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首页> 外文期刊>Soil Science and Plant Nutrition >Evaluation of nonexchangeable potassium content of agricultural soils in Japan by the boiling HNO3 extraction method in comparison with exchangeable potassium
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Evaluation of nonexchangeable potassium content of agricultural soils in Japan by the boiling HNO3 extraction method in comparison with exchangeable potassium

机译:沸腾的HNO3提取法与沸腾的钾相比评价日本农业土壤非产钾含量

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The nonexchangeable potassium (neK) content of 178 agricultural soils in Japan was determined by subtracting the amount of K extracted with 1mol L-1 ammonium acetate, i.e., exchangeable K (exK) from that extracted with boiling 1mol L-1 HNO3. The statistical relationships between the neK content and physico-chemical properties of the soils were examined to investigate the factors controlling neK content. The neK content of agricultural soils in Japan ranged from 0 to 1120mg kg(-1) with an arithmetic mean and median of 303 and 255mg kg(-1), respectively. It showed a significant positive correlation with the total K content, fixed ammonium content, and silt content (p&0.01) and a significant negative correlation with Alo+1/2 Feo content and total carbon content (p&0.01). These results suggest that the controlling factors of neK are mainly the total K content and 2:1 type phyllosilicates such as mica and vermiculite, with the indirect negative influence of organic matter and amorphous materials. Terrestrial Regosols, Brown Lowland soils, and Dark Red soils had relatively high neK contents. In contrast, Andosols, Wet Andosols, and Volcanogenous Regosols had relatively low neK contents. The neK content showed no significant correlation with exK content, suggesting that neK is a moderately to slowly available fraction of soil K, which is independent of exK. In conclusion, evaluation of nonexchangeable K in combination with exchangeable K would enhance the rational management of agricultural soils in terms of K fertility by taking account of longer term K-supplying power of soils.
机译:通过减去用1mol L-1乙酸铵萃取的K的量来确定日本的178个农业土壤中的非掺杂钾(Nek)含量,即,通过沸点1molL-1 HNO3提取的可更换K(exK)。检查了土壤中的NEK含量和物理化学性质之间的统计关系,研究了控制NEK含量的因素。日本农业土壤的NEK含量范围为0至1120mg kg(-1),分别具有303和255mg kg(-1)的算术平均值和中位数。它显示出与总K含量,固定铵含量和淤泥含量(P& 0.01)的显着正相关性,以及与AlO + 1/2 FeO含量和总碳含量的显着负相关(P& 0.01) 。这些结果表明,NEK的控制因子主要是总K含量和2:1型云母和蛭石,具有有机物质和非晶材料的间接负影响。陆地雷神经,棕色低地土壤和深红色土壤具有相对较高的奈克内容物。相比之下,糖醇,湿和糖醇和活性雷科尔斯的Nek含量相对较低。 Nek含量与exk含量没有显着相关性,表明Nek是一种适度的,以缓慢地慢慢获得土壤K,其与exk无关。总之,通过考虑到较长术语K供给水分的批量批准,与可交换k结合与可交换百合的非兴趣K的评估将提高农业土壤的合理管理。

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