Long-term fertilization effect of organic carbon and total nitrogen on floodplain soil

Md. Wasim Akram Majharul Islam, Md. Forhad Hossain, M. Mia, Md. Shaidul Islam, Md. Saikat Hossain Bhuiyan, Joynulalam Talukder, M. Kader
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引用次数: 2

Abstract

Soil organic matter is the most often reported indicator of soil quality and productivity and an evidence of previous soil management. Therefore, in 2017, a laboratory incubation study was carried out in the experimental filed of Bangladesh Institute of Nuclear Agriculture (BINA), Mymensingh, Bangladesh under control condition at 25°C for 104 days to investigate the influence of long term manuring and fertilization on soil respiration by means of C mineralization. Soil samples were collected from floodplain soil with rice-rice cropping pattern at Bangladesh Agricultural University (BAU) experimental farm having eight treatments. Long term (33 years) application of fertilizers and manure resulted in significant differences in soil organic carbon, total N content, and soil pH KCl between the treatments. The soil organic carbon and total N content varied among the different treatments from14.9 g OC kg-1 to 17.0 g OC kg-1 and1.60 g N kg-1 (control) to 1.78 g N kg-1 (application of NPK). The soil pH varied among the different treatments from 5.65(application of NK) to 4.89 (application of N). This result indicates that more stable organic carbon was formed in NPK treated soil which is less prone to decomposition if present crop management has been changed.    
河漫滩土壤有机碳和全氮的长期施肥效应
土壤有机质是最常被报道的土壤质量和生产力指标,也是过去土壤管理的证据。因此,2017年,在孟加拉国Mymensingh核农业研究所(BINA)试验田,在25°C的对照条件下,进行了104天的实验室孵化研究,通过C矿化的方式研究长期施肥对土壤呼吸的影响。在孟加拉国农业大学(BAU)试验农场采用8种处理方法采集了水稻-水稻种植模式的洪泛区土壤样品。长期(33年)施用化肥和有机肥导致土壤有机碳、全氮含量和土壤pH、KCl在不同处理间存在显著差异。不同处理土壤有机碳和全氮含量在14.9 ~ 17.0 g OC kg-1和1.60 g N kg-1(对照)~ 1.78 g N kg-1之间变化较大。不同处理的土壤pH值从5.65(施用NK)到4.89(施用N)变化较大。这表明,如果改变现有的作物管理方式,NPK处理的土壤形成了更多稳定的有机碳,不易分解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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