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首页> 外文期刊>Soil & Tillage Research >Patterns in phosphorus and corn root distribution and yield in long-term tillage systems with fertilizer application.
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Patterns in phosphorus and corn root distribution and yield in long-term tillage systems with fertilizer application.

机译:长期施用肥料的耕作系统中磷和玉米根系分布和产量的模式。

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摘要

The distribution of phosphorus in the soil profile as a function of soil tillage, fertilizer management system and cultivation time is strongly related to root distribution. As the dynamics of this process are not well understood, long-term experiments are useful to clarify the cumulative effect through time. The study evaluated an 18-year-old experiment carried out on Rhodic Paleudult soil, located in Rio Grande do Sul state - Brazil, with cover crops (black oat and vetch) in the winter and corn in the summer. In the 0- to 20-cm layer, the amounts of clay, silt and sand were 22, 14, and 64 g kg-1, respectively. This layer had a mean slope of 3%. The mean local annual rainfall is 1440 mm. The climate is subtropical with a warm humid summer (Cfa), according to the Koeppen classification. The treatments consisted of three soil managements (conventional tillage, no tillage and strip tillage) and three application modes (broadcast, row and strip) for triple superphosphate and potassium chloride fertilizers. Data for phosphorus and root distribution in the soil from the 1989/90, 1999/00 and 2006/07 growing seasons were used. Phosphorus stratification occurred through time, irrespective of soil and fertilizer management, mainly in the 0- to 5-cm layer. The tillage and fertilization systems promoted significant differences in the Pi and Pt fractions up to a depth of 20 cm. For the Po fraction, significant differences were found only in the 0- to 5- and 15- to 20-cm layers. Inorganic phosphorus accumulated in the fertilized zone (0-10 cm), with higher intensity in the no-tillage system under row fertilization with values around 150 mg dm-3. Root distribution presented a strong positive relationship with phosphorus distribution, exhibiting redistribution in the soil profile through time. This redistribution was accompanied by increases in organic phosphorus and total organic carbon content. Corn grain yield was not affected by long-term tillage systems.
机译:磷在土壤剖面中的分布与耕作,肥料管理系统和耕种时间的关系与根系分布密切相关。由于尚未充分了解此过程的动态性,因此长期实验可用于阐明随时间推移的累积效应。该研究评估了在巴西南里奥格兰德州的Rhodic Paleudult土壤上进行的一项长达18年的实验,该土壤在冬季有遮盖作物(黑燕麦和紫etch菜),夏季有玉米。在0至20厘米的层中,粘土,粉砂和沙子的含量分别为22、14和64 g kg -1 。该层的平均斜率为3%。本地平均年降雨量为1440 mm。根据Koeppen的分类,气候为亚热带,夏季温暖湿润(Cfa)。处理包括三重过磷酸钙和氯化钾肥的三种土壤管理方法(常规耕作,免耕和条形耕作)和三种施用模式(广播,行和条播)。使用了1989 / 90、1999 / 00和2006/07生长季土壤中磷和根的分布数据。磷分层会随时间而发生,与土壤和肥料管理无关,主要在0至5厘米的层中。耕作和施肥系统促进了高达20 cm深度的Pi和Pt组分的显着差异。对于Po分数,仅在0到5厘米和15到20厘米的层中发现显着差异。无机磷在施肥区(0-10 cm)累积,在免耕系统下连续施肥强度更高,其值约为150 mg dm -3 。根系分布与磷分布呈极强的正相关关系,表现出随时间在土壤剖面中的重新分布。这种重新分布伴随着有机磷和总有机碳含量的增加。玉米产量不受长期耕作制度的影响。

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