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Re-evaluation of manganese solubility as affected by soil sample preparation in the laboratory

机译:在实验室中重新评估受土壤样品制备影响的锰溶解度

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Laboratory experiments were conducted to re-evaluate the effects of drying and the time between drying and Mn analysis on soil Mn solubility using maize seedlings as test plant. Samples of five soil types were collected in the field, transferred to laboratory and submitted for the following treatments: dried in the shade at 25oC and dried at 65oC followed by Mn determination immediately and after 30 and 60 days. Ninety days later soil samples were rewetted at field capacity and maize seedlings were grown for 7 days. Evaluations included plant Mn content and soil Mn extracted with NH4OAc 1 mol L-1 pH 7. The lowest soil and plant Mn contents were found in soil samples dried in the shade at 25oC. Drying soil sample at 65oC and increasing the time between drying and Mn analysis increased Mn solubility and Mn uptake by maize. Oxisols showed higher soil and plant Mn contents than other soil types. The results indicated the extreme difficulty in interpreting soil Mn results due to the great effect of soil processes in the laboratory on Mn solubility. Routine soil analysis is not recommended to evaluate plant available Mn.
机译:进行了实验室实验,以玉米幼苗为试验植物,重新评估了干燥以及干燥与锰分析之间的时间对土壤锰溶解度的影响。在田间收集了五种土壤类型的样品,转移到实验室进行以下处理:在25oC的阴凉处干燥,在65oC的干燥温度,然后立即测定30天和60天的Mn。九十天后,将土壤样品在田间重新湿润,然后将玉米幼苗生长7天。评价包括植物Mn含量和用NH4OAc 1 mol L-1 pH 7萃取的土壤Mn。在25oC下阴凉干燥的土壤样品中,土壤和植物Mn含量最低。在65oC下干燥土壤样品并增加干燥和进行Mn分析之间的时间,从而增加了Mn的溶解度和玉米对Mn的吸收。氧化物显示出比其他土壤类型更高的土壤和植物锰含量。结果表明,由于实验室中土壤过程对锰溶解度的巨大影响,解释土壤锰结果极为困难。不建议使用常规土壤分析来评估植物中的有效锰。

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