不同磷源施肥土壤中磷的动态变化及莲对磷的吸收

C. E. Quintero
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引用次数: 0

摘要

在287 d的温室试验中,研究了粘质和砂质土壤与3种磷溶解度不同的磷源之间的反应动力学。用已存在磷、添加磷、提取磷和土壤磷试验提取后保留磷的方程来解释植物吸收磷随时间的变化。干产量和磷吸收量在不同土壤间和不同磷源间存在差异。在黏性土壤中,两种水溶性磷源的干产量和磷吸收量随时间差异不大,但在沙质土壤中,家禽凋落物的磷吸收量显著高于三元过磷酸钙。相对于两种水溶性磷源,磷矿的干产量和磷吸收量都较低。黏性土壤对三种磷源的吸收主要表现为吸收磷和保留磷的减少,而沙质土壤和磷矿土壤对磷的吸收主要表现为保留磷的减少,而吸收磷随时间不变。原生磷对两种土壤磷源的影响都不大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamic of Phosphorus in Soils Fertilized with different Phosphorus Sources and Phosphorus Acquisition by Lotus Corniculatus
The dynamic of the reaction between a clayey and sandy soil and three P-sources differing in P-solubility was study in a greenhouse experiment were Lotus corniculatus was cultivated and harvested several times during 287 days. The absorbed P by the plants with time was interpreted by an equation representing the P already present, added P, extracted P and the retained P even after the extraction by a soil-P test. The dry yield and P uptake differed between soils and for each soil among P-sources. In the clayey soil there was little difference with time between the two water soluble P-sources, both dry yield and P uptake, but in the sandy soil P uptake was significantly higher for poultry litter compared with triple superphosphate. Dry yield and P uptake were lower for phosphate rock with respect to both water soluble P-sources. In the clayey soil P uptake from the three P-sources with was mainly interpreted by the decrease of both the extracted and retained P, whereas in the sandy soil and for phosphate rock addition P uptake was described by the decrease of the retained P meanwhile extracted P was constant with time. Native P had little influence in both soil for all P-sources.
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