不同水平的氮磷钾、生物炭和氮化细菌对豇豆(Vigna unguiculata)土壤理化性质的影响

Manish Choudhary, T. Thomas, N. Swaroop, Vinay, Ashima Thomas
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摘要

有鉴于此,"不同水平的氮磷钾、生物炭和氮杂菌对豇豆土壤理化性质和产量属性的影响 "实验提出了以下目标,以计算各种氮磷钾、生物炭和氮杂菌用量对土壤理化性质的影响。从实验地挖掘出的土壤样本显示,土地地形从几乎平坦到倾斜 1%至 6%不等,土壤面积属于 Inceptisol 顺序。土壤质地为沙壤土,其中沙子占 62.65%,淤泥占 21.09%,粘土占 16.26%。土壤的 pH 值为 6.89,导电率(EC)为非碱性(0.42 ds m-1)。有机碳含量为中低水平,可利用氮为中低水平(280.78 千克/公顷-1),可利用磷为 17.34 千克/公顷-1,可利用钾为 168.16 千克/公顷-1。统计分析采用了两个因子,即 @NPK 0、50 和 100% ha-1 三个水平,@Biochar 0、50 和 100% ha-1 三个水平,以及随机区组设计。在田间试验中,共使用了九种不同的处理;最佳结果是显著的。结果表明,土壤的物理和化学参数,包括容重(1.39 和 1.41 mg m-3)、颗粒密度(2.46 和 2.47 mg m-3)和土壤 pH 值(6.89 和 6.91)的累积平均值,分别在 T1(绝对对照)的 0-15 厘米和 15-30 厘米深度达到最大值。此外,孔隙度百分比分别为 48.22% 和 47.39%,持水量分别为 44.14% 和 45.34%),电导率(EC)分别为 0.49 ds m-1 和 0.52 ds m-1,有机碳百分比为 0.可用氮为 299.78 千克/公顷和 295.76 千克/公顷,可用磷为 23.78 千克/公顷和 21.98 千克/公顷,可用钾为 179.25 千克/公顷和 176.56 千克/公顷。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Different Levels of NPK, Biochar and Azotobacter on Physico-chemical Properties of Soil on Cowpea (Vigna unguiculata)
In light of this, the following goals are present in the experiment "Effect of Different Levels of NPK and Biochar, Azotobacter on Physico-chemical Properties of Soil and Yield Attributes of Cowpea to calculate the impact of various NPK, Biochar, and Azotobacter dosages on the physical-chemical characteristics of soil. An excavated soil sample from the experimental site revealed that the land topography ranged from nearly level to sloped by 1% to 6%, with soil area falling into the Inceptisol order. The soil texture was sandy loam, with sand percentages of 62.65%, silt percentages of 21.09, and clay percentages of 16.26. The pH of soil was 6.89, and its electrical conductivity (EC) was non-saline (0.42 ds m-1). Organic carbon content was low to medium, available nitrogen was low to medium (280.78 kg ha-1), available phosphorus was 17.34 kg ha-1, and available potassium was 168.16 kg ha-1. Two factors with three levels of @NPK 0, 50, and 100% ha-1, three levels of @Biochar 0, 50, and 100% ha-1, and a randomized block design were used in the statistical analysis. During field testing, nine different treatments were used; the best outcomes were significant. The results indicate that the physical and chemical parameters of the soil, including the cumulative mean values for bulk density (1.39 and 1.41 mg m-3), particle density (2.46 and 2.47 mg m-3), and soil pH (6.89 and 6.91), attained their maximum in T1 (Absolute control) at depths of 0-15 cm and 15-30 cm, respectively. Additionally, the percentage pore space was found to be 48.22% and 47.39%, and the water holding capacity was found to be 44.14% and 45.34%), electrical conductivity (EC) was measured at 0.49 ds m-1 and 0.52 ds m-1, the percentage of organic carbon was determined to be 0.40%), and the available nitrogen was found to be (299.78 kg ha-1 and 295.76 kg ha-1, available phosphorus was (23.78 kg ha-1 and 21.98 kg ha-1), and the available potassium was (179.25 kg ha-1 and 176.56 kg ha-1).
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