Han Xiao-Fei, Gao Ming, Xie De-Ti, Wang Zi-Fang
College of Resources and Environment, Southwest University, Chongqing 400715, China.
Huan Jing Ke Xue. 2016 Jun 8;37(6):2284-2290. doi: 10.13227/j.hjkx.2016.06.036.
In this study the effects of tillage methods (rice-winter paddy field conventional farming, CF; rice-winter paddy field combing ridge with no-tillage, RNT1; rice-wheat or rape combing ridge with no-tillage, RNT2; rice-wheat or rape conventional paddy-upland rotation tillage, CR) on purple soil profile of different forms of inorganic phosphorus distribution characteristics were investigated in a long-term experimental site established in 1990, Chongqing City, China. The results showed that compared to the status before the experiment, the total phosphorus, available phosphorus and various morphologies of inorganic phosphorus all increased to a certain degree in the soils with different long-term tillage treatments,and the contents of different forms of inorganic phosphorus in soil size ranked as RNT2> CF> CR> RNT1. Except that the contents of Fe-P in the lower layer were higher than those in the upper layer, contents of Ca-P, Ca-P, Al-P, Ca-P and O-P in the arable layers were all higher than those in the lower layers. The effects of farming practices on the availability of various phosphorus forms were significant. They were in the order of CR> RNT> CF. Long-term conventional paddy-upland rotation tillage was more advantageous to crops in the absorption of phosphorus. It was shown by relevant analysis that the contribution of various groups of inorganic phosphorus to purple soil was in the order of Ca-P(0.9369)> Al-P(0.9158)> Ca-P(0.9012)> Fe-P(0.8287)> Ca-P(0.8059)> O-P(0.7472).
本研究于1990年在中国重庆市建立的长期试验田中,研究了耕作方式(水稻-冬水田传统耕作,CF;水稻-冬水田垄作免耕,RNT1;稻麦或油菜垄作免耕,RNT2;稻麦或油菜传统水旱轮作耕作,CR)对紫色土剖面不同形态无机磷分布特征的影响。结果表明,与试验前相比,不同长期耕作处理土壤中的全磷、有效磷及各形态无机磷均有一定程度增加,土壤不同形态无机磷含量排序为RNT2>CF>CR>RNT1。除下层铁磷含量高于上层外,耕层中钙磷、钙磷、铝磷、钙磷和闭蓄态磷含量均高于下层。耕作方式对各形态磷有效性影响显著,顺序为CR>RNT>CF。长期传统水旱轮作耕作更有利于作物对磷的吸收。相关分析表明,各形态无机磷对紫色土的贡献顺序为钙磷(0.9369)>铝磷(0.9158)>钙磷(0.9012)>铁磷(0.8287)>钙磷(0.8059)>闭蓄态磷(0.7472)。