马哈拉施特拉邦浦那地区不同有机肥氮素矿化动力学

S. Singh
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引用次数: 0

摘要

土壤中N矿化的数学描述如抛物线模型、指数模型、双曲模型、零阶模型等,是表征和量化有机质库和矿化常数速率的可能方法。单指数模型最广泛用于土壤N矿化,尽管其他类型也已经过测试。通常使用几种动力学模型来估计N矿化动力学,因此选择基于最高决定系数(r2)和最低标准误差的模型(Wijanarko & Purwanto, 2016)。通过长期培养程序的氮矿化能力。从他们的研究中,他们提出了一个氮矿化时间过程的渐近模型,使计算土壤的氮矿化潜力成为可能(Stanford & Smith, 1972)。矿化研究中的动力学参数有可能用于研究不同环境和管理条件下土壤的矿化-固定化过程。通过对不同有机质源氮矿化潜力的了解,可以提高氮素利用效率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Kinetic of Nitrogen Mineralization by Using Various Organic Manures of Pune Region, Maharashtra
The mathematical description of N mineralization in soils like parabolic model, exponential model, hyperbolic model, zero order models etc, is a possible 3 approach to characterize and quantify the organic matters pool and mineralization constant rate. The single exponential model most widely used for soil N mineralization, although other types have also been tested. Several kinetic models are often used to estimate the kinetic of N mineralization, thus a model is selected based on the highest coefficient of determination (r2) and the lowest standard error (Wijanarko & Purwanto, 2016). The N mineralization capacity through long term incubation procedures. From their studies they proposed an asymptotic model of time course of N mineralization, making it possible to calculate the N mineralization potential of the soils (Stanford & Smith, 1972). Kinetics parameters in mineralization study can be potentially used to access the mineralization-immobilization process in soils under varying environmental and management conditions. Nitrogen-use efficiency can be enhanced through the understanding of N-mineralization potential of different organic source.
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