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首页> 外文期刊>International Journal of Plant & Soil Science >Effect of Sulphur and Boron Levels on Soil Available Nutrients after Harvesting of Sesame (Sesamum indicum L.) in Red Soil of Mirzapur
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Effect of Sulphur and Boron Levels on Soil Available Nutrients after Harvesting of Sesame (Sesamum indicum L.) in Red Soil of Mirzapur

机译:米尔扎普尔红壤芝麻收获后硫,硼水平对土壤速效养分的影响

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摘要

To study the effect of sulphur and boron on post-harvest soil fertility status, a pot experiment was conducted at Department of Soil Science and Agricultural Chemistry, Institute of Agricultural sciences, Banaras Hindu University, Varanasi during the kharif season of 2017 taking sesame as a test crop in red soil of Mirzapur district of Uttar Pradesh. The available nitrogen, phosphorus, potassium, sulphur and boron contents were recorded significantly higher in soil after harvesting of the crop over control. The nitrogen, phosphorus, potash, sulphur and boron content recorded 131.58 kg hasup-1/sup, 9.25 kg hasup-1/sup, 228.48 kg hasup-1/sup, 32.79 kg hasup-1/sup and 5.58 mg kgsup-1/sup, respectively when soil treated with 50 kg S hasup-1 /supand 2 kg B hasup-1/sup after harvest of the crop. Correlation study of the data shows the a significant and positive interaction between soil properties. Available sulphur was positively correlated with available phosphorus (r = 0.875*) while as organic carbon was also significant and positively correlated with available nitrogen (r = 0.935*), phosphorus (r = 0.891*) and potash (r = 0.882*). Multiple regression equation revealed that more than 90% variation in available S was attributed by physicochemical properties of the soil.
机译:为了研究硫和硼对收获后土壤肥力状况的影响,在2017年的卡里夫季节期间,在瓦拉纳西Bananas印度大学农业科学研究所土壤科学和农业化学系进行了盆栽试验,以芝麻为生在北方邦米尔扎布尔地区的红色土壤中测试作物。收割过量的农作物后,土壤中的有效氮,磷,钾,硫和硼的含量明显增加。氮,磷,钾,硫和硼的含量记录为131.58 kg ha -1 ,9.25 kg ha -1 ,228.48 kg ha -1 当分别用50 kg S ha -1 和2 kg B ha处理土壤时,分别为32.79 kg ha -1 和5.58 mg kg -1 收成后 -1 数据的相关性研究表明土壤性质之间存在显着的正相关关系。有效硫与有效磷(r = 0.875 *)正相关,而有机碳也很重要,与有效氮(r = 0.935 *),磷(r = 0.891 *)和钾盐(r = 0.882 *)正相关。多元回归方程表明,可用土壤中90%以上的可用S的变化归因于土壤的理化性质。

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