Phosphorus forms and their distribution under long-term no tillage systems

被引:1
作者
Wei, Kai [1 ]
Chen, Zhenhua [1 ]
Zhang, Xiaoping [2 ]
Chen, Lijun [1 ]
机构
[1] Chinese Acad Sci, Inst Appl Ecol, Shenyang, Liaoning, Peoples R China
[2] Chinese Acad Sci, Northeast Inst Geog & Agroecol, Changchun, Jilin, Peoples R China
基金
中国国家自然科学基金;
关键词
nutrient; cMonoester; cDiesters; P-31 nuclear magnetic resonance; agriculture; SOIL; FERTILIZATION; PHOSPHATASE; MANURE; PH;
D O I
10.17221/270/2018-PSE
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Phosphorus (P) stratification in no-tillage (NT) systems has important implications for crop growth and potential P loss, but little is known about P forms and their distribution when mineral P fertilizers are placed to the depth of 5 cm in NT soil. A 10-year field experiment was used to study the effect of NT and mouldboard plough (MP) on soil P forms at three depths (0-5, 5-10 and 10-20 cm) and their relationship with Fe and Al oxides. The results indicated that stratification of organic P forms occurred under NT treatment, and Fe oxides may have a stronger capacity for adsorbing the P forms. When mineral P fertilizers were placed to the depth of 5 cm under NT treatment, there was no significant difference in P forms or crop yield between NT and MP treatment, and orthophosphate did not show any significant difference under NT treatment between 0-5 cm and 5-10 cm depth. Overall, the agricultural management practice that mineral P fertilizers are placed to the depth of 5 cm under NT treatment could result in stratification of P forms, while the changes in the distribution of P forms in soil profiles might help reduce potential P loss in surface runoff and do not make any difference to crop growth.
引用
收藏
页码:35 / 40
页数:6
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