
  • 出版日期:2015-08-20 发布日期:2015-08-20
  • 通讯作者: E-mail:houxy16@126.com
  • 作者简介:李新乐(1989-),男,内蒙古巴彦淖尔人,硕士。E-mail:nxylxl@126.com
  • 基金资助:
    “十二五”国家科技支撑计划(2012BAD12B02)资助

P fertilization effects on the accumulation, transformation and availability of soil phosphorus

LI Xin-Le1, 2, HOU Xiang-Yang1, *, MU Huai-Bin1, LI Xi-Liang1, GUO Feng-Hui1   

  1. 1.Grassland Research Institute of Chinese Academy of Agriculture Sciences, Huhhot 010010, China;
    2.Experimental Center of Desert Forestry, China Academy of Forestry, Dengkou 015200, China
  • Online:2015-08-20 Published:2015-08-20

摘要: 长期施磷肥对土壤磷素积累、形态转化以及有效性的影响是国内外土壤化学研究的热点之一。本研究利用从2008年开始在京南地区进行的紫花苜蓿连续6年施用磷肥定位试验,研究不同施肥处理对紫花苜蓿田土壤磷素积累、形态转化及其有效性的影响。试验地土壤为褐潮土,试验开始前耕层(0~20 cm)土壤有机质为11.2 g/kg,全磷为0.77 g/kg,速效磷为5.66 mg/kg,pH为8.3。结果表明,连续不施磷肥土壤的全磷、速效磷、无机磷各组分含量较连续施磷肥处理均明显降低,说明连续施用磷肥可显著扩大土壤中的有效磷库;不施磷肥处理耕层(0~20 cm)土壤全磷下降了6.94%,速效磷下降了16.3%,施用磷肥处理耕层土壤全磷增加1.3%~13%,速效磷增加164.7%~335.9%;不同的施磷肥处理对Ca2-P含量的影响最大,不施磷肥的土壤Ca2-P几乎耗竭,而施磷处理的Ca2-P增加幅度可达19~36倍;此外,施用磷肥也使土壤Ca8-P、Ca10-P、Al-P、Fe-P、O-P有不同程度的提高。通过2013年的停施磷肥试验可知继续施磷肥的处理(F2)与停施磷肥的处理(F2')在土壤磷素水平、苜蓿产量及养分含量上均没有显著差异,表明磷肥存在明显的后效作用,之前积累在土壤中的磷素具有生物有效性。

Abstract: The effects of phosphorus (P) fertilization on the accumulation, transformation and availability of P in soil chemistry have drawn much attention in recent years. This paper reports on a six-year fertilization experiment (beginning in 2008) with alfalfa grown in the south region of Beijing. The soil type in the study area is fluvo-aquic. Before the experiment was performed, soil organic matter was 11.2 g/kg, total P was 0.77 g/kg, available P was 5.66 mg/kg and soil pH was 8.3 in the topsoil (0-20 cm). The results showed that the contents of total P, available P and inorganic P in various forms decreased markedly without P fertilization and increased significantly when P fertilizer was applied. Total P and available P in soils without fertilization decreased by 6.94% and 16.3% respectively, while in soil treated with six years fertilization they increased by 1.3%-13.0% and 164.7%-335.9% respectively. The effects of different P fertilizer treatments on Ca2-P content were significant. Ca2-P content was almost depleted in the non-fertilization treatment, while levels in the fertilization treatment increased 19-36 times. P fertilization also increased the soil content of Ca8-P, Ca10-P, Al-P, Fe-P, O-P. When fertilization was stopped in 2013 it was found that no significant differences existed in soil P level, alfalfa yield and nutrient content between the treatments of continued fertilization (F2) and ceased fertilization (F2'). The results indicate that long term P fertilization has significant and continuous effects. The accumulation of P in soil contents should also enhance future biological performance.