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首页> 外文期刊>Journal of Pure & Applied Microbiology >Factors Responsible for Phosphorus Uptake Efficiencies of Crop Species in Hot Sub Humid Eco-region of Middle Gangetic Plains of India
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Factors Responsible for Phosphorus Uptake Efficiencies of Crop Species in Hot Sub Humid Eco-region of Middle Gangetic Plains of India

机译:印度恒河中部热亚湿润生态区农作物磷吸收效率的影响因素

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Phosphorus often limits the achievement of high crop yields in low P supplying soils, where P is strongly fixed and largely unavailable for crop uptake. These soils may not be low in total P, but most of it is present in a form of extremely low solubility of Fe/ AI or Ca phosphate. This may result in low P uptake. Even varieties of same species differ in their P efficiency i.e. ability to grow well at low P supply. These differences in P efficiency may be based on differences in the internal P requirement, the uptake efficiency and/or the rate of shoot growth. Several researchers have reported that differences in P efficiency are based on size and type of the root system i.e. root length, root radius and root hair density and rate of shoot growth rate . This shows that a number of reasons may contribute to differences in P efficiency among plants, and that those differences may arise at different stages of the growing cycle. Therefore, the aim of this study was to determine the phosphorus efficiency of wheat, maize and pea ,the factors and mechanisms responsible for the observed differences in P efficiency by measuring shoot and root properties during the growing cycle. To achieve these objectives, pot experiments were conducted with wheat ,maizeand pea during November 2011 to May 2013 in an acid soil of eastern Uttar Pradesh at the Department of Soil Science & Agricultural Chemistry, Institute of Agricultural Sciences, BHU, Varanasi, India. Main problem of this soil is a low fertilizer use efficiency due to P fixation mainly by oxide and hydro-oxide of iron and aluminum ,which are abundant in this soil .The soil has 14-16 %clay, organic carbon, 0.35 % and pH (H20)5.3. Treatments consisted of three P levels, P-0 (unfertilized, without P ), P-50(50 mg P/kg soil) and P-200 (200 mg P/kg soil) as potassium di hydrogen phosphate, four harvest intervals (covering the whole crop growth period) and 4 replications for wheat, maize and pea. Comparing the P uptake of different species at limiting P supply, i.e. mainly on the unfertilized plot, maize was able to absorb significantly higher amount compared to wheat or pea. From the model calculation it is pertinent that at P-0, in most cases the measured influx was higher, in maize up to nine times, thanthe calculated influx. For pea it was almost five times and in wheat it was close to three times. Reasonably good agreement between calculated and measured P influx into the roots of all crops was obtained at medium as well as high P levels.
机译:磷经常限制在低磷供应土壤中实现高产量,因为那里的磷含量很固定,在很大程度上无法吸收作物。这些土壤的总磷可能不低,但大多数以铁/铝或磷酸钙的极低溶解度形式存在。这可能导致低磷吸收。即使是同一物种的变种,其磷效率也不同,即在低磷供应下生长良好的能力。磷效率的这些差异可以基于内部磷需求量,吸收效率和/或枝条生长速率的差异。几位研究人员报告说,磷效率的差异取决于根系的大小和类型,即根长,根半径和根毛密度以及枝条生长速率。这表明许多原因可能导致植物间磷效率的差异,并且这些差异可能出现在生长周期的不同阶段。因此,本研究旨在确定小麦,玉米和豌豆的磷效率,并通过测量生长周期中的地上部和根系特性来确定观察到的磷效率差异的因素和机理。为了实现这些目标,2011年11月至2013年5月,在印度北方邦农业科学研究院土壤科学与农业化学系,北方邦东部的酸性土壤中,用小麦,玉米和豌豆进行了盆栽试验。该土壤的主要问题是土壤中含14-16%的粘土,有机碳,0.35%和pH值,主要是由于铁和铝的氧化物和氢氧化物对磷的固定作用导致肥料使用效率低。 (H20)5.3。处理包括三个磷水平:磷酸二氢钾P-0(未施肥,无磷),P-50(50 mg P / kg土壤)和P-200(200 mg P / kg土壤),两次收获间隔(涵盖整个农作物的整个生育期)和小麦,玉米和豌豆的4个重复样本。比较限制磷供应(即主要在未施肥的地块)上不同物种对磷的吸收,与小麦或豌豆相比,玉米吸收的磷含量高得多。从模型计算中可以看出,在P-0时,大多数情况下测得的玉米入库量是计算出的入库量的九倍。对于豌豆来说,几乎是五倍,而在小麦中则接近三倍。在中等和高磷水平下,计算和测得的所有作物根系中的磷流入量之间都取得了合理的良好一致性。

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