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有机酸对土壤无机态磷转化和速效磷的影响
引用本文:章爱群,贺立源,赵会娥,郭再华,崔雪梅.有机酸对土壤无机态磷转化和速效磷的影响[J].生态学报,2009,29(8):4061-4069.
作者姓名:章爱群  贺立源  赵会娥  郭再华  崔雪梅
作者单位:1. 孝感学院生命科学技术学院,湖北孝感,432100;华中农业大学资源与环境学院,武汉,430070
2. 华中农业大学资源与环境学院,武汉,430070
3. 孝感学院生命科学技术学院,湖北孝感,432100
基金项目:国家自然科学基金资助项目,湖北省教育厅科学技术研究组资助项目 
摘    要:土壤有效磷含量低是影响作物生产的重要限制因素之一.作物根分泌活化难溶性磷的有机酸对改善其磷素营养具有重要意义.采用张守敬和Jackson无机磷分级方法,以湖北省3种pH值土壤为材料,加入不同磷源和有机酸,经过室温培养后,测定速效磷含量和无机磷组分的变化.结果表明:施磷显著提高了土壤中速效磷含量,中性土、酸性土Fe-P和Al-P含量大幅上升, Fe-P占增加量的50%以上,而碱性土Ca-P含量显著增加.加施有机酸使中性土速效磷含量增多,除苹果酸处理的变幅较小外,草酸和柠檬酸的加入速效磷显著增加.由于有机酸的作用,中性土Al-P含量下降,Ca-P含量上升,变幅大小依次为草酸>柠檬酸>苹果酸;酸性土中Al-P含量呈下降趋势,碱性土中Ca-P含量有不同程度的减少,3种土壤中O-P含量均有所增加.说明有机酸活化的磷主要来源于中性土和酸性土Al-P、Fe-P及碱性土Ca-P中的磷,同时有机酸能够促进土壤中闭蓄态磷(O-P)的形成与积累.

关 键 词:有机酸  不同磷源  土壤  无机态磷
收稿时间:5/5/2008 12:00:00 AM
修稿时间:2009/2/12 0:00:00

Effect of organic acids on inorganic phosphorus transformation in soils and its readily available phosphate
ZHANG Ai-Qun,HE Li-Yuan,ZHAO Hui-E,GUO Zai-Hua,CUI Xue-Mei.Effect of organic acids on inorganic phosphorus transformation in soils and its readily available phosphate[J].Acta Ecologica Sinica,2009,29(8):4061-4069.
Authors:ZHANG Ai-Qun  HE Li-Yuan  ZHAO Hui-E  GUO Zai-Hua  CUI Xue-Mei
Abstract:Low of available phosphorous is one of the major limitations to crop production. Mobilization of insoluble phosphates by root exudates plays an important role in improving P nutrition of crops. Three types of soils collected from Hubei province were tested to analyze the changes of inorganic phosphorus fractions and available phosphorous after incubated with addition of various organic acids and different phosphorus sources. The results indicated that P added as fertilizer increased available phosphorous in all soils. On soils of pH4.6 and pH6.8 the fertilized phosphorus was transformed into Fe-P and Al-P mainly. However, on soil of pH8.3 the fertilized phosphorus significant increased content of Ca-P. Organic acids had significant influence on available phosphorous except malic acid. Application of organic acids decreased the content of Al-P and increased the content of Ca-P in neutral soil, in the order of Oxalic acid > Citric acid > Malic acid. Phosphorus was activated by organic acid mostly from the fractions of Al-P and Fe-P in acid soil and neutral soil, but fractions of Ca-P in alkali soil, at the same time, organic acid accelerated formation and accumulation of O-P in the three soils.
Keywords:organic acid  different phosphorus source  soil  inorganic phosphorus
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