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长期施肥下三类典型农田土壤小麦磷肥利用效率的差异
引用本文:高静,张淑香,徐明岗,黄绍敏,杨学云.长期施肥下三类典型农田土壤小麦磷肥利用效率的差异[J].应用生态学报,2009,20(9):2142-2148.
作者姓名:高静  张淑香  徐明岗  黄绍敏  杨学云
作者单位:1. 中国农业科学院农业资源与农业区划研究所农业部作物营养与施肥重点开放实验室,北京,100081
2. 河南省农业科学院植物营养与资源环境研究所,郑州,450002
3. 西北农林科技大学资源环境学院,陕西杨凌,712100
基金项目:国家基础性工作专项,国家重点科技支撑计划项目
摘    要:对我国北方长期施肥下三类典型农田土壤(塿土、潮土和褐潮土)的小麦产量、小麦磷肥农学利用效率、小麦磷肥利用率进行了研究.结果表明:长期施用磷肥处理(氮磷化肥配合施用、氮磷钾化肥配合施用、氮磷钾化肥和秸秆配合施用、氮磷钾化肥和有机肥配合施用)的小麦产量为2914~6219 kg·hm-2,较不施磷肥处理(不施肥对照、单施化肥氮、氮钾化肥配合施用)提高了2~4倍,各施磷肥处理之间无显著差异.试验起始年施用氮磷钾化肥处理的塿土、潮土和褐潮土上的小麦磷肥农学利用效率分别为17.0、20.3和13.3 kg·kg-1,小麦磷肥利用率分别为15.3%、31.2%和23.8%;施肥15年后,小麦磷肥农学利用效率每年分别增加3.9、2.5和2.8 kg·kg-1,小麦磷肥利用率每年分别增加1.3%、0.9%和1.0%.同一类型土壤不同施磷处理间的磷肥农学利用效率和利用率差异不显著.在我国北方地区,长期施用磷肥可以显著提高小麦产量和磷肥利用效率;氮磷钾化肥和有机肥配施处理下,塿土平均每年增长的小麦磷肥农学利用效率和磷肥利用率较潮土和褐潮土高.

关 键 词:长期施肥  小麦  产量  磷肥利用率  磷肥农学利用效率
收稿时间:2008-12-23

Phosphorus use efficiency of wheat on three typical farmland soils under long-term fertilization
GAO Jing,ZHANG Shu-xiang,XU Ming-gang,HUANG Shao-min,YANG Xue-yun.Phosphorus use efficiency of wheat on three typical farmland soils under long-term fertilization[J].Chinese Journal of Applied Ecology,2009,20(9):2142-2148.
Authors:GAO Jing  ZHANG Shu-xiang  XU Ming-gang  HUANG Shao-min  YANG Xue-yun
Institution:Ministry of Agriculture Key Laboratory of Crop Nutrition and Fertilization, Institute of Agriculture Resource and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing 100081, China;Institute of Plant Nutrition and Environment, Henan Academy of Agricultural Sciences, Zhengzhou 450002, China;College of Resource and Environment, Northwest A & F University, Yangling 712100, Shaanxi, China
Abstract:Field experiments were conducted on three typical farmland soils(10ess soil,fluvo-aquic soil,and cinnamon fluvo-aquic soil)in Northern China to study the grain yield.phosphorus agronomic efficiency(PAE),and phosphorus use efficiency(PUE)of wheat under effects of long-term fertilizations.Seven treatments were installed,i.e.,non-fertilization(CK),nitrogen fertilization200%-400% higher than those under no P fertilizations(treatments CK,N,and NK),and no significant differences were observed between the P fertilizations.In the early years of the experiment,the PAE in treatment NPK on the loess soil,fluvo-aquic soil,and cinnamon fluvo-aquic soil was 17.0 kg·kg~(-1),20.3 kg·kg~(-1),and 13.3 kg·kg~(-1),and the PUE was 15.3%,31.2%,and 23.8%,respectively.After 15-year fertilization,the PAE and PUE in treatment NPK increased annually by 3.9 kg·kg~(-1) and 1.3%on loess soil,2.5 kg·kg~(-1) and 0.9%on fluvo-aquic soil,and 2.8 kg·kg~(-1) and 1.0% on cinnamon fluvo-aquic soil.respectively.There were no significantdiflferences in the PAE and PUE among the P treatments for the same soils.In Northern China,long-term P fertilization could increase the wheat grain yield and PUE significantly,and the mean annual increase of PAE and PUE in treatment NPKM was higher on loess soil than on fluvo-aquic soil and cinnamon fluvo-aquic soil.
Keywords:long-term fertilization  wheat  yield  phosphorus use efficiency  agronomy efficiency of phosphorus
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